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Journal / Environment / 一个铁（II）的实验室模拟的前寒武纪富海洋上升流系统探索光合细菌生长…
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一个铁（II）的实验室模拟的前寒武纪富海洋上升流系统探索光合细菌生长
 
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一个铁（II）的实验室模拟的前寒武纪富海洋上升流系统探索光合细菌生长

Article DOI: 10.3791/54251-v • 09:45 min • July 24th, 2016
July 24th, 2016 •
1,2, 1, 1, 1,2
1Department of Geosciences, University of Tuebingen, 2Department of Geological and Atmospheric Sciences, Iowa State University

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我们在实验室规模的垂直流通柱模拟了前寒武纪海洋铁质系统上涌。我们的目标是了解O 2和Fe（II）如何地球化学剖面演变为蓝藻产生O 2。结果表明，由于通过光合作用产生氧气的Fe（II）氧化建立chemocline的。

Tags

环境科学，第113，地质微生物，水柱，铁（II）氧化，光合作用，太古海洋，蓝藻，大氧化事件，条带状含铁建造
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