石制品、动物化石

安徽东至华龙洞1号地点中更新统蛇类化石

  • 史静耸 ,
  • 胡海虔 ,
  • 邓国栋 ,
  • 金泽田
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  • 1.中国科学院古脊椎动物与古人类研究所,北京 100044
    2.云南大学生命科学学院脊椎动物演化研究中心,昆明 650500
    3.安徽省东至县文化和旅游局,东至 247200
史静耸,博士,主要从事新生代晚期蛇类多样性、系统发育与功能形态学研究。E-mail: shijingsong@ivpp.ac.cn

收稿日期: 2025-05-08

  修回日期: 2025-05-16

  网络出版日期: 2025-10-13

基金资助

国家自然科学基金(42202014);国家自然科学基金(42430207);国家重点研发计划(2023YFF0804502);国家重点研发计划(2023YFF0804500);中国博士后科学基金(2025MD774141)

Middle Pleistocene snakes from Hualongdong Site Loc.1, in Dongzhi County, Anhui

  • SHI Jingsong ,
  • HU Haiqian ,
  • DENG Guodong ,
  • JIN Zetian
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  • 1. Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044
    2. Center for Vertebrate Evolutionary Biology, Yunnan University, Kunming 650500
    3. Bureau of Culture and Tourism of Dongzhi County, Anhui, Dongzhi 247200

Received date: 2025-05-08

  Revised date: 2025-05-16

  Online published: 2025-10-13

摘要

安徽东至华龙洞是著名的中更新世晚期古人类活动遗址。本文对华龙洞遗址1号地点首次发现的一些蛇类头后骨骼化石进行了报道,通过与现生骨骼标本的对比研究,初步鉴定出3科、5属、6种,均可归为现生类群。并初步归纳了上述蛇类中段躯椎的属级鉴定特征。地理区系分析表明,这些蛇类按生态类型分别属于南中国型、东洋型和季风区型,以东洋热带型的黑网乌梢蛇(相似种)数量居多。该蛇类动物群的发现,表明在中更新世晚期时,安徽东至地区的气候可能较现今更为温暖和湿润。

本文引用格式

史静耸 , 胡海虔 , 邓国栋 , 金泽田 . 安徽东至华龙洞1号地点中更新统蛇类化石[J]. 人类学学报, 2025 , 44(05) : 850 -861 . DOI: 10.16359/j.1000-3193/AAS.2025.0073

Abstract

The Hualongdong Site in Dongzhi County, Anhui Province, is a well-known Middle Pleistocene archaeological site in East Asia associated with late archaic hominin activities. Here we initially report several postcranial snake fossils that discovered from Loc.1. In this study, we conducted a preliminary identification of these specimens based on integrative osteological comparison between fossils and extant snakes. Three families, five genera, and six extant species were identified, which can be attributed to extant taxa. Diagnosis for each identified genus was summarized. The zoogeographic composition of the snake assemblage is primarily characterized by South China, Oriental, and Monsoonal elements. Among them, the Oriental tropical type Ptyas cf. carinata is most frequently recorded. The snake fauna might reveal a warmer and more humid climate in Hualongdong Site during the late Middle Pleistocene compared to the present.

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