Journal
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
Volume 111, Issue 2, Pages 734-739Publisher
NATL ACAD SCIENCES
DOI: 10.1073/pnas.1314284111
Keywords
CH4; diazotrophy; mire; peat; phosphorus
Categories
Funding
- Academy of Finland [121535, 131409, 218101, 260797]
- Biological Interactions Graduate School
- Direct For Biological Sciences
- Division Of Environmental Biology [1019523] Funding Source: National Science Foundation
- Academy of Finland (AKA) [121535, 121535] Funding Source: Academy of Finland (AKA)
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Nitrogen (N) accumulation rates in peatland ecosystems indicate significant biological atmospheric N-2 fixation associated with Sphagnum mosses. Here, we show that the linkage between methanotrophic carbon cycling and N-2 fixation may constitute an important mechanism in the rapid accumulation of N during the primary succession of peatlands. In our experimental stable isotope enrichment study, previously overlooked methane-induced N-2 fixation explained more than one-third of the new N input in the younger peatland stages, where the highest N-2 fixation rates and highest methane oxidation activities co-occurred in the water-submerged moss vegetation.
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