High rates of microbial carbon turnover in sediments in the deepest oceanic trench on Earth-Reference-Cited by-同舟云学术

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High rates of microbial carbon turnover in sediments in the deepest oceanic trench on Earth

Published:2013-03-17 Issue:4 Volume:6 Page:284-288
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Glud Ronnie N.,Wenzhöfer Frank,Middelboe Mathias,Oguri Kazumasa,Turnewitsch Robert,Canfield Donald E.,Kitazato Hiroshi

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo1773.pdf

Reference28 articles.

1. Canfield, D. E. in Interactions Of C,N,P, And S Biogeochemical Cycles And Global Change (eds Wollast, R., F., Mackenzie, T. & Chou, L.) 333–363 (Springer, 1993).

2. Glud, R. N. Oxygen dynamics of marine sediments. Mar. Biol. Res. 4, 243–289 (2008).

3. Burdige, D. J. Geochemistry of Marine Sediments (Princeton Univ. Press,.

4. Jamieson, A. J. Ecology of deep oceans: Hadal trenches eLS http://dx.doi.org/10.1002/9780470015902.a0023606 (Wiley, 2011).

5. Taira, K., Kitagawa, S., Yamashiro, T. & Yanagimoto, D. Deep and bottom currents in the challenger deep, measured with super-deep current meters. J. Oceanogr. 60, 919–926 (2004).

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