The illusion of balance in the history of the biosphere

IF 2.7 2区 地球科学 Q2 BIOLOGY Geobiology Pub Date : 2024-01-12 DOI:10.1111/gbi.12584
Geerat J. Vermeij
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Abstract

Earth's surface has been irreversibly altered by the activity of organisms, a process that has accelerated as the power of the biosphere (the rate at which life extracts and deploys energy) has increased over time. This trend is incompatible with the expectation that the inputs to Earth's surface of life's materials from the crust and mantle be matched by export from Earth's surface to long-term reservoirs. Here, I suggest that the collective activity of organisms has always violated this balance. The biosphere's ability to extract, retain, recycle, and accumulate materials has allowed living biomass to increase and for exports to decrease over very long timescales. This collective metabolism implies a net transfer of materials from the planet's interior to its surface. The combination of metabolic innovations, competition, adaptive evolution, and the establishment of collaborative economic feedback in ecosystems created dynamic ecological stability despite great spatial and temporal heterogeneity in physical and biological inputs and export of nutrients into and out of the biosphere. Models of geochemical cycling must take the fundamental role of living organisms and the evolutionary changes in these roles into account to explain past and future conditions.

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生物圈历史上的平衡假象
地球表面已因生物的活动而发生了不可逆转的变化,随着时间的推移,生物圈的能量(生命汲取和利用能量的速度)不断增加,这一过程也随之加快。地壳和地幔中的生命物质向地球表面的输入与地球表面向长期储层的输出是相匹配的,但这一趋势与人们的期望不符。在此,我认为生物的集体活动一直在破坏这种平衡。生物圈提取、保留、循环和积累物质的能力使得生物量在很长的时间尺度内不断增加,而输出量则不断减少。这种集体新陈代谢意味着物质从地球内部向地表的净转移。新陈代谢的创新、竞争、适应性进化以及生态系统中协作性经济反馈的建立共同创造了动态的生态稳定性,尽管在物理和生物输入以及营养物质输出和输入生物圈方面存在巨大的时空异质性。地球化学循环模型必须考虑到生物体的基本作用以及这些作用的进化变化,以解释过去和未来的状况。
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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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