Sediment Characteristics and Methane Ebullition in Three Subarctic Lakes

Wik, Martin; Johnson, Joel E.; Crill, Patrick M.; DeStasio, Joel P.; Erickson, Lance; Halloran, Madison J.; Fahnestock, M. Florencia; Crawford, Maurice K.; Phillips, Stephen C.; Varner, Ruth K.

doi:10.1029/2017jg004298

Title: Sediment Characteristics and Methane Ebullition in Three Subarctic Lakes

Journal Article · Wed Jul 11 00:00:00 EDT 2018 · Journal of Geophysical Research. Biogeosciences

DOI:https://doi.org/10.1029/2017jg004298· OSTI ID:1539734

^[1];

^[2];

^[1]; DeStasio, Joel P. ^[2]; Erickson, Lance ^[2]; Halloran, Madison J. ^[2]; Fahnestock, M. Florencia ^[2]; Crawford, Maurice K. ^[3];

^[4];

^[2]

Stockholm Univ. (Sweden)
Univ. of New Hampshire, Durham, NH (United States)
Univ. of Maryland Eastern Shore, Princes Anne, MD (United States)
Univ. of New Hampshire, Durham, NH (United States); Univ. of Texas, Austin, TX (United States)

Abstract Ebullition (bubbling) from climate‐sensitive northern lakes remains an unconstrained source of atmospheric methane (CH ₄ ). Although the focus of many recent studies, ebullition is rarely linked to the physical characteristics of lakes. In this study we analyze the sediments of subarctic postglacial lakes and investigate how sediment properties relate to the large spatial variation in CH ₄ bubble flux, quantified over multiple years using bubble traps. The results show that the sediments from our lakes are rich in total organic carbon, containing 37 kg/m ³ on average. This number is roughly 40% higher than the average for yedoma deposits, which have been identified as high CH ₄ emitters. However, the quantity of total organic carbon is not a useful indicator of high emissions from the study lakes. Neither is the amount of CH ₄ in the sediment a reliable measure of ebullition potential. Instead, our data point to coarse detritus, partly from buried submerged aquatic vegetation and redeposited peat as spatial controls on fluxes, often in combination with previously established effects of incoming solar radiation and water depth. The results once again highlight the climate sensitivity of northern lakes, indicating that biological responses to warmer waters and increased energy input and heating of organic sediments during longer ice‐free seasons can substantially alter future CH ₄ emissions.

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Research Organization:: Univ. of Arizona, Tucson, AZ (United States)

Sponsoring Organization:: USDOE Office of Science (SC)

Grant/Contract Number:: SC0004632; SC0010580; DE‐SC0004632 and DE‐SC0010580

OSTI ID:: 1539734

Alternate ID(s):: OSTI ID: 1465892

Journal Information:: Journal of Geophysical Research. Biogeosciences, Vol. 123, Issue 8; ISSN 2169-8953

Publisher:: American Geophysical UnionCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 32 works

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