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甘肃临夏盆地晚中新世杨家山动物群的瞪羚化石
  • 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]中国科学院古脊椎动物与古人类研究所,中国科学院脊椎动物演化与人类起源重点实验室,北京100044, [2]中国科学院大学,北京100049
  • 相关基金:中国科学院战略性先导科技专项项目(批准号:XDB03020104)、国家自然科学基金重点项目(批准号:41430102)和国家重点基础研究发展规划项目(973项目)(批准号:2012CB821906)共同资助
作者: 李刈昆[1,2]
中文摘要:

文章记述了甘肃临夏盆地晚中新世杨家山动物群的瞪羚(Gazella)化石,将临夏材料归为保德瞪羚(Gazella paotehensis)、高氏瞪羚相似种(G.cf.gaudryi)和瞪羚未定种(G.sp.).G.paotehensis为有效种,与G.gaudryi区别在于G.paotehensis两角心分散度大,表面发育较深纵沟;与G.dorcadoides区别在于G.paotehensis角心向后外方伸出角度较高,侧视倾斜度小,脑颅部从额项缝开始呈弧形向后下方弯曲.依据临夏的瞪羚化石组合推测杨家山动物群的生活环境可能为温带开阔草原,有灌木丛为典型食叶者食用.依据脑颅轮廓,G.paotehensis应归入短头型,验证了G.paotehensis可能是G.blacki祖先的观点.

英文摘要:

Fossils of Gazella unearthed from the Linxia Basin, Gansu Province are studied in this paper.The fossils localities, Baihuacun(LX0205,35°23'43.2"N, 103°29'45.2"E) and Shilei(LX0031, 35°25'19.7"N, 103°27'30.3"E), locate in Guanghe County, Linxia Hui Autonomous Prefecture, Gansu Province.The fossiliferous layers correspond to the upper part of the Late Miocene Liushu Formation, and the associated fauna is indentified as Yangjiashan fauna.Seven individuals, including six skulls, one horn core, two half-mandibles and stylohyoids, are described here and can be classified into Gazella paotehensis, Gazella cf.gaudryi and Gazella sp.three species.Although Gazella fossils are very common in the formations from Late Miocene to Pleistocene, previously reported materials are usually isolated teeth and horn cores or have undergone diagenetic deformations, especially for those from Late Miocene.Due to above reasons, Late Miocene gazelles are confusing in the classifications.The materials from the Linxia basin belong to G.gaudryi type, different from G.dorcadoides type in having mesodont teeth with ribs on the metacones of M1 and M2, and longer premolar rows.G.paotehensis is viewed as a valid species, which is a small-sized, short braincased Gazella, similar to G.gaudryi and G.dorcadoides in size.G.paotehensis differs from G.gaudryi in having more divergent horn cores with developed longitudinal grooves, G.paotehensis differs from G.dorcadoides in having less inclined horn cores in side view and more slowly curved down cranial roof from the frontal-parietal suture.The maximum width of the cross section at the horn base locates behind the middle in G.cf.gaudryi, which is different from that in G.gaudryi. The material identified as G.sp.differs from former two species in having more upright horn cores in side view and narrow braincase, which is similar to G.cf.lydekkeri from Lantian in shape, and similar to G.lydekkeri from Siwalik in size.Gansu was once thought to be open environments, which is typica

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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