Glacial and deglacial climatic patterns in Australia and surrounding regions from 35 000 to 10 000 years ago reconstructed from terrestrial and near-shore proxy data

• Published in: Quaternary Science Reviews
• Main Authors: Williams, Martin A, Cook, Ellyn, van der Kaars, Willem Alexander (Sander), Barrows, Timothy, Shulmeister, J, Kershaw, Peter
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Pergamon-Elsevier Ltd
• Subjects: Keywords: Antarctic cold reversals; Antarctica; Australia; Chironomids; Climatic data; Climatic signals; Convergence zones; Deglacial; Deglaciations; Extreme flood events; Glacial advances; Indonesia; Intertropical convergence zone; Last Glacial Maximum; Late quate; Antarctic; The Antarctic; New Zealand; Antarc*
• Online Access: http://hdl.handle.net/1885/56021; https://doi.org/10.1016/j.quascirev.2009.04.020; https://openresearch-repository.anu.edu.au/bitstream/1885/56021/5/glacial_and_deglacial_climatic_patterns_in_aus.pdf.jpg; https://openresearch-repository.anu.edu.au/bitstream/1885/56021/7/01_Williams_Glacial_and_deglacial_climatic_2009.pdf.jpg

This study forms part of a wider investigation of late Quaternary environments in the Southern Hemisphere. We here review the terrestrial and near-shore proxy data from Australia, Indonesia, Papua New Guinea (PNG), New Zealand and surrounding oceans during 35-10 ka, an interval spanning the lead-up to the Last Glacial Maximum (LGM), the LGM proper (21 ± 2 ka), and the ensuing deglaciation. Sites selected for detailed discussion have a continuous or near continuous sedimentary record for this time interval, a stratigraphically consistent chronology, and one or more sources of proxy climatic data. Tropical Australia, Indonesia and PNG had LGM mean annual temperatures 3-7 °C below present values and summer precipitation reduced by at least 30%, consistent with a weaker summer monsoon and a northward displacement of the Intertropical Convergence Zone. The summer monsoon was re-established in northwest Australia by 14 ka. Precipitation in northeast Australia was reduced to less than 50% of present values until warmer and wetter conditions resumed at 17-16 ka, followed by a second warmer, wetter phase at 15-14 ka. LGM temperatures were up to 8 °C lower than today in mainland southeast Australia and up to 4 °C cooler in Tasmania. Winter rainfall was much reduced throughout much of southern Australia although periodic extreme flood events are evident in the fluvial record. Glacial advances in southeast Australia are dated to 32 ± 2.5, 19.1 ± 1.6 and 16.8 ± 1.4 ka, with periglacial activity concentrated towards 23-16 ka. Deglaciation was rapid in the Snowy Mountains, which were ice-free by 15.8 ka. Minimum effective precipitation in southern Australia was from 14 to 12 ka. In New Zealand the glacial advances date to ∼28, 21.5 and 19 ka, with the onset of major cooling at ∼28 ka, or well before the LGM. There is no convincing evidence for a Younger Dryas cooling event in or around New Zealand, but there are signs of the Antarctic Cold Reversal in and around New Zealand and off southern Australia. There remain unresolved ...