Premium
A glacial cryptic refuge in south‐east Australia: human occupation and mobility from 36 000 years ago in the Sydney Basin, New South Wales
Author(s) -
WILLIAMS ALAN N.,
ATKINSON FENELLA,
LAU MICHELLE,
TOMS PHILLIP S.
Publication year - 2014
Publication title -
journal of quaternary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.142
H-Index - 94
eISSN - 1099-1417
pISSN - 0267-8179
DOI - 10.1002/jqs.2742
Subject(s) - holocene , last glacial maximum , population , pleistocene , glacial period , archaeology , subsistence agriculture , geography , physical geography , structural basin , geology , paleontology , demography , sociology , agriculture
Excavations across a source‐bordering dune overlooking the Hawkesbury River in north‐west Sydney, Australia, suggest initial occupation of the region by at least 36 ka, with variable but uninterrupted use until the early Holocene; following abandonment, the site was then re‐occupied by ∼3 ka. Along with a handful of other sites, the results provide the earliest reliable evidence of permanent regional populations within south‐eastern Australia, and support a model in which early colonizers followed the coastal fringe with forays along the main river systems. The evidence is consistent with the demographic model of Williams, 2013 ( Proceedings of the Royal Society Series B 280 : 20130486), which suggested low, but established regional populations before the Last Glacial Maximum (LGM), a population nadir following the LGM and increasing use of the region from ∼12 to 8 ka. The site exhibits increased use at the onset and peak of the LGM, and provides an example of a cryptic refuge as defined by Smith, 2013 ( The Archaeology of Australia's Deserts . Cambridge University Press: New York). Specifically, changing artefact densities and attributes show the site was used repeatedly, but for shorter periods through this time, and suggest it formed one of a series of key localities in a point‐to‐point (rather than home‐base) subsistence strategy. This strategy was maintained until the site's abandonment in the early Holocene, despite changing population and climatic conditions through the Terminal Pleistocene.