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Warming promotes the use of organic matter as an electron acceptor in a peatland

Journal Article · · Geoderma
 [1];  [2];  [2];  [2];  [3];  [2]
  1. Chapman Univ., Orange, CA (United States); Univ. of Colorado, Boulder, CO (United States); OSTI
  2. Chapman Univ., Orange, CA (United States)
  3. Univ. of Oregon, Eugene, OR (United States)

Peatlands store approximately one-half of terrestrial soil organic carbon (C) and the future of this C in the face of ongoing global change remains a key question in global biogeochemistry. Particularly pressing is the need to understand if this C will remain in peatland soils or be returned to the atmosphere as the potent greenhouse gas methane (CH4) in response to warming. Past work has demonstrated that the microbial reduction of organic matter (OM) as an alternative terminal electron acceptor (TEA) under anaerobic conditions can suppress CH4 production and is a key mechanistic control of peatland CH4 dynamics. Here we show that warming directly enhances rates of potential OM reduction in peatland soils, enhancing acetate availability and allowing for a faster onset of CH4 production. Finally, using soils collected from the ecosystem-scale Spruce and Peatland Responses Under Changing Environments (SPRUCE) experiment, we also show that while there were no indirect effects of 2 years of soil warming on potential OM reduction through changes in soil quality, warming-mediated lowering of the water table increased the volume of oxidized OM which will suppress CH4 production following rewetting events.

Research Organization:
Chapman Univ., Orange, CA (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
SC0014416
OSTI ID:
1977160
Alternate ID(s):
OSTI ID: 1798945
Journal Information:
Geoderma, Journal Name: Geoderma Journal Issue: C Vol. 401; ISSN 0016-7061
Publisher:
ElsevierCopyright Statement
Country of Publication:
United States
Language:
English

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