High-precision U-series dating of the late Pleistocene – early Holocene rock paintings at Tiger Leaping Gorge, Jinsha River valley, southwestern China

2022 ◽  
Vol 138 ◽  
pp. 105535
Author(s):  
Yun Wu ◽  
Yanuo Jiao ◽  
Xueping Ji ◽  
Paul S.C. Taçon ◽  
Zhijian Yang ◽  
...  
Keyword(s):  
High Precision ◽  
Late Pleistocene ◽  
River Valley ◽  
Early Holocene ◽  
Southwestern China ◽  
Jinsha River ◽  
Rock Paintings

The Influence of climate on artiodactyl size during the Late Pleistocene-Early Holocene of the Southern Levant.

Paléorient ◽  
1997 ◽  
Vol 23 (2) ◽  
pp. 229-247 ◽  
Author(s):  
Pierre Ducos ◽  
L. R. Kolska Horwitz
Keyword(s):  
Late Pleistocene ◽  
Early Holocene ◽  
Southern Levant

scholarly journals Late Pleistocene and Early Holocene aeolian deposits of Tasmania and their climatic implications – Corrigendum

2021 ◽  
pp. 1-2
Author(s):  
Peter D. McIntosh ◽  
Christina Neudorf ◽  
Olav B. Lian ◽  
Adrian J. Slee ◽  
Brianna Walker ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Early Holocene ◽  
Aeolian Deposits

A multi-proxy reconstruction of climate during the late-Pleistocene to early Holocene transition in the northeastern, USA

2021 ◽  
pp. 1-17
Author(s):  
Laurie D. Grigg ◽  
Kevin J. Engle ◽  
Alison J. Smith ◽  
Bryan N. Shuman ◽  
Maximilian B. Mandl
Keyword(s):  
Late Pleistocene ◽  
Climatic Variability ◽  
Warming Trend ◽  
Early Holocene ◽  
Individual Species ◽  
Environmental Preferences ◽  
The North ◽  
Show Evidence ◽  
Dry Conditions ◽  
Components Analysis

Abstract A multiproxy record from Twin Ponds, VT, is used to reconstruct climatic variability during the late Pleistocene to early Holocene transition. Pollen, ostracodes, δ18O, and lithologic records from 13.5 to 9.0 cal ka BP are presented. Pollen- and ostracode-inferred climatic reconstructions are based on individual species’ environmental preferences and the modern analog technique. Principal components analysis of all proxies highlights the overall warming trend and centennial-scale climatic variability. During the Younger Dryas cooling event (YD), multiple proxies show evidence for cold winter conditions and increasing seasonality after 12.5 cal ka BP. The early Holocene shows an initial phase of rapid warming with a brief cold interval at 11.5 cal ka BP, followed by a more gradual warming; a cool, wet period from 11.2 to 10.8 cal ka BP; and cool, dry conditions from 10.8 to 10.2 cal ka BP. The record ends with steady warming and increasing moisture. Post-YD climatic variability has been observed at other sites in the northeastern United States and points to continued instability in the North Atlantic during the final phases of deglaciation.

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