Presence of oxygen and aerobic communities from sea floor to basement in deep-sea sediments

Authors

Steven D'hondt, Integrated Ocean Drilling Program Expedition
Fumio Inagaki, Integrated Ocean Drilling Program Expedition
Carlos Alvarez Zarikian, Integrated Ocean Drilling Program Expedition
Lewis J. Abrams, University of North Carolina Wilmington
Nathalie Dubois, Integrated Ocean Drilling Program Expedition
Tim Engelhardt, Integrated Ocean Drilling Program Expedition
Helen Evans, Integrated Ocean Drilling Program Expedition
Timothy Ferdelman, Integrated Ocean Drilling Program Expedition
Britta Gribsholt, Integrated Ocean Drilling Program Expedition
Robert N. Harris, Integrated Ocean Drilling Program Expedition
Bryce W. Hoppie, Integrated Ocean Drilling Program Expedition
Jung Ho Hyun, Integrated Ocean Drilling Program Expedition
Jens Kallmeyer, Integrated Ocean Drilling Program Expedition
Jinwook Kim, Integrated Ocean Drilling Program Expedition
Jill E. Lynch, Integrated Ocean Drilling Program Expedition
Claire C. Mckinley, Texas A&M University
Satoshi Mitsunobu, Integrated Ocean Drilling Program Expedition
Yuki Morono, Integrated Ocean Drilling Program Expedition
Richard W. Murray, Integrated Ocean Drilling Program Expedition
Robert Pockalny, University of Rhode Island
Justine Sauvage, University of Rhode Island
Takaya Shimono, Integrated Ocean Drilling Program Expedition
Fumito Shiraishi, Integrated Ocean Drilling Program Expedition
David C. Smith, Integrated Ocean Drilling Program Expedition
Christopher E. Smith-Duque, Integrated Ocean Drilling Program Expedition
Arthur J. Spivack, Integrated Ocean Drilling Program Expedition
Bjorn Olav Steinsbu, Integrated Ocean Drilling Program Expedition
Yohey Suzuki, Integrated Ocean Drilling Program Expedition
Michal Szpak, Integrated Ocean Drilling Program Expedition
Laurent Toffin, Integrated Ocean Drilling Program Expedition
Goichiro Uramoto, Integrated Ocean Drilling Program Expedition
Yasuhiko T. Yamaguchi, Integrated Ocean Drilling Program Expedition
Guo Liang Zhang, Integrated Ocean Drilling Program Expedition
Xiao Hua Zhang, Integrated Ocean Drilling Program Expedition
Wiebke Ziebis, Integrated Ocean Drilling Program Expedition

Document Type

Article

Date of Original Version

4-4-2015

Abstract

The depth of oxygen penetration into marine sediments differs considerably from one region to another. In areas with high rates of microbial respiration, O 2 penetrates only millimetres to centimetres into the sediments, but active anaerobic microbial communities are present in sediments hundreds of metres or more below the sea floor. In areas with low sedimentary respiration, O 2 penetrates much deeper but the depth to which microbial communities persist was previously unknown. The sediments underlying the South Pacific Gyre exhibit extremely low areal rates of respiration. Here we show that, in this region, microbial cells and aerobic respiration persist through the entire sediment sequence to depths of at least 75 metres below sea floor. Based on the Redfield stoichiometry of dissolved O 2 and nitrate, we suggest that net aerobic respiration in these sediments is coupled to oxidation of marine organic matter. We identify a relationship of O 2 penetration depth to sedimentation rate and sediment thickness. Extrapolating this relationship, we suggest that oxygen and aerobic communities may occur throughout the entire sediment sequence in 15-44% of the Pacific and 9-37% of the global sea floor. Subduction of the sediment and basalt from these regions is a source of oxidized material to the mantle.

Publication Title, e.g., Journal

Nature Geoscience

Volume

8

Issue

4

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