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Changes in global nitrogen cycling during the Holocene epoch.

Abstract:

Human activities have doubled the pre-industrial supply of reactive nitrogen on Earth, and future rates of increase are expected to accelerate. Yet little is known about the capacity of the biosphere to buffer increased nitrogen influx. Past changes in global ecosystems following deglaciation at the end of the Pleistocene epoch provide an opportunity to understand better how nitrogen cycling in the terrestrial biosphere responded to changes in carbon cycling. We analysed published records of ...

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Publication status:
Published

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Publisher copy:
10.1038/nature11916

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Institution:
University of Oxford
Department:
Oxford, MPLS, Zoology
Role:
Author
Journal:
Nature
Volume:
495
Issue:
7441
Pages:
352-355
Publication date:
2013-03-05
DOI:
EISSN:
1476-4687
ISSN:
0028-0836
URN:
uuid:3d30cec5-899c-439f-afee-35980d45c37d
Source identifiers:
395482
Local pid:
pubs:395482

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