Pleistocene Megafauna From Eastern Beringia: Paleoecological And Paleoenvironmental Interpretations Of Stable Carbon And Nitrogen Isotope And Radiocarbon Records (vol 261, Pg 30, 2008)

By K. Fox-Dobbs, P. Koch. 2008

184 citations recorded by the source corpus.

Subfields: Anthropology, Ecology, Paleontology

View Paper: https://www.semanticscholar.org/paper/078bb6551f820adfd701d77b68d7fd8acc2cb6be

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Citations in the corpus

Ice-age megafauna in Arctic Alaska: extinction, invasion, survival (2013, background): “The non-synchroneity of d15N in different megafaunal species on the North Slope contrasts with the synchroneity observed in Interior Alaska, where they are attributed to shifts in vegetation driven by regional climate change (Fox-Dobbs et al., 2008).”
Population Demography and Genetic Diversity in the Pleistocene Cave Lion (2015, background): “Stable isotope analysis shows that both scimitar-tooth cats and cave lions in Beringia appear to mainly have been either generalists or horse/bison specialists (Fox-Dobbs et al., 2008).”
The problem of isotopic baseline: Reconstructing the diet and trophic position of fossil animals (2011, background): “, 1993) or evaluate various aspects of trophic ecology before anthropogenic disturbance or in response to rapid climate change (Fox-Dobbs et al., 2008).”
Isotopic evidence for dietary ecology of cave lion (Panthera spelaea) in North-Western Europe: Prey choice, competition and implications for extinction (2011, background): “The isotopic pattern seen between herbivorous species con ﬁ rms the results presented previously and is most likely due to different dietary choice among the plants available in the steppe tundra (Bocherens et al., 1997; Bocherens, 2003; Fox-Dobbs et al., 2008).”
Extinction chronology of the woolly rhinoceros Coelodonta antiquitatis in the context of late Quaternary megafaunal extinctions in northern Eurasia (2012, background): “…(Harington, 2011), when the Bering Straits would have been flooded due to high sea levels, but others such as short-faced bear Arctodus simus, sabretooth Homotherium serum and helmeted musk ox Bootherium bombifrons are from the Last Glacial, within radiocarbon dating range (Fox-Dobbs et al., 2008).”
Carbon isotope compositions of terrestrial C3 plants as indicators of (paleo)ecology and (paleo)climate (2010, background): “3, point “c1”; 30), or lichen consumption (31).”
Late Quaternary megafaunal extinctions on the continents: a short review (2015, background): “A third megaherbivore, the woolly rhinoceros, shows yet another pattern, with complex range shifts at various times, much less marked response to the LGM and a progressive contraction of range, with the last populations probably surviving in north-eastern Siberia prior to global extinction.”