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首页> 外文期刊>Journal of South American earth sciences >Taphonomic aspects of the Pleistocene vertebrate assemblage of Itaborai, state of Rio de Janeiro, southeastern Brazil
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Taphonomic aspects of the Pleistocene vertebrate assemblage of Itaborai, state of Rio de Janeiro, southeastern Brazil

机译:巴西东南部里约热内卢州Itaborai的更新世脊椎动物组合的台词学方面

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摘要

Pleistocene vertebrates from Itaborai Basin have not been taphonomically studied prior to this work, limiting the understanding of the deposition and preservation of the only Pleistocene vertebrate accumulation known for the state of Rio de Janeiro. In this work, the taphonomic signatures of the Pleistocene vertebrate assemblage of Itaborai are identified and interpreted in order to increase the knowledge about the formation of this fossil association and the paleoecology of the region of Rio de Janeiro during the late Pleistocene. Our analysis shows that the thanatocoenosis was exposed to the biostratinomic processes during a small time span; that it is parautochthonous; and experienced short transport distances by normal fluvial streams and floods. Subsequently, the fossiliferous horizon was quickly covered by the superjacent soil. Yet, the skeletal elements were fractured and deformed during the sedimentary compaction. The differential preservation of megamammal bones is associated to the bone resistance against those destructive processes and to the specific anatomical features. Comparison between Itaborai and other Brazilian Pleistocene vertebrate accumulations shows that the Itaborai fossil accumulation was less affected by taphonomic processes, although it is also a time-averaged fossil concentration. Finally, some of the taphonomic features indicate an arid paleoclimate.
机译:在进行这项工作之前,尚未对Itaborai盆地的更新世脊椎动物进行染色体学研究,这限制了人们对里约热内卢州唯一已知的更新世脊椎动物积累的沉积和保存的了解。在这项工作中,确定并解释了Itaborai的更新世脊椎动物组合的拓朴特征,以增加有关该化石协会的形成和里约热内卢地区在更新世后期的古生态学的知识。我们的分析表明,囊腺狭窄在很短的时间内就暴露于生物地层学过程中。它是副声的;并且由于正常的河流和洪水而经历了短距离的运输。随后,化石层很快被上层土壤覆盖。然而,在沉积压实过程中,骨骼元素断裂并变形。巨乳骨骼的差异性保存与骨骼抵抗那些破坏性过程的抵抗力以及特定的解剖特征有关。比较Itaborai和其他巴西更新世的脊椎动物积累表明,Itaborai化石的积累受塔基过程的影响较小,尽管它也是时间平均化石的浓度。最后,某些Thophonomic特征表明干旱为古气候。

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  • 来源
    《Journal of South American earth sciences 》 |2013年第10期| 26-34| 共9页
  • 作者单位

    Universidade Federal do Rio de Janeiro, Programa de Pos-Graduacao em Geoiogia, Institute de Geociencias, CCMN, Cidade Universitaria, Ilha do Fundao,Av. Athos da Silveira Ramos, 274, Bloco G, 21941-916 Rio de Janeiro, RJ, Brazil;

    Universidade Federal do Rio de Janeiro, Programa de Pos-Graduacao em Geoiogia, Institute de Geociencias, CCMN, Cidade Universitaria, Ilha do Fundao,Av. Athos da Silveira Ramos, 274, Bloco G, 21941-916 Rio de Janeiro, RJ, Brazil;

    Universidade Federal do Rio Grande do Sul, Instituto de Geociencias, Laboratorio de Modelagem de Bacias, Av. Bento Goncalves 9500, Predio 43130,Campus do Vale, 91501-970, Brazil;

    Universidade Federal do Estado do Rio de Janeiro (UNIRIO), Departamento de Zoologia, Laboratorio de Mastezoologia, Av. Pasteur, 458, sala 501, Urca,222290-240 Rio de Janeiro, RJ, Brazil;

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

    Taphonomy; Vertebrates; Late Pleistocene; Itaborai; State of Rio de Janeiro;

    机译:语音脊椎动物;晚更新世;Itaborai;里约热内卢州;

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