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Updated: Jun 17, 2025

Methods of Soil Resampling to Monitor Changes in the Chemical Concentrations of Forest Soils
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Published on: November 25, 2016

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大约在侧面的氧化还原变异性. 1.9 亿年前的海洋环境是由有机碳和同位素组成的海洋环境

Kento Motomura1,2, Andrey Bekker1,3, Minoru Ikehara4

  • 1Department of Earth and Planetary Sciences, University of California, Riverside, California, USA.

Geobiology
|August 12, 2024
PubMed
概括

早期的真核生物大概在19亿年前在富含营养的海洋中壮成长. 高的生物生产率和循环支持可居住的环境,即使是在岛屿弧线附近的开放海洋环境中.

关键词:
深海环境中的海洋环境.晚期的巴列奥普罗特罗纪时期.气循环是指气循环的循环.氧化还原条件的情况.

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