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Sequence stratigraphy and taphonomic signatures of marine invertebrates: A Devonian (Pragian/Eifelian) example of the Parana Basin, Brazil

机译:海洋无脊椎动物的层序地层学和地形学特征:巴西帕拉纳盆地的泥盆纪(普拉扬/伊非系)实例

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摘要

The latest Pragian to the early Eifelian succession of the Devonian of the eastern border of the Parana Basin (Brazil) is approached integrating taphonomy and sequence stratigraphy, providing new insights to the analysis of intracratonic siliciclastic Paleozoic seas. The high-resolution study of six outcrops revealed a mud-prone succession, composed predominantly of distal tempestites, with minor preservation of foreshore/shoreface depositional systems, and permitted the acquisition of sensible fossil and sedimentary data in relation to environments within the general depositional tendencies of the lowstand (LST), trangressive (TST) and highstand (HST) systems tracts of the succession. The LST has fragmented fossils preserved that indicate proximity to the shoreline; also, can preserve fossils that live in the foreshore/shoreface zone by proximal obrution events. In general, the TST records an epoch of moderate to high faunal diversity, low rates of sedimentation, with occurrence of obrution deposits in its middle part. Concretions with phosphatic animals can be preserved at the maximum transgressive surface, where the calcareous shells are preferentially dissolved. Stringers and rosette orientations below storm wave base are explained by flow lifting of distal muddy turbidity currents. The HST presents higher faunal diversity, with abundance of fragmented valves; sedimentation rates are moderated. Specific lingulid taphofacies displayed a very good correlation with the environmental conditions in each depositional environment. The lingulid taphofacies could be used as a more sensible tool in order to analyze environmental conditions in ancient seas. Therefore taphonomic signatures and biofabrics of the fossils (their occurrences and diversities) showed correlation with the general principles of sequence stratigraphy, and seem to be controlled by the system tracts where they were preserved.
机译:将帕纳纳盆地(巴西)东部边界的泥盆纪最新的普拉格期到早期的艾菲尔时期接替,将地形学和层序地层学结合起来,为内部克拉通硅质碎屑古生界的分析提供了新的见识。对六个露头的高分辨率研究表明,泥浆俯冲连续,主要由远侧的风暴组成,对前岸/滨海沉积系统的保护较小,并允许获取与一般沉积趋势内的环境有关的敏感化石和沉积数据低位(LST),海侵(TST)和高位(HST)系统序列的连续性。 LST的碎片化石保存完好,表明靠近海岸线。此外,还可以通过近端阻塞事件来保存生活在前岸/滨海区的化石。总的来说,TST记录了一个中等到较高动物区系,低沉积速率的时期,在中部出现了阻塞沉积物。可以将磷酸盐动物的粪便保存在最大的海藻表面,在此钙质壳优先溶解。风暴波基下方的桁条和花环方向通过远端泥泞浊流的流动提升来解释。 HST表现出更高的动物多样性,并且瓣膜很多。沉淀速度适中。特定语言的酒谱与每个沉积环境中的环境条件都显示出很好的相关性。可以使用语言标签作为更明智的工具,以分析古代海洋中的环境条件。因此,化石的局部标记和生物构造(它们的出现和多样性)显示出与层序地层学的一般原理相关,并且似乎受保存它们的系统区域的控制。

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  • 来源
    《Journal of South American earth sciences》 |2012年第1期|p.8-20|共13页
  • 作者单位

    Center for Biological and Health Sciences, Universidade Positive (UP), 5300, Prof. Pedro Viriato Parigot de Souza Street, Curitiba, PR 81280-330, Brazil;

    Geosciences Institute, Universidade Federal da Bahia (UFBA) Campus Universitario de Ondina s, Rua Barao de Jeremoabo, Salvador, BA 40170-115, Brazil;

    Geosciences Department, Universidade Estadual de Ponta Grossa (UEPG), 164, Otaviano Macedo Ribas Street, Ponta Grossa, PR 84070-540, Brazil;

    Geosciences Institute, Universidade Federal do Rio Grande do Sul (UFRGS), 9500, Bento Goncalves Av., Porto Alegre, RS 91501-970, Brazil;

    Geosciences Institute, Universidade Federal do Rio Grande do Sul (UFRGS), 9500, Bento Goncalves Av., Porto Alegre, RS 91501-970, Brazil;

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

    sequence stratigraphy; taphonomy; marine invertebrates; devonian; parana basin;

    机译:层序地层学拓朴海洋无脊椎动物;泥盆纪巴拉那盆地;

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