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American Association for the Advancement of Science, Science, 6161(342), p. 964-966, 2013

DOI: 10.1126/science.1238920

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Constraints on the Late Holocene Anthropogenic Contribution to the Atmospheric Methane Budget

Journal article published in 2013 by Logan Mitchell ORCID, Ed Brook, James E. Lee, Christo Buizert ORCID, Todd Sowers
This paper is available in a repository.
This paper is available in a repository.

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Abstract

Bipolar Signature Atmospheric methane has increased approximately 2.5-fold since the start of the industrial revolution, a consequence of human activity. However, a smaller and more gradual rise began around 6000 years ago, near the time when human agriculture began to develop and expand. Mitchell et al. (p. 964 ) present two, high-resolution ice core methane records of the past 2500 years, one from each pole. Methane emissions were primarily from the tropics, with secondary contributions from the higher latitudes where most humans lived. Thus, both natural and human sources are needed to explain the late-Holocene atmospheric methane record.