The DOI matches its Crossref record; 21 of the 21 references it cites were found in a registry or an index.
A Contemporary Microbially Maintained Subglacial Ferrous "Ocean"
Abstract
An active microbial assemblage cycles sulfur in a sulfate-rich, ancient marine brine beneath Taylor Glacier, an outlet glacier of the East Antarctic Ice Sheet, with Fe(III) serving as the terminal electron acceptor. Isotopic measurements of sulfate, water, carbonate, and ferrous iron and functional gene analyses of adenosine 5′-phosphosulfate reductase imply that a microbial consortium facilitates a catalytic sulfur cycle. These metabolic pathways result from a limited organic carbon supply because of the absence of contemporary photosynthesis, yielding a subglacial ferrous brine that is anoxic but not sulfidic. Coupled biogeochemical processes below the glacier enable subglacial microbes to grow in extended isolation, demonstrating how analogous organic-starved systems, such as Neoproterozoic oceans, accumulated Fe(II) despite the presence of an active sulfur cycle.
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Cites
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Self-citationA new model for Proterozoic ocean chemistry
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Cited by
Johnston, D. T., Poulton, S. W., Dehler, C., Porter, S., Husson, J., Canfield, D. E., & Knoll, A. H. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2009.11.059 · Cited by 216
Self-citationGlacial ecosystems are essential to understanding biodiversity responses to glacier retreat
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From Water and Ions to Crowded Biomacromolecules: In Vivo Structuring of a Prokaryotic Cell
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Metadata
- Authors
- Mikucki, J. A., Pearson, A., Johnston, D. T., Turchyn, A. V., Farquhar, J., Schrag, D. P., Anbar, A. D., Priscu, J. C., & Lee, P. A.
- Venue
- Science
- Published
- 2009-04-17
- Volume
- 324
- Issue
- 5925
- Pages
- 397-400
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2016576552
- Cited by
- 288
- References
- 21
- FWCI
- 17.36
- Type
- journal article
- Language
- en
- Open access
- closed
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