Literature DB >> 28055128

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

David Olefeldt1,2, Eugénie S Euskirchen3, Jennifer Harden4, Evan Kane5, A David McGuire6, Mark P Waldrop4, Merritt R Turetsky1.   

Abstract

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 (FCH4 ), 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 FCH4 , 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 ~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 inter-annual 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, FCH4 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 FCH4 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 FCH4 , but droughts caused no inter-annual lag effects on FCH4 . 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.
© 2017 John Wiley & Sons Ltd.

Entities:  

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

Mesh:

Substances:

Year:  2017        PMID: 28055128     DOI: 10.1111/gcb.13612

Source DB:  PubMed          Journal:  Glob Chang Biol        ISSN: 1354-1013            Impact factor:   10.863


  3 in total

1.  The Rhizosphere Responds: Rich Fen Peat and Root Microbial Ecology after Long-Term Water Table Manipulation.

Authors:  Danielle L Rupp; Louis J Lamit; Stephen M Techtmann; Evan S Kane; Erik A Lilleskov; Merritt R Turetsky
Journal:  Appl Environ Microbiol       Date:  2021-05-26       Impact factor: 4.792

2.  Soil nitrogen determines greenhouse gas emissions from northern peatlands under concurrent warming and vegetation shifting.

Authors:  Junwei Luan; Jianghua Wu; Shirong Liu; Nigel Roulet; Mei Wang
Journal:  Commun Biol       Date:  2019-04-18

3.  Measuring CO2 and CH4 with a portable gas analyzer: Closed-loop operation, optimization and assessment.

Authors:  Jeremy Wilkinson; Christoph Bors; Florian Burgis; Andreas Lorke; Pascal Bodmer
Journal:  PLoS One       Date:  2018-04-04       Impact factor: 3.240

  3 in total

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