The latest woolly mammoths (Mammuthus primigenius Blumenbach) in Europe and Asia: a review of the current evidence

By A. Stuart, L. Sulerzhitsky, L. Orlova, Y. Kuzmin, A. Lister. 2002

145 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science, Paleontology

View Paper: https://www.semanticscholar.org/paper/9c33028ff6c13afa045bd7e5c813b5a70f8e1545

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Citations in the corpus

Extinction chronology of the cave lion Panthera spelaea (2011, background): “Woolly mammoth M. primigenius also underwent a drastic reduction in geographical range within the LGI, at ca. 13.6 cal ka BP, soon after the beginning of the Allerød (Greenland Interstadial GI-1aec) (Stuart et al., 2002; Stuart and Lister, 2007).”
The impact of climate change on large mammal distribution and extinction: Evidence from the last glacial/interglacial transition (2008, unknown): “In earlier papers [22,23] we highlighted two taxa, woolly mammoth Mammuthus primigenius and giant”
Extinction chronology of the woolly rhinoceros Coelodonta antiquitatis in the context of late Quaternary megafaunal extinctions in northern Eurasia (2012, background): “These have made it possible to construct detailed chronologies for several of the extinct species, including mammoth (Stuart et al., 2002), giant deer (Stuart et al., 2004), cave bear (Pacher and Stuart, 2009) and cave lion (Stuart and Lister, 2011); see also syntheses and other taxa in Lister and…”
Late Quaternary Extinctions: State of the Debate (2006, background): “Comprehensive dating campaigns in Eurasia and the extension of Eurasian steppe biomes in Alaska and the Yukon reveal that the extinction occurred in two pulses (Guthrie 2003, 2004; MacPhee et al. 2002; Stuart et al. 2002, 2004).”
A long-term perspective on ungulate–vegetation interactions (2003, background): “The precise timing of these events is uncertain and the subject of current research (Stuart et al., 2002).”
The ecology and adaptation of Neanderthals during the non-analogue environment of Oxygen Isotope Stage 3 (2005, background): “There was also the disappearance from Europe of the mammoth (Stuart et al., 2002), the best-known cold element of the Late Pleistocene and the megafaunal taxon with the northernmost distribution in Europe during OIS 3 (Ukkonen et al.”
The extinction of woolly mammoth (Mammuthus primigenius) and straight-tusked elephant (Palaeoloxodon antiquus) in Europe (2005, background): “This event occurred soon after, but not coincidentally with the rapid warming that marks the beginning of the Holocene, and can be plausibly correlated with the loss of the steppe-tundra biome and widespread establishment of temperate and boreal forests in mid latitudes and boggy tundra in the far n”
Extinction chronology and palaeobiology of the cave bear (Ursus spelaeus) (2009, background): “…at the end of the Pleistocene (woolly mammoth (Mammuthus primigenius), giant deer (Megaloceros giganteus)) – are now known to have undergone dramatic shifts in distribution and survived in limited areas well into the Holocene (Vartanyan et al. 1993; Stuart et al. 2002, 2004; Stuart & Lister 2007).”
Late Quaternary megafaunal extinctions on the continents: a short review (2015, background): “…to construct detailed chronologies for most of the extinct species and also many of the survivors (Sulerzhitsky and Romanenko, 1997; MacPhee et al., 2002; Stuart et al., 2002, 2004; Stuart and Lister, 2007, 2011, 2012, 2014; Lister and Stuart, 2008; Pacher and Stuart, 2009; Nikolskiy et al., 2011).”
Species-specific responses of Late Quaternary megafauna to climate and humans (2011, unknown): “For woolly mammoth, this pattern is also supported by fossil evidenc”