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Late Pliocene rodents from the Irrawaddy sediments of central Myanmar and their palaeogeographical significance

机译:缅甸中部伊洛瓦底江沉积物中的上新世啮齿动物及其古地理意义

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摘要

The Upper Pliocene Irrawaddy sediments in the Gwebin area of central Myanmar recently yielded a rodent assemblage that contains nine species belonging to four families: four species of Muridae, three of Hystricidae, one of Spalacidae, and one of Sciuridae. The murids consist of Hapalomys cf. longicaudatus, Maxomys pliosurifer sp. nov., Rattus jaegeri and cf. Rattus sp. indet., which include both extinct and extant forms. Maxomys pliosurifer is relatively similar to Maxomys surifer that lives in South-East Asia in terms of tooth morphology but retains plesiomorphic features shared with the ancestral rat, Karnimata, and possible sister genera of Maxomys, such as Ratchaburimys and Millardia. The three hystricids belong to the genus Hystrix and consist of two extinct brachydont species (Hystrix paukensis and Hystrix sp. indet.) and one hypsodont species similar to living form (Hystrix cf. brachyura). This finding indicates that primitive brachydont species and derived hypsodont species of Hystrix had likely coexisted in the locality, but the brachydont species are significantly more common amongst specimens collected from the Gwebin area. The spalacid species is Cannomys cf. badius and the sciurid species is Menetes sp. indet. These two rodents are similar to living species in continental South-East Asia although they show minor differences in tooth characteristics compared to the living forms. Some species and genera of the fossil rodent assemblage from the Gwebin area also occur in Upper Pliocene localities of Thailand, suggesting chronological correlation between these two faunas. Moreover, these fossil rodent assemblages are composed primarily of the species distributed endemically in continental South-East Asia. Late Pliocene rodents of continental South-East Asia were affected by river barriers that formed during the Mio-Pliocene, and they were probably not able to disperse from South-East Asia into South and East Asia.
机译:最近,缅甸中部格韦宾地区的上新世伊洛瓦底江上层沉积物产生了一种啮齿动物组合,其中包含九个物种,属于四个科:鼠科四种,three科三种,one科一种和Sc科。这些杂种动物由Hapalomys cf. longicaudatus,Maxomys pliosurifer sp.。十一月,Rattus jaegeri和cf.褐家鼠indet。,包括既有形式和既有形式。就牙齿形态而言,Maxomys pliosurifer与居住在东南亚的Maxomys surifer相对相似,但保留了祖先大鼠,Karnimata和Maxomys的可能姊妹属(如叻atch鱼和Millardia)共有的多形特征。这三种菌丝属于Hystrix属,由两种灭绝的腕藻物种(Hystrix paukensis和Hystrix sp。indet。)和一种与生活形式相似的假鳞齿物种(Hystrix cf. brachyura)组成。这一发现表明,Hystrix的原始腕足动物和衍生的拟犬齿物种可能在该地区共存,但是腕足动物在从Gwebin地区收集的标本中更为常见。 spalacid物种是Cannomyscf。巴迪乌斯(Badisus)和针茅科物种是Menetes sp。 indet。这两种啮齿动物与东南亚大陆上的生物物种相似,但与活体形式相比,它们的牙齿特征显示出细微的差异。来自Gwebin地区的化石啮齿动物组合的某些物种和属也出现在泰国的上新世地区,这表明这两种动物在时间上具有相关性。此外,这些化石啮齿动物组合主要由东南亚大陆流行的物种组成。东南亚大陆上的上新世啮齿动物受到了上新世以来形成的河道屏障的影响,它们很可能无法从东南亚扩散到南亚和东亚。

著录项

  • 来源
    《Journal of Systematic Palaeontology》 |2015年第4期|287-314|共28页
  • 作者单位

    Primate Research Institute, Kyoto University, Inuyama, 484-8506, Japan;

    Primate Research Institute, Kyoto University, Inuyama, 484-8506, Japan;

    Primate Research Institute, Kyoto University, Inuyama, 484-8506, Japan;

    Department of Geology, Shwebo University, Shwebo, Myanmar;

    Department of Geology, Mandalay University, Mandalay, Myanmar;

    Primate Research Institute, Kyoto University, Inuyama, 484-8506, Japan;

    Hayashibara Museum of Natural Sciences, Setouchi, 701-4212, Japan,Department of Biosphere-Geosphere Science, Okayama University of Science, Okayama, 700-0005, Japan,Department of Earth Sciences, Faculty of Science, Ehime University, Matsuyama, 790-8577, Japan;

    Department of Geology, Magway University, Magway, Myanmar;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Rodentia; Pliocene; Irrawaddy sediments; biogeography; Myanmar; South-East Asia;

    机译:啮齿类;上新世;伊洛瓦底江沉积物;生物地理学缅甸;东南亚;

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