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首页> 外文期刊>Journal of vertebrate paleontology >A Last Glacial anuran assemblage from the inland Pampas of South America provides insights into climate and environments during Marine Isotope Stage 3
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A Last Glacial anuran assemblage from the inland Pampas of South America provides insights into climate and environments during Marine Isotope Stage 3

机译:来自南美洲内陆潘帕斯的最后一艘冰川Anuran集会在海洋同位素第3阶段提供了对气候和环境的洞察力

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摘要

Environmental and climatic conditions of the South American temperate grasslands (Pampas) during the Last Glacial Period have typically been regarded as mostly arid and cold, whereas humid and mild conditions such as those prevailing today may have been established only recently. This hypothesis has been built mostly upon fossil mammals that come from coastal areas and date from the end phase of this period and thus provide both temporally and geographically biased data. Other fossil vertebrates, including anurans, have been overlooked when addressing these conditions in spite of being potentially very informative due to their ecological requirements. Here, we analyze an anuran assemblage from the Last Glacial Period of the inland Pampas. In addition to the description of new records, we discuss the taphonomic settings and the correlation of the fossil-bearing beds with levels referred to the interstadial Marine Isotope Stage (MIS) 3 from other Pampean localities. Based on this evidence, together with what is known for extant anurans, we discuss the environmental and climatic conditions of the Pampas during the Last Glacial Period. The presence of Rhinella arenarum and, particularly, Ceratophrys ornata in the fossil assemblage and their persistence in the Pampas throughout the Quaternary suggest that the range of environmental changes in the region during the Last Glacial Period might have been more limited than has traditionally been acknowledged. In this regard, this study highlights the value of anuran fossil assemblages when addressing environmental and climatic conditions during the Quaternary.
机译:最后一次冰川期间南美温带草地(PAMPAS)的环境和气候条件通常被认为是大多数干旱和寒冷,而今天可能已经建立了潮湿和温和的条件,例如当今普遍的普遍存在。这一假设主要是在从沿海地区和本期结束阶段的沿海地区和日期来的化石哺乳动物构建的,因此在时间上和地理位置偏见的数据中提供。在包括灭官州的其他化石脊椎动物,在解决这些条件时,尽管潜在的生态要求是非常富有信息的。在这里,我们从内陆潘帕斯的最后一个冰川期间分析了一个Anuran组合。除了对新记录的描述之外,我们还讨论了从其他胶扑地区中提到了洞穴海洋同位素阶段(MIS)3的水平的化石横覆盖床的相关性和相关性。基于这一证据,与现存的Anurans所知,我们在最后一次冰川期间讨论了PAMPAS的环境和气候条件。在整个第四纪的化石组合中的犀牛群和特别是Ceratophrys ornata的存在,并且在整个第四纪的PAMPAS中的持久性表明,在最后一次冰川期间,该地区的环境变化范围可能比传统上的承认更大。在这方面,本研究突出了在第四纪期间解决环境和气候条件时的抗南芥组合的价值。

著录项

  • 来源
    《Journal of vertebrate paleontology》 |2019年第3期|共11页
  • 作者单位

    Univ Buenos Aires Fac Ciencias Exactas &

    Nat CONICET Dept Ciencias Geol Ciudad Univ RA-1428 Buenos Aires DF Argentina;

    Univ Buenos Aires Fac Ciencias Exactas &

    Nat CONICET Dept Ciencias Geol Ciudad Univ RA-1428 Buenos Aires DF Argentina;

    Univ Buenos Aires Fac Ciencias Exactas &

    Nat CONICET Dept Ciencias Geol Ciudad Univ RA-1428 Buenos Aires DF Argentina;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 古生物学;
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