Evidence map›Paper›PMID 25642212›Full record

ArticleFrontiers in microbiology2014

Activity and phylogenetic diversity of sulfate-reducing microorganisms in low-temperature subsurface fluids within the upper oceanic crust.

Alberto Robador, Sean P Jungbluth, Douglas E LaRowe, Robert M Bowers, Michael S Rappé, Jan P Amend, James P Cowen

Open access · goldAbstract read
In one paragraph

Article in Frontiers in microbiology, 2014. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 23 papers.

0numbers the graph read from it
0cells of the map it votes in
23citing papers in PubMed
7.2field-weighted citation impact, top 3% of its field
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

23 citing papers in PubMed, 47 citations in OpenAlex.

  1. Article
  2. Species-resolved, single-cell respiration rates reveal dominance of sulfate reduction in a deep continental subsurface ecosystem.Proceedings of the National Academy of Sciences of the United States of America · 2024
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  10. Ecology of Subseafloor Crustal Biofilms.Frontiers in microbiology · 2019
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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

7 authors at 2 institutions in 1 country.

Alberto RobadorNASA Astrobiology Institute, University of Hawaii Honolulu, HI, USA.
Sean P JungbluthHawaii Institute of Marine Biology, School of Ocean and Earth Science and Technology, University of Hawaii Kaneohe, HI, USA ; Department of Oceanography, School of Ocean and Earth Science and Technology, University of Hawaii Honolulu, HI, USA.
Douglas E LaRoweDepartment of Earth Sciences, University of Southern California Los Angeles, CA, USA.
Robert M BowersNASA Astrobiology Institute, University of Hawaii Honolulu, HI, USA.
Michael S RappéHawaii Institute of Marine Biology, School of Ocean and Earth Science and Technology, University of Hawaii Kaneohe, HI, USA.
Jan P AmendDepartment of Earth Sciences, University of Southern California Los Angeles, CA, USA ; Department of Biological Sciences, University of Southern California Los Angeles, CA, USA.
James P CowenDepartment of Oceanography, School of Ocean and Earth Science and Technology, University of Hawaii Honolulu, HI, USA.
University of Hawaii System · USUniversity of Southern California · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The basaltic ocean crust is the largest aquifer system on Earth, yet the rates of biological activity in this environment are unknown. Low-temperature (<100°C) fluid samples were investigated from two borehole observatories in the Juan de Fuca Ridge (JFR) flank, representing a range of upper oceanic basement thermal and geochemical properties. Microbial sulfate reduction rates (SRR) were measured in laboratory incubations with (35)S-sulfate over a range of temperatures and the identity of the corresponding sulfate-reducing microorganisms (SRM) was studied by analyzing the sequence diversity of the functional marker dissimilatory (bi)sulfite reductase (dsrAB) gene. We found that microbial sulfate reduction was limited by the decreasing availability of organic electron donors in higher temperature, more altered fluids. Thermodynamic calculations indicate energetic constraints for metabolism, which together with relatively higher cell-specific SRR reveal increased maintenance requirements, consistent with novel species-level dsrAB phylotypes of thermophilic SRM. Our estimates suggest that microbially-mediated sulfate reduction may account for the removal of organic matter in fluids within the upper oceanic crust and underscore the potential quantitative impact of microbial processes in deep subsurface marine crustal fluids on marine and global biogeochemical carbon cycling.

Indexed as

basaltic ocean fluidsfunctional diversitymetabolic activitysubseafloor lifesulfate reduction

Identifiers

PMID25642212
PMCPMC4295021
OpenAlexW2036387492

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.