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The Quaternary vertebrate fauna of the limestone cave Gruta do Ioio, northeastern Brazil

机译:巴西东北部,石灰岩洞穴,第四纪的季奥第纪脊椎动物区系

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摘要

The present study reports the Quaternary vertebrate fauna of Gruta do Ioio, a partially submerged limestone cave located in central Bahia, northeastern Brazil. A semi-arid weather prevails nowadays in the area, which is mostly covered by a xeric low arboreal scrubland known as Caatinga. The identified taxa include: Rhamdia (Osteichtyes, Siluriformes), Caiman (Crocodyliformes, Caimaninae), Myocastor cf. Myocastor coypus (Rodentia, Myocastoridae), Holochilus sciureus (Rodentia, Sigmodontinae), Natalus cf. Natalus macrourus (Chiroptera, Natalidae), Tonatia bidens, Trachops cirrhosus (Chiroptera, Phyllostomi-dae), and Eira cf. Eira barbara (Carnivora, Mustelidae). Whereas Rhamdia and Caiman have scarce fossil records, the recovered mammals have already been reported from Quaternary localities of northeastern Brazil, although only two of them are present in the current local fauna. Taphonomic signatures and the nature of the fossiliferous site indicate that the vertebrates lived inside or nearby the cave, including the swamp by its main entrance. Radiocarbon dating of dental bioapatite yielded calibrated ages between 19,980 and 22,040 BP. This indicates that the accumulation started at least during the late Pleistocene, within the Last Glacial Maximum. In agreement with the mode of life of most taxa recognized here, previous studies indicated that this was a wetter period in the region.
机译:本研究报告了位于巴西东北巴伊亚州中部的部分淹没的石灰岩洞穴Gruta do Ioio的第四纪脊椎动物。如今,该地区盛行半干旱天气,大部分地区被称为Caatinga的干旱低乔木灌丛覆盖。识别出的分类单元包括:Rhamdia(Osteichtyes,Siluriformes),Caiman(Crocodyliformes,Caimaninae),Myocastorcf。食蟹猴(Myocastor coypus)(啮齿类动物,Myocastoridae),och鼠(Sholmodus sciureus)(Rodentia,Sigmodontinae),Natalus cf.纳塔卢斯巨蜥(Chiroptera,Natalidae),Tonatiabidens,Trachops cirrhosus(Chiroptera,Phyllostomi-dae)和Eira cf.埃拉·芭芭拉(食肉动物,鼬科)。尽管Rhamdia和Caiman的化石记录很少,但已经从巴西东北部第四纪地区报告了回收的哺乳动物,尽管在目前的当地动物群中只存在其中的两个。排字特征和化石部位的性质表明,脊椎动物生活在洞穴内部或附近,包括其主要入口处的沼泽。牙科生物磷灰石的放射性碳测年得出的标定年龄介于19,980和22,040 BP之间。这表明,至少在晚更新世末期,即最后冰川期,开始积累。与此处公认的大多数分类单元的生活方式一致,以前的研究表明这是该地区较湿的时期。

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  • 来源
    《Quaternary International》 |2014年第26期|164-175|共12页
  • 作者单位

    Division Paleontologia de Vertebrados, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque s, B1900FWA La Plata, Buenos Aires, Argentina;

    Departmento de Zoologia, Instituto de Biociencias, UNESP, Av. 24A 1515, 13506-900 Rio Claro, Sao Paulo, Brazil;

    Faculdade de Filosofia Ciencias e Letras de Ribeirao Preto, Universidade de Sao Paulo, Av. Bandeirantes 3900,14040-901 Ribeirao Preto, Sao Paulo, Brazil;

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

    Gruta do Ioio; Quaternary; Pleistocene; Bahia; Brazil; Cave deposits;

    机译:艾奥瓦州第四纪更新世;巴伊亚巴西;洞穴沉积;

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