Reconstruction of past methane availability in an Arctic Alaska wetland indicates climate influenced methane release during the past ~12,000 years

Wooller, Matthew J., Pohlman, John W., Gaglioti, Benjamin V., Langdon, Peter, Jones, Miriam, Walter Antony, Katey M., Becker, Kevin W., Hinrichs, Kai-Uwe and Elvert, Marcus (2012) Reconstruction of past methane availability in an Arctic Alaska wetland indicates climate influenced methane release during the past ~12,000 years [in special issue: Holocene paleoenvironmental records from Arctic lake sediment] Journal of Paleolimnology, 48, (1), pp. 27-42. (doi:10.1007/s10933-012-9591-8).


[img] PDF Wooller_et_al_JoPL_2012.pdf - Version of Record
Restricted to Repository staff only

Download (856kB)


Atmospheric contributions of methane from Arctic wetlands during the Holocene are dynamic and linked to climate oscillations. However, long-term records linking climate variability to methane availability in Arctic wetlands are lacking. We present a multi-proxy ~12,000 year paleoecological reconstruction of intermittent methane availability from a radiocarbon-dated sediment core (LQ-West) taken from a shallow tundra lake (Qalluuraq Lake) in Arctic Alaska. Specifically, stable carbon isotopic values of photosynthetic biomarkers and methane are utilized to estimate the proportional contribution of methane-derived carbon to lake-sediment-preserved benthic (chironomids) and pelagic (cladocerans) components over the last *12,000 years. These results were compared to temperature, hydrologic, and habitat reconstructions from the same site using chironomid assemblage data, oxygen isotopes of chironomid head capsules, and radiocarbon ages of plant macrofossils. Cladoceran ephippia from ~4,000 cal year
BP sediments have d13C values that range from ~-39 to -31%, suggesting peak methane carbon assimilation at that time. These low d13C values coincide with an apparent decrease in effective moisture and development of a wetland that included Sphagnum subsecundum. Incorporation of methane derived carbon by chironomids and cladocerans decreased from ~2,500 to 1,500 cal year BP, coinciding with a temperature decrease. Live-collected chironomids with a radiocarbon age of 1,640 cal year BP, and fossil chironomids from 1,500 cal year BP in the core illustrate that ‘old’ carbon has also contributed to the development of the aquatic ecosystem since ~1,500 cal year BP. The relatively low d13C values of aquatic invertebrates (as low as -40.5%) provide evidence of methane incorporation by lake invertebrates, and suggest intermittent climate-linked methane release from the lake throughout the Holocene.

Item Type: Article
Digital Object Identifier (DOI): doi:10.1007/s10933-012-9591-8
ISSNs: 0921-2728 (print)
Keywords: chironomids, temperature, isotopes, oxygen, carbon, biomarkers

Organisations: Palaeoenvironment Laboratory (PLUS)
ePrint ID: 339657
Date :
Date Event
June 2012Published
Date Deposited: 29 May 2012 09:14
Last Modified: 17 Apr 2017 17:04
Further Information:Google Scholar

Actions (login required)

View Item View Item