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Updated: Jul 1, 2025

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

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在过去的20亿年里,地球表面Mg循环的演变

Zhiguang Xia1,2,3,4, Shilei Li2,5, Zhongya Hu1,6

  • 1State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, Jiangsu, China.

Science advances
|March 1, 2024
PubMed
概括

同位素记录显示,石头石的净埋葬量下降了20亿年,影响了地球的气候. 这项研究将多洛石的气候变化和埋葬周期与长期气候演变联系起来.

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Published on: June 13, 2015

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Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment

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