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首页> 外文期刊>Proceedings of the National Academy of Sciences of the United States of America >Microbial taxa in deep-sea sediment linked to geochemical variations
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Microbial taxa in deep-sea sediment linked to geochemical variations

机译:深海沉积物中的微生物分类与地球化学变化有关

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Marine sediments host the largest reservoir of organic carbon and support the highest microbial abundance on Earth. Though the metabolic processes of these communities profoundly affect global biogeochemical cycles, the physiological activities of most subsurface microorganisms remain largely uncharacterized. Steffen J0rgensen et al. (pp. 16764-16765) report that microbial community structure directly correlates to geochemistry, providing a means to determine factors that shape community composition and predict the metabolic properties of Earth's most abundant deep-sea sediment microbes. The authors generated an extensive geochemical dataset of microbial profiles from two Arctic Mid-Ocean Ridge system sediment cores and found correlations between changes in the relative abundance of taxonomic groups and geochemical variations.
机译:海洋沉积物拥有最大的有机碳库,并支持地球上最高的微生物丰度。尽管这些群落的代谢过程深刻影响着全球生物地球化学循环,但大多数地下微生物的生理活性仍未完全表征。 Steffen J0rgensen等。 (pp。16764-16765)报告说,微生物群落结构与地球化学直接相关,为确定影响群落组成的因素和预测地球上最丰富的深海沉积物微生物的代谢特性提供了一种手段。作者从两个北极中洋海岭系统沉积物核心生成了广泛的微生物剖面地球化学数据集,并发现了分类群相对丰富度的变化与地球化学变化之间的相关性。

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