4.8 Article

A decade of boreal rich fen greenhouse gas fluxes in response to natural and experimental water table variability

Journal

GLOBAL CHANGE BIOLOGY
Volume 23, Issue 6, Pages 2428-2440

Publisher

WILEY
DOI: 10.1111/gcb.13612

Keywords

carbon dioxide; climate change; ecosystem respiration; methane; peatland; soil temperature; water table; wetland

Funding

  1. National Science Foundation [DEB-0425328, DEB-0724514, DEB-0830997]
  2. Bonanza Creek Long-Term Ecological Research program - NSF [DEB-0620579]
  3. Bonanza Creek Long-Term Ecological Research program - USDA Forest Service Pacific Northwest Research Grant [PNW01-JV11261952-231]
  4. U.S. Geological Survey Climate and Land Use Change Program
  5. Climate Science Center grant funds
  6. Campus Alberta Innovates Program
  7. Direct For Biological Sciences
  8. Division Of Environmental Biology [1354370] Funding Source: National Science Foundation
  9. Division Of Environmental Biology
  10. Direct For Biological Sciences [1354007] Funding Source: National Science Foundation

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Rich fens are common boreal ecosystems with distinct hydrology, biogeochemistry and ecology that influence their carbon (C) balance. We present growing season soil chamber methane emission (F-CH4), ecosystem respiration (ER), net ecosystem exchange (NEE) and gross primary production (GPP) fluxes from a 9-years water table manipulation experiment in an Alaskan rich fen. The study included major flood and drought years, where wetting and drying treatments further modified the severity of droughts. Results support previous findings from peatlands that drought causes reduced magnitude of growing season F-CH4, GPP and NEE, thus reducing or reversing their C sink function. Experimentally exacerbated droughts further reduced the capacity for the fen to act as a C sink by causing shifts in vegetation and thus reducing magnitude of maximum growing season GPP in subsequent flood years by similar to 15% compared to control plots. Conversely, water table position had only a weak influence on ER, but dominant contribution to ER switched from autotrophic respiration in wet years to heterotrophic in dry years. Droughts did not cause interannual lag effects on ER in this rich fen, as has been observed in several nutrient-poor peatlands. While ER was dependent on soil temperatures at 2 cm depth, F-CH4 was linked to soil temperatures at 25 cm. Inter-annual variability of deep soil temperatures was in turn dependent on wetness rather than air temperature, and higher F-CH4 in flooded years was thus equally due to increased methane production at depth and decreased methane oxidation near the surface. Short-term fluctuations in wetness caused significant lag effects on F-CH4, but droughts caused no inter-annual lag effects on F-CH4. Our results show that frequency and severity of droughts and floods can have characteristic effects on the exchange of greenhouse gases, and emphasize the need to project future hydrological regimes in rich fens.

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