寒武纪辐射时期作为生态系统工程师的分支古土生动物

IF 2.7 2区 地球科学 Q2 BIOLOGY
Geobiology Pub Date : 2022-08-25 DOI:10.1111/gbi.12521
Ryan A. Manzuk, Adam C. Maloof, Jaap A. Kaandorp, Mark Webster
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引用次数: 2

摘要

在寒武纪早期,主要动物身体结构的迅速形成和多样化与地球上第一个动物建造的框架礁的兴起相吻合。鉴于硬核珊瑚在现代海洋中作为生态促进者的重要性,我们研究了在寒武纪辐射期间,古藻类(古藻纲)珊瑚礁作为工程生态系统的影响。在这项研究中,我们首次展示了来自劳伦森古大陆三个地点的分支古ocyathide (Archaeocyathida目)个体的高分辨率三维重建。由于海绵和珊瑚的分支形式显示出表型可塑性,从而保留了周围生长环境的特征,因此我们将化石标本的形态学测量结果与现代珊瑚的形态学测量结果进行比较,以推断地球上第一批珊瑚礁的表面条件。这些数据表明,古石可以承受和影响水流,容纳光共生体,并建立地形复杂和稳定的结构,就像今天的珊瑚一样。我们还认识到下寒武纪珊瑚礁环境的粗糙度逐步增加,这将为更丰富和多样化的共同进化动物群奠定基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Branching archaeocyaths as ecosystem engineers during the Cambrian radiation

The rapid origination and diversification of major animal body plans during the early Cambrian coincide with the rise of Earth's first animal-built framework reefs. Given the importance of scleractinian coral reefs as ecological facilitators in modern oceans, we investigate the impact of archaeocyathan (Class Archaeocyatha) reefs as engineered ecosystems during the Cambrian radiation. In this study, we present the first high-resolution, three-dimensional (3D) reconstructions of branching archaeocyathide (Order Archaeocyathida) individuals from three localities on the Laurentian paleocontinent. Because branched forms in sponges and corals display phenotypic plasticity that preserve the characteristics of the surrounding growth environment, we compare morphological measurements from our fossil specimens to those of modern corals to infer the surface conditions of Earth's first reefs. These data demonstrate that archaeocyaths could withstand and influence the flow of water, accommodate photosymbionts, and build topographically complex and stable structures much like corals today. We also recognize a stepwise increase in the roughness of reef environments in the lower Cambrian, which would have laid a foundation for more abundant and diverse coevolving fauna.

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来源期刊
Geobiology
Geobiology 生物-地球科学综合
CiteScore
6.80
自引率
5.40%
发文量
56
审稿时长
3 months
期刊介绍: The field of geobiology explores the relationship between life and the Earth''s physical and chemical environment. Geobiology, launched in 2003, aims to provide a natural home for geobiological research, allowing the cross-fertilization of critical ideas, and promoting cooperation and advancement in this emerging field. We also aim to provide you with a forum for the rapid publication of your results in an international journal of high standing. We are particularly interested in papers crossing disciplines and containing both geological and biological elements, emphasizing the co-evolutionary interactions between life and its physical environment over geological time. Geobiology invites submission of high-quality articles in the following areas: Origins and evolution of life Co-evolution of the atmosphere, hydrosphere and biosphere The sedimentary rock record and geobiology of critical intervals Paleobiology and evolutionary ecology Biogeochemistry and global elemental cycles Microbe-mineral interactions Biomarkers Molecular ecology and phylogenetics.
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