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重庆万州盐井沟地区黄昏爪兽(爪兽科,奇蹄目)化石新发现
  • ISSN号:1001-7410
  • 期刊名称:《第四纪研究》
  • 时间:0
  • 分类:Q911.5[天文地球—古生物学与地层学;生物学—古生物学] Q915.877[天文地球—古生物学与地层学;生物学—古生物学]
  • 作者机构:[1]重庆中国三峡博物馆三峡古人类研究所,重庆400015, [2]重庆市地质调查院,重庆401122, [3]云阳县文物保护管理所,重庆404500, [4]重庆市地勘局208水文地质工程地质队,重庆400700
  • 相关基金:国家自然科学基金重点项目(批准号:41430102)、国家重点基础研究发展规划项目(973项目)(批准号:2012CB821906)和第一批重庆市“青年文化优才”培养计划项目(批准号:2014QNWHYC01)共同资助.致谢 参加盐井沟大垭口调查与发掘的还有中国科学院古脊椎动物与古人类研究所的黄万波研究员、河南省文物考古研究所的张小虎博士、常州市博物馆的张华、万州区博物馆的别令芬以及巫山县博物馆的裴健;万州区新田镇高家村村长姜元顺提供化石线索并协助发掘,张真龙和龙代清修理化石;对审稿专家和编辑部杨美芳老师提出的修改意见深表感谢.
中文摘要:

黄昏爪兽(Hesperotherium)是我国早更新世代表物种之一,因发现标本稀少,其形态特征和灭绝时间是存疑的。重庆市万州区盐井沟大垭口地点发现了多件Hesperotherium化石,其中多数骨骼属首次发现,新材料增加了我们对该类动物的骨骼形态学的认识,其后肢骨骼在进化过程中较为保守,可能正是这种进化过程中的保守性导致其不能适应第四纪多变的气候环境,最终灭绝。同时通过对已知含Hesperotherium动物群的分析,认为Hesperotherium可以作为早更新世早-中期的代表物种,对应于邱占祥命名的NCMQ 1或欧洲的维拉方中-晚期。

英文摘要:

Chalicothere is one of the most peculiar mammals in Pleistocene, characterized by bifid claws but not hooves as other ungulates. Hesperotherium is the most derived genus among Chalicotheriinae, and its morphology and extinction is still controversial. New specimens of this genus have been found from the Dayakou locality(30°37'37.1"N, 108°26'56.9"E) in Yanjinggou area, Wanzhou District, Chongqing Municipality, represented by four cheek teeth and ten phalanxes of pes, adding to our knowledge about chalicothere anatomy. The cheek teeth resemble Hesperotherium sinense from other localities in most respects. P2 and P3 lack the protoconule, and their paracone and metacone are not obviously separated on the ectoloph. The m2 is double V-shaped, and the "metastylid" will be fused with metaconid after worn. Some of the postcranial bones of this animal are discovered for the first time. The proximal facet of the pes proximal phalanx is large and inclines extremely in the dorsal direction. The pes medial phalanx is much depressed in the ulnar-radial section, with equally developed proximal volar and dorsal process. The pes distal phalanxes from Dayakou are broken, but they show the typical feature of chalicotheres known as the bifid claw. The morphology of pes phalanxes is similar with early chalicotheriines except the size somewhat larger or smaller, which indicating the evolution of the pes is conservative. Probably for this conservatism, chalicothere couldn't adapt to the climate fluctuation and became extinct in Early Pleistocene. By now, Hesperotherium fossils have been found from 17 Early Pleistocene localities in China and Myanmar(in figure 4). The chronological analyses show that all these localities should be correlated to early to middle Early Pleistocene. In this view, we propose that Hesperotherium can be a representative genus of early to middle Early Pleistocene, equal to NCMQ(North China Mammal Quaternary)1 named by Zhanxiang Qiu or mid-late Villafranchian of Europe.

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期刊信息
  • 《第四纪研究》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国科学院地质与地球物理研究所 中国第四纪研究委员会
  • 主编:郭正堂
  • 地址:北京9825信箱
  • 邮编:100029
  • 邮箱:dsj@mail.igcas.ac.cn dsjs@mail.igcas.ac.cn
  • 电话:010-82998119
  • 国际标准刊号:ISSN:1001-7410
  • 国内统一刊号:ISSN:11-2708/P
  • 邮发代号:82-428
  • 获奖情况:
  • 1996年被国务院学位委员会地球物理及地质学科评议...,2001年入中国期刊方阵,2007年获中国科学院出版基金科技期刊排行榜三等奖
  • 国内外数据库收录:
  • 美国化学文摘(网络版),英国动物学记录,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:17826