特刊社论前言:转型中的生命与环境:新元古代-早古生代世界

IF 4 1区 地球科学 Q1 GEOGRAPHY, PHYSICAL
Meng Cheng , Eva E. Stüeken , Zongjun Yin , Thomas J. Algeo , Chao Li
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引用次数: 0

摘要

这个虚拟特刊(VSI)寻求从元古宙-早期古生代世界的见解,这是地球历史上生命和环境共同进化的关键时期。本VSI的16篇论文大致分为三个主题。第一个主题是在一个精确的地质年代学框架内展示新的化石发现,揭示了埃迪卡拉纪海洋中有限的生物竞争和强大的环境控制对生命空间分布的影响。第二个主题是古环境重建。研究结果表明,海洋氧化还原条件、碳循环和大陆风化是一个复杂的非线性进化过程,挑战了生物进化中简单的环境控制的观点。第三个主题强调了海洋氧化还原条件在磷锰矿石形成中的关键作用。总之,这些研究表明,理解新元古代-早古生代生命和环境的共同进化需要一个地球系统的视角,将相互关联的构造、气候、海洋、生态和生物进化驱动因素结合起来。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Editorial preface to special issue: Life and environments in transition: The Neoproterozoic-early Paleozoic world
This Virtual Special Issue (VSI) presents insights from the Proterozoic-early Paleozoic world, a critical interval for the co-evolution of life and environments in Earth's history. The 16 papers in this VSI are broadly organized into three themes. The first theme presents new fossil discoveries within a refined geochronological framework, revealing limited biotic competition and a strong palaeoenvironmental control on the spatial distribution of life in the Ediacaran ocean. The second theme focuses on paleoenvironmental reconstruction. The results point to a complex, non-linear evolution of marine redox conditions, carbon cycling and continental weathering, challenging the idea of a simple environmental control on biological evolution. The third theme highlights the key role of oceanic redox conditions in the formation of phosphorus and manganese ores. Together, these studies suggest that understanding the co-evolution of life and environments during the Neoproterozoic-early Paleozoic requires a geosystems perspective incorporating a combination of interconnected tectonic, climatic, oceanic, ecological, and bioevolutionary drivers.
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来源期刊
Global and Planetary Change
Global and Planetary Change 地学天文-地球科学综合
CiteScore
7.40
自引率
10.30%
发文量
226
审稿时长
63 days
期刊介绍: The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems. Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged. Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.
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