Wall, Alexander Forster: Hydrological interpretations from tropical Australian environmental archives [dataset]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.989983 (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 table of interpreted hydrological periods and climate signals for each archive. This includes earliest/latest age anchors, their calibrated equivalents, resolution metrics, and qualitative hydrological classifications.
Source:
Allen, K J; Freund, M B; Palmer, J G; Simkin, R; Williams, L; Brookhouse, M; Cook, E R; Stewart, S; Baker, P J (2020): Hydroclimate extremes in a north Australian drought reconstruction asymmetrically linked with Central Pacific Sea surface temperatures. Global and Planetary Change, 195, 103329, https://doi.org/10.1016/j.gloplacha.2020.103329
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Bowler, James M; Wyrwoll, Karl-Heinz; Yanchou, Lu (2001): Variations of the northwest Australian summer monsoon over the last 300,000 years: the paleohydrological record of the Gregory (Mulan) Lakes System. Quaternary International, 83-85, 63-80, https://doi.org/10.1016/S1040-6182(01)00031-3
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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
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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
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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
Nanson, Gerald C; Price, David M; Short, Stephen A; Young, Robert W; Jones, Brian G (1991): Comparative Uranium-Thorium and Thermoluminescence Dating of Weathered Quaternary Alluvium in the Tropics of Northern Australia. Quaternary Research, 35(3-Part1), 347-366, https://doi.org/10.1016/0033-5894(91)90050-F
Nott, Jonathan; Price, David (1999): Waterfalls, floods and climate change: evidence from tropical Australia. Earth and Planetary Science Letters, 171(2), 267-276, https://doi.org/10.1016/S0012-821X(99)00152-1
Nott, Jonathan F; Price, David M; Bryant, Edward A (1996): A 30,000 year record of extreme floods in tropical Australia from relict plunge‐pool deposits: Implications for future climate change. Geophysical Research Letters, 23(4), 379-382, https://doi.org/10.1029/96GL00262
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))
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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: -14.860040 * Median Longitude: 131.935567 * 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: -1875 m a.s.l. * Maximum ELEVATION: 330 m a.s.l.
Event(s):
Comment:
• Ages are left unmodelled here; age-modelled timelines must be generated via the public R scripts.
• Hydrological interpretations follow the criteria described in the associated manuscript.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Identification | ID | Wall, Alexander Forster | unique row label | ||
| 2 | Event label | Event | Wall, Alexander Forster | sample; archive/site identifier | ||
| 3 | LATITUDE | Latitude | Wall, Alexander Forster | Geocode | ||
| 4 | LONGITUDE | Longitude | Wall, Alexander Forster | Geocode | ||
| 5 | ELEVATION | Elevation | m a.s.l. | Wall, Alexander Forster | Geocode | |
| 6 | Location | Location | Wall, Alexander Forster | site name or locality string | ||
| 7 | Area/locality | Area | Wall, Alexander Forster | geographic region | ||
| 8 | Country | Country | Wall, Alexander Forster | |||
| 9 | Archive | Archive | Wall, Alexander Forster | archive type (lake, speleothem, marine core, etc.) | ||
| 10 | Age, minimum/young | Age min | ka | Wall, Alexander Forster | lower bound of interpreted interval (uncalibrated, if applicable) | |
| 11 | Age, minimum/young, error | Age min e | ± | Wall, Alexander Forster | reported uncertainty | |
| 12 | Age, maximum/old | Age max | ka | Wall, Alexander Forster | upper bound of interpreted interval | |
| 13 | Age, maximum/old, error | Age max e | ± | Wall, Alexander Forster | reported uncertainty | |
| 14 | Calendar age, minimum/young | Cal age min | ka BP | Wall, Alexander Forster | calibrated/translated earliest age | |
| 15 | Calendar age, maximum/old | Cal age max | ka BP | Wall, Alexander Forster | calibrated/translated latest age | |
| 16 | Time resolution | Time res | ka | Wall, Alexander Forster | archive temporal resolution (ka/sample) | |
| 17 | Number of proxies | Proxies | # | Wall, Alexander Forster | number of proxies analysed | |
| 18 | Interpretation | Interpretation | Wall, Alexander Forster | water availability categorical interpretation (-2 = very arid, -1 = arid, 1 = hydric, and 2 = very hydric) | ||
| 19 | Evidence | Evidence | Wall, Alexander Forster | supporting proxy evidence | ||
| 20 | Reference/source | Reference | Wall, Alexander Forster |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0) (License comes into effect after moratorium ends)
Size:
3418 data points
Data
| 1 ID | 2 Event | 3 Latitude | 4 Longitude | 5 Elevation [m a.s.l.] | 6 Location | 7 Area | 8 Country | 9 Archive | 10 Age min [ka] | 11 Age min e [±] | 12 Age max [ka] | 13 Age max e [±] | 14 Cal age min [ka BP] | 15 Cal age max [ka BP] | 16 Time res [ka] | 17 Proxies [#] | 18 Interpretation | 19 Evidence | 20 Reference |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 1 | TAEAC_Parnkupirti | -20.250000 | 127.500000 | Parnkupirti | Western Australia | Australia | aeolian | 91.500 | 1.700 | 50.000 | 1.000 | 91.500 | 50.000 | 21.000 | 1 | -2 | Formation of desert dunes postdating MIS 5 regression | Fitzsimmons et al. (2012) | |
| 1 | TAEAC_Parnkupirti | -20.250000 | 127.500000 | Parnkupirti | Western Australia | Australia | aeolian | 50.000 | 1.000 | 35.000 | 1.000 | 50.000 | 35.000 | 21.000 | 1 | -1 | Transitional phase coinciding with early MIS 3 | Fitzsimmons et al. (2012) | |
| 1 | TAEAC_Parnkupirti | -20.250000 | 127.500000 | Parnkupirti | Western Australia | Australia | aeolian | 35.000 | 1.000 | 11.500 | 0.500 | 35.000 | 11.500 | 21.000 | 1 | -1 | Renewed dune formation including the Last Glacial Maximum | Fitzsimmons et al. (2012) | |
| 1 | TAEAC_Parnkupirti | -20.250000 | 127.500000 | Parnkupirti | Western Australia | Australia | aeolian | 11.500 | 0.500 | 14.000 | 0.500 | 11.500 | 14.000 | 21.000 | 1 | 1 | Monsoon strengthening and subsequent environmental changes around 14 ka | Fitzsimmons et al. (2012) | |
| 1 | TAEAC_Parnkupirti | -20.250000 | 127.500000 | Parnkupirti | Western Australia | Australia | aeolian | 5.000 | 0.500 | 4.000 | 0.500 | 5.000 | 4.000 | 21.000 | 1 | -1 | Rapid mid-Holocene arid event | Fitzsimmons et al. (2012) | |
| 3 | TAEAC_CT | -15.800000 | 128.800000 | Wonnamarring | Kimberley | Australia | aeolian | 37.000 | 35.000 | 37.000 | 35.000 | 15.000 | 1 | 1 | Significant fluvial activity | Wende et al. (1997) | |||
| 3 | TAEAC_CT | -15.800000 | 128.800000 | Wonnamarring | Kimberley | Australia | aeolian | 35.000 | 22.000 | 35.000 | 22.000 | 15.000 | 1 | -1 | Limited fluvial activity | Wende et al. (1997) | |||
| 3 | TAEAC_CT | -15.800000 | 128.800000 | Wonnamarring | Kimberley | Australia | aeolian | 22.000 | 12.000 | 22.000 | 12.000 | 15.000 | 1 | -1 | Subdued fluvial activity | Wende et al. (1997) | |||
| 3 | TAEAC_CT | -15.800000 | 128.800000 | Wonnamarring | Kimberley | Australia | aeolian | 12.000 | 6.000 | 12.000 | 6.000 | 15.000 | 1 | 1 | Substantial overbank deposition | Wende et al. (1997) | |||
| 3 | TAEAC_CT | -15.800000 | 128.800000 | Wonnamarring | Kimberley | Australia | aeolian | 6.000 | 5.000 | 6.000 | 5.000 | 15.000 | 1 | -2 | Increased aeolian activity and reduced fluvial deposition | Wende et al. (1997) | |||
| 4 | TAEAC_Core89_1 | -13.810000 | 136.870000 | Groote_Eylandt | Gulf of Carpentaria | Australia | aeolian | 136.000 | 17.000 | 135.000 | 17.000 | 136.000 | 135.000 | 1.000 | 1 | -1 | Basal dune activity | Shulmeister and Lees (1992) | |
| 4 | TAEAC_Core89_1 | -13.810000 | 136.870000 | Groote_Eylandt | Gulf of Carpentaria | Australia | aeolian | 6.000 | 0.300 | 4.000 | 0.700 | 6.000 | 4.000 | 1.000 | 1 | 1 | Stabilization event | Shulmeister and Lees (1992) | |
| 4 | TAEAC_Core89_1 | -13.810000 | 136.870000 | Groote_Eylandt | Gulf of Carpentaria | Australia | aeolian | 4.000 | 0.700 | 2.800 | 4.000 | 2.800 | 1.000 | 1 | -1 | Post-stabilization period | Shulmeister and Lees (1992) | ||
| 4 | TAEAC_Core89_1 | -13.810000 | 136.870000 | Groote_Eylandt | Gulf of Carpentaria | Australia | aeolian | 2.800 | 1.500 | 2.800 | 1.500 | 1.000 | 1 | -1 | Active dune period | Shulmeister and Lees (1992) | |||
| 4 | TAEAC_Core89_1 | -13.810000 | 136.870000 | Groote_Eylandt | Gulf of Carpentaria | Australia | aeolian | 1.500 | 0.000 | 1.500 | 0.000 | 1.000 | 1 | -1 | Recent active dunes | Shulmeister and Lees (1992) | |||
| 17 | TAEAC_Karumba | -17.690000 | 140.420000 | Karumba | Gulf of Carpentaria | Australia | coastal | 5.600 | 0.000 | 5.600 | 0.000 | 0.500 | 1 | 1 | Fluctuating sediment supply related to rainfall | Rhodes et al. (1982) | |||
| 18 | TAEAC_Pandanus_Yard | -17.690000 | 139.930000 | Pandanus_Yard | Gulf of Carpentaria | Australia | coastal | 5.400 | 0.000 | 5.400 | 0.000 | 0.500 | 1 | -1 | Drying of high-tide flats and dune formation | Rhodes et al. (1982) | |||
| 21 | TAEAC_Gilbert_River | -17.320000 | 141.750000 | Gilbert_River | Gulf of Carpentaria | Australia | fluvial | 120.000 | 85.000 | 120.000 | 85.000 | 1.000 | 1 | 2 | Extensive sand body indicating major fluvial activity | Nanson et al. (1991) | |||
| 21 | TAEAC_Gilbert_River | -17.320000 | 141.750000 | Gilbert_River | Gulf of Carpentaria | Australia | fluvial | 85.000 | 50.000 | 85.000 | 50.000 | 1.000 | 1 | -1 | Mud and fine sandy mud deposition | Nanson et al. (1991) | |||
| 21 | TAEAC_Gilbert_River | -17.320000 | 141.750000 | Gilbert_River | Gulf of Carpentaria | Australia | fluvial | 50.000 | 40.000 | 50.000 | 40.000 | 1.000 | 1 | 1 | Sand deposition indicating increased fluvial activity | Nanson et al. (1991) | |||
| 21 | TAEAC_Gilbert_River | -17.320000 | 141.750000 | Gilbert_River | Gulf of Carpentaria | Australia | fluvial | 40.000 | 8.900 | 1.200 | 40.000 | 8.900 | 1.000 | 1 | -1 | Return to mud deposition | Nanson et al. (1991) | ||
| 21 | TAEAC_Gilbert_River | -17.320000 | 141.750000 | Gilbert_River | Gulf of Carpentaria | Australia | fluvial | 8.900 | 1.200 | 7.000 | 8.900 | 7.000 | 1.000 | 1 | 2 | Early Holocene fluvial phase, more active than present | Nanson et al. (1991) | ||
| 21 | TAEAC_Gilbert_River | -17.320000 | 141.750000 | Gilbert_River | Gulf of Carpentaria | Australia | fluvial | 7.000 | 0.000 | 7.000 | 0.000 | 1.000 | 1 | 1 | Ongoing mud and sandy mud deposition | Nanson et al. (1991) | |||
| 22 | TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | Fitzroy_Estuary | Western Australia | Australia | coastal | 8.400 | 7.400 | 8.400 | 7.400 | 0.500 | 1 | -1 | Desert dune formation | Jennings (1975) | |||
| 22 | TAEAC_Fitzroy_Estuary | -17.310000 | 123.570000 | Fitzroy_Estuary | Western Australia | Australia | coastal | 7.400 | 0.000 | 7.400 | 0.000 | 0.500 | 1 | 1 | Estuarine sedimentation | Jennings (1975) | |||
| 28 | TAEAC_King_River | -15.520000 | 128.120000 | King_River | Western Australia | Australia | fluvial | 9.200 | 8.700 | 9.200 | 8.700 | 0.500 | 1 | 1 | Peak in Proteaceae, indicative of high, non-seasonal rainfall | Proske et al. (2014) | |||
| 28 | TAEAC_King_River | -15.520000 | 128.120000 | King_River | Western Australia | Australia | fluvial | 8.700 | 7.400 | 8.700 | 7.400 | 0.500 | 1 | 1 | Increase in summer monsoon rainfall and mangrove biodiversity | Proske et al. (2014) | |||
| 28 | TAEAC_King_River | -15.520000 | 128.120000 | King_River | Western Australia | Australia | fluvial | 7.400 | 6.500 | 7.400 | 6.500 | 0.500 | 1 | -1 | Start of contraction in mangrove forest, indicating decreased moisture availability | Proske et al. (2014) | |||
| 28 | TAEAC_King_River | -15.520000 | 128.120000 | King_River | Western Australia | Australia | fluvial | 6.500 | 0.000 | 6.500 | 0.000 | 0.500 | 1 | -2 | Late Holocene aridification, expansion of hypersaline flats, and transition to intermittent wetlands | Proske et al. (2014) | |||
| 33 | TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | Cape_St._Lambert | East Kimberleys | Australia | aeolian | 3.000 | 3.000 | 3.000 | 3.000 | 0.500 | 1 | -1 | Late Holocene dune emplacement | Lees et al. (1992) | |||
| 33 | TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | Cape_St._Lambert | East Kimberleys | Australia | aeolian | 1.600 | 1.600 | 1.600 | 1.600 | 0.500 | 1 | -1 | Late Holocene dune emplacement | Lees et al. (1992) | |||
| 33 | TAEAC_Cap_St_Lambert | -14.310000 | 127.760000 | Cape_St._Lambert | East Kimberleys | Australia | aeolian | 1.000 | 0.000 | 1.000 | 0.000 | 0.500 | 1 | -1 | Late Holocene dune emplacement | Lees et al. (1992) | |||
| 37 | TAEAC_Mary_River | -12.480000 | 131.680000 | Mary_River | Northern Territory | Australia | fluvial | 7.000 | 6.000 | 7.000 | 6.000 | 0.500 | 1 | 1 | Transgressive phase and mangrove forest development | Mulrennan and Woodroffe (1998) | |||
| 37 | TAEAC_Mary_River | -12.480000 | 131.680000 | Mary_River | Northern Territory | Australia | fluvial | 6.000 | 4.000 | 6.000 | 4.000 | 0.500 | 1 | 1 | Big swamp phase with widespread mangrove forest development | Mulrennan and Woodroffe (1998) | |||
| 37 | TAEAC_Mary_River | -12.480000 | 131.680000 | Mary_River | Northern Territory | Australia | fluvial | 4.000 | 2.600 | 4.000 | 2.600 | 0.500 | 1 | -1 | Start of channel switching and palaeochannel infill | Mulrennan and Woodroffe (1998) | |||
| 37 | TAEAC_Mary_River | -12.480000 | 131.680000 | Mary_River | Northern Territory | Australia | fluvial | 2.600 | 1.300 | 2.600 | 1.300 | 0.500 | 1 | -1 | Continued palaeochannel infill and channel switching | Mulrennan and Woodroffe (1998) | |||
| 43 | TAEAC_Dune_W_Cape_York | -12.280000 | 141.720000 | Western_Cape_York | Gulf of Carpentaria | Australia | aeolian | 8.300 | 5.200 | 8.300 | 5.200 | 0.500 | 1 | -1 | Early and mid-Holocene dune transgression and stabilization | Lees et al. (1993) | |||
| 59 | TAEAC_PC | -13.610000 | 132.210000 | PC | northern Australia | Australia | dendro | 0.149 | 0.000 | 0.144 | 0.000 | 0.149 | 0.144 | 0.001 | 1 | 1 | High SPEI | Allen et al. (2020) | |
| 60 | TAEAC_HAY | -13.600000 | 131.530000 | HAY | northern Australia | Australia | dendro | 0.132 | 0.000 | 0.131 | 0.000 | 0.132 | 0.131 | 0.001 | 1 | 1 | High SPEI | Allen et al. (2020) | |
| 61 | TAEAC_LIT | -13.290000 | 130.850000 | LIT | northern Australia | Australia | dendro | 0.116 | 0.000 | 0.115 | 0.000 | 0.116 | 0.115 | 0.001 | 1 | 1 | High SPEI | Allen et al. (2020) | |
| 62 | TAEAC_KOR | -12.650000 | 134.320000 | KOR | northern Australia | Australia | dendro | 0.079 | 0.000 | 0.068 | 0.000 | 0.079 | 0.068 | 0.001 | 1 | 1 | High SPEI | Allen et al. (2020) | |
| 63 | TAEAC_MAN | -12.050000 | 134.250000 | MAN | northern Australia | Australia | dendro | 0.056 | 0.000 | 0.054 | 0.000 | 0.056 | 0.054 | 0.001 | 1 | 1 | High SPEI | Allen et al. (2020) | |
| 64 | TAEAC_TIWI | -11.710000 | 130.830000 | TIWI | northern Australia | Australia | dendro | 0.023 | 0.000 | 0.019 | 0.000 | 0.023 | 0.019 | 0.001 | 1 | 1 | High SPEI | Allen et al. (2020) | |
| 65 | TAEAC_MUR | -11.500000 | 132.700000 | MUR | northern Australia | Australia | dendro | 0.185 | 0.000 | 0.175 | 0.000 | 0.185 | 0.175 | 0.001 | 1 | -1 | Low SPEI | Allen et al. (2020) | |
| 59 | TAEAC_PC | -13.610000 | 132.210000 | PC | northern Australia | Australia | dendro | 0.143 | 0.000 | 0.138 | 0.000 | 0.143 | 0.138 | 0.001 | 1 | -1 | Low SPEI | Allen et al. (2020) | |
| 59 | TAEAC_PC | -13.610000 | 132.210000 | PC | northern Australia | Australia | dendro | 0.113 | 0.000 | 0.104 | 0.000 | 0.113 | 0.104 | 0.001 | 1 | -1 | Low SPEI | Allen et al. (2020) | |
| 59 | TAEAC_PC | -13.610000 | 132.210000 | PC | northern Australia | Australia | dendro | 0.008 | 0.000 | -0.002 | 0.000 | 0.008 | -0.002 | 0.001 | 1 | -1 | Low SPEI | Allen et al. (2020) | |
| 59 | TAEAC_PC | -13.610000 | 132.210000 | PC | northern Australia | Australia | dendro | -0.011 | 0.000 | -0.012 | 0.000 | -0.011 | -0.012 | 0.001 | 1 | -1 | Low SPEI | Allen et al. (2020) | |
| 59 | TAEAC_PC | -13.610000 | 132.210000 | PC | northern Australia | Australia | dendro | -0.052 | 0.000 | -0.053 | 0.000 | -0.052 | -0.053 | 0.001 | 1 | -1 | Low SPEI | Allen et al. (2020) | |
| 66 | TAEAC_Gilwah | -20.130000 | 127.410000 | Gregory_Lakes | Western Australia | fluvial | 14.000 | 0.380 | 11.000 | 0.420 | 14.000 | 11.000 | 1.000 | 3 | 1 | Monsoon initiation | Wyrwoll and Miller (2001) | ||
| 66 | TAEAC_Gilwah | -20.130000 | 127.410000 | Gregory_Lakes | Western Australia | fluvial | 11.000 | 0.420 | 5.000 | 0.150 | 11.000 | 5.000 | 1.000 | 3 | 2 | Persistent monsoon | Wyrwoll and Miller (2001) | ||
| 66 | TAEAC_Gilwah | -20.130000 | 127.410000 | Gregory_Lakes | Western Australia | fluvial | 5.000 | 0.150 | 0.000 | 0.065 | 5.000 | 0.000 | 1.000 | 3 | 1 | Diminished monsoon | Wyrwoll and Miller (2001) | ||
| 70 | TAEAC_PL04_05 | -15.540000 | 128.250000 | Parry_Lagoons | Australia | fluvial | 8.000 | 0.030 | 7.400 | 0.035 | 7.619 | 7.432 | 1.200 | 1 | 1 | Increased mangrove pollen | Proske (2016) | ||
| 70 | TAEAC_PL04_05 | -15.540000 | 128.250000 | Parry_Lagoons | Australia | fluvial | 7.400 | 0.040 | 6.300 | 0.055 | 7.432 | 6.477 | 1.200 | 1 | -1 | Reduced mangrove pollen, increase in hypersaline mudflat indicators | Proske (2016) | ||
| 70 | TAEAC_PL04_05 | -15.540000 | 128.250000 | Parry_Lagoons | Australia | fluvial | 6.300 | 0.060 | 1.300 | 0.110 | 6.477 | 1.301 | 1.200 | 1 | 1 | Reappearance and dominance of mangrove pollen | Proske (2016) | ||
| 70 | TAEAC_PL04_05 | -15.540000 | 128.250000 | Parry_Lagoons | Australia | fluvial | 1.300 | 0.010 | 0.000 | 0.060 | 1.301 | 0.002 | 1.200 | 1 | -1 | Decline in mangrove pollen and increase in grass and salt marsh pollen | Proske (2016) | ||
| 72 | TAEAC_Nott1999_01 | -14.320000 | 132.470000 | Lily_Ponds | Northern_Territory | Australia | fluvial | 6.900 | 0.600 | 5.900 | 0.600 | 6.900 | 5.900 | 7.500 | 1 | 1 | Extreme flood evidence | Nott and Price (1999) | |
| 72 | TAEAC_Nott1999_01 | -14.320000 | 132.470000 | Lily_Ponds | Northern_Territory | Australia | fluvial | 6.900 | 0.600 | 5.600 | 0.600 | 6.900 | 5.600 | 7.500 | 1 | 1 | Extreme flood evidence | Nott and Price (1999) | |
| 72 | TAEAC_Nott1999_01 | -14.320000 | 132.470000 | Lily_Ponds | Northern_Territory | Australia | fluvial | 17.500 | 1.900 | 16.500 | 1.900 | 17.500 | 16.500 | 7.500 | 1 | 1 | Extreme flood evidence | Nott and Price (1999) | |
| 72 | TAEAC_Nott1999_01 | -14.320000 | 132.470000 | Lily_Ponds | Northern_Territory | Australia | fluvial | 21.500 | 1.900 | 20.500 | 1.900 | 21.500 | 20.500 | 7.500 | 1 | 1 | Extreme flood evidence | Nott and Price (1999) | |
| 72 | TAEAC_Nott1999_01 | -14.320000 | 132.470000 | Lily_Ponds | Northern_Territory | Australia | fluvial | 28.900 | 2.600 | 27.900 | 2.600 | 28.900 | 27.900 | 7.500 | 1 | 1 | Extreme flood evidence | Nott and Price (1999) | |
| 72 | TAEAC_Nott1999_01 | -14.320000 | 132.470000 | Lily_Ponds | Northern_Territory | Australia | fluvial | 2.400 | 0.200 | 2.300 | 0.200 | 2.400 | 2.300 | 7.500 | 1 | 1 | Extreme flood evidence | Nott and Price (1999) | |
| 73 | TAEAC_Nott1996_01 | -13.150000 | 130.680000 | Wangi_Waterfall | Northern_Territory | Australia | fluvial | 30.000 | 20.000 | 30.000 | 20.000 | 2.000 | 1 | 1 | Extreme flood evidence | Nott et al. (1996) | |||
| 74 | TAEAC_Nott1996_02 | -13.420000 | 132.420000 | Wangi_Waterfall | Northern_Territory | Australia | fluvial | 11.000 | 4.000 | 11.000 | 4.000 | 1.300 | 1 | 1 | Extreme flood evidence | Nott et al. (1996) | |||
| 75 | TAEAC_E_Alligator_R | -12.560000 | 133.110000 | East_Alligator_River | Northern Territory | Australia | fluvial | 8.400 | 0.400 | 6.380 | 0.400 | 8.400 | 6.380 | 0.500 | 1 | 1 | flood deposits | Saynor et al. (2020) | |
| 75 | TAEAC_E_Alligator_R | -12.560000 | 133.110000 | East_Alligator_River | Northern Territory | Australia | fluvial | 3.100 | 0.200 | 2.910 | 0.350 | 3.100 | 2.910 | 0.500 | 1 | 1 | flood deposits | Saynor et al. (2020) | |
| 75 | TAEAC_E_Alligator_R | -12.560000 | 133.110000 | East_Alligator_River | Northern Territory | Australia | fluvial | 1.940 | 0.270 | 1.070 | 0.160 | 1.940 | 1.070 | 0.500 | 1 | 1 | flood deposits | Saynor et al. (2020) | |
| 75 | TAEAC_E_Alligator_R | -12.560000 | 133.110000 | East_Alligator_River | Northern Territory | Australia | fluvial | 0.590 | 0.110 | 0.340 | 0.030 | 0.590 | 0.340 | 0.500 | 1 | 1 | flood deposits | Saynor et al. (2020) | |
| 76 | TAEAC_Lake_Lewis | -22.920000 | 132.530000 | Lake_Lewis | Northern Territory | Australia | lake | 18.650 | 0.860 | 7.680 | 0.720 | 18.650 | 7.680 | 0.500 | 2 | 1 | Flood deposits overlying alluvial fan | English et al. (2001) | |
| 76 | TAEAC_Lake_Lewis | -22.920000 | 132.530000 | Lake_Lewis | Northern Territory | Australia | lake | 14.800 | 0.480 | 11.170 | 0.480 | 14.800 | 11.170 | 0.500 | 2 | -1 | Homogeneous dune deposits | English et al. (2001) | |
| 76 | TAEAC_Lake_Lewis | -22.920000 | 132.530000 | Lake_Lewis | Northern Territory | Australia | lake | 2.190 | 0.080 | 2.190 | 0.080 | 2.190 | 2.190 | 0.500 | 2 | 1 | OSL dating of fluvial deposits | English et al. (2001) | |
| 76 | TAEAC_Lake_Lewis | -22.920000 | 132.530000 | Lake_Lewis | Northern Territory | Australia | lake | 95.000 | 94.000 | 95.000 | 94.000 | 0.500 | 2 | -2 | OSL dating of dune indicating aeolian activity | English et al. (2001) | |||
| 76 | TAEAC_Lake_Lewis | -22.920000 | 132.530000 | Lake_Lewis | Northern Territory | Australia | lake | 4.980 | 0.200 | 4.980 | 0.200 | 4.980 | 4.980 | 0.500 | 2 | 1 | OSL dating indicating inundation of playa | English et al. (2001) | |
| 77 | TAEAC_Mulan | -20.210000 | 127.440000 | Mulan | Kimberley | Australia | aeolian | 300.000 | 300.000 | 300.000 | 300.000 | 10.000 | 1 | 2 | Large lake expansion, water level above 294 m, area > 6000 km² | Bowler et al. (2001) | |||
| 77 | TAEAC_Mulan | -20.210000 | 127.440000 | Mulan | Kimberley | Australia | aeolian | 200.000 | 200.000 | 200.000 | 200.000 | 10.000 | 1 | 1 | Formation of Rillyi Rillyi barrier-dune system, lake area around 4600 km² | Bowler et al. (2001) | |||
| 77 | TAEAC_Mulan | -20.210000 | 127.440000 | Mulan | Kimberley | Australia | aeolian | 100.000 | 100.000 | 100.000 | 100.000 | 10.000 | 1 | 1 | Another expansion, water level above 275m but less than 280m, area around 1500-2000 km² | Bowler et al. (2001) | |||
| 78 | TAEAC_WCC99_04 | -19.170000 | 127.800000 | 330 | Wolfe_Creek_Crater | Western_Australia | Australia | lake | 120.000 | 120.000 | 120.000 | 120.000 | 1.000 | 2 | 2 | C3 trees and shrubs, algae evidence | Miller et al. (2018) | ||
| 78 | TAEAC_WCC99_04 | -19.170000 | 127.800000 | 330 | Wolfe_Creek_Crater | Western_Australia | Australia | lake | 60.000 | 35.000 | 60.000 | 35.000 | 1.000 | 2 | 1 | Transition period with fluctuating water levels and varying sedimentation rates. | Miller et al. (2018) | ||
| 78 | TAEAC_WCC99_04 | -19.170000 | 127.800000 | 330 | Wolfe_Creek_Crater | Western_Australia | Australia | lake | 35.000 | 14.000 | 35.000 | 14.412 | 1.000 | 2 | -2 | Decrease in water table, drier conditions during Last Glacial Maximum (LGM). | Miller et al. (2018) | ||
| 78 | TAEAC_WCC99_04 | -19.170000 | 127.800000 | 330 | Wolfe_Creek_Crater | Western_Australia | Australia | lake | 14.000 | 12.000 | 14.412 | 12.061 | 1.000 | 2 | 1 | Increased rainfall from ~14 ka, water table rise intercepting crater floor before 13 ka. | Miller et al. (2018) | ||
| 78 | TAEAC_WCC99_04 | -19.170000 | 127.800000 | 330 | Wolfe_Creek_Crater | Western_Australia | Australia | lake | 12.000 | 6.000 | 12.061 | 6.075 | 1.000 | 2 | 1 | Rapid increase in water table after 12 ka indicating significantly wetter conditions. | Miller et al. (2018) | ||
| 80 | TAEAC_MARR04 | -17.070000 | 139.490000 | Bentinck_Island | Gulf of Carpentaria | Australia | lake | 1.250 | 0.030 | 0.800 | 0.030 | 1.069 | 0.804 | 0.010 | 2 | 1 | Initial development of Marralda Wetlands, transition from coastal to wetland environment | Mackenzie et al. (2017) | |
| 79 | TAEAC_WCS01 | -17.070000 | 139.490000 | Bentinck_Island | Gulf of Carpentaria | Australia | lake | 0.800 | 0.025 | 0.400 | 0.025 | 0.800 | 0.400 | 0.010 | 2 | 2 | Further development of wetlands, indicating increased wetness and productivity in the region | Mackenzie et al. (2017) | |
| 79 | TAEAC_WS01 | -17.070000 | 139.490000 | Bentinck_Island | Gulf of Carpentaria | Australia | lake | 0.400 | 0.025 | 0.000 | 0.400 | 0.000 | 0.010 | 2 | 2 | Continued wetland expansion and higher organic content, suggesting a recent wet phase | Mackenzie et al. (2017) | ||
| 81 | TAEAC_MARR02 | -17.070000 | 139.490000 | Bentinck_Island | Gulf of Carpentaria | Australia | lake | 2.600 | 0.025 | 0.500 | 0.026 | 2.600 | 0.973 | 0.160 | 2 | -1 | indicating a coastal setting transitioning to mangrove forest. | Moss et al. (2015) | |
| 81 | TAEAC_MARR04 | -17.070000 | 139.490000 | Bentinck_Island | Gulf of Carpentaria | Australia | lake | 0.500 | 0.026 | 0.000 | 0.503 | 0.001 | 0.160 | 2 | 1 | transition to estuarine mangrove forest | Moss et al. (2015) | ||
| 81 | TAEAC_MARR04 | -17.070000 | 139.490000 | Bentinck_Island | Gulf of Carpentaria | Australia | lake | 0.000 | -0.065 | 0.001 | -0.065 | 0.160 | 2 | 2 | Development of a freshwater swamp | Moss et al. (2015) | |||
| 82 | TAEAC_ELZ02 | -16.400000 | 126.130000 | Gap_Springs | Western Australia | Australia | lake | 14.800 | 0.045 | 8.910 | 0.060 | 14.449 | 8.929 | 0.100 | 2 | 2 | Presence of wetland taxa in older part of the record. | Field et al. (2018) | |
| 82 | TAEAC_ELZ02 | -16.400000 | 126.130000 | Gap_Springs | Western Australia | Australia | lake | 8.910 | 0.060 | 3.130 | 0.035 | 8.929 | 3.099 | 0.100 | 2 | -1 | Transition in pollen assemblages, changes in wetland conditions and climate. | Field et al. (2018) | |
| 82 | TAEAC_ELZ02 | -16.400000 | 126.130000 | Gap_Springs | Western Australia | Australia | lake | 3.130 | 0.035 | 1.650 | 0.030 | 3.099 | 1.666 | 0.100 | 2 | -2 | Decline in wetland taxa, change in regional pollen sum. | Field et al. (2018) | |
| 82 | TAEAC_ELZ02 | -16.400000 | 126.130000 | Gap_Springs | Western Australia | Australia | lake | 1.650 | 0.030 | 0.000 | 1.666 | 0.013 | 0.100 | 2 | 1 | Increase in wetland taxa, high non-pollen palynomorph accumulation rates. | Field et al. (2018) | ||
| 83 | TAEAC_FRN02 | -15.940000 | 126.280000 | Fern_Pool | Western Australia | Australia | lake | 12.050 | 0.030 | 11.570 | 0.030 | 12.050 | 11.571 | 0.100 | 2 | 2 | High abundance of wetland taxa, low regional pollen sum variability. | Field et al. (2018) | |
| 83 | TAEAC_FRN02 | -15.940000 | 126.280000 | Fern_Pool | Western Australia | Australia | lake | 11.570 | 0.030 | 9.940 | 0.035 | 11.571 | 9.952 | 0.100 | 2 | 1 | Increase in wetland taxa, decline in spring taxa. | Field et al. (2018) | |
| 83 | TAEAC_FRN02 | -15.940000 | 126.280000 | Fern_Pool | Western Australia | Australia | lake | 9.940 | 0.035 | 3.700 | 0.040 | 9.952 | 3.722 | 0.100 | 2 | -1 | Pollen assemblage changes, reflecting variations in spring dynamics and local climate. | Field et al. (2018) | |
| 83 | TAEAC_FRN02 | -15.940000 | 126.280000 | Fern_Pool | Western Australia | Australia | lake | 3.700 | 0.040 | 0.740 | 0.045 | 3.722 | 0.740 | 0.100 | 2 | -2 | Decline in wetland taxa, increase in Eucalyptus. | Field et al. (2018) | |
| 83 | TAEAC_FRN02 | -15.940000 | 126.280000 | Fern_Pool | Western Australia | Australia | lake | 0.740 | 0.045 | 0.000 | 0.740 | 0.000 | 0.100 | 2 | 1 | Increased wetland taxa, high non-pollen palynomorph accumulation rates. | Field et al. (2018) | ||
| 85 | TAEAC_BSP02 | -15.630000 | 126.390000 | Black_Springs | Western Australia | Australia | lake | 2.600 | 1.000 | 2.600 | 1.000 | 0.100 | 2 | -2 | Marked reduction in monsoonal precipitation | Field et al. (2018) | |||
| 85 | TAEAC_BSP02 | -15.630000 | 126.390000 | Black_Springs | Western Australia | Australia | lake | 14.520 | 0.030 | 14.040 | 0.030 | 14.520 | 13.914 | 0.100 | 2 | 2 | Wetland pollen dominated, low pollen and charcoal rates, no non-pollen palynomorphs. | Field et al. (2018) | |
| 85 | TAEAC_BSP02 | -15.630000 | 126.390000 | Black_Springs | Western Australia | Australia | lake | 14.040 | 0.030 | 9.120 | 0.035 | 13.914 | 9.131 | 0.100 | 2 | 1 | Increase in wetland and spring taxa pollen, wetland taxa decline up-core. | Field et al. (2018) | |
| 85 | TAEAC_BSP02 | -15.630000 | 126.390000 | Black_Springs | Western Australia | Australia | lake | 9.120 | 0.035 | 7.730 | 0.040 | 9.131 | 7.749 | 0.100 | 2 | -1 | Vegetation transition, spring taxa increase, wetland taxa decrease. | Field et al. (2018) | |
| 85 | TAEAC_BSP02 | -15.630000 | 126.390000 | Black_Springs | Western Australia | Australia | lake | 7.730 | 0.040 | 4.280 | 0.040 | 7.749 | 4.248 | 0.100 | 2 | -2 | Wetland taxa decline, spring taxa increase, regional pollen sum changes. | Field et al. (2018) | |
| 85 | TAEAC_BSP02 | -15.630000 | 126.390000 | Black_Springs | Western Australia | Australia | lake | 4.280 | 0.040 | 0.580 | 0.040 | 4.248 | 0.580 | 0.100 | 2 | -1 | Eucalyptus increase, Poaceae decrease, regional pollen sum composition changes. | Field et al. (2018) | |
| 85 | TAEAC_BSP02 | -15.630000 | 126.390000 | Black_Springs | Western Australia | Australia | lake | 0.580 | 0.040 | 0.000 | 0.580 | 0.000 | 0.100 | 2 | 1 | High non-pollen palynomorph accumulation rates, indicating environmental changes. | Field et al. (2018) | ||
| 84 | TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | Vanderlin_Island | Gulf of Carpentaria | Australia | lake | 8.450 | 0.080 | 6.430 | 0.050 | 8.383 | 6.393 | 0.500 | 1 | 2 | Early Holocene marine transgression, mangrove expansion. | Prebble et al. (2005) | |
| 84 | TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | Vanderlin_Island | Gulf of Carpentaria | Australia | lake | 6.430 | 0.050 | 4.190 | 0.050 | 6.393 | 4.154 | 0.500 | 1 | 1 | Development of dense Melaleuca forest in a swamp. | Prebble et al. (2005) | |
| 84 | TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | Vanderlin_Island | Gulf of Carpentaria | Australia | lake | 4.190 | 0.050 | 3.110 | 0.050 | 4.154 | 3.061 | 0.500 | 1 | -1 | Transition to a more open environment. | Prebble et al. (2005) | |
| 84 | TAEAC_Walala_Core_2 | -15.680000 | 137.030000 | Vanderlin_Island | Gulf of Carpentaria | Australia | lake | 3.110 | 0.050 | 0.000 | 0.050 | 3.061 | 0.010 | 0.500 | 1 | 1 | Formation of perennial lake conditions. | Prebble et al. (2005) | |
| 86 | TAEAC_Black_Springs | -15.630000 | 126.380000 | Black_Springs | Western Australia | Australia | lake | 6.300 | 0.037 | 3.000 | 0.050 | 6.314 | 3.012 | 0.230 | 3 | -2 | Increased aeolian dust deposition and reduced monsoon activity. | McGowan et al. (2012) | |
| 86 | TAEAC_Black_Springs | -15.630000 | 126.380000 | Black_Springs | Western Australia | Australia | lake | 3.000 | 1.500 | 3.012 | 1.512 | 0.230 | 3 | -2 | Continued dominance of aeolian dust deposition | McGowan et al. (2012) | |||
| 86 | TAEAC_Black_Springs | -15.630000 | 126.380000 | Black_Springs | Western Australia | Australia | lake | 1.500 | 1.200 | 1.512 | 1.206 | 0.230 | 3 | 1 | Increased fluvial deposits | McGowan et al. (2012) | |||
| 86 | TAEAC_Black_Springs | -15.630000 | 126.380000 | Black_Springs | Western Australia | Australia | lake | 1.200 | 0.000 | 1.206 | 0.001 | 0.230 | 3 | -1 | Transition to modern monsoon climate with increased rainfall and monsoon activity. | McGowan et al. (2012) | |||
| 87 | TAEAC_BSP | -15.630000 | 126.380000 | Black_Springs | Kimberley | Australia | lake | 15.000 | 0.040 | 14.000 | 0.040 | 15.000 | 14.000 | 0.100 | 3 | 2 | Dominance of Myrtaceae and Poaceae. | Field et al. (2017) | |
| 87 | TAEAC_BSP | -15.630000 | 126.380000 | Black_Springs | Kimberley | Australia | lake | 14.000 | 0.040 | 10.000 | 0.040 | 14.000 | 9.421 | 0.100 | 3 | 1 | Increase in spring taxa and wetland taxa. | Field et al. (2017) | |
| 87 | TAEAC_BSP | -15.630000 | 126.380000 | Black_Springs | Kimberley | Australia | lake | 10.000 | 0.040 | 6.840 | 0.035 | 9.421 | 6.826 | 0.100 | 3 | -1 | High abundance of mound spring taxa. | Field et al. (2017) | |
| 87 | TAEAC_BSP | -15.630000 | 126.380000 | Black_Springs | Kimberley | Australia | lake | 6.840 | 0.035 | 4.940 | 0.035 | 6.826 | 4.959 | 0.100 | 3 | -2 | Decline in wetland taxa, increase in tropical savanna. | Field et al. (2017) | |
| 87 | TAEAC_BSP | -15.630000 | 126.380000 | Black_Springs | Kimberley | Australia | lake | 4.940 | 0.035 | 2.620 | 0.035 | 4.959 | 2.633 | 0.100 | 3 | -1 | Increase in Terminalia and tropical savanna taxa. | Field et al. (2017) | |
| 87 | TAEAC_BSP | -15.630000 | 126.380000 | Black_Springs | Kimberley | Australia | lake | 2.620 | 0.035 | 0.550 | 0.030 | 2.633 | 0.552 | 0.100 | 3 | -2 | Decline in wetland taxa, increase in savanna taxa. | Field et al. (2017) | |
| 87 | TAEAC_BSP | -15.630000 | 126.380000 | Black_Springs | Kimberley | Australia | lake | 0.550 | 0.030 | 0.230 | 0.030 | 0.552 | 0.230 | 0.100 | 3 | -1 | High charcoal accumulation rates. | Field et al. (2017) | |
| 87 | TAEAC_BSP | -15.630000 | 126.380000 | Black_Springs | Kimberley | Australia | lake | 0.230 | 0.030 | 0.000 | 0.230 | 0.000 | 0.100 | 3 | 1 | Increased wetland taxa in recent times. | Field et al. (2017) | ||
| 92 | TAEAC_Core89_1 | -13.860000 | 136.780000 | Groote_Eylandt | Northern Territory | Australia | lake | 10.000 | 0.075 | 7.500 | 0.200 | 10.000 | 7.500 | 0.170 | 2 | 2 | Marine transgression and mangrove expansion. | Shulmeister (1992) | |
| 92 | TAEAC_Core89_1 | -13.860000 | 136.780000 | Groote_Eylandt | Northern Territory | Australia | lake | 7.500 | 0.200 | 5.000 | 0.100 | 7.500 | 5.000 | 0.170 | 2 | 1 | Development of Eucalyptus open forest and acacias. | Shulmeister (1992) | |
| 92 | TAEAC_Core89_1 | -13.860000 | 136.780000 | Groote_Eylandt | Northern Territory | Australia | lake | 5.000 | 0.100 | 3.800 | 0.170 | 5.000 | 3.800 | 0.170 | 2 | -1 | Shift to more open habitats, possibly indicating less moisture. | Shulmeister (1992) | |
| 92 | TAEAC_Core89_1 | -13.860000 | 136.780000 | Groote_Eylandt | Northern Territory | Australia | lake | 3.800 | 0.170 | 1.000 | 0.170 | 3.800 | 1.000 | 0.170 | 2 | 1 | Increase in Eucalyptus and vine thickets. | Shulmeister (1992) | |
| 92 | TAEAC_Core89_1 | -13.860000 | 136.780000 | Groote_Eylandt | Northern Territory | Australia | lake | 1.000 | 0.170 | 0.000 | 1.000 | 0.000 | 0.170 | 2 | 2 | Increase in wetland indicators and swamp taxa. | Shulmeister (1992) | ||
| 93 | TAEAC_Core89_1 | -13.850000 | 136.780000 | Groote_Eylandt | Northern Territory | lake | 10.000 | 0.075 | 7.500 | 0.090 | 11.465 | 8.303 | 0.340 | 1 | -1 | Slow decline in arid adapted pollen. | Shulmeister and Lees (1992) | ||
| 93 | TAEAC_Core89_1 | -13.850000 | 136.780000 | Groote_Eylandt | Northern Territory | lake | 7.500 | 0.090 | 3.800 | 0.100 | 8.303 | 4.122 | 0.340 | 1 | 1 | Raised water tables. | Shulmeister and Lees (1992) | ||
| 93 | TAEAC_Core89_1 | -13.850000 | 136.780000 | Groote_Eylandt | Northern Territory | lake | 4.200 | 3.500 | 4.668 | 3.732 | 0.340 | 1 | 1 | Sharp decline in pollen influx and organic sed. | Shulmeister and Lees (1992) | ||||
| 93 | TAEAC_Core89_1 | -13.850000 | 136.780000 | Groote_Eylandt | Northern Territory | lake | 3.500 | 1.000 | 3.732 | 0.884 | 0.340 | 1 | -1 | Decrease in pollen influx | Shulmeister and Lees (1992) | ||||
| 93 | TAEAC_Core89_1 | -13.850000 | 136.780000 | Groote_Eylandt | Northern Territory | lake | 1.000 | 0.000 | 0.884 | 0.000 | 0.340 | 1 | 1 | Establishment of modern levels, | Shulmeister and Lees (1992) | ||||
| 97 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 11.900 | 5.500 | 11.949 | 5.513 | 0.200 | 2 | 1 | Expansion of grass cover, reduction in eucalypts. | Rowe et al. (2019) | ||
| 97 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 4.100 | 0.350 | 4.117 | 0.340 | 0.200 | 2 | -1 | Decline in grass cover, increase in Eucalyptus abundance. | Rowe et al. (2019) | ||
| 97 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 0.350 | 0.000 | 0.340 | -0.002 | 0.200 | 2 | 1 | Swamp fringe expansion. | Rowe et al. (2019) | ||
| 98 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 26.500 | 0.160 | 21.000 | 0.090 | 26.500 | 21.000 | 1.200 | 2 | -1 | Abundant grasses with sparse trees and shrubs | Rowe et al. (2020) |
| 98 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 21.000 | 0.090 | 18.000 | 0.080 | 21.000 | 18.000 | 1.200 | 2 | -2 | Maximum abundance of grasses, exclusion of herbs, and reduction in tree cover. | Rowe et al. (2020) |
| 101 | FR10/95-GC17 | -22.130000 | 113.500000 | -1093 | Western Australia | Australia | marine_core | 100.000 | 10.000 | 64.000 | 6.500 | 100.000 | 64.000 | 5.000 | 1 | 1 | Presence of open grass-rich Eucalyptus woodland pollen. | Van der Kaars et al. (2006) | |
| 101 | FR10/95-GC17 | -22.130000 | 113.500000 | -1093 | Western Australia | Australia | marine_core | 40.650 | 1.130 | 35.000 | 1.130 | 40.650 | 35.000 | 1.000 | 1 | -1 | Reduced presence of Eucalyptus pollen and increased presence of arid-adapted taxa. | Van der Kaars et al. (2006) | |
| 101 | FR10/95-GC17 | -22.130000 | 113.500000 | -1093 | Western Australia | Australia | marine_core | 35.000 | 1.130 | 19.250 | 0.280 | 35.000 | 19.514 | 1.000 | 1 | -2 | Dominance of herb (Asteraceae, Poaceae, Chenopodiaceae) pollen and presence of Callitris. | Van der Kaars et al. (2006) | |
| 101 | FR10/95-GC17 | -22.130000 | 113.500000 | -1093 | Western Australia | Australia | marine_core | 13.080 | 0.110 | 0.000 | 0.185 | 12.941 | -0.002 | 1.000 | 1 | 1 | Increased presence of wet-adapted pollen type. | Van der Kaars et al. (2006) | |
| 119 | GC-2 | -13.070000 | 140.200000 | Gulf_of_Carpentaria | Australia | marine_core | 35.330 | 26.000 | 35.330 | 26.000 | 1.000 | 2 | 1 | Aquatic pollen | Torgersen et al. (1988) | ||||
| 119 | TAEAC_GC_10A | -13.070000 | 140.200000 | Gulf_of_Carpentaria | Australia | marine_core | 23.000 | 11.800 | 25.753 | 12.578 | 1.000 | 2 | -1 | Grasses and high charcoal, savannah-like | Torgersen et al. (1988) | ||||
| 127 | MD97-2129 | -10.789333 | 138.720000 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 74.000 | 64.700 | 74.000 | 64.700 | 3.000 | 2 | -1 | Enhanced fluvial activity is suggested | Reeves et al. (2008) | |||
| 127 | MD97-2130 | -12.266833 | 138.748667 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 74.000 | 64.700 | 74.000 | 64.700 | 3.000 | 2 | -1 | Enhanced fluvial activity is suggested | Reeves et al. (2008) | |||
| 127 | MD97-2131 | -12.066000 | 138.749667 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 74.000 | 64.700 | 74.000 | 64.700 | 3.000 | 2 | -1 | Enhanced fluvial activity is suggested | Reeves et al. (2008) | |||
| 127 | MD97-2132 | -12.313167 | 139.978833 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 116.000 | 103.000 | 137.468 | 122.730 | 3.000 | 2 | 1 | Increased fluvial activity. | Reeves et al. (2008) | |||
| 127 | MD97-2132 | -12.313167 | 139.978833 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 70.000 | 85.000 | 83.419 | 102.860 | 3.000 | 2 | -1 | shallow, restricted, low-energy environment represents the lowstand of MIS 5.2, in comparison, and a decrease in surface water may be postulated | Reeves et al. (2008) | |||
| 127 | MD97-2132 | -12.313167 | 139.978833 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 85.000 | 74.000 | 102.860 | 88.960 | 3.000 | 2 | 1 | Increased fluvial activity. | Reeves et al. (2008) | |||
| 127 | MD97-2132 | -12.313167 | 139.978833 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 74.000 | 64.700 | 88.960 | 76.627 | 3.000 | 2 | 1 | Enhanced fluvial activity is suggested | Reeves et al. (2008) | |||
| 127 | MD97-2132 | -12.313167 | 139.978833 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 23.000 | 19.000 | 23.859 | 18.669 | 3.000 | 2 | -2 | It's just kind of implied cryptically if you look at the climatic interpretation, unit descriptions, and Table 3. Like The Davinci Code in here | Reeves et al. (2008) | |||
| 127 | MD97-2132 | -12.313167 | 139.978833 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 19.000 | 17.100 | 18.669 | 16.734 | 3.000 | 2 | -1 | Enhanced fluvial activity is suggested | Reeves et al. (2008) | |||
| 127 | MD97-2133 | -12.390000 | 140.340000 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 74.000 | 64.700 | 68.398 | 61.367 | 3.000 | 2 | -1 | Evidence of effective precipitation and monsoon activity, supported by carbon isotopic analysis of fossil emu eggshells from Lake Eyre indicating increased C4 grasses. | Reeves et al. (2008) | |||
| 127 | MD97-2133 | -12.390000 | 140.340000 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 65.000 | 46.000 | 61.713 | 47.472 | 3.000 | 2 | 1 | Evidence of effective precipitation and monsoon activity, supported by carbon isotopic analysis of fossil emu eggshells from Lake Eyre indicating increased C4 grasses. | Reeves et al. (2008) | |||
| 127 | MD97-2133 | -12.390000 | 140.340000 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 29.000 | 29.000 | 30.950 | 30.950 | 3.000 | 2 | 1 | Establishment of lacustrine conditions in the deeper section of the basin, indicative of sufficient precipitation. | Reeves et al. (2008) | |||
| 127 | MD97-2133 | -12.390000 | 140.340000 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 23.000 | 19.000 | 24.245 | 19.506 | 3.000 | 2 | -1 | Temporary contraction of the lake during the Last Glacial Maximum, with continued fluvial activity. | Reeves et al. (2008) | |||
| 127 | MD97-2133 | -12.390000 | 140.340000 | Lake_Carpentaria | Gulf of Carpentaria | Australia | marine_core | 14.000 | 14.000 | 14.724 | 14.724 | 3.000 | 2 | 1 | Expansion of the lake following the LGM, indicating increased precipitation and a productive environment. | Reeves et al. (2008) | |||
| 165 | TAEAC_G5_6_149P2 | -9.000000 | 128.000000 | Indonesia | marine_core | 43.000 | 3.950 | 47.543 | 3.772 | 1.000 | 1 | -1 | Eucalypt open forest vegetation replaced by grasslands | van der Kaars (1989) | |||||
| 165 | TAEAC_G5_6_149P2 | -9.000000 | 128.000000 | Indonesia | marine_core | 17.000 | 0.000 | 19.666 | 0.000 | 1.000 | 1 | 1 | Reduction in grassland and sedge area, followed by establishment of extensive mangrove forests in New Guinea around 14,500 BP, expansion of mountain rainforests from 10,000 BP, indicating an increase in temperature and rainfall. | van der Kaars (1989) | |||||
| 167 | GIK18506-2 | -8.790000 | 128.640000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 15.000 | 13.000 | 0.500 | 14.950 | 12.835 | 2.000 | 2 | -1 | The ACR is characterized by the lowest values in XRF-scanner-derived geochemical proxies for riverine input (ln(K/Ca) and ln((Al+K)/Ca) | Kuhnt et al. (2015) | |
| 201 | MD01-2378 | -13.080000 | 121.790000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 15.000 | 11.600 | 0.200 | 14.916 | 11.608 | 2.000 | 2 | -1 | The ACR is characterized by the lowest values in XRF-scanner-derived geochemical proxies for riverine input (ln(K/Ca) and ln((Al+K)/Ca) | Kuhnt et al. (2015) | |
| 202 | GIK18479-4 | -12.450000 | 121.370000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 15.000 | 12.500 | 0.400 | 14.901 | 12.423 | 2.000 | 2 | -1 | The ACR is characterized by the lowest values in XRF-scanner-derived geochemical proxies for riverine input (ln(K/Ca) and ln((Al+K)/Ca) | Kuhnt et al. (2015) | |
| 167 | GIK18506-2 | -8.790000 | 128.640000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 13.000 | 0.500 | 8.000 | 0.500 | 12.835 | 7.793 | 2.000 | 2 | 1 | terrigenous flux increase | Kuhnt et al. (2015) |
| 201 | MD01-2378 | -13.080000 | 121.790000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 11.600 | 0.200 | 8.000 | 0.200 | 11.608 | 7.820 | 2.000 | 2 | 1 | terrigenous flux increase | Kuhnt et al. (2015) |
| 202 | GIK18479-4 | -12.450000 | 121.370000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 12.500 | 0.400 | 8.000 | 0.400 | 12.423 | 7.842 | 2.000 | 2 | 1 | terrigenous flux increase | Kuhnt et al. (2015) |
| 167 | GIK18506-2 | -8.790000 | 128.640000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 7.000 | 6.700 | 0.100 | 6.807 | 6.504 | 2.000 | 2 | -1 | decrease in ln(K/Ca), runoff minimum | Kuhnt et al. (2015) | |
| 201 | MD01-2378 | -13.080000 | 121.790000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 8.000 | 0.200 | 6.600 | 0.100 | 7.820 | 6.396 | 2.000 | 2 | -1 | decrease in ln(K/Ca), runoff minimum | Kuhnt et al. (2015) |
| 202 | GIK18479-4 | -12.450000 | 121.370000 | -1875 | Timor_Sea | Timor Sea | Australia | marine_core | 8.000 | 0.400 | 4.600 | 0.900 | 7.842 | 4.435 | 2.000 | 2 | -1 | decrease in ln(K/Ca), runoff minimum | Kuhnt et al. (2015) |
| 178 | TAEAC_BGC14 | -17.030000 | 125.000000 | Ball_Gown_Cave | Western_Australia | speleothem | 24.000 | 1.000 | 20.000 | 1.000 | 24.000 | 20.000 | 0.090 | 1 | -1 | negative isotope anomalies | Denniston et al. (2013) | ||
| 178 | TAEAC_BGC6 | -17.030000 | 125.000000 | Ball_Gown_Cave | Western_Australia | speleothem | 16.000 | 2.000 | 13.000 | 2.000 | 16.000 | 13.000 | 0.090 | 1 | -1 | negative isotope anomalies | Denniston et al. (2013) | ||
| 178 | TAEAC_BGC6 | -17.030000 | 125.000000 | Ball_Gown_Cave | Western_Australia | speleothem | 11.500 | 1.000 | 8.000 | 11.500 | 8.000 | 0.090 | 1 | 1 | positive isotope excusion | Denniston et al. (2013) | |||
| 179 | TAEAC_KNI_51_11 | -15.180000 | 128.370000 | 100 | Cave_KNI-51 | Australia | speleothem | 0.600 | 0.500 | 0.600 | 0.500 | 0.001 | 3 | 1 | Elevated occurrence rates of extreme rainfall events | Denniston et al. (2015) | |||
| 179 | TAEAC_KNI_51_11 | -15.180000 | 128.370000 | 100 | Cave_KNI-51 | Australia | speleothem | 0.500 | 0.300 | 0.500 | 0.300 | 0.001 | 3 | -1 | Reduced activity marking the period 1450–1650 CE. | Denniston et al. (2015) | |||
| 179 | TAEAC_KNI_51_11 | -15.180000 | 128.370000 | 100 | Cave_KNI-51 | Australia | speleothem | 1.900 | 1.550 | 1.900 | 1.550 | 0.001 | 3 | 1 | Elevated occurrence rates of extreme rainfall events from 50–400 CE. | Denniston et al. (2015) | |||
| 179 | TAEAC_KNI_51_11 | -15.180000 | 128.370000 | 100 | Cave_KNI-51 | Australia | speleothem | 1.450 | 1.100 | 1.450 | 1.100 | 0.001 | 3 | -1 | Reduced activity marking the period 500–850 CE. | Denniston et al. (2015) | |||
| 179 | TAEAC_KNI_51_11 | -15.180000 | 128.370000 | 100 | Cave_KNI-51 | Australia | speleothem | 0.150 | -0.050 | 0.150 | -0.050 | 0.001 | 3 | 1 | Elevated occurrence rates of extreme rainfall events from 50–400 CE. | Denniston et al. (2015) | |||
| 180 | TAEAC_KNI_51_1 | -15.180000 | 128.370000 | Cave_KNI-51 | Australia | speleothem | 13.400 | 11.700 | 13.400 | 11.700 | 0.025 | 3 | 1 | Enriched d13C | Denniston et al. (2017) | ||||
| 180 | TAEAC_KNI_51_3 | -15.180000 | 128.370000 | Cave_KNI-51 | Australia | speleothem | 16.500 | 14.800 | 16.500 | 14.800 | 0.025 | 3 | 1 | Enriched d13C | Denniston et al. (2017) | ||||
| 180 | TAEAC_KNI_51_3 | -15.180000 | 128.370000 | Cave_KNI-51 | Australia | speleothem | 18.300 | 17.300 | 18.300 | 17.300 | 0.025 | 3 | 1 | Enriched d13C | Denniston et al. (2017) | ||||
| 180 | TAEAC_KNI_51_1 | -15.180000 | 128.370000 | Cave_KNI-51 | Australia | speleothem | 9.500 | 9.000 | 9.500 | 9.000 | 0.025 | 3 | 1 | Enriched d13C | Denniston et al. (2017) | ||||
| 181 | TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | Cobourg Peninsula | Northern_Territory | Australia | aeolian | 8.600 | 1.400 | 7.500 | 1.400 | 8.600 | 7.500 | 1.000 | 1 | -1 | Dune emplacement | Lees et al. (1990) | |
| 181 | TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | Cobourg Peninsula | Northern_Territory | Australia | aeolian | 2.800 | 0.500 | 2.600 | 0.300 | 2.800 | 2.600 | 1.000 | 1 | -1 | Dune emplacement | Lees et al. (1990) | |
| 181 | TAEAC_Cobourg_Peninsula | -11.280000 | 132.200000 | Cobourg Peninsula | Northern_Territory | Australia | aeolian | 1.900 | 0.400 | 1.900 | 0.400 | 1.900 | 1.900 | 1.000 | 1 | -1 | Dune emplacement | Lees et al. (1990) | |
| 181 | TAEAC_Shelburne_Bay | -11.920000 | 142.910000 | Shelburne Bay | Northern_Territory | Australia | aeolian | 23.800 | 2.400 | 17.600 | 1.400 | 23.800 | 17.600 | 1.000 | 1 | -1 | Dune emplacement | Lees et al. (1990) | |
| 181 | TAEAC_Shelburne_Bay | -11.920000 | 142.910000 | Shelburne Bay | Northern_Territory | Australia | aeolian | 29.900 | 2.400 | 28.400 | 1.300 | 29.900 | 28.400 | 1.000 | 1 | -1 | Dune emplacement | Lees et al. (1990) | |
| 181 | TAEAC_Cape_Flattery | -15.080000 | 145.240000 | Cape Flattery | Northern_Territory | Australia | aeolian | 22.700 | 2.800 | 19.200 | 3.400 | 22.700 | 19.200 | 1.000 | 1 | -1 | Dune emplacement | Lees et al. (1990) | |
| 181 | TAEAC_Cape_Flattery | -15.080000 | 145.240000 | Cape Flattery | Northern_Territory | Australia | aeolian | 2.000 | 1.000 | 2.000 | 1.000 | 2.000 | 2.000 | 1.000 | 1 | -1 | Dune emplacement | Lees et al. (1990) | |
| 187 | TAEAC_BW01 | -12.657000 | 141.998000 | Big_Willum_Swamp | Cape_York | Australia | lake | 7.216 | 0.032 | 2.200 | 0.025 | 7.070 | 2.196 | 0.300 | 2 | -1 | Initiation of swamp-like conditions | Stevenson et al. (2015) | |
| 187 | TAEAC_BW01 | -12.657000 | 141.998000 | Big_Willum_Swamp | Cape_York | Australia | lake | 2.200 | 0.025 | 0.600 | 0.033 | 2.196 | 0.596 | 0.300 | 2 | 1 | Transition to a permanent deep water body | Stevenson et al. (2015) | |
| 187 | TAEAC_BW01 | -12.657000 | 141.998000 | Big_Willum_Swamp | Cape_York | Australia | lake | 0.600 | 0.033 | 0.400 | 0.050 | 0.596 | 0.397 | 0.300 | 2 | 1 | Swamp reaches present-day extent | Stevenson et al. (2015) | |
| 196 | TAEAC_Lake_Woods | -17.850000 | 133.500000 | Lake_Woods | Northern_Territory | Australia | lake | 130.000 | 96.000 | 10.000 | 130.000 | 96.000 | 1.000 | 2 | 2 | Greatly expanded lake in late stage 7 | Bowler et al. (1998) | ||
| 196 | TAEAC_Lake_Woods | -17.850000 | 133.500000 | Lake_Woods | Northern_Territory | Australia | lake | 64.000 | 30.000 | 64.000 | 30.000 | 1.000 | 2 | 1 | Expanded lake | Bowler et al. (1998) | |||
| 196 | TAEAC_Lake_Woods | -17.850000 | 133.500000 | Lake_Woods | Northern_Territory | Australia | lake | 28.900 | 5.500 | 26.800 | 3.500 | 28.900 | 26.800 | 1.000 | 2 | -1 | Dune emplacement | Bowler et al. (1998) | |
| 196 | TAEAC_Lake_Woods | -17.850000 | 133.500000 | Lake_Woods | Northern_Territory | Australia | lake | 12.000 | 0.000 | 12.000 | 0.000 | 1.000 | 2 | 1 | Expanded lake | Bowler et al. (1998) | |||
| 197 | TAEAC_SAN1a | -11.120000 | 142.350000 | 15 | Sanamere_Lagoon | Cape_York | Australia | lake | 7.795 | 0.030 | 7.700 | 0.035 | 7.795 | 7.700 | 0.040 | 2 | 1 | Peak charcoal and pyrogenic carbon fluxes occurred at the start of the SAN1 record from 8,150 to 7,900 cal BP, initially at high intensities, along with consistently low δ13C values for bulk pyrogenic carbon (Figures 4, 5). | Rehn et al. (2021a) |
| 197 | TAEAC_SAN1a | -11.120000 | 142.350000 | 15 | Sanamere_Lagoon | Cape_York | Australia | lake | 7.700 | 0.035 | 6.600 | 0.035 | 7.700 | 6.600 | 0.040 | 2 | 2 | An abrupt decline in sedimentation rate as well as charcoal and pyrogenic carbon fluxes at Sanamere Lagoon at 7,900 cal BP suggests a potential expansion of the site under the increasingly wet conditions of the mid-Holocene. | Rehn et al. (2021a) |
| 197 | TAEAC_SAN1a | -11.120000 | 142.350000 | 15 | Sanamere_Lagoon | Cape_York | Australia | lake | 6.600 | 0.035 | 5.880 | 0.035 | 6.600 | 5.880 | 0.040 | 2 | 1 | Charcoal flux increased again at the lagoon from ∼6,800–6,000 cal BP, but at lower levels than those seen prior to 7,900 cal BP. | Rehn et al. (2021a) |
| 198 | TAEAC_BWIL2 | -12.657000 | 141.998000 | 30 | Big_Willum_Swamp | Cape_York | Australia | lake | 3.445 | 0.035 | 1.700 | 0.035 | 3.445 | 1.700 | 0.150 | 3 | 1 | The oldest modeled age for core BWIL2 is ∼3,920 cal BP, associated with low sedimentation rates and minimal charcoal and pyrogenic carbon. | Rehn et al. (2021a) |
| 198 | TAEAC_BWIL2 | -12.657000 | 141.998000 | 30 | Big_Willum_Swamp | Cape_York | Australia | lake | 1.700 | 0.035 | 0.400 | 0.035 | 1.700 | 0.400 | 0.150 | 3 | 2 | Organic input (represented by Mo ratio) and sediment accumulation increased noticeably after ∼1,700 cal BP at Big Willum Swamp | Rehn et al. (2021a) |
| 198 | TAEAC_BWIL2 | -12.657000 | 141.998000 | 30 | Big_Willum_Swamp | Cape_York | Australia | lake | 0.400 | 0.035 | -0.065 | 0.000 | 0.400 | -0.065 | 0.150 | 3 | 1 | Stevenson et al. (2015) noted wet conditions from 600 to 400 cal BP at Big Willum Swamp, reflected in the BWIL2 record as increased charcoal and pyrogenic carbon fluxes from some time after 600 cal BP coincident with increased sedimentation rates. | Rehn et al. (2021a) |
| 199 | TAEAC_MAR2 | -13.409000 | 135.774000 | 50 | Maurura_Sinkhole | Northern_Territory | Australia | lake | 4.155 | 0.050 | 2.555 | 0.040 | 4.155 | 2.555 | 0.030 | 2 | 1 | Peak charcoal and pyrogenic carbon influxes at Marura (~4000 cal BP) coincide with this regional transition from higher effective precipitation in the mid-Holocene to drier and/or more variable conditions into the late-Holocene | Rehn et al. (2021b) |
| 199 | TAEAC_MAR2 | -13.409000 | 135.774000 | 50 | Maurura_Sinkhole | Northern_Territory | Australia | lake | 2.555 | 0.040 | 1.105 | 0.030 | 2.555 | 1.105 | 0.030 | 2 | -1 | Lower overall fire incidence compared to Phase I is likely due to continuing dry conditions producing less biomass than during the mid-Holocene precipitation maximum. | Rehn et al. (2021b) |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 150.000 | 10.400 | 120.000 | 10.400 | 150.000 | 120.000 | 0.550 | 4 | 1 | Large, individual negative excursions in δ2Hpam accompanied by coeval increases in tree cover | Bird et al. (2024) |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 120.000 | 10.400 | 115.000 | 12.000 | 120.000 | 115.000 | 0.550 | 4 | 1 | Bird et al. (2024) | |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 115.000 | 12.000 | 110.000 | 13.100 | 115.000 | 110.000 | 0.550 | 4 | 2 | Most intense monsoon on record, effectively closed forest | Bird et al. (2024) |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 110.000 | 13.100 | 91.000 | 8.200 | 110.000 | 91.000 | 0.550 | 4 | -1 | Bird et al. (2024) | |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 91.000 | 8.200 | 85.000 | 6.000 | 91.000 | 85.000 | 0.550 | 4 | 2 | Large peak in monsoonal activity | Bird et al. (2024) |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 85.000 | 6.000 | 69.000 | 5.800 | 85.000 | 69.000 | 0.550 | 4 | -2 | Bird et al. (2024) | |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 69.000 | 5.800 | 52.000 | 3.200 | 69.000 | 52.000 | 0.550 | 4 | -1 | Bird et al. (2024) | |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 52.000 | 3.200 | 17.500 | 1.300 | 52.000 | 17.500 | 0.550 | 4 | -2 | Bird et al. (2024) | |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 17.500 | 1.300 | 14.500 | 0.700 | 17.500 | 14.500 | 0.550 | 4 | 2 | Large increase in tree cover, though not TOC | Bird et al. (2024) |
| 200 | TAEAC_Girraween | -12.520000 | 131.080000 | 20 | Girraween_Lagoon | Northern Territory | Australia | lake | 14.500 | 0.700 | 0.000 | 0.000 | 14.500 | 0.000 | 0.550 | 4 | 1 | Bird et al. (2024) | |
| 203 | TAEAC_TableTopSwamp_b | -13.178000 | 130.746000 | 200 | Table_Top_Swamp | Northern Territory | Australia | lake | 35.000 | 25.000 | 31.340 | 24.489 | 0.150 | 5 | -2 | conditions were drier and more stable than present, with a more grass dominated savanna and limited wetland development, implying reduced IASM activity. | Marx et al. (2021) | ||
| 203 | TAEAC_TableTopSwamp_b | -13.178000 | 130.746000 | 200 | Table_Top_Swamp | Northern Territory | Australia | lake | 25.000 | 10.000 | 24.489 | 9.891 | 0.150 | 5 | 1 | increased moisture at the study site, but also increased IASM variability | Marx et al. (2021) | ||
| 203 | TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | 200 | Table_Top_Swamp | Northern Territory | Australia | lake | 10.000 | 5.000 | 10.000 | 5.049 | 0.050 | 5 | 2 | increasing moisture advection to the study site and resulting in establishment of a quasi-permeant wetland. | Marx et al. (2021) | ||
| 203 | TAEAC_TableTopSwamp_a | -13.178000 | 130.746000 | 200 | Table_Top_Swamp | Northern Territory | Australia | lake | 5.000 | 0.000 | 5.049 | 0.006 | 0.050 | 5 | 1 | After 5 ka the pollen assemblage in TTS became indicative of a drier vegetation mosaic. | Marx et al. (2021) | ||
| 204 | TAEAC_BR-BU | -15.466500 | 129.785000 | 7 | Bullo_River | Kimberley | Australia | fluvial | 17.600 | 1.000 | 12.900 | 0.900 | 17.600 | 12.900 | 0.500 | 6 | -1 | "our results mostly indicate less wet season precipitation during the deglacial" | Dixon et al. (2025) |
| 204 | TAEAC_BR-BU | -15.466500 | 129.785000 | 7 | Bullo_River | Kimberley | Australia | fluvial | 12.900 | 0.900 | 5.100 | 0.100 | 12.900 | 5.100 | 0.500 | 6 | 1 | "small increases in wet season precipitation" | Dixon et al. (2025) |
| 204 | TAEAC_BR-BU | -15.466500 | 129.785000 | 7 | Bullo_River | Kimberley | Australia | fluvial | 5.100 | 0.100 | 0.900 | 0.400 | 5.100 | 0.900 | 0.500 | 6 | -1 | "clear that this interval was drier" | Dixon et al. (2025) |
| 204 | TAEAC_BR-BU | -15.466500 | 129.785000 | 7 | Bullo_River | Kimberley | Australia | fluvial | 0.900 | 0.400 | 0.000 | 0.040 | 0.900 | 0.000 | 0.500 | 6 | 1 | "increased moisture availability" | Dixon et al. (2025) |
| 205 | TAEAC_SkullSprings | -15.210000 | 125.728000 | Skull_Springs | Kimberley | Australia | lake | 16.055 | 0.040 | 14.000 | 0.040 | 16.055 | 14.000 | 0.500 | 6 | -1 | "low sedimentation rate ... may reflect drier conditions" Really no interpretation for this time period | Rudd et al. (2025) | |
| 205 | TAEAC_SkullSprings | -15.210000 | 125.728000 | Skull_Springs | Kimberley | Australia | lake | 14.000 | 0.040 | 10.000 | 0.040 | 14.000 | 10.000 | 0.500 | 6 | 1 | "[rainforest] taxa increase in relative abundance after 14k cal a bp" | Rudd et al. (2025) | |
| 205 | TAEAC_SkullSprings | -15.210000 | 125.728000 | Skull_Springs | Kimberley | Australia | lake | 10.000 | 0.040 | 6.000 | 0.022 | 10.000 | 6.000 | 0.500 | 6 | 2 | "[rainforest taxa are] more prevalent from 10k cal a bp onwards" | Rudd et al. (2025) | |
| 205 | TAEAC_SkullSprings | -15.210000 | 125.728000 | Skull_Springs | Kimberley | Australia | lake | 6.000 | 0.022 | 3.000 | 0.022 | 6.000 | 3.000 | 0.500 | 6 | 1 | "abundance of monsoon rainforest-associated taxa and pteridophytes at Skull Springs decreases" | Rudd et al. (2025) | |
| 205 | TAEAC_SkullSprings | -15.210000 | 125.728000 | Skull_Springs | Kimberley | Australia | lake | 3.000 | 0.022 | 2.000 | 0.022 | 3.000 | 2.000 | 0.500 | 6 | -1 | This 1000 period is not described. I assume that if hydric indicators decrease until now, then increase after now, it must be relatively dry. | Rudd et al. (2025) | |
| 205 | TAEAC_SkullSprings | -15.210000 | 125.728000 | Skull_Springs | Kimberley | Australia | lake | 2.000 | 0.022 | 0.000 | 0.000 | 2.000 | 0.000 | 0.500 | 6 | 1 | "monsoon rainforest-associated taxa gradually increasing again in the last ~2000 years" | Rudd et al. (2025) | |
| 206 | TAEAC_SAN1b | -11.120000 | 142.360000 | Sanamere_Lagoon | Cape_York | Australia | lake | 33.000 | 29.100 | 33.000 | 29.100 | 0.800 | 6 | -1 | low nitrogen, coarse sand, but high sedimentation | Rivera-Araya et al. (2023) | |||
| 206 | TAEAC_SAN1b | -11.120000 | 142.360000 | Sanamere_Lagoon | Cape_York | Australia | lake | 29.100 | 18.200 | 29.100 | 18.200 | 0.800 | 6 | -2 | wind-blown features indicate seasonally dry | Rivera-Araya et al. (2023) | |||
| 206 | TAEAC_SAN1b | -11.120000 | 142.360000 | Sanamere_Lagoon | Cape_York | Australia | lake | 18.200 | 10.800 | 18.200 | 10.800 | 0.800 | 6 | 1 | decrease in coarse sand, Ti suggest larger lagoon | Rivera-Araya et al. (2023) | |||
| 206 | TAEAC_SAN1b | -11.120000 | 142.360000 | Sanamere_Lagoon | Cape_York | Australia | lake | 10.800 | 4.700 | 10.800 | 4.700 | 0.800 | 6 | 2 | increase in terrestrial inputs, lake deepening, open water diatoms | Rivera-Araya et al. (2023) | |||
| 206 | TAEAC_SAN1b | -11.120000 | 142.360000 | Sanamere_Lagoon | Cape_York | Australia | lake | 4.700 | 0.000 | 4.700 | 0.000 | 0.800 | 6 | 1 | organic matter and terrestrial input decrease/stabilisation | Rivera-Araya et al. (2023) |