首页> 外文期刊>Quaternary International >Megafauna from the Late Pleistocene-Holocene deposits of the Upper Ribeira karst area, southeast Brazil
【24h】

Megafauna from the Late Pleistocene-Holocene deposits of the Upper Ribeira karst area, southeast Brazil

机译:巴西东南部上里贝拉喀斯特地区晚更新世-全新世沉积的大型动物

获取原文
获取原文并翻译 | 示例
           

摘要

The carbonate caves of the Upper Ribeira Valley, southeastern Sao Paulo State, Brazil, preserve an abundant fossil record of Pleistocene-Holocene South American megafauna. Nevertheless, in comparison with other localities of the country, its paleontological knowledge still can be considered sparse and in need of further research. This work presents an update taxonomic survey of the megafauna material collected since the beginning of the explorations in the area. Based on this, it discusses paleobiogeo-graphic and paleoecological questions. The fossil megafauna of the Upper Ribeira karst region include: Eremotherium laurillardi, Nothrotherium maquinense, Lestodon armatus, Catonyx cuvieri, 'Ocnopus gracilis', Ahytherium aff. aureum, Glyptodon clavipes, G. reticulatus, Hoplophorus cf., Toxodon spp., Stegomastodon waringi, Equidae (Hippidion cf.), Tapirvs terrestris, Panthera onca and Smilodon populator. Only P. onca and T. terrestris still remain in the region. Despite the occurrence of some typical taxa of the pampean paleobiogeographical province, the fossil assemblage recorded shows greater affinity to the mega-mammal community of the intertropical region. The ecology of species found suggests the previous occurrence of fairly different environmental settings than the existing one in the area. There were more temperate climates - both dry and wet - until the current mesophytic forest was finally established. The studied material does not show any kind of chrono-correlation, given the type of genesis of the cave accumulations. These fossils depict different faunistic moments related to climate changes during the Quaternary. To better understand the information provided by these deposits, efforts on dating and detailed taphonomic investigations should be conducted. The studies of the Quaternary fauna in the state of Sao Paulo fill an important gap in the intricate biogeographical history of the South American megafauna.
机译:巴西圣保罗州东南部的里贝拉河谷上游的碳酸盐岩洞穴保存着丰富的化石记录,其中包括更新世-全新世南美大型动物群。尽管如此,与该国其他地区相比,其古生物学知识仍被认为是稀疏的,需要进一步研究。这项工作介绍了自该地区开始勘探以来所收集的大型动物的最新分类学调查。在此基础上,讨论了古生物地理学和古生态问题。上里贝拉喀斯特地区的大型动物区系包括:月桂叶草(Ereemotherium laurillardi),夜蛾红藻(Nothrotherium maquinense),莱斯托顿(Lestodon armatus),山茱Cat(Catonix cuvieri),'Ocnopus gracilis',Ahytherium aff。金黄色葡萄球菌,锁骨Glytictodon刺网,G。reticulatus,Hoplophorus cf.,Toxodon spp。,Stegagostodon waringi,Equidae(Hippidion cf。),Tapirvs terrestris,Panthera onca和Smilodon种群。该地区仅剩下P. onca和T. terrestris。尽管发生了黄褐色古生物地理省的一些典型分类群,但记录的化石组合显示出与热带地区巨型哺乳动物群落的亲和力更高。发现的物种生态学表明该地区先前发生的环境设置与该地区现有环境设置完全不同。直到现在的中生森林最终建立之前,气候都比较干燥和潮湿。考虑到洞穴堆积的成因类型,所研究的材料没有显示出任何时间相关性。这些化石描绘了第四纪期间与气候变化有关的不同的泥沼纪元。为了更好地了解这些沉积物提供的信息,应该进行日期测定和详细的染色体研究。对圣保罗州第四纪动物区系的研究填补了南美巨型动物群复杂的生物地理历史中的一个重要空白。

著录项

  • 来源
    《Quaternary International》 |2011年第2期|p.369-378|共10页
  • 作者单位

    Universidade Federal de Sao Carlos (UESCar), Departamento de Ecologia e Biologia Evolutiva (DEBE), Rodovia Washington Luis, SP-310. km 235, 13565-906, Sao Carlos, SP, Brazil;

    Universidade Federal de Sao Carlos (UESCar), Departamento de Ecologia e Biologia Evolutiva (DEBE), Rodovia Washington Luis, SP-310. km 235, 13565-906, Sao Carlos, SP, Brazil;

    Universidade Federal de Sao Carlos (UESCar), Departamento de Ecologia e Biologia Evolutiva (DEBE), Rodovia Washington Luis, SP-310. km 235, 13565-906, Sao Carlos, SP, Brazil;

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

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号