The Last Glacial Maximum

By Edward S. Buckler, Jim Holland, Peter J. Bradbury, C. Acharya, P. Brown, C. Browne, Elhan Ersoz, Sherry Flint-Garcia, A. García, Jeffrey Glaubitz and 17 more. Science, 2009

3,342 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/265b6f8e5e8afa1cc41e7a44ad7eb80aed7fa752

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In Anthropology

1. D. Woodruff
2. E. Rohling

In Atmospheric Science

1. A. Hall
2. J. Heyman
3. K. Andreassen
4. H. Patton
5. A. Hubbard
6. A. Stroeven
7. M. Winsborrow
8. Gerrit Lohmann

Citations in the corpus

• Biogeography and conservation in Southeast Asia: how 2.7 million years of repeated environmental fluctuations affect today’s patterns and the future of the remaining refugial-phase biodiversity (2010, background): “0 m between 4,850 and 4,450 years ago, and then falling to 0 m at 3 ka (Horton et al. 2005; Sathiamurthy and Voris 2006; Clark et al. 2009; Hanebuth et al. 2009).”
• The Greenland Ice Sheet as a hot spot of phosphorus weathering and export in the Arctic (2016, background): “These ice masses discharged significant quantities of glacial meltwater and associated sediments into the oceans during the glacial period, and during initial deglaciation [Clark et al., 2009].”
• Changing perspectives on regeneration ecology and genetic diversity in western quaking aspen: implications for silviculture (2012, neutral): “Clark, P.U., Dyke, A.S., Shakun, J.D., Carlson, A.E., Clark, J., Wohlfarth, B., Mitrovica, J.X., Hostetler, S.W., and McCabe, A.M. 2009.”
• Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciation (2013, background): “…(Duplessy et al., 1988; Bard et al., 2000; Adkins et al., 2002; Pflaumann, 2003; Peltier, 2004; Gersonde et al., 2005; LynchStieglitz et al., 2007; Clark et al., 2009; Gutjahr and Lippold, 2011; Hesse et al., 2011), the Last Glacial Maximum (LGM, about 21 000 yr before present, hereafter 21 ka…”
• Shifting seas: the impacts of Pleistocene sea‐level fluctuations on the evolution of tropical marine taxa (2015, background): “Low sea levels culminated in coastlines 115–130 m below current level, reaching a minimum during the Last Glacial Maximum (LGM) c. 17–19 ka (Fairbanks, 1989; Hanebuth et al., 2000; Voris, 2000; Bintanja et al., 2005; Bintanja & van de Wal, 2008; Clark et al., 2009).”
• Sea-level probability for the last deglaciation: A statistical analysis of far-field records (2011, background): “These findings were recently confirmed by a re-analysis of datings of glacial retreat evidence (Clark et al., 2009).”
• Consensus between genes and stones in the biogeographic and evolutionary history of Central America (2013, background): “The climatic event that has been most frequently referred to in genetic studies for CA species is the last glacial maximum (LGM) that took place 26,500 to 19,000 years ago (according to Clark et al., 2009).”
• Deglaciation of the Eurasian ice sheet complex (2017, background): “Northern Eurasia was covered by three semi-independent ice sheets that between 26 and 19 ka BP (Clark et al., 2009) coalesced to form a single Eurasian ice sheet complex (EISC) during the last nder the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/). glacial maximum (LGM)…”