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作 者:Marina V.SOTNIKOVA Irina V.FORONOVA
机构地区:[1]Geological Institute of Russian Academy of Sciences,Moscow,Russia [2]V.S.Sobolev Institute of Geology and Mineralogy,Siberian Branch of Russian Academy of Sciences,Novosibirsk,Russia
出 处:《Integrative Zoology》2014年第4期517-530,共14页整合动物学(英文版)
基 金:We gratefully acknowledge Nikolai Ovodov for providing additional data on the material from Kurtak archaeological area.We thank Alexey Tesakov for scientific discussion that critically improved the paper.We are also indebted to Katya Firsova and Igor Foronov,who kindly prepared the design of figures for the purpose of this study.M.Sotnikova acknowledges the financial support from the Russian Foundation for Basic Research,project 12-05-00-904a.
摘 要:A lion-like pantherine felid is described as Panthera(Leo)fossilis from the late Early Pleistocene sediments of the Kuznetsk Basin(Western Siberia,Russia).The find of P.fossilis first recorded in Asia considerably extends the current notion of the eastward expansion of the most ancient lions.The Siberian lion is geologically the oldest form and is dimensionally among the largest members of the group of fossil lions on the Eurasian continent.Although known by mandibular remains only,it is readily distinguished from Panthera(Leo)spelaea by a heavy built mandibular corpus with rectangular profile in the cheek teeth area,a deep,well-outlined and narrow anterior section of the masseteric fossa,and a largeр4 supported by a big unreduced anterior root.The Siberian lion shares these features with the European Middle Pleistocene P.fossilis and the American Late Pleistocene P.(Leo)atrox,which suggests their close relationship.P.atrox originated from P.fossilis and was isolated in North America south of the Late Pleistocene ice sheets.This explains why the American lion has retained more primitive features than the coeval Eurasian cave lion P.(L.)spelaea.
关 键 词:Early Pleistocene evolution Panthera fossilis relationships Western Siberia
分 类 号:P53[天文地球—古生物学与地层学]
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