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所有三叶虫都是完全生活在海洋中的吗?三叶虫在古生代早期向微咸水区域的扩张。

Were all trilobites fully marine? Trilobite expansion into brackish water during the early Palaeozoic.

作者信息

Mángano M Gabriela, Buatois Luis A, Waisfeld Beatriz G, Muñoz Diego F, Vaccari N Emilio, Astini Ricardo A

机构信息

Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, Saskatchewan S7N 5E2, Canada.

Facultad de Ciencias Exactas, Físicas y Naturales, Universidad Nacional de Córdoba, Vélez Sarsfield 1611, Ciudad Universitaria, Córdoba X5016CGA, Argentina.

出版信息

Proc Biol Sci. 2021 Feb 10;288(1944):20202263. doi: 10.1098/rspb.2020.2263. Epub 2021 Feb 3.

Abstract

Trilobites, key components of early Palaeozoic communities, are considered to have been invariably fully marine. Through the integration of ichnological, palaeobiological, and sedimentological datasets within a sequence-stratigraphical framework, we challenge this assumption. Here, we report uncontroversial trace and body fossil evidence of their presence in brackish-water settings. Our approach allows tracking of some trilobite groups foraying into tide-dominated estuaries. These trilobites were tolerant to salinity stress and able to make use of the ecological advantages offered by marginal-marine environments migrating up-estuary, following salt wedges either reflecting amphidromy or as euryhaline marine wanderers. Our data indicate two attempts of landward exploration via brackish water: phase 1 in which the outer portion of estuaries were colonized by olenids (Furongian-early late Tremadocian) and phase 2 involving exploration of the inner to middle estuarine zones by asaphids (Dapingian-Darriwilian). This study indicates that tolerance to salinity stress arose independently among different trilobite groups.

摘要

三叶虫是早古生代群落的关键组成部分,一直被认为完全生活在海洋环境中。通过在层序地层框架内整合遗迹学、古生物学和沉积学数据集,我们对这一假设提出了质疑。在此,我们报告了它们在咸水环境中存在的无可争议的遗迹化石和实体化石证据。我们的方法能够追踪一些三叶虫群体进入受潮汐主导的河口的情况。这些三叶虫能够耐受盐度胁迫,并能够利用边缘海洋环境向上游河口迁移所提供的生态优势,跟随反映双向洄游的盐楔或作为广盐性海洋漫游者。我们的数据表明有两次通过咸水向陆地探索的尝试:第一阶段,河口外部被油栉虫类(芙蓉期—晚特里马道克世早期)占据,第二阶段,蚜头虫类(达坪阶—达瑞威尔阶)探索河口内至中部区域。这项研究表明,不同三叶虫群体对盐度胁迫的耐受性是独立产生的。

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