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Updated: May 8, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
09:45

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

在富含铁的地下水排放区中,甲类古生物的垂直分布

Katsunori Yanagawa1, Misaki Okabeppu1, Sakiko Kikuchi2

  • 1Faculty of Environmental Engineering, The University of Kitakyushu, Kitakyushu, Fukuoka, Japan.

PloS one
|February 24, 2025
PubMed
概括

在日本的淡水池中观察到甲与铁减少 (Fe-AOM) 的无氧氧化,显示出显著的甲去除率. 这项研究阐明了推动这一关键生物地化学过程的环境因素和微生物群落.

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Published on: September 11, 2016

Experimental Column Setup for Studying Anaerobic Biogeochemical Interactions Between Iron (Oxy)Hydroxides, Trace Elements, and Bacteria06:52

Experimental Column Setup for Studying Anaerobic Biogeochemical Interactions Between Iron (Oxy)Hydroxides, Trace Elements, and Bacteria

Published on: December 19, 2017

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The Sulfur Cycle01:22

The Sulfur Cycle

Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
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