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DOI :
10.3791/54251-v
July 24th, 2016
Chapters
0:05
Title
1:17
Preface and Column Assembly
3:15
Flushing Oxygen and Loading Medium
6:07
Inoculation and Sampling
7:33
Results: Cyanobacteria Inoculation
8:50
Conclusion
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。
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