Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation

Adrian Schilt (), Edward J. Brook, Thomas K. Bauska, Daniel Baggenstos, Hubertus Fischer, Fortunat Joos, Vasilii V. Petrenko, Hinrich Schaefer, Jochen Schmitt, Jeffrey P. Severinghaus, Renato Spahni and Thomas F. Stocker
Additional contact information
Adrian Schilt: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Edward J. Brook: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Thomas K. Bauska: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Daniel Baggenstos: Scripps Institution of Oceanography, University of California
Hubertus Fischer: Climate and Environmental Physics, Physics Institute, and Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
Fortunat Joos: Climate and Environmental Physics, Physics Institute, and Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
Vasilii V. Petrenko: University of Rochester
Hinrich Schaefer: National Institute of Water and Atmospheric Research, Wellington 6021, New Zealand
Jochen Schmitt: Climate and Environmental Physics, Physics Institute, and Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
Jeffrey P. Severinghaus: Scripps Institution of Oceanography, University of California
Renato Spahni: Climate and Environmental Physics, Physics Institute, and Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
Thomas F. Stocker: Climate and Environmental Physics, Physics Institute, and Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland

Nature, 2014, vol. 516, issue 7530, 234-237

Abstract: Analysis of air trapped in Antarctic ice between 16,000 and 10,000 years before present yields nitrous oxide concentrations and isotopic data showing that the relative contributions from marine and terrestrial sources to nitrous oxide emission changes were equal during that period, but that terrestrial emissions dominated on centennial timescales.

Date: 2014
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DOI: 10.1038/nature13971

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