The distribution of active iron cycling bacteria in marine and freshwater sediments is decoupled from geochemical gradients.
Otte, Julia M.
ORCID: https://orcid.org/0000-0001-8012-0413, Harter, J., Laufer, K., Blackwell, N., Kappler, A. and Kleindienst, S.
;
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julia.otte [ at ] awi.de
Abstract
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Article
Authors
Otte, Julia M.
ORCID: https://orcid.org/0000-0001-8012-0413, Harter, J., Laufer, K., Blackwell, N., Kappler, A. and Kleindienst, S.
;

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Published
Eprint ID
50953
DOI
10.1111/1462-2920.14260
Cite as
Otte, J. M.
,
Harter, J.
,
Laufer, K.
,
Blackwell, N.
,
Kappler, A.
and
Kleindienst, S.
(2018):
The distribution of active iron cycling bacteria in marine and freshwater sediments is decoupled from geochemical gradients.
,
Environmental Microbiology,
20
(7),
pp. 2483-2499
.
doi: 10.1111/1462-2920.14260
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