The Eurasian mammoth distribution during the second half of the Late Pleistocene and the Holocene: Regional aspects

Based on geographic information (database PALEOFAUNA), in combination with C-14 and other methods of paleo dating (1584 localities, 4033 dates, including 1501 direct dates), we first examined details of changes of mammoth distribution in Eurasia on the whole and in single parts of the range over the...

Full description

Bibliographic Details
Published in:Quaternary International
Main Authors: Puzachenko, A. Yu., Markova, A. K., Kosintsev, P. A., van Kolfschoten, T., van der Plicht, J., Kuznetsova, T. V., Tikhonov, A. N., Ponomarev, D. V., Kuitems, M., Bachura, O. P.
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
ICE-CORE
WRANGEL ISLAND
QUATERNARY MEGAFAUNAL EXTINCTIONS
RHINOCEROS COELODONTA-ANTIQUITATIS
MAMMUTHUS-PRIMIGENIUS BLUM
LAST GLACIAL PERIOD
OXFORD AMS SYSTEM
WOOLLY MAMMOTH
RADIOCARBON-DATES
NORTHERN EURASIA
Wrangel Island
ice core
Siberia
Online Access:https://hdl.handle.net/11370/7589116e-b951-4e60-873c-6470214804d3
https://research.rug.nl/en/publications/7589116e-b951-4e60-873c-6470214804d3
https://doi.org/10.1016/j.quaint.2016.05.019
https://pure.rug.nl/ws/files/53466716/The_Eurasian_mammoth_distribution_during_the_second_half_of_the_Late_Pleistocene_and_the_Holocene.pdf
http://adsabs.harvard.edu/abs/2017QuInt.445.71P
Description
Summary:Based on geographic information (database PALEOFAUNA), in combination with C-14 and other methods of paleo dating (1584 localities, 4033 dates, including 1501 direct dates), we first examined details of changes of mammoth distribution in Eurasia on the whole and in single parts of the range over the last 50ky. The analysis of regional features in the dynamics of mammoth range and the quantity of dated localities acknowledged a leading role of the climatic (environmental) factor in these processes. The maximum size of the Eurasian range, the largest number of remains of mammoths from dated localities and, probably, the maximum total number of population were established for the range of 38.2-8.6 cal ky BP (Denekamp interstadial = Bryansk interstadial). In Western and Central Europe, the increase of population was observed during Huneborg stadial (40.8-38.2 cal ky BP). In eastern Siberia, the maximum population growth occurred in the Last Glacial Maximum (28.6-22.5 cal ky BP), and in Western Siberia - during Deglaciation (22.5-14.7 cal ky BP). The population dynamics at the periphery of the range (Islands of Japan, British Isles, Northern Europe, Southern Siberia and Northern China, and, but to lesser extent, South-Eastern Europe) differs from the dynamics of its main part. The southernmost parts of the range - Southern Siberia and southeastern Europe experienced similar changes. Population dynamics in the Iberian Peninsula was much alike the changes in Western and Central Europe. We suggested that some peripheral populations could periodically be isolated from the populations of the main part of the range. Direct calibrated radiocarbon dates fixed upper boundary of extinction of this species in different parts of range within time interval from 21 (the Iberian Peninsula) to 4 (northeastern Siberia) thousands years BP. The hypotheses about the causes of the dynamics of the area and population of the mammoth in Eurasia, including those related to the extinction of certain genetic lines of a mammoth in the Late ...

Similar Items