/* DATA DESCRIPTION: Citation: 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. Keyword(s): age-depth model; Australia; Holocene; Hydroclimate; OSL; palaeoclimate; Radiocarbon 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 Bird, Michael I; Brand, Michael; Comley, Rainy; Hadeen, Xennephone; Jacobs, Zenobia; Rowe, Cassandra; Saltré, Frédérik; Wurster, Christopher M; Zwart, Costijn; Bradshaw, Corey J A (2025): A 150,000-year lacustrine record of the Indo-Australian monsoon from northern Australia. Quaternary Science Reviews, 366, 109504, https://doi.org/10.1016/j.quascirev.2025.109504 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 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 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 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)) 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; Ulm, Sean; Bird, Michael I (2023): A 33,000-year paleohydrological record from Sanamere Lagoon, north-eastern tropical savannas of Australia. Quaternary Research, 113, 146-161, https://doi.org/10.1017/qua.2022.59 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 Rowe, Cassandra; Wurster, Christopher M; Zwart, Costijn; Brand, Michael; Hutley, Lindsay B; Levchenko, Vladimir; Bird, Michael I (2021): Vegetation over the last glacial maximum at Girraween Lagoon, monsoonal northern Australia. Quaternary Research, 102, 39-52, https://doi.org/10.1017/qua.2020.50 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 Saynor, Mike; Wasson, Robert; Erskine, Wayne; Lam, Daryl (2020): Holocene palaeohydrology of the East Alligator River, for application to mine site rehabilitation, Northern Australia. Quaternary Science Reviews, 249, 106552, https://doi.org/10.1016/j.quascirev.2020.106552 Shulmeister, James (1992): A Holocene Pollen record from Lowland Tropical Australia. The Holocene, 2(2), 107-116, https://doi.org/10.1177/095968369200200202 Shulmeister, James; Lees, Brian G (1992): Morphology and chronostratigraphy of a coastal dunefield; Groote Eylandt, northern Australia. Geomorphology, 5(6), 521-534, https://doi.org/10.1016/0169-555X(92)90023-H 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) (URI: https://www.arc.gov.au/), grant/award no. CE170100015: ARC Centre of Excellence for Australian Biodiversity and Heritage (URI: https://dataportal.arc.gov.au/RGS/Web/Grants/CE170100015) Australian Research Council (ARC) (URI: https://www.arc.gov.au/), grant/award no. CE230100009: ARC Centre of Excellence for Indigenous and Environmental Histories and Futures (URI: https://dataportal.arc.gov.au/RGS/Web/Grants/CE230100009) Australian Research Council (ARC) (URI: https://www.arc.gov.au/), grant/award no. DE240100340: Identifying key fire drivers in Australia; biomass, climate or people (URI: https://dataportal.arc.gov.au/RGS/Web/Grants/DE240100340) Australian Research Council (ARC) (URI: https://www.arc.gov.au/), grant/award no. FT180100524: Climate extremes and landscape responses across continental Australia (URI: https://dataportal.arc.gov.au/RGS/Web/Grants/FT180100524) 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): FR10/95-GC17 * LATITUDE: -22.130000 * LONGITUDE: 113.500000 * ELEVATION: -1093.0 m * LOCATION: Indian Ocean * METHOD/DEVICE: Gravity corer (GC) GC-2 * LATITUDE: -12.519667 * LONGITUDE: 140.352333 * ELEVATION: -10.0 m * Recovery: 2.1 m * LOCATION: Arafura Sea * METHOD/DEVICE: Gravity corer (GC) GIK18479-4 * LATITUDE: -12.453280 * LONGITUDE: 121.373250 * DATE/TIME: 2005-09-23T22:03:00 * ELEVATION: -2974.0 m * Penetration: 25 m * LOCATION: Indian Ocean * CAMPAIGN: SO185 (VITAL) (URI: https://doi.org/10.2312/cr_so185) * BASIS: Sonne (URI: https://en.wikipedia.org/wiki/RV_Sonne) * METHOD/DEVICE: Piston corer (BGR type) (KL) GIK18506-2 * LATITUDE: -15.310930 * LONGITUDE: 119.500870 * DATE/TIME: 2005-10-01T04:42:00 * ELEVATION: -2410.0 m * Penetration: 20 m * Recovery: 15.59 m * LOCATION: Indian Ocean * CAMPAIGN: SO185 (VITAL) (URI: https://doi.org/10.2312/cr_so185) * BASIS: Sonne (URI: https://en.wikipedia.org/wiki/RV_Sonne) * METHOD/DEVICE: Piston corer (BGR type) (KL) MD01-2378 (MD012378) * LATITUDE: -13.082500 * LONGITUDE: 121.788000 * DATE/TIME: 2001-05-03T21:05:00 * ELEVATION: -1783.0 m * Recovery: 40.73 m * LOCATION: Timor Sea * CAMPAIGN: MD122 (IMAGES VII - WEPAMA) * BASIS: Marion Dufresne (1995) (URI: https://en.wikipedia.org/wiki/Marion_Dufresne_(1994)) * METHOD/DEVICE: Giant piston corer (GPC) MD97-2129 (MD972129) * LATITUDE: -10.789000 * LONGITUDE: 138.718000 * Recovery: 6.24 m * CAMPAIGN: MD106 (IMAGES III - IPHIS) (URI: http://www.ifremer.fr/sismer/UK/catal/campagne/campagnea.htql?crno=97200010) * BASIS: Marion Dufresne (1995) (URI: https://en.wikipedia.org/wiki/Marion_Dufresne_(1994)) * METHOD/DEVICE: Calypso Corer (CALYPSO) MD97-2130 (MD972130) * LATITUDE: -12.266000 * LONGITUDE: 138.748000 * Recovery: 8.05 m * CAMPAIGN: MD106 (IMAGES III - IPHIS) (URI: http://www.ifremer.fr/sismer/UK/catal/campagne/campagnea.htql?crno=97200010) * BASIS: Marion Dufresne (1995) (URI: https://en.wikipedia.org/wiki/Marion_Dufresne_(1994)) * METHOD/DEVICE: Calypso Corer (CALYPSO) MD97-2131 (MD972131) * LATITUDE: -12.066000 * LONGITUDE: 138.749000 * Recovery: 13.59 m * CAMPAIGN: MD106 (IMAGES III - IPHIS) (URI: http://www.ifremer.fr/sismer/UK/catal/campagne/campagnea.htql?crno=97200010) * BASIS: Marion Dufresne (1995) (URI: https://en.wikipedia.org/wiki/Marion_Dufresne_(1994)) * METHOD/DEVICE: Calypso Corer (CALYPSO) MD97-2132 (MD972132) * LATITUDE: -12.313000 * LONGITUDE: 138.978000 * Recovery: 15.2 m * CAMPAIGN: MD106 (IMAGES III - IPHIS) (URI: http://www.ifremer.fr/sismer/UK/catal/campagne/campagnea.htql?crno=97200010) * BASIS: Marion Dufresne (1995) (URI: https://en.wikipedia.org/wiki/Marion_Dufresne_(1994)) * METHOD/DEVICE: Calypso Corer (CALYPSO) MD97-2133 (MD972133) * LATITUDE: -12.392000 * LONGITUDE: 140.338000 * Recovery: 6.56 m * CAMPAIGN: MD106 (IMAGES III - IPHIS) (URI: http://www.ifremer.fr/sismer/UK/catal/campagne/campagnea.htql?crno=97200010) * BASIS: Marion Dufresne (1995) (URI: https://en.wikipedia.org/wiki/Marion_Dufresne_(1994)) * METHOD/DEVICE: Calypso Corer (CALYPSO) TAEAC_BGC6 * LATITUDE: -17.030000 * LONGITUDE: 125.000000 * METHOD/DEVICE: Speleothem sample (SPS) * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: speleothem. TAEAC_BGC14 * LATITUDE: -17.030000 * LONGITUDE: 125.000000 * METHOD/DEVICE: Speleothem sample (SPS) * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: speleothem. TAEAC_Black_Springs * LATITUDE: -15.630000 * LONGITUDE: 126.380000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_BR-BU * LATITUDE: -15.466500 * LONGITUDE: 129.785000 * ELEVATION: 7.0 m * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_BSP * LATITUDE: -15.630000 * LONGITUDE: 126.380000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_BSP02 * LATITUDE: -15.630000 * LONGITUDE: 126.390000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_BW01 * LATITUDE: -12.657000 * LONGITUDE: 141.998000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_BWIL2 * LATITUDE: -12.657000 * LONGITUDE: 141.998000 * ELEVATION: 30.0 m * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_Cap_St_Lambert * LATITUDE: -14.310000 * LONGITUDE: 127.760000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_Cape_Flattery * LATITUDE: -15.080000 * LONGITUDE: 145.240000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_Cobourg_Peninsula * LATITUDE: -11.280000 * LONGITUDE: 132.200000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_Core89_1 * LATITUDE: -13.810000 * LONGITUDE: 136.870000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_CT * LATITUDE: -15.800000 * LONGITUDE: 128.800000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_Dune_W_Cape_York * LATITUDE: -12.280000 * LONGITUDE: 141.720000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_E_Alligator_R * LATITUDE: -12.560000 * LONGITUDE: 133.110000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_ELZ02 * LATITUDE: -16.400000 * LONGITUDE: 126.130000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_Fitzroy_Estuary * LATITUDE: -17.310000 * LONGITUDE: 123.570000 * METHOD/DEVICE: Coastal coring/sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: coastal. TAEAC_FRN02 * LATITUDE: -15.940000 * LONGITUDE: 126.280000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_G5_6_149P2 * LATITUDE: -9.000000 * LONGITUDE: 128.000000 * METHOD/DEVICE: Marine sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: marine_core. TAEAC_GC_10A * LATITUDE: -13.070000 * LONGITUDE: 140.200000 * METHOD/DEVICE: Marine sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: marine_core. TAEAC_Gilbert_River * LATITUDE: -17.320000 * LONGITUDE: 141.750000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_Gilwah * LATITUDE: -20.130000 * LONGITUDE: 127.410000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_Girraween * LATITUDE: -12.520000 * LONGITUDE: 131.080000 * ELEVATION: 20.0 m * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_HAY * LATITUDE: -13.600000 * LONGITUDE: 131.530000 * METHOD/DEVICE: Dendrochronology * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: dendro. TAEAC_Karumba * LATITUDE: -17.690000 * LONGITUDE: 140.420000 * METHOD/DEVICE: Coastal coring/sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: coastal. TAEAC_King_River * LATITUDE: -15.520000 * LONGITUDE: 128.120000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_KNI_51_1 * LATITUDE: -15.180000 * LONGITUDE: 128.370000 * METHOD/DEVICE: Speleothem sample (SPS) * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: speleothem. TAEAC_KNI_51_3 * LATITUDE: -15.180000 * LONGITUDE: 128.370000 * METHOD/DEVICE: Speleothem sample (SPS) * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: speleothem. TAEAC_KNI_51_11 * LATITUDE: -15.180000 * LONGITUDE: 128.370000 * ELEVATION: 100.0 m * METHOD/DEVICE: Speleothem sample (SPS) * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: speleothem. TAEAC_KOR * LATITUDE: -12.650000 * LONGITUDE: 134.320000 * METHOD/DEVICE: Dendrochronology * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: dendro. TAEAC_Lake_Lewis * LATITUDE: -22.920000 * LONGITUDE: 132.530000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_Lake_Woods * LATITUDE: -17.850000 * LONGITUDE: 133.500000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_LIT * LATITUDE: -13.290000 * LONGITUDE: 130.850000 * METHOD/DEVICE: Dendrochronology * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: dendro. TAEAC_MAN * LATITUDE: -12.050000 * LONGITUDE: 134.250000 * METHOD/DEVICE: Dendrochronology * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: dendro. TAEAC_MAR2 * LATITUDE: -13.409000 * LONGITUDE: 135.774000 * ELEVATION: 50.0 m * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_MARR02 * LATITUDE: -17.070000 * LONGITUDE: 139.490000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_MARR04 * LATITUDE: -17.070000 * LONGITUDE: 139.490000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_Mary_River * LATITUDE: -12.480000 * LONGITUDE: 131.680000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_Mulan * LATITUDE: -20.210000 * LONGITUDE: 127.440000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_MUR * LATITUDE: -11.500000 * LONGITUDE: 132.700000 * METHOD/DEVICE: Dendrochronology * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: dendro. TAEAC_Nott1996_01 * LATITUDE: -13.150000 * LONGITUDE: 130.680000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_Nott1996_02 * LATITUDE: -13.420000 * LONGITUDE: 132.420000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_Nott1999_01 * LATITUDE: -14.320000 * LONGITUDE: 132.470000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_Pandanus_Yard * LATITUDE: -17.690000 * LONGITUDE: 139.930000 * METHOD/DEVICE: Coastal coring/sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: coastal. TAEAC_Parnkupirti * LATITUDE: -20.250000 * LONGITUDE: 127.500000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_PC * LATITUDE: -13.610000 * LONGITUDE: 132.210000 * METHOD/DEVICE: Dendrochronology * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: dendro. TAEAC_PL04_05 * LATITUDE: -15.540000 * LONGITUDE: 128.250000 * METHOD/DEVICE: Fluvial coring/channel sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: fluvial. TAEAC_SAN1a * LATITUDE: -11.120000 * LONGITUDE: 142.350000 * ELEVATION: 15.0 m * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_SAN1b * LATITUDE: -11.120000 * LONGITUDE: 142.360000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_Shelburne_Bay * LATITUDE: -11.920000 * LONGITUDE: 142.910000 * METHOD/DEVICE: Dune coring/sand pit sampling * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: aeolian. TAEAC_SkullSprings * LATITUDE: -15.210000 * LONGITUDE: 125.728000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_TableTopSwamp_a * LATITUDE: -13.178000 * LONGITUDE: 130.746000 * ELEVATION: 200.0 m * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_TableTopSwamp_b * LATITUDE: -13.178000 * LONGITUDE: 130.746000 * ELEVATION: 200.0 m * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_TIWI * LATITUDE: -11.710000 * LONGITUDE: 130.830000 * METHOD/DEVICE: Dendrochronology * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: dendro. TAEAC_Walala_Core_2 * LATITUDE: -15.680000 * LONGITUDE: 137.030000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_WCC99_04 * LATITUDE: -19.170000 * LONGITUDE: 127.800000 * ELEVATION: 330.0 m * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_WCS01 * LATITUDE: -17.070000 * LONGITUDE: 139.490000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. TAEAC_WS01 * LATITUDE: -17.070000 * LONGITUDE: 139.490000 * METHOD/DEVICE: Lake sediment coring * COMMENT: Hydrological and geochronological data compiled from published sources. Original archive type: lake. 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): Identification (ID) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: unique row label Event label (Event) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: sample; archive/site identifier LATITUDE (Latitude) * GEOCODE * PI: Wall, Alexander Forster (alexfwall@gmail.com) LONGITUDE (Longitude) * GEOCODE * PI: Wall, Alexander Forster (alexfwall@gmail.com) ELEVATION [m a.s.l.] (Elevation) * GEOCODE * PI: Wall, Alexander Forster (alexfwall@gmail.com) Location (Location) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: site name or locality string Area/locality (Area) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: geographic region Country (Country) * PI: Wall, Alexander Forster (alexfwall@gmail.com) Archive (Archive) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: archive type (lake, speleothem, marine core, etc.) Age, minimum/young [ka] (Age min) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: lower bound of interpreted interval (uncalibrated, if applicable) Age, minimum/young, error [±] (Age min e) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: reported uncertainty Age, maximum/old [ka] (Age max) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: upper bound of interpreted interval Age, maximum/old, error [±] (Age max e) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: reported uncertainty Calendar age, minimum/young [ka BP] (Cal age min) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: calibrated/translated earliest age Calendar age, maximum/old [ka BP] (Cal age max) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: calibrated/translated latest age Time resolution [ka] (Time res) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: archive temporal resolution (ka/sample) Number of proxies [#] (Proxies) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: number of proxies analysed Interpretation (Interpretation) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: water availability categorical interpretation (-2 = very arid, -1 = arid, 1 = hydric, and 2 = very hydric) Evidence (Evidence) * PI: Wall, Alexander Forster (alexfwall@gmail.com) * COMMENT: supporting proxy evidence Reference/source (Reference) * PI: Wall, Alexander Forster (alexfwall@gmail.com) License: Creative Commons Attribution 4.0 International (CC-BY-4.0) (URI: https://creativecommons.org/licenses/by/4.0/) (License comes into effect after moratorium ends) Size: 3418 data points */ ID Event Latitude Longitude Elevation [m a.s.l.] Location Area Country Archive Age min [ka] Age min e [±] Age max [ka] Age max e [±] Cal age min [ka BP] Cal age max [ka BP] Time res [ka] Proxies [#] Interpretation Evidence 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)