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Cited by 288

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"

Mikucki, Jill A., Pearson, Ann, Johnston, David T., Turchyn, Alexandra V., Farquhar, James, Schrag, Daniel P., Anbar, Ariel D., Priscu, John C., Lee, Peter A.·2009·Science

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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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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CoChat. (2026). Citation check: A Contemporary Microbially Maintained Subglacial Ferrous "Ocean". https://app.cochat.ai/papers/10.1126/science.1167350
The paper
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. (2009). A Contemporary Microbially Maintained Subglacial Ferrous "Ocean". Science. https://doi.org/10.1126/science.1167350

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