Wall, Alexander Forster: Harmonised chronological data from tropical Australian environmental archives [dataset]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.989982 (dataset in review), In: Wall, AF: Chronology and hydrological interpretations of tropical Australian environmental archives (0–130 ka) [dataset bundled publication]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.989939 (dataset in review)
Abstract:
A harmonised compilation of all radiocarbon, OSL, and other dated samples used in the chronological synthesis. Each row represents an individual dating result with metadata required for recalibration and re-modelling.
Source:
Bird, Michael I; Brand, Michael; Comley, Rainy; Fu, Xiao; Hadeen, Xennephone; Jacobs, Zenobia; Rowe, Cassandra; Wurster, Christopher M; Zwart, Costijn; Bradshaw, Corey J A (2024): Late Pleistocene emergence of an anthropogenic fire regime in Australia’s tropical savannahs. Nature Geoscience, 17(3), 233-240, https://doi.org/10.1038/s41561-024-01388-3
Bowler, J M; Duller, G A T; Perret, N; Prescott, J R; Wyrwoll, Karl-Heinz (1998): Hydrologic changes in monsoonal climates of the last glacial cycle: stratigraphy and lumenescence dating of Lake Woods, N.T., Australia. Palaeoclimates, 3 (1-3), 179-207
Denniston, R F; Asmerom, Y; Polyak, V J; Wanamaker, A D Jr; Ummenhofer, C C; Humphreys, W F; Cugley, John; Woods, David; Lucker, S (2017): Decoupling of monsoon activity across the northern and southern Indo-Pacific during the Late Glacial. Quaternary Science Reviews, 176, 101-105, https://doi.org/10.1016/j.quascirev.2017.09.014
Denniston, Rhawn F; Villarini, Gabriele; Gonzales, Angelique N; Wyrwoll, Karl-Heinz; Polyak, Victor J; Ummenhofer, Caroline C; Lachniet, Matthew S; Wanamaker, Alan D Jr; Humphreys, William F; Woods, David; Cugley, John (2015): Extreme rainfall activity in the Australian tropics reflects changes in the El Niño/Southern Oscillation over the last two millennia. Proceedings of the National Academy of Sciences of the United States of America, 112(15), 4576-4581, https://doi.org/10.1073/pnas.1422270112
Denniston, Rhawn F; Wyrwoll, Karl-Heinz; Asmerom, Yemane; Polyak, Victor J; Humphreys, William F; Cugley, John; Woods, David; LaPointe, Zachary; Peota, Julian; Greaves, Elizabeth (2013): North Atlantic forcing of millennial-scale Indo-Australian monsoon dynamics during the Last Glacial period. Quaternary Science Reviews, 72, 159-168, https://doi.org/10.1016/j.quascirev.2013.04.012
Dixon, Teresa; Rudd, Rachel; Kemp, Justine; Marx, Samuel K; Moss, Patrick T; Callow, John Nikolaus; Hall, Philip Anthony; Hua, Quan; McGowan, Hamish A (2025): Hydroclimate variability in the eastern Kimberley, Australia, since the last deglaciation. Journal of Quaternary Science, 40(5), 893-912, https://doi.org/10.1002/jqs.3710
English, P; Spooner, N A; Chappell, J; Questiaux, D G; Hill, N G (2001): Lake Lewis basin, central Australia: environmental evolution and OSL chronology. Quaternary International, 83-85, 81-101, https://doi.org/10.1016/S1040-6182(01)00032-5
Field, Emily; McGowan, Hamish A; Moss, Patrick T; Marx, Samuel K (2017): A late Quaternary record of monsoon variability in the northwest Kimberley, Australia. Quaternary International, 449, 119-135, https://doi.org/10.1016/j.quaint.2017.02.019
Field, Emily; Tyler, Jonathan James; Gadd, Patricia S; Moss, Patrick T; McGowan, Hamish A; Marx, Samuel K (2018): Coherent patterns of environmental change at multiple organic spring sites in northwest Australia: Evidence of Indonesian-Australian summer monsoon variability over the last 14,500 years. Quaternary Science Reviews, 196, 193-216, https://doi.org/10.1016/j.quascirev.2018.07.018
Fitzsimmons, Kathryn E; Miller, G H; Spooner, N A; Magee, John W (2012): Aridity in the monsoon zone as indicated by desert dune formation in the Gregory Lakes basin, northwestern Australia. Australian Journal of Earth Sciences, 59(4), 469-478, https://doi.org/10.1080/08120099.2012.686171
Jennings, J N (1975): Desert dunes and estuarine fill in the Fitzroy estuary (North-Western Australia). CATENA, 2, 215-262, https://doi.org/10.1016/S0341-8162(75)80015-4
Kuhnt, Wolfgang; Holbourn, Ann E; Xu, Jian; Opdyke, Bradley N; De Deckker, Patrick; Röhl, Ursula; Mudelsee, Manfred (2015): Southern Hemisphere control on Australian monsoon variability during the late deglaciation and Holocene. Nature Communications, 6, 5916, https://doi.org/10.1038/ncomms6916
Lees, Brian G; Hayne, Matthew; Price, David M (1993): Marine transgression and dune initiation on western Cape York, northern Australia. Marine Geology, 114(1-2), 81-89, https://doi.org/10.1016/0025-3227(93)90040-3
Lees, Brian G; Yanchou, Lu; Head, John (1990): Reconnaissance Thermoluminescence Dating of Northern Australian Coastal Dune Systems. Quaternary Research, 34(2), 169-185, https://doi.org/10.1016/0033-5894(90)90029-K
Lees, Brian G; Yanehou, Lu; Price, David M (1992): Thermoluminescence dating of dunes at Cape St. Lambert, East Kimberleys, northwestern Australia. Marine Geology, 106(1-2), 131-139, https://doi.org/10.1016/0025-3227(92)90058-P
Mackenzie, Lydia; Heijnis, Henk; Gadd, Patricia S; Moss, Patrick T; Shulmeister, James (2017): Geochemical investigation of the South Wellesley Island wetlands: Insight into wetland development during the Holocene in tropical northern Australia. The Holocene, 27(4), 566-578, https://doi.org/10.1177/0959683616670219
Marx, Samuel K; Reynolds, William; May, Jan-Hendrik; Forbes, Matthew S; Stromsoe, Nicola; Fletcher, Michael-Shawn; Cohen, Timothy J; Moss, Patrick T; Mazumder, Debashish; Gadd, Patricia S (2021): Monsoon driven ecosystem and landscape change in the 'Top End' of Australia during the past 35 kyr. Palaeogeography, Palaeoclimatology, Palaeoecology, 583, 110659, https://doi.org/10.1016/j.palaeo.2021.110659
McGowan, Hamish A; Marx, Samuel K; Moss, Patrick T; Hammond, Andrew P (2012): Evidence of ENSO mega-drought triggered collapse of prehistory Aboriginal society in northwest Australia. Geophysical Research Letters, 39(22), 2012GL053916, https://doi.org/10.1029/2012GL053916
Miller, Gifford H; Magee, John W; Fogel, Marilyn L; Wooller, Matthew J; Hesse, Paul P; Spooner, Nigel A; Johnson, Beverly J; Wallis, Lynley (2018): Wolfe Creek Crater: A continuous sediment fill in the Australian Arid Zone records changes in monsoon strength through the Late Quaternary. Quaternary Science Reviews, 199, 108-125, https://doi.org/10.1016/j.quascirev.2018.07.019
Moss, Patrick T; Mackenzie, Lydia; Ulm, Sean; Sloss, Craig; Rosendahl, Daniel; Petherick, Lynda M; Steinberger, Lincoln; Wallis, Lynley; Heijnis, Henk; Petchey, Fiona; Jacobsen, Geraldine (2015): Environmental context for late Holocene human occupation of the South Wellesley Archipelago, Gulf of Carpentaria, northern Australia. Quaternary International, 385, 136-144, https://doi.org/10.1016/j.quaint.2015.02.051
Mulrennan, M E; Woodroffe, Colin D (1998): Holocene development of the lower Mary River plains, Northern Territory, Australia. The Holocene, 8(5), 565-579, https://doi.org/10.1191/095968398676885724
Prebble, Matiu; Sim, Robin; Finn, Janet; Fink, David (2005): A Holocene Pollen and Diatom Record from Vanderlin Island, Gulf of Carpentaria, Lowland Tropical Australia. Quaternary Research, 64(3), 357-371, https://doi.org/10.1016/j.yqres.2005.08.005
Proske, Ulrike (2016): Holocene freshwater wetland and mangrove dynamics in the eastern Kimberley, Australia. Journal of Quaternary Science, 31(1), 1-11, https://doi.org/10.1002/jqs.2827
Proske, Ulrike; Heslop, David; Haberle, Simon G (2014): A Holocene record of coastal landscape dynamics in the eastern Kimberley region, Australia. Journal of Quaternary Science, 29(2), 163-174, https://doi.org/10.1002/jqs.2691
Reeves, Jessica M; Chivas, Allan R; García, Adriana; Holt, Sabine; Couapel, Martine J J; Jones, Brian G; Cendón, Dioni I; Fink, David (2008): The sedimentary record of palaeoenvironments and sea-level change in the Gulf of Carpentaria, Australia, through the last glacial cycle. Quaternary International, 183(1), 3-22, https://doi.org/10.1016/j.quaint.2007.11.019
Rehn, Emma; Rowe, Cassandra; Ulm, Sean; Gadd, Patricia S; Zawadzki, Atun; Jacobsen, Geraldine E; Woodward, Craig; Bird, Michael (2021): Multiproxy Holocene Fire Records From the Tropical Savannas of Northern Cape York Peninsula, Queensland, Australia. Frontiers in Ecology and Evolution, 9, 771700, https://doi.org/10.3389/fevo.2021.771700 (Rehn et al. (2021a))
Rehn, Emma; Rowe, Cassandra; Ulm, Sean; Woodward, Craig; Bird, Michael (2021): A late-Holocene multiproxy fire record from a tropical savanna, eastern Arnhem Land, Northern Territory, Australia. The Holocene, 31(5), 870-883, https://doi.org/10.1177/0959683620988030 (Rehn et al. (2021b))
Rhodes, E G (1982): Depositional model for a chenier plain, Gulf of Carpentaria, Australia. Sedimentology, 29(2), 201-221, https://doi.org/10.1111/j.1365-3091.1982.tb01719.x
Rivera-Araya, Maria; Rowe, Cassandra; Levchenko, Vladimir; Ulm, Sean; Bird, Michael I (2022): A radiocarbon chronology for Sanamere Lagoon, Cape York Peninsula, using multiple organic fractions. Quaternary Geochronology, 70, 101273, https://doi.org/10.1016/j.quageo.2022.101273
Rowe, Cassandra; Brand, Michael; Hutley, Lindsay B; Wurster, Christopher M; Zwart, Costijn; Levchenko, Vlad; Bird, Michael I (2019): Holocene savanna dynamics in the seasonal tropics of northern Australia. Review of Palaeobotany and Palynology, 267, 17-31, https://doi.org/10.1016/j.revpalbo.2019.05.004
Rudd, Rachel; Dixon, Teresa; Callow, John Nikolaus; Gadd, Patricia S; Maizma, Sabika; Jacobsen, Geraldine; Moss, Patrick T; McGowan, Hamish A (2025): A record of monsoon rainforest variability from the Kimberley region in northwestern Australia. Journal of Quaternary Science, 40(2), 243-256, https://doi.org/10.1002/jqs.3693
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Shulmeister, James; Lees, Brian G (1995): Pollen evidence from tropical Australia for the onset of an ENSO-dominated climate at c. 4000 BP. The Holocene, 5(1), 10-18, https://doi.org/10.1177/095968369500500102
Stevenson, Janelle; Brockwell, Sally; Rowe, Cassandra; Proske, Ulrike; Shiner, Justin (2015): The palaeo-environmental history of Big Willum Swamp, Weipa: An environmental context for the archaeological record. Australian Archaeology, 80(1), 17-31, https://doi.org/10.1080/03122417.2015.11682041
Torgersen, T; Luly, J; De Deckker, Patrick; Jones, M R; Searle, D E; Chivas, A R; Ullman, W J (1988): Late quaternary environments of the Carpentaria Basin, Australia. Palaeogeography, Palaeoclimatology, Palaeoecology, 67(3-4), 245-261, https://doi.org/10.1016/0031-0182(88)90155-1
van der Kaars, Sander; De Deckker, Patrick; Gingele, Franz X (2006): A 100 000‐year record of annual and seasonal rainfall and temperature for northwestern Australia based on a pollen record obtained offshore. Journal of Quaternary Science, 21(8), 879-889, https://doi.org/10.1002/jqs.1010
van der Kaars, W A (1989): Aspects of late quaternary palynology of Eastern Indonesian deep-sea cores. Netherlands Journal of Sea Research, 24(4), 495-500, https://doi.org/10.1016/0077-7579(89)90127-0
Wende, R; Nanson, G C; Price, D M (1997): Aeolian and fluvial evidence for late Quaternary environmental change in the east Kimberley of Western Australia. Australian Journal of Earth Sciences, 44(4), 519-526, https://doi.org/10.1080/08120099708728331
Wyrwoll, Karl-Heinz; Miller, Gifford H (2001): Initiation of the Australian summer monsoon 14,000 years ago. Quaternary International, 83-85, 119-128, https://doi.org/10.1016/S1040-6182(01)00034-9
Funding:
Australian Research Council (ARC), grant/award no. CE170100015: ARC Centre of Excellence for Australian Biodiversity and Heritage
Australian Research Council (ARC), grant/award no. CE230100009: ARC Centre of Excellence for Indigenous and Environmental Histories and Futures
Australian Research Council (ARC), grant/award no. DE240100340: Identifying key fire drivers in Australia; biomass, climate or people
Australian Research Council (ARC), grant/award no. FT180100524: Climate extremes and landscape responses across continental Australia
Coverage:
Median Latitude: -14.154278 * Median Longitude: 130.794996 * South-bound Latitude: -22.920000 * West-bound Longitude: 113.500000 * North-bound Latitude: -8.790000 * East-bound Longitude: 145.240000
Date/Time Start: 2001-05-03T21:05:00 * Date/Time End: 2005-10-01T04:42:00
Minimum Elevation: -2974.0 m * Maximum Elevation: 330.0 m
Event(s):
Comment:
• Calibration curves themselves are not included here (publicly available), but the column identifiers match standard Bchron curve names.
• Reservoir corrections are stored as reported; NA indicates none was applied.
• No calibrated ages are stored; these must be generated by the user using the accompanying code.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | Wall, Alexander Forster | sample; archive/site identifier | ||
| 2 | LATITUDE | Latitude | Wall, Alexander Forster | Geocode | ||
| 3 | LONGITUDE | Longitude | Wall, Alexander Forster | Geocode | ||
| 4 | Archive | Archive | Wall, Alexander Forster | |||
| 5 | Laboratory code/label | Lab label | Wall, Alexander Forster | LAB ID | ||
| 6 | Age, dating method | Dating meth | Wall, Alexander Forster | Chronology | ||
| 7 | DEPTH, sediment/rock | Depth sed | m | Wall, Alexander Forster | Geocode | |
| 8 | DISTANCE | Distance | cm | Wall, Alexander Forster | Geocode | |
| 9 | Age, dated | Age dated | ka | Wall, Alexander Forster | reported uncalibrated age (radiocarbon) or equivalent age | |
| 10 | Age, dated, error to older | Age e + | ka + | Wall, Alexander Forster | positive error term (1 σ) | |
| 11 | Reservoir age | Res age | ka | Wall, Alexander Forster | reservoir correction (if applicable) | |
| 12 | Calibration | Calibration | Wall, Alexander Forster | original calibration curve used in the publication | ||
| 13 | Calibration | Calibration | Wall, Alexander Forster | updated calibration curve to be used for re-analysis | ||
| 14 | Year of publication | Year pub | Wall, Alexander Forster | publication year of the original age determination | ||
| 15 | Reference/source | Reference | Wall, Alexander Forster | bibliographic reference for the date |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0) (License comes into effect after moratorium ends)
Size:
5851 data points
Data
| 1 Event (sample; archive/site identifier) | 2 Latitude | 3 Longitude | 4 Archive | 5 Lab label (LAB ID) | 6 Dating meth (Chronology) | 7 Depth sed [m] | 8 Distance [cm] | 9 Age dated [ka] (reported uncalibrated age (ra...) | 10 Age e + [ka +] (positive error term (1 σ)) | 11 Res age [ka] (reservoir correction (if appl...) | 12 Calibration (original calibration curve us...) | 13 Calibration (updated calibration curve to ...) | 14 Year pub (publication year of the origi...) | 15 Reference (bibliographic reference for t...) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| TAEAC_BGC10 | -17.030000 | 125.000000 | speleothem | 10.4 | U/Th | 31.5 | 38.640 | 0.550 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC10 | -17.030000 | 125.000000 | speleothem | 10.3 | U/Th | 43.1 | 39.110 | 0.230 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC10 | -17.030000 | 125.000000 | speleothem | 10.2 | U/Th | 54.6 | 38.170 | 0.290 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC10 | -17.030000 | 125.000000 | speleothem | 10.1 | U/Th | 60.2 | 36.350 | 0.430 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC11 | -17.030000 | 125.000000 | speleothem | 11.3 | U/Th | 9.1 | 10.070 | 0.740 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC11 | -17.030000 | 125.000000 | speleothem | 11.2 | U/Th | 11.3 | 9.620 | 1.930 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC11 | -17.030000 | 125.000000 | speleothem | 11.1 | U/Th | 15.1 | 10.290 | 1.720 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC14 | -17.030000 | 125.000000 | speleothem | 14.5 | U/Th | 0.8 | 23.820 | 1.000 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC14 | -17.030000 | 125.000000 | speleothem | 14.4 | U/Th | 6.3 | 21.260 | 0.990 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC14 | -17.030000 | 125.000000 | speleothem | 14.3 | U/Th | 7.2 | 21.870 | 0.640 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC14 | -17.030000 | 125.000000 | speleothem | 14.2 | U/Th | 8.9 | 22.440 | 1.260 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC14 | -17.030000 | 125.000000 | speleothem | 14.1 | U/Th | 13.9 | 18.790 | 2.220 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC16 | -17.030000 | 125.000000 | speleothem | 16.3 | U/Th | 18.7 | 37.040 | 0.480 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC16 | -17.030000 | 125.000000 | speleothem | 16.5 | U/Th | 33.9 | 34.520 | 0.720 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC16 | -17.030000 | 125.000000 | speleothem | 16.2 | U/Th | 50.6 | 36.870 | 1.220 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC16 | -17.030000 | 125.000000 | speleothem | 16.4 | U/Th | 72.4 | 33.140 | 0.360 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC16 | -17.030000 | 125.000000 | speleothem | 16.1 | U/Th | 81.9 | 32.070 | 0.790 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC5 | -17.030000 | 125.000000 | speleothem | 5.6 | U/Th | 29.7 | 27.230 | 1.040 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC5 | -17.030000 | 125.000000 | speleothem | 5.5 | U/Th | 36.1 | 25.570 | 2.150 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC5 | -17.030000 | 125.000000 | speleothem | 5.4 | U/Th | 43.5 | 26.090 | 0.790 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC5 | -17.030000 | 125.000000 | speleothem | 5.3 | U/Th | 46.3 | 25.420 | 0.500 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC5 | -17.030000 | 125.000000 | speleothem | 5.2 | U/Th | 72.7 | 25.500 | 2.650 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC5 | -17.030000 | 125.000000 | speleothem | 5.1 | U/Th | 76.9 | 26.000 | 1.730 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.18 | U/Th | 3.3 | 16.690 | 1.000 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.15 | U/Th | 25.5 | 13.590 | 2.900 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.14 | U/Th | 25.5 | 15.020 | 5.430 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.12 | U/Th | 25.5 | 15.100 | 1.500 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.13 | U/Th | 25.5 | 15.200 | 3.480 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.16 | U/Th | 25.5 | 17.760 | 0.270 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.17 | U/Th | 25.5 | 19.410 | 0.440 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.11 | U/Th | 35.6 | 12.330 | 1.680 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.10 | U/Th | 42.3 | 11.720 | 2.420 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.9 | U/Th | 46.3 | 11.090 | 2.830 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.8 | U/Th | 47.2 | 11.390 | 0.410 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.7 | U/Th | 48.4 | 10.740 | 2.050 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.6 | U/Th | 49.6 | 11.110 | 0.920 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.5 | U/Th | 52.6 | 10.850 | 0.990 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.4 | U/Th | 56.5 | 9.710 | 1.270 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.3 | U/Th | 64.9 | 7.220 | 2.140 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.2 | U/Th | 66.4 | 6.070 | 2.510 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_BGC6 | -17.030000 | 125.000000 | speleothem | 6.1 | U/Th | 67.4 | 6.550 | 1.640 | normal | normal | 2013 | Denniston et al. (2013) | ||
| TAEAC_Black_Springs | -15.630000 | 126.380000 | lake | Wk-29127 | radiocarbon | 0.2250 | 0.516 | 0.035 | shcal04 | shcal20 | 2012 | McGowan et al. (2012) | ||
| TAEAC_Black_Springs | -15.630000 | 126.380000 | lake | Wk-28374 | radiocarbon | 0.4500 | 3.455 | 0.050 | shcal04 | shcal20 | 2012 | McGowan et al. (2012) | ||
| TAEAC_Black_Springs | -15.630000 | 126.380000 | lake | Wk-19128 | radiocarbon | 0.5500 | 4.671 | 0.032 | shcal04 | shcal20 | 2012 | McGowan et al. (2012) | ||
| TAEAC_Black_Springs | -15.630000 | 126.380000 | lake | Wk-29129 | radiocarbon | 0.7900 | 6.938 | 0.037 | shcal04 | shcal20 | 2012 | McGowan et al. (2012) | ||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | lead-210 | 0.0050 | -0.069 | 0.000 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | lead-210 | 0.0100 | -0.067 | 0.001 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | lead-210 | 0.0225 | -0.057 | 0.001 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | lead-210 | 0.0300 | -0.049 | 0.001 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | lead-210 | 0.0400 | -0.045 | 0.002 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | lead-210 | 0.0525 | -0.010 | 0.003 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | radiocarbon | 0.3500 | 3.767 | 0.028 | shcal20 | shcal20 | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 0.4000 | 4.029 | 0.400 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 0.6000 | 5.229 | 0.400 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 1.2000 | 14.829 | 1.500 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 1.5550 | 15.029 | 1.500 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 1.6850 | 29.129 | 3.000 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 1.7800 | 49.929 | 6.000 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 1.8600 | 57.929 | 8.000 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 2.0700 | 55.929 | 6.000 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 2.2050 | 60.929 | 7.000 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BR-BU | -15.466500 | 129.785000 | fluvial | OSL | 2.3850 | 71.929 | 9.000 | normal | normal | 2025 | Dixon et al. (2025) | |||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-29127 | radiocarbon | 0.2250 | 0.516 | 0.035 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-28374 | radiocarbon | 0.4500 | 3.455 | 0.050 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-19128 | radiocarbon | 0.5500 | 4.671 | 0.032 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-29129 | radiocarbon | 0.7900 | 6.938 | 0.037 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-28376 | radiocarbon | 0.9450 | 8.186 | 0.035 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-29130 | radiocarbon | 1.0400 | 7.081 | 0.040 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-41825 | radiocarbon | 1.1270 | 6.151 | 0.084 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-28377 | radiocarbon | 1.2650 | 5.713 | 0.030 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-29131 | radiocarbon | 1.4000 | 7.439 | 0.036 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-28375 | radiocarbon | 1.5250 | 7.033 | 0.031 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP | -15.630000 | 126.380000 | lake | Wk-41826 | radiocarbon | 1.6430 | 5.437 | 0.022 | shcal13 | shcal20 | 2017 | Field et al. (2017) | ||
| TAEAC_BSP02 | -15.630000 | 126.390000 | lake | Wk-44690 | radiocarbon | 0.7500 | 3.014 | 0.020 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_BSP02 | -15.630000 | 126.390000 | lake | Wk-44691 | radiocarbon | 1.4900 | 6.430 | 0.023 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_BSP02 | -15.630000 | 126.390000 | lake | OZT912 | radiocarbon | 1.8700 | 8.890 | 0.060 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_BSP02 | -15.630000 | 126.390000 | lake | Wk-44692 | radiocarbon | 1.8900 | 8.944 | 0.029 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_BSP02 | -15.630000 | 126.390000 | lake | OZU455 | radiocarbon | 2.3300 | 12.100 | 0.040 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_BW01 | -12.657000 | 141.998000 | lake | Wk34027 | radiocarbon | 0.1050 | 1.063 | 0.026 | shcal13 | shcal20 | 2015 | Stevenson et al. (2015) | ||
| TAEAC_BW01 | -12.657000 | 141.998000 | lake | Wk34028 | radiocarbon | 0.1850 | 1.491 | 0.025 | shcal13 | shcal20 | 2015 | Stevenson et al. (2015) | ||
| TAEAC_BW01 | -12.657000 | 141.998000 | lake | Wk35162 | radiocarbon | 0.2150 | 2.275 | 0.025 | shcal13 | shcal20 | 2015 | Stevenson et al. (2015) | ||
| TAEAC_BW01 | -12.657000 | 141.998000 | lake | D-AMS001835 | radiocarbon | 0.2350 | 4.244 | 0.027 | shcal13 | shcal20 | 2015 | Stevenson et al. (2015) | ||
| TAEAC_BW01 | -12.657000 | 141.998000 | lake | Wk35163 | radiocarbon | 0.2550 | 4.993 | 0.039 | shcal13 | shcal20 | 2015 | Stevenson et al. (2015) | ||
| TAEAC_BW01 | -12.657000 | 141.998000 | lake | Wk34029 | radiocarbon | 0.2850 | 6.217 | 0.040 | shcal13 | shcal20 | 2015 | Stevenson et al. (2015) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U090 | lead-210 | 0.0000 | -0.070 | 0.005 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U093 | lead-210 | 0.0150 | -0.032 | 0.006 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U094 | lead-210 | 0.0200 | -0.020 | 0.006 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U095 | lead-210 | 0.0250 | -0.009 | 0.006 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U096 | lead-210 | 0.0300 | 0.003 | 0.007 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U097 | lead-210 | 0.0350 | 0.016 | 0.007 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U098 | lead-210 | 0.0400 | 0.031 | 0.008 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U099 | lead-210 | 0.0450 | 0.075 | 0.009 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U530 | lead-210 | 0.0500 | 0.606 | 0.009 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | OZX211 | radiocarbon | 0.0500 | 0.760 | 0.020 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | U534 | lead-210 | 0.0650 | 0.714 | 0.011 | normal | normal | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | OZW504 | radiocarbon | 0.0800 | 1.280 | 0.020 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | OZW505 | radiocarbon | 0.0900 | 1.510 | 0.035 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | OZW506 | radiocarbon | 0.1000 | 1.730 | 0.030 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | OZW507 | radiocarbon | 0.1100 | 3.145 | 0.040 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_BWIL2 | -12.657000 | 141.998000 | lake | OZW508 | radiocarbon | 0.1200 | 3.445 | 0.035 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | W894 | TL | 0.400 | 0.200 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | W899 | TL | 0.550 | 0.200 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | W895 | TL | 0.700 | 0.250 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | W898 | TL | 0.850 | 0.500 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | XAL097 | TL | 1.500 | 0.200 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | XAL098 | TL | 1.600 | 0.200 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | W900 | TL | 1.650 | 0.450 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | W897 | TL | 2.950 | 0.900 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | XAL100 | TL | 3.400 | 0.300 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | XAL099 | TL | 4.700 | 0.500 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | W896 | TL | 4.900 | 1.350 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | aeolian | XAL096 | TL | 5.600 | 0.800 | normal | normal | 1992 | Lees et al. (1992) | |||
| TAEAC_Cape_Flattery | -15.080000 | 145.240000 | aeolian | ANU-6171 | radiocarbon | 0.220 | 0.070 | normal | shcal20 | 1990 | Lees et al. (1990) | |||
| TAEAC_Cape_Flattery | -15.080000 | 145.240000 | aeolian | Au-03 | TL | 2.000 | 1.000 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cape_Flattery | -15.080000 | 145.240000 | aeolian | Au-18 | TL | 19.200 | 3.400 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cape_Flattery | -15.080000 | 145.240000 | aeolian | Au-04 | TL | 19.800 | 2.300 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cape_Flattery | -15.080000 | 145.240000 | aeolian | Au-19 | TL | 22.700 | 2.800 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cape_Flattery | -15.080000 | 145.240000 | aeolian | Au-05 | TL | 171.000 | 13.000 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | aeolian | ANU-6029 | radiocarbon | 0.180 | 0.105 | normal | shcal20 | 1990 | Lees et al. (1990) | |||
| TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | aeolian | Au-15 | TL | 1.900 | 0.400 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | aeolian | Au-17 | TL | 2.600 | 0.300 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | aeolian | Au-16 | TL | 2.800 | 0.700 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | aeolian | Au-13 | TL | 8.600 | 1.400 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | aeolian | Au-11 | TL | 9.300 | 1.100 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | aeolian | Au-12 | TL | 81.400 | 8.500 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Core89_1 | -13.850000 | 136.780000 | lake | ANU7108 | radiocarbon | 0.1500 | 0.980 | 0.170 | normal | shcal20 | 1995 | Shulmeister and Lees (1995) | ||
| TAEAC_Core89_1 | -13.850000 | 136.780000 | lake | ANU7109 | radiocarbon | 0.4500 | 3.960 | 0.170 | normal | shcal20 | 1995 | Shulmeister and Lees (1995) | ||
| TAEAC_Core89_1 | -13.850000 | 136.780000 | lake | ANU7110 | radiocarbon | 0.7500 | 4.200 | 0.100 | normal | shcal20 | 1995 | Shulmeister and Lees (1995) | ||
| TAEAC_Core89_1 | -13.850000 | 136.780000 | lake | ANU7111 | radiocarbon | 1.1000 | 7.450 | 0.090 | normal | shcal20 | 1995 | Shulmeister and Lees (1995) | ||
| TAEAC_Core89_1 | -13.850000 | 136.780000 | lake | ANU7112 | radiocarbon | 1.2000 | 9.250 | 0.230 | normal | shcal20 | 1995 | Shulmeister and Lees (1995) | ||
| TAEAC_Core89_1 | -13.850000 | 136.780000 | lake | ANU7113 | radiocarbon | 1.2500 | 8.690 | 0.200 | normal | shcal20 | 1995 | Shulmeister and Lees (1995) | ||
| TAEAC_Core89_1 | -13.850000 | 136.780000 | lake | AA6460 | radiocarbon | 1.5500 | 10.000 | 0.075 | normal | shcal20 | 1995 | Shulmeister and Lees (1995) | ||
| TAEAC_CT | -15.800000 | 128.800000 | aeolian | W2015 | TL | 1.8000 | 6.100 | 0.500 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_CT | -15.800000 | 128.800000 | aeolian | W2016 | TL | 3.5000 | 5.300 | 0.400 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_CT | -15.800000 | 128.800000 | aeolian | W1773 | TL | 4.5000 | 9.000 | 0.700 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_CT | -15.800000 | 128.800000 | aeolian | W1772 | TL | 4.7000 | 12.600 | 1.000 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_CT | -15.800000 | 128.800000 | aeolian | W2019 | TL | 5.5000 | 37.400 | 6.100 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_CT | -15.800000 | 128.800000 | aeolian | W2017 | TL | 6.0000 | 9.800 | 1.000 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_CT | -15.800000 | 128.800000 | aeolian | W2018 | TL | 6.2000 | 10.400 | 1.000 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_CT | -15.800000 | 128.800000 | aeolian | W1771 | TL | 7.5000 | 37.000 | 3.100 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_Dune_W_Cape_York | -12.280000 | 141.720000 | aeolian | W1272 | TL | 5.200 | 1.800 | normal | normal | 1993 | Lees et al. (1993) | |||
| TAEAC_Dune_W_Cape_York | -12.280000 | 141.720000 | aeolian | W1273 | TL | 5.300 | 2.100 | normal | normal | 1993 | Lees et al. (1993) | |||
| TAEAC_Dune_W_Cape_York | -12.280000 | 141.720000 | aeolian | W1275 | TL | 8.300 | 1.100 | normal | normal | 1993 | Lees et al. (1993) | |||
| TAEAC_Dune_W_Cape_York | -12.280000 | 141.720000 | aeolian | W1276 | TL | 8.300 | 0.600 | normal | normal | 1993 | Lees et al. (1993) | |||
| TAEAC_Dune_W_Cape_York | -12.280000 | 141.720000 | aeolian | W1274 | TL | 11.200 | 1.800 | normal | normal | 1993 | Lees et al. (1993) | |||
| TAEAC_E_Alligator_R | -12.560000 | 133.110000 | fluvial | EALa1 | OSL | 0.340 | 0.030 | normal | normal | 2020 | Saynor et al. (2020) | |||
| TAEAC_E_Alligator_R | -12.560000 | 133.110000 | fluvial | EALa2 | OSL | 0.480 | 0.120 | normal | normal | 2020 | Saynor et al. (2020) | |||
| TAEAC_E_Alligator_R | -12.560000 | 133.110000 | fluvial | Nt1-5 | OSL | 0.590 | 0.110 | normal | normal | 2020 | Saynor et al. (2020) | |||
| TAEAC_E_Alligator_R | -12.560000 | 133.110000 | fluvial | Nt5-0 | OSL | 1.070 | 0.160 | normal | normal | 2020 | Saynor et al. (2020) | |||
| TAEAC_E_Alligator_R | -12.560000 | 133.110000 | fluvial | Nt7-5 | OSL | 1.940 | 0.270 | normal | normal | 2020 | Saynor et al. (2020) | |||
| TAEAC_E_Alligator_R | -12.560000 | 133.110000 | fluvial | EALa3 | OSL | 2.910 | 0.350 | normal | normal | 2020 | Saynor et al. (2020) | |||
| TAEAC_E_Alligator_R | -12.560000 | 133.110000 | fluvial | EALa4 | OSL | 3.100 | 0.200 | normal | normal | 2020 | Saynor et al. (2020) | |||
| TAEAC_E_Alligator_R | -12.560000 | 133.110000 | fluvial | EALa5 | OSL | 8.400 | 0.400 | normal | normal | 2020 | Saynor et al. (2020) | |||
| TAEAC_ELZ02 | -16.400000 | 126.130000 | lake | OZU456 | radiocarbon | 0.3500 | 3.175 | 0.025 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_ELZ02 | -16.400000 | 126.130000 | lake | OZU457 | radiocarbon | 0.5600 | 5.355 | 0.035 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_ELZ02 | -16.400000 | 126.130000 | lake | OZU458 | radiocarbon | 0.7600 | 7.790 | 0.035 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_ELZ02 | -16.400000 | 126.130000 | lake | Wk-44693 | radiocarbon | 0.9600 | 8.859 | 0.033 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_ELZ02 | -16.400000 | 126.130000 | lake | OZU459 | radiocarbon | 1.1600 | 12.430 | 0.045 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | ANU1194A | radiocarbon | 0.144 | 0.012 | normal | postbomb_SH3 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | ANU1074 | radiocarbon | 0.153 | 0.012 | normal | postbomb_SH3 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | ANU1194B | radiocarbon | 0.350 | 0.080 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | GAK3843 | radiocarbon | 0.500 | 0.080 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | GAK3840 | radiocarbon | 0.910 | 0.080 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | GAK3842 | radiocarbon | 1.190 | 0.080 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | GAK2020 | radiocarbon | 5.840 | 0.110 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | ANU378 | radiocarbon | 5.990 | 0.190 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | GAK019 | radiocarbon | 6.050 | 0.130 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | ANU377 | radiocarbon | 6.140 | 0.120 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | GAK201 | radiocarbon | 6.160 | 0.190 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | ANU1075 | radiocarbon | 6.570 | 0.080 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | GAK2017 | radiocarbon | 7.400 | 0.110 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | coastal | ANU188 | radiocarbon | 7.450 | 0.770 | normal | shcal20 | 1975 | Jennings (1975) | |||
| TAEAC_Fitzroy_River | -20.130000 | 127.410000 | fluvial | Wk2404b | radiocarbon | 11.700 | 0.150 | shcal98 | shcal20 | 2001 | Wyrwoll and Miller (2001) | |||
| TAEAC_Fitzroy_River | -20.130000 | 127.410000 | fluvial | Wk2403 | radiocarbon | 11.850 | 0.380 | shcal98 | shcal20 | 2001 | Wyrwoll and Miller (2001) | |||
| TAEAC_Fitzroy_River | -20.130000 | 127.410000 | fluvial | Wk2404a | radiocarbon | 12.050 | 0.420 | shcal98 | shcal20 | 2001 | Wyrwoll and Miller (2001) | |||
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13031 | radiocarbon | 0.0750 | 1.630 | 0.185 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13030 | radiocarbon | 0.1950 | 2.150 | 0.600 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13029 | radiocarbon | 0.4550 | 4.050 | 0.225 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13028 | radiocarbon | 0.5750 | 4.760 | 0.220 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13027 | radiocarbon | 0.6550 | 6.200 | 0.180 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13026 | radiocarbon | 0.7550 | 7.370 | 0.190 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13025 | radiocarbon | 0.8350 | 7.930 | 0.220 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA6124 | radiocarbon | 0.9750 | 9.420 | 0.230 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13024 | radiocarbon | 1.0550 | 11.330 | 0.260 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | OZD499 | radiocarbon | 1.1750 | 13.080 | 0.110 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | OZD741 | radiocarbon | 1.2350 | 14.300 | 0.110 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | OZD744 | radiocarbon | 1.3950 | 19.250 | 0.280 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13023 | radiocarbon | 1.4950 | 20.240 | 0.550 | 0.4000 | intcal98 | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13022 | radiocarbon | 1.8250 | 27.820 | 0.780 | 0.4000 | hughen | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| FR10/95-GC17 | -22.130000 | 113.500000 | marine_core | ANUA13020 | radiocarbon | 2.5000 | 40.650 | 1.130 | 0.4000 | hughen | shcal20 | 2006 | Van der Kaars et al. (2006) | |
| TAEAC_FRN02 | -15.940000 | 126.280000 | lake | OZU460 | radiocarbon | 0.4900 | 1.215 | 0.025 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_FRN02 | -15.940000 | 126.280000 | lake | OZT918 | radiocarbon | 0.5000 | 1.030 | 0.030 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_FRN02 | -15.940000 | 126.280000 | lake | OZU461 | radiocarbon | 0.9500 | 3.505 | 0.025 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_FRN02 | -15.940000 | 126.280000 | lake | OZT163 | radiocarbon | 1.0000 | 3.395 | 0.040 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_FRN02 | -15.940000 | 126.280000 | lake | OZT162 | radiocarbon | 1.4800 | 6.960 | 0.040 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_FRN02 | -15.940000 | 126.280000 | lake | OZT917 | radiocarbon | 1.5000 | 6.980 | 0.210 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_FRN02 | -15.940000 | 126.280000 | lake | OZU462 | radiocarbon | 1.9600 | 10.110 | 0.035 | shcal13 | shcal20 | 2018 | Field et al. (2018) | ||
| TAEAC_G5_6_149P2 | -9.000000 | 128.000000 | marine_core | radiocarbon | 0.0000 | 3.950 | 0.100 | normal | marine20 | 1989 | van der Kaars et al. (1989) | |||
| TAEAC_G5_6_149P2 | -9.000000 | 128.000000 | marine_core | radiocarbon | 2.0000 | 18.800 | 0.300 | normal | marine20 | 1989 | van der Kaars et al. (1989) | |||
| TAEAC_G5_6_149P2 | -9.000000 | 128.000000 | marine_core | radiocarbon | 4.0000 | 34.000 | 2.000 | normal | marine20 | 1989 | van der Kaars et al. (1989) | |||
| TAEAC_G5_6_149P2 | -9.000000 | 128.000000 | marine_core | radiocarbon | 5.5000 | 43.000 | 7.000 | normal | marine20 | 1989 | van der Kaars et al. (1989) | |||
| TAEAC_GC_10A | -13.070000 | 140.200000 | marine_core | ANU3691 | radiocarbon | 1.0050 | 26.960 | 0.580 | normal | marine20 | 1988 | Torgersen et al. (1988) | ||
| TAEAC_GC_10A | -13.070000 | 140.200000 | marine_core | ANU3692 | radiocarbon | 1.1100 | 35.440 | 1.050 | normal | marine20 | 1988 | Torgersen et al. (1988) | ||
| TAEAC_GC_10A | -13.070000 | 140.200000 | marine_core | ANU3690 | radiocarbon | 1.2050 | 35.330 | 1.520 | normal | marine20 | 1988 | Torgersen et al. (1988) | ||
| GC-2 | -13.070000 | 140.200000 | marine_core | ANU3695 | radiocarbon | 0.0000 | 6.290 | 0.120 | normal | marine20 | 1988 | Torgersen et al. (1988) | ||
| GC-2 | -13.070000 | 140.200000 | marine_core | ANU4800 | radiocarbon | 0.0350 | 5.170 | 0.130 | normal | marine20 | 1988 | Torgersen et al. (1988) | ||
| GC-2 | -13.070000 | 140.200000 | marine_core | ANU4801 | radiocarbon | 0.2850 | 7.240 | 0.160 | normal | marine20 | 1988 | Torgersen et al. (1988) | ||
| GC-2 | -13.070000 | 140.200000 | marine_core | ANU4802 | radiocarbon | 0.3300 | 9.800 | 0.340 | normal | marine20 | 1988 | Torgersen et al. (1988) | ||
| GC-2 | -13.070000 | 140.200000 | marine_core | ANU4804 | radiocarbon | 0.6900 | 14.170 | 0.390 | normal | marine20 | 1988 | Torgersen et al. (1988) | ||
| TAEAC_Gilwah | -20.130000 | 127.410000 | fluvial | OS23434 | radiocarbon | 0.001 | 0.000 | postbomb_SH3 | postbomb_SH3 | 2001 | Wyrwoll and Miller (2001) | |||
| TAEAC_Gilwah | -20.130000 | 127.410000 | fluvial | AA33402 | radiocarbon | 12.505 | 0.080 | shcal98 | shcal20 | 2001 | Wyrwoll and Miller (2001) | |||
| TAEAC_Gilwah | -20.130000 | 127.410000 | fluvial | OS23433 | radiocarbon | 12.550 | 0.110 | shcal98 | shcal20 | 2001 | Wyrwoll and Miller (2001) | |||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | OZV436 | radiocarbon | 0.4100 | 0.780 | 0.025 | shcal13 | shcal20 | 2019 | Rowe et al. (2019) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | OZV437 | radiocarbon | 1.1500 | 0.940 | 0.025 | shcal13 | shcal20 | 2019 | Rowe et al. (2019) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | OZV438 | radiocarbon | 2.1400 | 3.535 | 0.025 | shcal13 | shcal20 | 2019 | Rowe et al. (2019) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | OZV439 | radiocarbon | 2.5800 | 5.060 | 0.035 | shcal13 | shcal20 | 2019 | Rowe et al. (2019) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | OZV440 | radiocarbon | 3.1300 | 7.780 | 0.035 | shcal13 | shcal20 | 2019 | Rowe et al. (2019) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | OZV441 | radiocarbon | 3.9000 | 9.150 | 0.035 | shcal13 | shcal20 | 2019 | Rowe et al. (2019) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | OZV442 | radiocarbon | 4.5500 | 12.970 | 0.080 | shcal13 | shcal20 | 2019 | Rowe et al. (2019) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-E-55 | OSL | 4.6700 | 10.400 | 0.700 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-F-18 | OSL | 5.1800 | 23.100 | 1.300 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-F-45 | OSL | 5.4500 | 28.900 | 1.700 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-F-75 | OSL | 5.7900 | 32.600 | 2.000 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-G-60 | OSL | 6.5600 | 32.500 | 2.100 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-H-30 | OSL | 7.0300 | 42.700 | 2.900 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-H-70 | OSL | 7.4300 | 49.100 | 3.300 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-I-5 | OSL | 7.6700 | 54.300 | 3.200 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-I-30 | OSL | 7.9200 | 58.300 | 3.900 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-I-65 | OSL | 8.2500 | 58.300 | 3.600 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-J-13 | OSL | 8.7300 | 62.400 | 4.800 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-L-50 | OSL | 9.5000 | 67.900 | 5.800 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-M-8 | OSL | 10.0800 | 77.600 | 5.400 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-N-50 | OSL | 10.5000 | 83.100 | 6.000 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-N-75 | OSL | 10.9700 | 88.500 | 6.700 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-O-28 | OSL | 11.2800 | 91.400 | 7.500 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-O-42 | OSL | 11.4200 | 90.800 | 8.200 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-O-1992 | OSL | 11.9000 | 97.100 | 11.400 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-P-20 | OSL | 12.2500 | 88.800 | 7.500 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-Q-25 | OSL | 13.3000 | 102.000 | 12.100 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-R-1993 | OSL | 14.9000 | 116.700 | 13.100 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-S-5 | OSL | 15.1000 | 115.900 | 12.000 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-S-95 | OSL | 15.9800 | 116.600 | 8.800 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Girraween | -12.520000 | 131.080000 | lake | GIR3-T-65 | OSL | 16.7000 | 121.600 | 10.400 | normal | normal | 2024 | Bird et al. (2024) | ||
| TAEAC_Karumba | -17.690000 | 140.420000 | coastal | ANU188 | radiocarbon | 5.600 | normal | normal | 1982 | Rhodes (1982) | ||||
| TAEAC_King_River | -15.570360 | 128.139650 | fluvial | ANU-35405 | radiocarbon | 1.830 | 0.010 | shcal13 | shcal20 | 2014 | Proske et al. (2014) | |||
| TAEAC_King_River | -16.570360 | 129.139650 | fluvial | ANU-35406 | radiocarbon | 6.500 | 0.035 | shcal13 | shcal20 | 2014 | Proske et al. (2014) | |||
| TAEAC_King_River | -17.570360 | 130.139650 | fluvial | ANU-31709 | radiocarbon | 6.550 | 0.045 | shcal13 | shcal20 | 2014 | Proske et al. (2014) | |||
| TAEAC_King_River | -18.570360 | 131.139650 | fluvial | ANU-32712 | radiocarbon | 6.610 | 0.060 | shcal13 | shcal20 | 2014 | Proske et al. (2014) | |||
| TAEAC_King_River | -20.570360 | 133.139650 | fluvial | ANU-33413 | radiocarbon | 6.900 | 0.060 | shcal13 | shcal20 | 2014 | Proske et al. (2014) | |||
| TAEAC_King_River | -19.570360 | 132.139650 | fluvial | ANU-32713 | radiocarbon | 7.470 | 0.110 | shcal13 | shcal20 | 2014 | Proske et al. (2014) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 2.4 | 22.502 | 1.601 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 8.8 | 25.256 | 0.537 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 11.7 | 19.978 | 0.101 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 16.6 | 21.349 | 0.138 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 23.1 | 15.265 | 0.189 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 24.3 | 14.741 | 0.273 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 24.9 | 11.249 | 0.530 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 26.1 | 10.341 | 0.659 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 29.2 | 8.019 | 0.067 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_1 | -15.180000 | 128.370000 | speleothem | U/Th | 34.1 | 8.021 | 0.186 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.21 | U/Th | 2.4 | 0.183 | 0.017 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.20 | U/Th | 4.4 | 0.163 | 0.005 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.19 | U/Th | 9.3 | 1.770 | 0.012 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.18 | U/Th | 20.0 | 0.054 | 0.002 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.17 | U/Th | 20.6 | 0.054 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.16 | U/Th | 23.1 | 0.044 | 0.002 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.15 | U/Th | 25.5 | 0.029 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.14 | U/Th | 26.6 | 0.026 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.13 | U/Th | 27.3 | 0.022 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.12 | U/Th | 28.0 | 0.016 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.10 | U/Th | 29.2 | 0.001 | 0.007 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.9 | U/Th | 29.7 | 0.002 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.8 | U/Th | 30.3 | 0.005 | 0.002 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.7 | U/Th | 31.1 | 0.000 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.6 | U/Th | 33.4 | -0.020 | 0.002 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.5 | U/Th | 34.3 | -0.029 | 0.002 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.4 | U/Th | 35.4 | -0.035 | 0.002 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.3 | U/Th | 37.5 | -0.049 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.2 | U/Th | 39.4 | -0.055 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_11 | -15.180000 | 128.370000 | speleothem | 11.1 | U/Th | 40.5 | -0.060 | 0.001 | normal | normal | 2015 | Denniston et al. (2015) | ||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 4.3 | 21.768 | 0.240 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 4.8 | 22.013 | 0.207 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 6.3 | 19.394 | 0.173 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 10.1 | 19.202 | 0.227 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 10.8 | 18.154 | 0.129 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 16.5 | 17.734 | 0.151 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 18.9 | 17.155 | 0.128 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 24.7 | 16.429 | 0.254 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 25.4 | 14.838 | 0.167 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_3 | -15.180000 | 128.370000 | speleothem | U/Th | 26.2 | 14.151 | 0.148 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 0.3 | 21.596 | 1.377 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 0.8 | 21.182 | 0.248 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 3.4 | 21.175 | 0.248 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 4.3 | 19.114 | 2.451 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 6.0 | 18.892 | 0.327 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 7.6 | 18.034 | 0.113 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 8.5 | 17.052 | 0.233 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 10.5 | 16.537 | 0.185 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 12.2 | 16.273 | 0.275 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 13.0 | 15.177 | 0.277 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 13.5 | 13.018 | 0.338 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_KNI_51_8 | -15.180000 | 128.370000 | speleothem | U/Th | 14.0 | 12.740 | 0.127 | normal | normal | 2017 | Denniston et al. (2017) | |||
| TAEAC_Lake_Lewis | -22.920000 | 132.530000 | lake | 95017 | OSL | 2.190 | 0.080 | normal | normal | 2001 | English et al. (2001) | |||
| TAEAC_Lake_Lewis | -22.920000 | 132.530000 | lake | 95012 | OSL | 4.980 | 0.200 | normal | normal | 2001 | English et al. (2001) | |||
| TAEAC_Lake_Lewis | -22.920000 | 132.530000 | lake | 95016A | OSL | 7.680 | 0.220 | normal | normal | 2001 | English et al. (2001) | |||
| TAEAC_Lake_Lewis | -22.920000 | 132.530000 | lake | 95018A | OSL | 8.160 | 0.320 | normal | normal | 2001 | English et al. (2001) | |||
| TAEAC_Lake_Lewis | -22.920000 | 132.530000 | lake | 95018B | OSL | 11.170 | 0.480 | normal | normal | 2001 | English et al. (2001) | |||
| TAEAC_Lake_Lewis | -22.920000 | 132.530000 | lake | 95016B | OSL | 14.800 | 0.560 | normal | normal | 2001 | English et al. (2001) | |||
| TAEAC_Lake_Lewis | -22.920000 | 132.530000 | lake | 95016C | OSL | 18.120 | 0.810 | normal | normal | 2001 | English et al. (2001) | |||
| TAEAC_Lake_Lewis | -22.920000 | 132.530000 | lake | 95016D | OSL | 18.650 | 0.860 | normal | normal | 2001 | English et al. (2001) | |||
| TAEAC_Lake_Woods | -17.850000 | 133.500000 | lake | adLD95003 | OSL | 26.800 | 3.500 | normal | normal | 1998 | Bowler et al. (1998) | |||
| TAEAC_Lake_Woods | -17.850000 | 133.500000 | lake | adLD95006 | OSL | 28.900 | 0.550 | normal | normal | 1998 | Bowler et al. (1998) | |||
| TAEAC_Lake_Woods | -17.850000 | 133.500000 | lake | adLD95004 | OSL | 53.000 | 5.000 | normal | normal | 1998 | Bowler et al. (1998) | |||
| TAEAC_Lake_Woods | -17.850000 | 133.500000 | lake | adLD95007 | OSL | 61.000 | 0.800 | normal | normal | 1998 | Bowler et al. (1998) | |||
| TAEAC_Lake_Woods | -17.850000 | 133.500000 | lake | adLD95008 | OSL | 96.000 | 10.000 | normal | normal | 1998 | Bowler et al. (1998) | |||
| TAEAC_Lake_Woods | -17.850000 | 133.500000 | lake | adLD95005 | OSL | 180.000 | 20.000 | normal | normal | 1998 | Bowler et al. (1998) | |||
| TAEAC_LG99 | -20.130000 | 127.410000 | fluvial | OS26200 | radiocarbon | 12.170 | 0.170 | shcal98 | shcal20 | 2001 | Wyrwoll and Miller (2001) | |||
| TAEAC_LG99 | -20.130000 | 127.410000 | fluvial | OS24884 | radiocarbon | 13.020 | 0.065 | shcal98 | shcal20 | 2001 | Wyrwoll and Miller (2001) | |||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | U087 | lead-210 | 0.1000 | -0.018 | 0.014 | normal | normal | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | U088 | lead-210 | 0.1500 | 0.004 | 0.021 | normal | normal | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | U089 | lead-210 | 0.2000 | 0.026 | 0.028 | normal | normal | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | OZW494 | radiocarbon | 0.4400 | 1.105 | 0.030 | shcal20 | shcal20 | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | OZW495 | radiocarbon | 0.7200 | 1.360 | 0.035 | shcal20 | shcal20 | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | OZW496 | radiocarbon | 1.4400 | 2.055 | 0.035 | shcal20 | shcal20 | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | OZW497 | radiocarbon | 1.8400 | 2.555 | 0.040 | shcal20 | shcal20 | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | OZW498 | radiocarbon | 2.4400 | 3.535 | 0.035 | shcal20 | shcal20 | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MAR2 | -13.409000 | 135.774000 | lake | OZW499 | radiocarbon | 2.8400 | 4.155 | 0.050 | shcal20 | shcal20 | 2021 | Rehn et al. (2021b) | ||
| TAEAC_MARR01 | -17.070000 | 139.490000 | lake | OZR376 | radiocarbon | 0.5000 | 0.465 | 0.035 | intcal13 | shcal20 | 2015 | Moss et al. (2015) | ||
| TAEAC_MARR02 | -17.070000 | 139.490000 | lake | OZO075 | radiocarbon | 0.3900 | 0.000 | 0.050 | postbomb_SH3 | postbomb_SH3 | 2015 | Moss et al. (2015) | ||
| TAEAC_MARR02 | -17.070000 | 139.490000 | lake | Wk-38216 | radiocarbon | 0.4600 | 0.000 | 0.050 | postbomb_SH3 | postbomb_SH3 | 2015 | Moss et al. (2015) | ||
| TAEAC_MARR02 | -17.070000 | 139.490000 | lake | Wk-38884 | radiocarbon | 0.5800 | 0.364 | 0.026 | intcal13 | shcal20 | 2015 | Moss et al. (2015) | ||
| TAEAC_MARR02 | -17.070000 | 139.490000 | lake | Wk-38885 | radiocarbon | 0.7500 | 2.611 | 0.025 | marine13 | marine20 | 2015 | Moss et al. (2015) | ||
| TAEAC_MARR03 | -17.070000 | 139.490000 | lake | OZR374 | radiocarbon | 0.5000 | 0.650 | 0.030 | intcal13 | shcal20 | 2015 | Moss et al. (2015) | ||
| TAEAC_MARR04 | -17.070000 | 139.490000 | lake | P486 | lead-210 | 0.0050 | -0.066 | 0.001 | normal | normal | 2017 | Mackenzie et al. (2017) | ||
| TAEAC_MARR04 | -17.070000 | 139.490000 | lake | P487 | lead-210 | 0.0250 | -0.061 | 0.002 | normal | normal | 2017 | Mackenzie et al. (2017) | ||
| TAEAC_MARR04 | -17.070000 | 139.490000 | lake | P488 | lead-210 | 0.0550 | -0.052 | 0.003 | normal | normal | 2017 | Mackenzie et al. (2017) | ||
| TAEAC_MARR04 | -17.070000 | 139.490000 | lake | P489 | lead-210 | 0.1050 | -0.032 | 0.005 | normal | normal | 2017 | Mackenzie et al. (2017) | ||
| TAEAC_MARR04 | -17.070000 | 139.490000 | lake | P490 | lead-210 | 0.1550 | -0.022 | 0.007 | normal | normal | 2017 | Mackenzie et al. (2017) | ||
| TAEAC_MARR04 | -17.070000 | 139.490000 | lake | P491 | lead-210 | 0.2050 | -0.008 | 0.009 | normal | normal | 2017 | Mackenzie et al. (2017) | ||
| TAEAC_MARR04 | -17.070000 | 139.490000 | lake | OZS567 | radiocarbon | 0.3550 | 0.570 | 0.020 | shcal13 | shcal20 | 2017 | Mackenzie et al. (2017) | ||
| TAEAC_MARR04 | -17.070000 | 139.490000 | lake | OZR035 | radiocarbon | 0.4650 | 1.240 | 0.030 | shcal13 | shcal20 | 2017 | Mackenzie et al. (2017) | ||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7144 | radiocarbon | 0.000 | 0.001 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7745 | radiocarbon | 0.000 | 0.001 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7151 | radiocarbon | 0.390 | 0.340 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-6652 | radiocarbon | 0.600 | 0.270 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7153 | radiocarbon | 0.890 | 0.210 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7139 | radiocarbon | 1.000 | 0.120 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7143 | radiocarbon | 1.190 | 0.120 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7145 | radiocarbon | 1.210 | 0.110 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7156 | radiocarbon | 1.310 | 0.320 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7146 | radiocarbon | 1.440 | 0.180 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7140 | radiocarbon | 1.520 | 0.070 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | OZA-376 | radiocarbon | 1.910 | 0.100 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7147 | radiocarbon | 1.920 | 0.190 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-6651 | radiocarbon | 1.960 | 0.200 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7150 | radiocarbon | 2.360 | 0.200 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-8195 | radiocarbon | 2.640 | 0.060 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7724 | radiocarbon | 3.210 | 0.170 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-6658 | radiocarbon | 3.280 | 0.340 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | Beta-55847 | radiocarbon | 3.340 | 0.070 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | Beta-55846 | radiocarbon | 3.390 | 0.100 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | Beta-55845 | radiocarbon | 3.640 | 0.070 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-6657 | radiocarbon | 3.690 | 0.190 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7161 | radiocarbon | 3.820 | 0.450 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7149 | radiocarbon | 3.920 | 0.270 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | OZA-373 | radiocarbon | 4.070 | 0.120 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7744 | radiocarbon | 4.150 | 0.400 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-8191 | radiocarbon | 4.190 | 0.080 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7727 | radiocarbon | 4.300 | 0.320 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7141 | radiocarbon | 4.450 | 0.130 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7725 | radiocarbon | 4.690 | 0.210 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7165 | radiocarbon | 4.740 | 0.140 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7728 | radiocarbon | 4.860 | 0.290 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7746 | radiocarbon | 4.860 | 0.090 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | OZA-374 | radiocarbon | 4.950 | 0.130 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-8193 | radiocarbon | 4.990 | 0.080 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7159 | radiocarbon | 5.070 | 0.260 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-6656 | radiocarbon | 5.170 | 0.200 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-8192 | radiocarbon | 5.190 | 0.080 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-6653 | radiocarbon | 5.330 | 0.210 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7735 | radiocarbon | 5.350 | 0.210 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-8194 | radiocarbon | 5.350 | 0.200 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7740 | radiocarbon | 5.380 | 0.150 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7162 | radiocarbon | 5.430 | 0.340 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7736 | radiocarbon | 5.470 | 0.240 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7737 | radiocarbon | 5.480 | 0.180 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-6654 | radiocarbon | 5.500 | 0.260 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7741 | radiocarbon | 5.500 | 0.210 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7730 | radiocarbon | 5.600 | 0.210 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | OZA-375 | radiocarbon | 5.690 | 0.140 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7738 | radiocarbon | 5.780 | 0.140 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7731 | radiocarbon | 5.850 | 0.170 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7726 | radiocarbon | 5.960 | 0.190 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7164 | radiocarbon | 6.130 | 0.190 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7733 | radiocarbon | 6.240 | 0.170 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7729 | radiocarbon | 6.280 | 0.270 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7742 | radiocarbon | 6.490 | 0.200 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-6655 | radiocarbon | 6.650 | 0.430 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7158 | radiocarbon | 6.770 | 0.240 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7739 | radiocarbon | 6.790 | 0.400 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7743 | radiocarbon | 7.030 | 0.160 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7732 | radiocarbon | 7.030 | 0.220 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7155 | radiocarbon | 7.080 | 0.140 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| TAEAC_Mary_River | -12.480000 | 131.680000 | fluvial | ANU-7734 | radiocarbon | 7.290 | 0.160 | normal | shcal20 | 1998 | Mulrennan and Woodroffe (1998) | |||
| MD97-2128 | -12.313167 | 139.978833 | marine_core | OZG-374 | radiocarbon | 0.6000 | 10.260 | 0.080 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2128 | -12.313167 | 139.978833 | marine_core | OZG-373 | radiocarbon | 0.7000 | 14.960 | 0.090 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2128 | -12.313167 | 139.978833 | marine_core | OZG-375 | radiocarbon | 0.7500 | 14.280 | 0.090 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2129 | -10.789333 | 138.720000 | marine_core | OZF283 | radiocarbon | 0.0500 | 0.820 | 0.045 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2129 | -10.789333 | 138.720000 | marine_core | OZE259 | radiocarbon | 0.2000 | 9.810 | 0.090 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2129 | -10.789333 | 138.720000 | marine_core | OZI053 | radiocarbon | 3.2500 | 40.600 | 2.000 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZF284 | radiocarbon | 0.0000 | 8.270 | 0.060 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZG230 | radiocarbon | 0.0500 | 1.655 | 0.050 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZG381 | radiocarbon | 0.3000 | 4.860 | 0.050 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZG285 | radiocarbon | 0.6000 | 9.330 | 0.070 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZE255 | radiocarbon | 0.6500 | 4.310 | 0.060 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZE250 | radiocarbon | 0.7000 | 10.410 | 0.080 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZG-231 | radiocarbon | 0.8000 | 10.430 | 0.080 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZG-382 | radiocarbon | 0.9000 | 10.680 | 0.070 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2130 | -12.266833 | 138.748667 | marine_core | OZG386 | radiocarbon | 1.5000 | 11.880 | 0.170 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZE262 | radiocarbon | 0.0000 | 6.840 | 0.050 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZE262U2 | radiocarbon | 0.0000 | 7.790 | 0.060 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZG220 | radiocarbon | 0.0500 | 3.770 | 0.040 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZF287 | radiocarbon | 0.1000 | 10.020 | 0.060 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZG383 | radiocarbon | 0.3000 | 2.290 | 0.045 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZG221 | radiocarbon | 0.5500 | 1.930 | 0.040 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZE256 | radiocarbon | 0.5500 | 6.910 | 0.080 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZG377 | radiocarbon | 0.6000 | 0.735 | 0.035 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZE251 | radiocarbon | 0.6500 | 10.350 | 0.100 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZG-222 | radiocarbon | 0.7500 | 10.320 | 0.060 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZI-054 | radiocarbon | 1.4000 | 10.990 | 0.110 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZG232 | radiocarbon | 1.8000 | 3.810 | 0.100 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZG233 | radiocarbon | 3.2000 | 46.100 | 2.000 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2131 | -12.066000 | 138.749667 | marine_core | OZG234 | radiocarbon | 3.3000 | 45.800 | 1.700 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZF-290 | radiocarbon | 0.0035 | 10.380 | 0.070 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZF-291 | radiocarbon | 0.4000 | 11.440 | 0.080 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZF-292 | radiocarbon | 0.7000 | 12.390 | 0.080 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZG-378 | radiocarbon | 0.7500 | 14.390 | 0.080 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZG-385 | radiocarbon | 1.0000 | 14.907 | 0.130 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZG-386 | radiocarbon | 1.2000 | 14.330 | 0.090 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZG-388 | radiocarbon | 1.4500 | 14.330 | 0.100 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZF-293 | radiocarbon | 1.5000 | 15.390 | 0.110 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OZI-055 | radiocarbon | 2.3400 | 18.320 | 0.170 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | AARMD32a | AAR | 12.5000 | 122.000 | 18.000 | 0.0000 | normal | normal | 2008 | Reeves et al. (2008) | |
| MD97-2132 | -12.313167 | 139.978833 | marine_core | AARMD32b | AAR | 13.0000 | 108.000 | 16.000 | 0.0000 | normal | normal | 2008 | Reeves et al. (2008) | |
| MD97-2132 | -12.313167 | 139.978833 | marine_core | TLMD32b | TL | 15.0000 | 123.000 | 16.000 | normal | normal | 2008 | Reeves et al. (2008) | ||
| MD97-2132 | -12.313167 | 139.978833 | marine_core | OSLMD32 | OSL | 15.0000 | 125.000 | 15.000 | normal | normal | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZF294 | radiocarbon | 0.0000 | 2.010 | 0.080 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZG236 | radiocarbon | 0.0000 | 2.575 | 0.045 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZF294 | radiocarbon | 0.0050 | 2.010 | 0.080 | 0.0520 | marine04 | marine20 | 2008 | Reeves et al. (2008) | |
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZG236 | radiocarbon | 0.0050 | 2.575 | 0.045 | 0.0520 | marine04 | marine20 | 2008 | Reeves et al. (2008) | |
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZG237 | radiocarbon | 0.1000 | 1.310 | 0.040 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZG237 | radiocarbon | 0.1050 | 1.310 | 0.040 | normal | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZE258 | radiocarbon | 0.2000 | 0.470 | 0.050 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZF295 | radiocarbon | 0.2000 | 0.700 | 0.030 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZE258 | radiocarbon | 0.2050 | 0.470 | 0.050 | 0.0520 | marine04 | shcal20 | 2008 | Reeves et al. (2008) | |
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZF295 | radiocarbon | 0.2050 | 0.700 | 0.030 | normal | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZG389 | radiocarbon | 0.3000 | 0.820 | 0.050 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZG389 | radiocarbon | 0.3050 | 0.820 | 0.050 | normal | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZE253 | radiocarbon | 0.7700 | 14.550 | 0.100 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZE252 | radiocarbon | 0.7700 | 15.760 | 0.090 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZE253 | radiocarbon | 0.7750 | 14.550 | 0.100 | intcal04 | shcal20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZE252 | radiocarbon | 0.7750 | 15.760 | 0.090 | intcal04 | shcal20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZI057 | radiocarbon | 2.0000 | 39.840 | 0.980 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZI058 | radiocarbon | 2.0050 | 39.840 | 0.980 | normal | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZG224 | radiocarbon | 2.1000 | 40.000 | 0.600 | marine04 | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | OZG224 | radiocarbon | 2.1050 | 40.000 | 0.600 | normal | marine20 | 2008 | Reeves et al. (2008) | ||
| MD97-2133 | -12.390000 | 140.340000 | marine_core | TLMD32a | TL | 5.5000 | 64.300 | 7.000 | normal | normal | 2008 | Reeves et al. (2008) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 0.0100 | 1.515 | 0.030 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 0.1500 | 2.130 | 0.040 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 0.3500 | 2.780 | 0.040 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 0.5300 | 3.465 | 0.035 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 0.7300 | 4.295 | 0.030 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 1.0500 | 5.405 | 0.035 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 1.2100 | 6.190 | 0.035 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 1.5000 | 7.485 | 0.045 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 1.6800 | 8.575 | 0.040 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.0200 | 9.660 | 0.045 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.2800 | 10.370 | 0.050 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.4600 | 9.690 | 0.045 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.4900 | 10.905 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.5200 | 11.415 | 0.050 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.5500 | 10.995 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.5800 | 11.375 | 0.050 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.6200 | 11.670 | 0.050 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.6400 | 12.260 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.6700 | 12.260 | 0.070 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.6900 | 12.150 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.7300 | 12.080 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.7600 | 12.705 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.8000 | 12.430 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.8500 | 12.660 | 0.058 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.8800 | 12.610 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.9200 | 13.020 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.9600 | 12.580 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 2.9800 | 13.270 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.0100 | 13.470 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.0500 | 13.580 | 0.065 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.0700 | 13.640 | 0.070 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.1100 | 13.725 | 0.065 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.1500 | 13.940 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.1700 | 14.260 | 0.070 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.2100 | 14.500 | 0.070 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.3100 | 14.930 | 0.085 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.3500 | 15.160 | 0.070 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.3900 | 15.230 | 0.075 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.3900 | 15.410 | 0.070 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.4500 | 15.310 | 0.070 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.5100 | 15.390 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.5600 | 15.625 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.5900 | 15.480 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.6200 | 16.210 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.6400 | 16.310 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.6500 | 16.340 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.6700 | 16.530 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.6900 | 16.500 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.7300 | 16.790 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.7900 | 16.950 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.8300 | 17.470 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.8700 | 17.370 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.8900 | 17.410 | 0.095 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.9100 | 17.440 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.9500 | 17.740 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 3.9800 | 17.830 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.0100 | 16.880 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.0300 | 17.890 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.0500 | 17.725 | 0.100 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.0600 | 18.340 | 0.140 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.0700 | 18.410 | 0.110 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.0900 | 18.440 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.1300 | 18.490 | 0.100 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.1500 | 17.820 | 0.100 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.1800 | 18.670 | 0.110 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.2100 | 18.890 | 0.120 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.2500 | 18.990 | 0.100 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.3000 | 19.050 | 0.100 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.3300 | 18.790 | 0.110 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.3500 | 18.220 | 0.110 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.3700 | 19.260 | 0.110 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.3900 | 19.060 | 0.100 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.4100 | 19.960 | 0.110 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 4.4600 | 20.280 | 0.120 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| MD01-2378 | -13.080000 | 121.790000 | marine_core | radiocarbon | 5.9200 | 29.920 | 0.330 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| TAEAC_Mulan | -20.130000 | 127.410000 | fluvial | ANU11098 | radiocarbon | 0.000 | 0.060 | postbomb_SH3 | postbomb_SH3 | 2001 | Wyrwoll and Miller (2001) | |||
| TAEAC_OD | -15.800000 | 128.800000 | aeolian | W1595 | TL | 3.4000 | 0.500 | 0.100 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_OD | -15.800000 | 128.800000 | aeolian | W1596 | TL | 6.3000 | 5.900 | 1.000 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_OD | -15.800000 | 128.800000 | aeolian | W1597 | TL | 8.3000 | 21.700 | 2.900 | normal | normal | 1997 | Wende et al. (1997) | ||
| TAEAC_Pandanus_Yard | -17.690000 | 139.930000 | coastal | ANU378 | radiocarbon | 5.400 | normal | normal | 1982 | Rhodes (1982) | ||||
| TAEAC_Parnkupirti | -20.250000 | 127.500000 | aeolian | K1534 | OSL | 5.600 | 0.300 | normal | normal | 2012 | Fitzsimmons et al. (2012) | |||
| TAEAC_Parnkupirti | -20.250000 | 127.500000 | aeolian | K1532 | OSL | 11.400 | 1.300 | normal | normal | 2012 | Fitzsimmons et al. (2012) | |||
| TAEAC_Parnkupirti | -20.250000 | 127.500000 | aeolian | K1531 | OSL | 20.100 | 1.400 | normal | normal | 2012 | Fitzsimmons et al. (2012) | |||
| TAEAC_Parnkupirti | -20.250000 | 127.500000 | aeolian | K1533 | OSL | 91.500 | 4.300 | normal | normal | 2012 | Fitzsimmons et al. (2012) | |||
| TAEAC_PL04_05 | -15.540000 | 128.250000 | fluvial | ANU-35837 | radiocarbon | 0.1500 | 0.630 | 0.030 | shcal13 | shcal20 | 2016 | Proske (2016) | ||
| TAEAC_PL04_05 | -15.540000 | 128.250000 | fluvial | ANU-31712 | radiocarbon | 0.4700 | 3.210 | 0.070 | shcal13 | shcal20 | 2016 | Proske (2016) | ||
| TAEAC_PL04_05 | -15.540000 | 128.250000 | fluvial | ANU-35528 | radiocarbon | 2.1200 | 6.640 | 0.040 | shcal13 | shcal20 | 2016 | Proske (2016) | ||
| TAEAC_PL04_05 | -15.540000 | 128.250000 | fluvial | ANU-33416 | radiocarbon | 2.6100 | 6.565 | 0.055 | shcal13 | shcal20 | 2016 | Proske (2016) | ||
| TAEAC_PL04_05 | -15.540000 | 128.250000 | fluvial | ANU-35529 | radiocarbon | 3.4600 | 6.765 | 0.035 | shcal13 | shcal20 | 2016 | Proske (2016) | ||
| TAEAC_SAN1a | -11.120000 | 142.350000 | lake | OZX213 | radiocarbon | 0.0500 | 5.880 | 0.035 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_SAN1a | -11.120000 | 142.350000 | lake | OZX214 | radiocarbon | 0.0700 | 6.535 | 0.050 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_SAN1a | -11.120000 | 142.350000 | lake | OZW500 | radiocarbon | 0.1000 | 7.230 | 0.070 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_SAN1a | -11.120000 | 142.350000 | lake | OZW502 | radiocarbon | 0.2200 | 7.200 | 0.030 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_SAN1a | -11.120000 | 142.350000 | lake | OZW503 | radiocarbon | 0.5000 | 7.795 | 0.030 | shcal20 | shcal20 | 2021 | Rehn et al. (2021a) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY416 | radiocarbon | 0.0300 | 2.690 | 0.070 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY423 | radiocarbon | 0.0300 | 10.200 | 0.140 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX672 | radiocarbon | 0.0600 | 3.840 | 0.045 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX765U1 | radiocarbon | 0.0600 | 4.120 | 0.100 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX765 | radiocarbon | 0.0600 | 4.165 | 0.035 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX765U2 | radiocarbon | 0.0600 | 4.180 | 0.140 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY131 | radiocarbon | 0.0600 | 4.450 | 0.030 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY417 | radiocarbon | 0.1250 | 4.180 | 0.070 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY418 | radiocarbon | 0.2300 | 7.040 | 0.080 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY333 | radiocarbon | 0.3200 | 6.435 | 0.030 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY419 | radiocarbon | 0.4200 | 5.990 | 0.080 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX766 | radiocarbon | 0.4300 | 7.750 | 0.035 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX673 | radiocarbon | 0.4300 | 8.660 | 0.040 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX767 | radiocarbon | 0.6700 | 9.900 | 0.050 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX674 | radiocarbon | 0.6700 | 15.240 | 0.060 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY420 | radiocarbon | 0.7600 | 17.360 | 0.160 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY758 | radiocarbon | 0.8200 | 10.590 | 0.100 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY421 | radiocarbon | 0.9000 | 19.450 | 0.080 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY422 | radiocarbon | 1.0500 | 17.960 | 0.160 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | Wk50327 | radiocarbon | 1.1400 | 23.549 | 0.126 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX768 | radiocarbon | 1.3700 | 15.560 | 0.090 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX675 | radiocarbon | 1.3700 | 24.340 | 0.190 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZY132 | radiocarbon | 1.4600 | 11.920 | 0.040 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX769 | radiocarbon | 1.4600 | 16.270 | 0.070 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX676 | radiocarbon | 1.4600 | 26.290 | 0.260 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | Wk50328 | radiocarbon | 1.5000 | 25.931 | 0.167 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_SAN1b | -11.120000 | 142.360000 | lake | OZX677 | radiocarbon | 1.6200 | 27.100 | 0.140 | intcal13 | intcal20 | 2022 | Rivera-Araya et al. (2022) | ||
| TAEAC_Shelburne_Bay | -11.920000 | 142.910000 | aeolian | Au-06 | TL | 23.800 | 2.400 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Shelburne_Bay | -11.920000 | 142.910000 | aeolian | ALPHA-2597 | TL | 23.800 | 2.400 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Shelburne_Bay | -11.920000 | 142.910000 | aeolian | Au-07 | TL | 28.400 | 1.300 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_Shelburne_Bay | -11.920000 | 142.910000 | aeolian | ANU-4890 | radiocarbon | 29.740 | 3.030 | normal | shcal20 | 1990 | Lees et al. (1990) | |||
| TAEAC_Shelburne_Bay | -11.920000 | 142.910000 | aeolian | Au-09 | TL | 29.900 | 2.400 | normal | normal | 1990 | Lees et al. (1990) | |||
| TAEAC_SkullSprings | -15.210000 | 125.728000 | lake | OZAX77 | radiocarbon | 0.1450 | 0.000 | 0.075 | postbomb_SH3 | postbomb_SH3 | 2025 | Rudd et al. (2025) | ||
| TAEAC_SkullSprings | -15.210000 | 125.728000 | lake | OZAX78 | radiocarbon | 0.2950 | 0.000 | 0.075 | postbomb_SH3 | postbomb_SH3 | 2025 | Rudd et al. (2025) | ||
| TAEAC_SkullSprings | -15.210000 | 125.728000 | lake | OZAX79 | radiocarbon | 0.4450 | 2.160 | 0.025 | shcal20 | shcal20 | 2025 | Rudd et al. (2025) | ||
| TAEAC_SkullSprings | -15.210000 | 125.728000 | lake | OZAX80 | radiocarbon | 0.5950 | 2.505 | 0.025 | shcal20 | shcal20 | 2025 | Rudd et al. (2025) | ||
| TAEAC_SkullSprings | -15.210000 | 125.728000 | lake | Wk54533 | radiocarbon | 0.7600 | 7.795 | 0.020 | shcal20 | shcal20 | 2025 | Rudd et al. (2025) | ||
| TAEAC_SkullSprings | -15.210000 | 125.728000 | lake | Wk53969 | radiocarbon | 0.7800 | 4.534 | 0.022 | shcal20 | shcal20 | 2025 | Rudd et al. (2025) | ||
| TAEAC_SkullSprings | -15.210000 | 125.728000 | lake | OZAX81 | radiocarbon | 0.8650 | 16.055 | 0.040 | shcal20 | shcal20 | 2025 | Rudd et al. (2025) | ||
| GIK18479-4 | -12.450000 | 121.370000 | marine_core | radiocarbon | 0.1900 | 1.255 | 0.030 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18479-4 | -12.450000 | 121.370000 | marine_core | radiocarbon | 1.1900 | 7.480 | 0.045 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18479-4 | -12.450000 | 121.370000 | marine_core | radiocarbon | 1.5900 | 10.365 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18479-4 | -12.450000 | 121.370000 | marine_core | radiocarbon | 1.9900 | 12.570 | 0.070 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18479-4 | -12.450000 | 121.370000 | marine_core | radiocarbon | 2.3900 | 14.240 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18479-4 | -12.450000 | 121.370000 | marine_core | radiocarbon | 2.7000 | 15.590 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.0100 | 1.950 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.0400 | 2.920 | 0.025 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.1200 | 4.370 | 0.030 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.1800 | 4.830 | 0.030 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.2400 | 6.215 | 0.030 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.2800 | 7.015 | 0.035 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.3300 | 8.380 | 0.045 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.3800 | 9.640 | 0.045 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.4300 | 10.575 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.4600 | 11.005 | 0.045 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.4800 | 11.245 | 0.050 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.5000 | 11.580 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.5300 | 11.425 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.5800 | 12.225 | 0.060 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.6000 | 12.530 | 0.055 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.6200 | 13.310 | 0.110 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.6800 | 14.660 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.7200 | 15.100 | 0.080 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.7800 | 15.720 | 0.090 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.8200 | 17.100 | 0.100 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.8600 | 17.540 | 0.120 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.9200 | 17.760 | 0.100 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 0.9800 | 19.390 | 0.120 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| GIK18506-2 | -8.790000 | 128.640000 | marine_core | radiocarbon | 1.0600 | 20.930 | 0.130 | 0.4000 | marine04 | marine20 | 2015 | Kuhnt et al. (2015) | ||
| TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | lake | Wk39261 | radiocarbon | 0.1180 | 0.100 | 0.000 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | lake | Wk39263 | radiocarbon | 0.1180 | 0.506 | 0.025 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | lake | OZS777 | radiocarbon | 0.1820 | 2.035 | 0.025 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | lake | Wk39262 | radiocarbon | 0.2460 | 4.350 | 0.025 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | lake | Wk39264 | radiocarbon | 0.2460 | 7.437 | 0.035 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | lake | OZS778 | radiocarbon | 0.3080 | 7.125 | 0.050 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | lake | OZS780 | radiocarbon | 0.3980 | 8.110 | 0.050 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_b | -13.178000 | 130.746000 | lake | Wk39265 | radiocarbon | 0.5450 | 9.778 | 0.051 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_b | -13.178000 | 130.746000 | lake | TS425-750 | OSL | 0.7500 | 24.610 | 2.020 | normal | normal | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_b | -13.178000 | 130.746000 | lake | Wk39266 | radiocarbon | 0.7750 | 9.244 | 0.043 | shcal13 | shcal20 | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_c | -13.178000 | 130.746000 | lake | TS425-950 | OSL | 0.9500 | 31.280 | 3.270 | normal | normal | 2018 | Marx et al. (2021) | ||
| TAEAC_TableTopSwamp_c | -13.178000 | 130.746000 | lake | TS425-1080 | OSL | 1.0800 | 32.170 | 3.070 | normal | normal | 2018 | Marx et al. (2021) | ||
| TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | lake | OZH347 | radiocarbon | 0.2900 | 3.110 | 0.050 | intcal98 | shcal20 | 2005 | Prebble et al. (2005) | ||
| TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | lake | OZH120 | radiocarbon | 0.4500 | 4.190 | 0.050 | intcal98 | shcal20 | 2005 | Prebble et al. (2005) | ||
| TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | lake | OZH121 | radiocarbon | 0.5500 | 5.760 | 0.050 | intcal98 | shcal20 | 2005 | Prebble et al. (2005) | ||
| TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | lake | OZH123 | radiocarbon | 0.6500 | 6.430 | 0.050 | intcal98 | shcal20 | 2005 | Prebble et al. (2005) | ||
| TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | lake | OZH348 | radiocarbon | 0.9000 | 8.450 | 0.080 | intcal98 | shcal20 | 2005 | Prebble et al. (2005) | ||
| TAEAC_WCC99_04 | -19.170000 | 127.800000 | lake | NSRL-13177 | radiocarbon | 0.7500 | 4.800 | 0.030 | shcal13 | shcal20 | 2018 | Miller et al. (2018) | ||
| TAEAC_WCC99_04 | -19.170000 | 127.800000 | lake | NSRL-11170 | radiocarbon | 0.7500 | 4.970 | 0.065 | shcal13 | shcal20 | 2018 | Miller et al. (2018) | ||
| TAEAC_WCC99_04 | -19.170000 | 127.800000 | lake | NSRL-13038 | radiocarbon | 3.6300 | 11.550 | 0.045 | shcal13 | shcal20 | 2018 | Miller et al. (2018) | ||
| TAEAC_WCC99_04 | -19.170000 | 127.800000 | lake | NSRL-11171 | radiocarbon | 3.6700 | 9.820 | 0.090 | shcal13 | shcal20 | 2018 | Miller et al. (2018) | ||
| TAEAC_WCS01 | -17.070000 | 139.490000 | lake | OZR-036 | lead-210 | 0.575 | 0.025 | shcal13 | shcal20 | 2017 | Mackenzie et al. (2017) | |||
| TAEAC_WS01 | -17.070000 | 139.490000 | lake | OZR-037 | lead-210 | 0.420 | 0.025 | shcal13 | shcal20 | 2017 | Mackenzie et al. (2017) | |||
| TAEAC_Yuenbi | -20.130000 | 127.410000 | fluvial | AA33399 | radiocarbon | 11.145 | 0.075 | shcal98 | shcal20 | 2001 | Wyrwoll and Miller (2001) |
