Ecological processes dominate the ¹³C land disequilibrium in a Rocky Mountain subalpine forest
Fossil fuel combustion has increased atmospheric COâ byâ~â115 µmol mol-1 since 1750 and decreased its carbon isotope composition (δ¹³C) by 1.7-2â° (the ¹³C Suess effect). Because carbon is stored in the terrestrial biosphere for decades and longer, the δ¹³C of COâ released by terrestrial ecosystems is expected to differ from the δ¹³C of COâ assimilated by land plants during photosynthesis. This isotopic difference between land-atmosphere respiration (δR) and photosynthetic assimilation (δA) fluxes gives rise to the ¹³C land disequilibrium (D). Contemporary understanding suggests that over annual and longer time scales, D is determined primarily by the Suess effect, and thus, D is generally positive (δRâ>âδA). A 7 year record of biosphere-atmosphere carbon exchange was used to evaluate the seasonality of δA and δR, and the ¹³C land disequilibrium, in a subalpine conifer forest. A novel isotopic mixing model was employed to determine the δ¹³C of net land-atmosphere exchange during day and night and combined with tower-based flux observations to assess δA and δR. The disequilibrium varied seasonally and when flux-weighted was opposite in sign than expected from the Suess effect (Dâ=ââ0.75â±â0.21â° or â0.88â±â0.10â° depending on method). Seasonality in D appeared to be driven by photosynthetic discrimination (Îcanopy) responding to environmental factors. Possible explanations for negative D include (1) changes in Îcanopy over decades as COâ and temperature have risen, and/or (2) post-photosynthetic fractionation processes leading to sequestration of isotopically enriched carbon in long-lived pools like wood and soil.
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https://n2t.org/ark:/85065/d7r78g5f
eng
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2016-01-01T00:00:00Z
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2014-04-01T00:00:00Z
Copyright 2014 American Geophysical Union.
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