{"title":"日本上新世犀牛的分类学、生物地层学和古生物地理学综述","authors":"Naoto Handa, Keiichi Takahashi","doi":"10.1016/j.jseaes.2024.106357","DOIUrl":null,"url":null,"abstract":"<div><div>The Rhinocerotidae were distributed in Eurasia and Africa during the late Neogene. In particular, the subtribe Rhinocerotina which includes the living species, diversified during the Plio-Pleistocene in Eurasia. Japan, which is situated in Far East Asia, has also yielded Plio-Pleistocene rhinocerotids, but their taxonomic position has not been revised since their first descriptions. Considering recent taxonomic revisions of many Eurasian Rhinocerotidae, it is necessary to also revise the Japanese remains. Here, taxonomy and fossil records of the Plio-Pleistocene Japanese rhinocerotids are reviewed. A total of 16 bones and teeth remains have been found from the mid-Pliocene to the middle Middle Pleistocene. Three Pliocene rhinocerotids are identified as Rhinocerotina gen. et sp. indet. In the earliest Pliocene, the close relative of the Japanese Pliocene rhinocerotid migrated from continental Asia. <em>Stephanorhinus kirchbergensis</em> was distributed in central to southwestern Japan during the middle Middle Pleistocene. In addition, indeterminate species were also present in the Early to Middle Pleistocene. The Late Pleistocene fossil record is uncertain due to the lack of stratigraphic and chronological data. Japanese <em>S</em>. <em>kirchbergensis</em> immigrated from the continental Asia (middle part of China) at ca. 0.65 Ma with a species of <em>Stegodon</em> together.</div></div>","PeriodicalId":50253,"journal":{"name":"Journal of Asian Earth Sciences","volume":"276 ","pages":"Article 106357"},"PeriodicalIF":2.7000,"publicationDate":"2024-10-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A review of the taxonomy, biostratigraphy and paleobiogeography of Plio-Pleistocene rhinoceroses in Japan\",\"authors\":\"Naoto Handa, Keiichi Takahashi\",\"doi\":\"10.1016/j.jseaes.2024.106357\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The Rhinocerotidae were distributed in Eurasia and Africa during the late Neogene. In particular, the subtribe Rhinocerotina which includes the living species, diversified during the Plio-Pleistocene in Eurasia. Japan, which is situated in Far East Asia, has also yielded Plio-Pleistocene rhinocerotids, but their taxonomic position has not been revised since their first descriptions. Considering recent taxonomic revisions of many Eurasian Rhinocerotidae, it is necessary to also revise the Japanese remains. Here, taxonomy and fossil records of the Plio-Pleistocene Japanese rhinocerotids are reviewed. A total of 16 bones and teeth remains have been found from the mid-Pliocene to the middle Middle Pleistocene. Three Pliocene rhinocerotids are identified as Rhinocerotina gen. et sp. indet. In the earliest Pliocene, the close relative of the Japanese Pliocene rhinocerotid migrated from continental Asia. <em>Stephanorhinus kirchbergensis</em> was distributed in central to southwestern Japan during the middle Middle Pleistocene. In addition, indeterminate species were also present in the Early to Middle Pleistocene. The Late Pleistocene fossil record is uncertain due to the lack of stratigraphic and chronological data. Japanese <em>S</em>. <em>kirchbergensis</em> immigrated from the continental Asia (middle part of China) at ca. 0.65 Ma with a species of <em>Stegodon</em> together.</div></div>\",\"PeriodicalId\":50253,\"journal\":{\"name\":\"Journal of Asian Earth Sciences\",\"volume\":\"276 \",\"pages\":\"Article 106357\"},\"PeriodicalIF\":2.7000,\"publicationDate\":\"2024-10-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Asian Earth Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1367912024003523\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Asian Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1367912024003523","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
摘要
犀牛科动物在新近纪晚期分布于欧亚大陆和非洲。尤其是包括现生物种在内的犀牛亚目,在欧亚大陆的上新世时期就已经出现了多样化。位于远东亚洲的日本也发现了上新世的犀牛类,但自首次描述以来,其分类学地位尚未得到修订。考虑到最近对许多欧亚犀科动物的分类学修订,有必要对日本的犀科动物进行修订。本文回顾了上新世-更新世日本犀牛科的分类和化石记录。从上新世中期到中更新世中期,共发现了16块骨骼和牙齿遗迹。三个上新世的犀牛类被鉴定为犀牛属等。在上新世早期,日本上新世犀类的近亲从亚洲大陆迁徙而来。在中更新世中期,Stephanorhinus kirchbergensis分布于日本中部至西南部。此外,早更新世到中更新世还出现了不定种。由于缺乏地层和年代数据,晚更新世的化石记录尚不确定。日本的 S. kirchbergensis 于约 0.65 Ma 时从亚洲大陆(中国中部)移民而来。日本的S. kirchbergensis是在大约0.65Ma时从亚洲大陆(中国中部)移民过来的。
A review of the taxonomy, biostratigraphy and paleobiogeography of Plio-Pleistocene rhinoceroses in Japan
The Rhinocerotidae were distributed in Eurasia and Africa during the late Neogene. In particular, the subtribe Rhinocerotina which includes the living species, diversified during the Plio-Pleistocene in Eurasia. Japan, which is situated in Far East Asia, has also yielded Plio-Pleistocene rhinocerotids, but their taxonomic position has not been revised since their first descriptions. Considering recent taxonomic revisions of many Eurasian Rhinocerotidae, it is necessary to also revise the Japanese remains. Here, taxonomy and fossil records of the Plio-Pleistocene Japanese rhinocerotids are reviewed. A total of 16 bones and teeth remains have been found from the mid-Pliocene to the middle Middle Pleistocene. Three Pliocene rhinocerotids are identified as Rhinocerotina gen. et sp. indet. In the earliest Pliocene, the close relative of the Japanese Pliocene rhinocerotid migrated from continental Asia. Stephanorhinus kirchbergensis was distributed in central to southwestern Japan during the middle Middle Pleistocene. In addition, indeterminate species were also present in the Early to Middle Pleistocene. The Late Pleistocene fossil record is uncertain due to the lack of stratigraphic and chronological data. Japanese S. kirchbergensis immigrated from the continental Asia (middle part of China) at ca. 0.65 Ma with a species of Stegodon together.
期刊介绍:
Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review.
The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology, tectonics, geochemistry and geophysics of Asia. It will be devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be included. Papers must have international appeal and should present work of more than local significance.
The scope includes deep processes of the Asian continent and its adjacent oceans; seismology and earthquakes; orogeny, magmatism, metamorphism and volcanism; growth, deformation and destruction of the Asian crust; crust-mantle interaction; evolution of life (early life, biostratigraphy, biogeography and mass-extinction); fluids, fluxes and reservoirs of mineral and energy resources; surface processes (weathering, erosion, transport and deposition of sediments) and resulting geomorphology; and the response of the Earth to global climate change as viewed within the Asian continent and surrounding oceans.