Variability in the Chronology of Late Holocene Aboriginal Occupation on the Arid Margin of Southeastern Australia

2002 ◽  
Vol 29 (4) ◽  
pp. 351-363 ◽  
Author(s):  
Simon J. Holdaway ◽  
Patricia C. Fanning ◽  
Martin Jones ◽  
Justin Shiner ◽  
Dan C. Witter ◽  
...  
Keyword(s):  
Late Holocene ◽  
Southeastern Australia

Geomorphic evidence for mid–late Holocene higher sea level from southeastern Australia

2010 ◽  
Vol 221 (1-2) ◽  
pp. 13-22 ◽  
Author(s):  
Adam D. Switzer ◽  
Craig R. Sloss ◽  
Brian G. Jones ◽  
Charles S. Bristow
Keyword(s):  
Sea Level ◽  
Late Holocene ◽  
Southeastern Australia

scholarly journals A late Holocene onset of Aboriginal burning in southeastern Australia

Geology ◽  
2016 ◽  
Vol 44 (2) ◽  
pp. 131-134 ◽  
Author(s):  
Eric W. Portenga ◽  
Dylan H. Rood ◽  
Paul Bishop ◽  
Paul R. Bierman
Keyword(s):  
Late Holocene ◽  
Southeastern Australia ◽  
Aboriginal Burning

scholarly journals Development of a Training Set of Contemporary Salt-Marsh Foraminifera for Late Holocene Sea- Level Reconstructions in southeastern Australia

10.5334/oq.93 ◽  
2021 ◽  
Vol 7 (1) ◽  
pp. 4
Author(s):  
Sophie Williams ◽  
Ed Garrett ◽  
Patrick Moss ◽  
Rebecca Bartlett ◽  
Roland Gehrels
Keyword(s):  
Salt Marsh ◽  
Sea Level ◽  
Late Holocene ◽  
Training Set ◽  
Southeastern Australia ◽  
Holocene Sea Level

Holocene Vegetation and Paleoclimatic and Paleomagnetic History from Lake Johnston, Tasmania

2001 ◽  
Vol 56 (2) ◽  
pp. 264-274 ◽  
Author(s):  
Sharon A. Anker ◽  
Eric A. Colhoun ◽  
Charles E. Barton ◽  
Mike Peterson ◽  
Mike Barbetti
Keyword(s):  
Magnetic Susceptibility ◽  
Master Curve ◽  
Late Holocene ◽  
Climate Changes ◽  
Holocene Climate ◽  
Radiocarbon Dates ◽  
Southeastern Australia ◽  
Lagarostrobos Franklinii ◽  
Glacial Relict ◽  
Vegetation And Climate

AbstractLake Johnston cirque contains some of the best subalpine rainforest in Tasmania. Pollen from the sediments shows Lagarostrobos franklinii, which presently reaches 1040 m, may be a glacial relict. Nothofagus cunninghamii–Nothofagus gunnii subalpine rainforest developed between 9000 and 6000 14C yr B.P., with a maximum at 8700 14C yr B.P. After 6000 14C yr B.P. Nothofagus gunnii became more important, and from 3600 14C yr B.P. sclerophyll and heath components increased. Partial burning of the catchment occurred periodically. Early Holocene climate was warmer and wetter than late Holocene climate. The vegetation and climate changes are similar to those recorded from western South Island New Zealand and Chile. Radiocarbon dates give a sedimentation rate of 0.43 mm/yr. Cores are correlated by magnetic susceptibility. Magnetic ages are assigned by matching with the 14C-dated secular variation master curve for southeastern Australia. Magnetic ages are consistent with the 14C chronology when the former are adjusted by 350 years.

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