Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1044927 | Quaternary International | 2006 | 17 Pages |
Abstract
During a series of expeditions organized by CERPOLEX/Mammuthus to the Taimyr region in northern Siberia several mammoth (Mammuthus primigenius) carcasses were discovered and subsequently excavated and studied. The oldest specimen is the Arilakh Mammoth (ca. 55,800Â BP). Much younger are the Jarkov Mammoth (ca. 20,380Â BP) and the Fishhook Mammoth (ca. 20,620Â BP), and still much younger are well-preserved Holocene mammoth remains (<10,000Â BP). Some paleobotanical data and descriptions of accompanying fauna provide insight into the ecology of the region during Late Pleistocene times. The faunal collapse at the end of the Pleistocene seems to be the result of increasing temperatures, greater humidity, increased snow cover, formation of insulating plant layers, later thawing of the soil, and a lower herbivore density amplifying the climatic effects.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Dick Mol, Alexei Tikhonov, Johannes van der Plicht, Ralf-Dietrich Kahlke, Regis Debruyne, Bas van Geel, Guido van Reenen, Jan Peter Pals, Christian de Marliave, Jelle W.F. Reumer,