大氧化事件前海水氧的波动演化

IF 16.1 1区地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY

Nature Geoscience Pub Date : 2025-05-01 DOI:10.1038/s41561-025-01688-2

引用次数: 0

摘要

在大氧化事件期间，由海洋提供的大气氧气急剧上升。我们对之前海水氧合演化的研究表明，在大氧化事件发生之前，海水的氧化还原状态在缺氧和缺氧条件之间振荡，然后海洋氧合再次增加。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Fluctuating evolution of seawater oxygen before the Great Oxidation Event

查看原文本刊更多论文

Fluctuating evolution of seawater oxygen before the Great Oxidation Event

Atmospheric oxygen, supplied from the oceans, dramatically rose during the Great Oxidation Event. Our examination of the preceding evolution of seawater oxygenation revealed that the redox state in seawater oscillated between oxic and anoxic conditions before oceanic oxygenation again increased towards the dawn of the Great Oxidation Event.

求助全文

通过发布文献求助，成功后即可免费获取论文全文。去求助

来源期刊

Nature Geoscience 地学-地球科学综合

CiteScore

26.70

自引率

1.60%

发文量

187

审稿时长

3.3 months

期刊介绍： Nature Geoscience is a monthly interdisciplinary journal that gathers top-tier research spanning Earth Sciences and related fields. The journal covers all geoscience disciplines, including fieldwork, modeling, and theoretical studies. Topics include atmospheric science, biogeochemistry, climate science, geobiology, geochemistry, geoinformatics, remote sensing, geology, geomagnetism, paleomagnetism, geomorphology, geophysics, glaciology, hydrology, limnology, mineralogy, oceanography, paleontology, paleoclimatology, paleoceanography, petrology, planetary science, seismology, space physics, tectonics, and volcanology. Nature Geoscience upholds its commitment to publishing significant, high-quality Earth Sciences research through fair, rapid, and rigorous peer review, overseen by a team of full-time professional editors.