Iron reduction and mineralization of deep‐sea iron reducing bacterium Shewanella piezotolerans WP3 at elevated hydrostatic pressures. Issue 6 (17th September 2013)

• Record Type: Journal Article
• Authors: Wu, W. F.; Wang, F. P.; Li, J. H.; Yang, X. W.; Xiao, X.; Pan, Y. X.
• Is Part Of: Geobiology. Volume 11:Issue 6(2013:Nov.)
• Page Start: 593
• Page End: 601
• Publication Date: 2013-09-17
• Subjects: Geobiology -- Periodicals; Biogeochemistry -- Periodicals; Ecology -- Periodicals; 551
• DOI: 10.1111/gbi.12061
• Languages: English
• ISSNs: 1472-4677

Abstract

<abstract abstract-type="main" id="gbi12061-abs-0001"> <title>Abstract</title> <p>In this study, iron reduction and concomitant biomineralization of a deep‐sea iron reducing bacterium (IRB), <italic>Shewanella piezotolerans </italic>WP3, were systematically examined at different hydrostatic pressures (0.1, 5, 20, and 50 MPa). Our results indicate that bacterial iron reduction and induced biomineralization are influenced by hydrostatic pressure. Specifically, the iron reduction rate and extent consistently decreases with the increase in hydrostatic pressure. By extrapolation, the iron reduction rate should drop to zero by ~68 MPa, which suggests a possible shut‐off of enzymatic iron reduction of WP3 at this pressure. Nano‐sized superparamagnetic magnetite minerals are formed under all the experimental pressures; nevertheless, even as magnetite production decreases, the crystallinity and grain size of magnetite minerals increase at higher pressure. These results imply that IRB may play an important role in iron reduction, biomineralization, and biogeochemical cycling in deep‐sea environments.</p> </abstract>