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首页> 外文期刊>PALAIOS >The Non-Actualistic Early Triassic Gastropod Fauna:A Case Study of the Lower Triassic SinbadLimestone Member
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The Non-Actualistic Early Triassic Gastropod Fauna:A Case Study of the Lower Triassic SinbadLimestone Member

机译:非实际的早期三叠纪腹足动物区系:以下三叠纪辛巴达石灰岩成员为例

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摘要

Through a detailed regional study of the Lower Triassic (Nammalian) Sinbad Limestone Member of the Moenkopi Formation in southeastern Utah, previously qualitative paleoecological observations on Early Triassic gastropods have been quantified. Paleocommunities of the Lower Triassic Sinbad Limestone Member are dominated by gastropod juveniles and small-size adult gastropods (99% of the gastropods are smaller than 1 cm) that form numerous microgastropod packstones and grainstones that were deposited subtidally. The results from this case study of the Sinbad Limestone Member reflect a global Early Triassic phenomenon of microgastropod-dominated open-shelf environments. These characteristics of the paleoecology of Early Triassic gastropod faunas are non-actualistic since, during Ecological Evolutionary Units (EEUs), larger gastropods and normal-marine communities are invariably common somewhere contemporaneous with the occurrence of microgastropod-dominated faunas. Early Triassic microgastropods behaved as repopulation-interval opportunists during the aftermath of the end-Permian mass extinction, proliferating into vacated ecospace after most groups became extinct or dropped to very low numbers as a result of the end- Permian mass extinction. Small-sized adults and numerous juveniles are characteristics of opportunists and of groups inhabiting physiologically and/or chemically harsh environments. The characteristics of the Early Triassic microgastropod fauna indicate prolonged environmental stresses related to the causes of the end-Paleozoic biotic crisis.
机译:通过对犹他州东南部 东南部Moenkopi组的下三叠世(Nammalian) Sinbad石灰岩成员的详细区域研究,先前对 早期的定性古生态观测三叠纪腹足动物已被量化。下三叠世辛巴达石灰岩成员的古群落 主要由腹足纲幼体和小型成年腹足纲(99% 小于1)控制厘米),形成许多 微腹足类的结石和粒状结石,这些结石 很好地沉积。该Sinbad石灰石 成员的案例研究的结果反映了微腹足动物为主的 开放式货架环境的全球早期三叠纪现象。早三叠世腹足动物区系的古生态学特征是不现实的,因为在生态演化单位(EEUs),较大腹足动物sups和正常动物中,与小腹足纲动物为主的 动物的发生同时发生,海洋群落总是常见的。在二叠纪末期生物灭绝后,早期的三叠纪微腹足类动物表现为繁殖间隔 机会主义者,大多数团体成为 绝种后, 扩散到空旷的生态空间。或由于二叠纪末次灭绝而下降到非常低的数字。小型成年人和许多少年 是在生理和/或化学条件恶劣的环境中居住的机会主义者和团体的特征。早期三叠纪微腹足动物群的特征 表明与古生代末期生物危机起因有关的延长的 环境压力。 上>

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  • 来源
    《PALAIOS》 |2004年第3期|00000259-00000275|共17页
  • 作者单位

    Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089,fraiser@usc.edu;

    Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089,fraiser@usc.edu;

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