首页> 外文期刊>Journal of Paleontology >A new paleoecological look at the dinwoody formation (lower triassic, Western USA): Intrinsic versus extrinsic controls on ecosystem recovery after the end-permian mass extinction
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A new paleoecological look at the dinwoody formation (lower triassic, Western USA): Intrinsic versus extrinsic controls on ecosystem recovery after the end-permian mass extinction

机译:dinwoody形成的新的古生态观(下三叠纪,美国西部):二叠纪末次生物大灭绝后生态系统恢复的内在控制与外在控制

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摘要

The Dinwoody Formation of the western United States represents an important archive of Early Triassic ecosystems in the immediate aftermath of the end-Permian mass extinction. We present a systematic description and a quantitative paleoecological analysis of its benthic faunas in order to reconstruct benthic associations and to explore the temporal and spatial variations of diversity, ecological structure and taxonomic composition throughout the earliest Triassic of the western United States. A total of 15 bivalve species, two gastropod species, and two brachiopod species are recognized in the study area. The paleoecological analysis shows that the oldest Dinwoody communities are characterized by low diversity, low ecological complexity and high dominance of few species. We suggest that this low diversity most likely reflects the consequences of the mass extinction in the first place and not necessarily the persistence of environmental stress. Whereas this diversity pattern persists into younger strata of the Dinwoody Formation in outer shelf environments, an increase in richness, evenness and guild diversity occurred around the Griesbachian-Dienerian boundary in more shallow marine habitats. This incipient recovery towards the end of the Griesbachian is in accordance with observations from other regions and thus probably represents an interregional signal. In contrast to increasing richness within communities (alpha-diversity), beta-diversity remained low during the Griesbachian and Dienerian in the study area. This low beta-diversity reflects a wide environmental and geographical range of taxa during the earliest Triassic, indicating that the increase of within-habitat diversity has not yet led to significant competitive exclusion. We hypothesize that the well-known prevalence of generalized taxa in post-extinction faunas is primarily an effect of reduced competition that allows species to exist through the full range of their fundamental niches, rather than being caused by unusual and uniform environmental stress.
机译:美国西部的Dinwoody地层是二叠纪末大灭绝后的早期三叠纪生态系统的重要档案。我们对底栖动物群进行系统的描述和定量的古生态分析,以重建底栖动物协会并探索美国西部最早的三叠纪的多样性,生态结构和分类学组成的时空变化。在研究区域内总共确认了15种双壳类,两种腹足类和两种腕足类。古生态分析表明,最古老的Dinwoody群落具有多样性低,生态复杂度低和少数物种占优势的特点。我们建议,这种低多样性很可能首先反映了大规模灭绝的后果,并不一定反映了环境压力的持续存在。尽管这种多样性模式在外陆架环境中一直存在于Dinwoody组的年轻地层中,但在更浅的海洋栖息地的Griesbachian-Dienerian边界周围,丰富度,均匀性和行会多样性有所增加。到格里斯巴赫式末期的初期恢复与其他地区的观察一致,因此可能代表了地区间的信号。与增加社区内的丰富度(α多样性)相反,在研究区域的Griesbachian和Dienerian期间,β多样性仍然较低。这种低的β多样性反映了最早的三叠纪时期分类单元的广泛环境和地理范围,这表明,栖息地内部多样性的增加尚未导致明显的竞争排斥。我们假设灭绝后动物群中普遍存在的类群流行主要是竞争减少的影响,这种竞争使物种能够通过其基本生态位的整个范围生存,而不是由异常且均匀的环境压力引起。

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