Physiology, Fe(II) oxidation, and Fe mineral formation by a marine planktonic cyanobacterium grown under ferruginous conditions
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چکیده
Citation: Swanner ED, Wu W, Hao L, Wüstner ML, Obst M, Moran DM, McIlvin MR, Saito MA and Kappler A (2015) Physiology, Fe(II) oxidation, and Fe mineral formation by a marine planktonic cyanobacterium grown under ferruginous conditions. Front. Earth Sci. 3:60. doi: 10.3389/feart.2015.00060 Physiology, Fe(II) oxidation, and Fe mineral formation by a marine planktonic cyanobacterium grown under ferruginous conditions
منابع مشابه
Phototrophic Fe(II)-oxidation in the chemocline of a ferruginous meromictic lake
Precambrian Banded Iron Formation (BIF) deposition was conventionally attributed to the precipitation of iron-oxides resulting from the abiotic reaction of ferrous iron (Fe(II)) with photosynthetically produced oxygen. Earliest traces of oxygen date from 2.7 Ga, thus raising questions as to what may have caused BIF precipitation before oxygenic photosynthesis evolved. The discovery of anoxygeni...
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تاریخ انتشار 2015