A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China

By E. Eizirik, S. O'Brien, O. Madsen, M. Scally, C. Douady, E. Teeling, Oliver A. Ryder, M. Stanhope, W. W. D. Jong. Science, 2001

3,191 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science, Ecology

View Paper: https://www.semanticscholar.org/paper/cb25aeb6d8ca024394833c5e4c2c89bc2be68002

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Citations in the corpus

The repeated replacement model – Rapid climate change and population dynamics in Late Pleistocene Europe (2012, methodology): “Hulu ages (Wang et al., 2001) according to the Greenland GISP2Hulu time-scale Weninger and Jöris (2008).”
High plant endemism in China is partially linked to reduced glacial‐interglacial climate change (2016, background): “Also, several studies reported high millennial-scale variability in monsoon strength and precipitation in China across the Late Pleistocene and Holocene (Wang et al., 2001, 2008).”
Climatic Fluctuations and Early Farming in West and East Asia (2011, background): “Among the eastern sites, Hulu Cave, near Nanjing (Wang et al. 2001), produced a long paleoclimatic curve that best fits the GISP2 ice core.”
Wet periods in northeastern Brazil over the past 210 kyr linked to distant climate anomalies (2004, background): “(2) Top and bottom sub-samples were analysed whenever possible in order to check for stratigraphic order.”
New modeling of the Vostok ice flow line and implication for the glaciological chronology of the Vostok ice core (2004, methodology): “Moreover this event is synchronous with Dansgaard-Oeschger event number 10 [ Yiou et al. , 1997], an event that has been identified in records from speleothems [ Wang et al. , 2001; Genty et al. , 2003] and accurately dated by the uranium-thorium method.”
Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years (2008, background): “Our data further indicate that (1) the duration and frequency of the millennial-scale events change systematically throughout the course of a glacial period, and (2) that the general nature of these changes is reproducible for the last two glacial periods.”
Astronomical and glacial forcing of East Asian summer monsoon variability (2015, neutral): “…and isotopic composition of speleothems, although the extent to which these proxies can be interpreted as a pure summer monsoon indicator is still debated (Wang et al., 2001, 2008b; Cheng et al., 2009, 2012; Clemens et al., 2010; Dayem et al., 2010; Pausata et al., 2011; Maher and Thompson, 2012).”