The iron, manganese and phosphorus depositions in response to the Earth-Life system evolution across the Proterozoic and early Paleozoic transition
摘要截稿:
全文截稿: 2024-10-01
影响因子: 2.833
期刊难度:
CCF分类: 无
中科院JCR分区:
• 大类 : 地球科学 - 2区
• 小类 : 自然地理 - 3区
• 小类 : 地球科学综合 - 2区
• 小类 : 古生物学 - 1区
Overview
The Proterozoic-Paleozoic transition (ca. 720-520 Ma) witnessed notable changes in tectonic activity, global climate and environment, and biological evolution, including the breakup and assembly of supercontinents, the Snowball Earth events, global atmospheric and oceanic oxygenation, and the early animal radiation. As a result of co-evolution of life and environment, the Proterozoic-Paleozoic transition was also characterized by abundant ore depositions (e.g., P, Mn, Fe) that have been considered tightly related to changes in Earth’s surface environments, elemental cycles, and biological activity.
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Guest editors:
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Assoc. Prof. Guangyi Wei, PhDNanjing University, Nanjing, China
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Dr. Wenchao Yu, PhDChina University of Geosciences, Wuhan, China
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Dr. Haifeng Fan, PhDInstitute of Geochemistry, Chinese Academy of Sciences, Guizhou, China
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Dr. Jianbo Chen, PhDYunnan University, Kunming, China