Authors

Kai Uwe Hinrichs, University of Bremen
Verena B. Heuer, University of Bremen
Fumio Inagaki, Japan Agency for Marine-Earth Science and Technology
Yuki Morono, Japan Agency for Marine-Earth Science and Technology
Yusuke Kubo, Japan Agency for Marine-Earth Science and Technology
Arthur J. Spivack, University of Rhode Island
Bernhard Viehweger, University of Bremen
Tina Treude, University of California at Los Angeles
Felix Beulig, Aarhus University
Florence Schubotz, University of Bremen
Satoshi Tonai, Kochi University
Stephen A. Bowden, University of Aberdeen
Margaret Cramm, University of Calgary
Susann Henkel, Alfred Wegener Institute - Helmholtz Centre for Polar and Marine Research
Takehiro Hirose, Japan Agency for Marine-Earth Science and Technology
Kira Homola, University of Rhode Island
Tatsuhiko Hoshino, Japan Agency for Marine-Earth Science and Technology
Akira Ijiri, Japan Agency for Marine-Earth Science and Technology
Hiroyuki Imachi, Japan Agency for Marine-Earth Science and Technology
Nana Kamiya, Nihon University
Masanori Kaneko, National Institute of Advanced Industrial Science and Technology
Lorenzo Lagostina, Swiss Federal Institute of Technology Zurich
Hayley Manners, School of Geography, Earth and Environmental Sciences
Harry Luke McClelland, Washington University St. Louis
Kyle Metcalfe, California Institute of Technology
Natsumi Okutsu, The University of Tokyo
Donald Pan, Japan Agency for Marine-Earth Science and Technology
Maija J. Raudsepp, University of Queensland
Justine Sauvage, University of Rhode Island
Man Yin Tsang, University of Toronto
Emily Whitaker
Yuzuru Yamamoto
Kiho Yang
Lena Maeda
Rishi R. Adhikari
Clemens Glombitza
Yohei Hamada
Jens Kallmeyer
Jenny Wendt
Lars Wörmer
Yasuhiro Yamada
Masataka Kinoshita
Kai Uwe Hinrichs

ORCID

Abstract

Microorganisms in marine subsurface sediments substantially contribute to global biomass. Sediments warmer than 40°C account for roughly half the marine sediment volume, but the processes mediated by microbial populations in these hard-to-access environments are poorly understood. We investigated microbial life in up to 1.2-kilometer-deep and up to 120°C hot sediments in the Nankai Trough subduction zone. Above 45°C, concentrations of vegetative cells drop two orders of magnitude and endospores become more than 6000 times more abundant than vegetative cells. Methane is biologically produced and oxidized until sediments reach 80° to 85°C. In 100° to 120°C sediments, isotopic evidence and increased cell concentrations demonstrate the activity of acetate-degrading hyperthermophiles. Above 45°C, populated zones alternate with zones up to 192 meters thick where microbes were undetectable.

Publication Date

2020-12-04

Publication Title

Science

Volume

370

Issue

6521

ISSN

0036-8075

Embargo Period

2020-12-16

First Page

1230

Last Page

1234

10.1126/science.abd7934" data-hide-no-mentions="true">

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