Anchient jawed polychates: evolution and palaeogeography in the Lower Palaeozoic

古代有颌多毛类动物：下古生代的演化和古地理

• 批准号: 511973862
• 负责人: Dr. Peter Königshof
• 金额: --
• 依托单位: Senckenberg Forschungsinstitut und Naturmuseum
• 依托单位国家: 德国
• 项目类别: Research Grants
• 资助国家: 德国
• 项目状态: 未结题
• 来源: https://gepris.dfg.de/gepris/projekt/511973862?language=en
• 关键词: Anchient; jawed; polychates; evolution; palaeogeography

Polychaete worms are one of the most common components of benthic invertebrate faunas in the present-day oceans. The origin of the group dates back to the Cambrian and the abundance and diversity was steeply rising since Ordovician. Despite of this fact the studies of this group are geographically and stratigraphically rather limited. To fill this gap, we have chosen to study and compile data on fossil polychaetes from various palaeocontinents – Gondwana (Prague Basin, Iran, Argentine Precordillera), Avalonia (Eifel synclines), and Baltica (Estonia). Within this project we intend to intergrade taxonomic analysis with sedimentological and microfacies data, and to focus on sedimentological successions within the Ordovician – Devonian, especially where fundamental environmental changes were recorded, e.g. extinction events. Understanding such events in Earth`s history will provide insights in evolutionary and environmental changes which are nowadays key issues. This approach should elucidate strategies of fossil eunicids during ecological perturbations over a long time-span and also test their facial dependence. The main goal is to integrate and interpret data gained from taxonomic analysis of Ordovician to Devonian polychaete communities from different palaeogeographic regions. These studies will be combined with sedimentological, geochemical (isotope studies) and microfacies analysis and will particularly focus on specific stratigraphic levels where fundamental environmental changes (such as events) were recorded.

多毛类蠕虫是当今海洋中底栖无脊椎动物群最常见的组成部分之一。该群体的起源可以追溯到寒武纪，自奥陶纪以来，其丰富度和多样性急剧上升。尽管如此，该小组的研究在地理和地层学上相当有限。为了填补这一空白，我们选择研究和汇编来自不同古大陆的多毛类化石数据——冈瓦纳古陆（伊朗布拉格盆地、阿根廷普雷迪勒拉）、阿瓦隆尼亚（埃菲尔向斜）和波罗的海（爱沙尼亚）。在这个项目中，我们打算将分类分析与沉积学和微相数据结合起来，并重点关注奥陶纪-泥盆纪的沉积演替，特别是记录了基本环境变化的地方，例如。灭绝事件。了解地球历史上的此类事件将为进化和环境变化提供见解，而这些都是当今的关键问题。这种方法应该能够阐明化石eunicids在长期生态扰动期间的策略，并测试它们的面部依赖性。主要目标是整合和解释从不同古地理区域的奥陶纪到泥盆纪多毛类群落的分类分析中获得的数据。这些研究将与沉积学、地球化学（同位素研究）和微相分析相结合，并将特别关注记录基本环境变化（例如事件）的特定地层水平。