Landscape-Scale Variability of Organic Carbon Burial by SW Greenland Lakes

Lakes are a key feature of arctic landscapes and can be an important component of regional organic carbon (OC) budgets, but C burial rates are not well estimated. 210 Pb-dated sediment cores and carbon and organic matter (as loss-on-ignition) content were used to estimate OC burial for 16 lakes in S...

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Bibliographic Details
Main Authors: Anderson, NJ, Appleby, PG, Bindler, R, Renberg, I, Conley, DJ, Fritz, SC, Jones, VJ, Whiteford, EJ, Yang, H
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Nitrogen
arctic
diatoms
tundra
biogenic silica
DOC
soil carbon
Arctic
Greenland
Tundra
Online Access:https://discovery.ucl.ac.uk/id/eprint/10074859/1/Anderson2019_Article_Landscape-ScaleVariabilityOfOr.pdf
https://discovery.ucl.ac.uk/id/eprint/10074859/
Description
Summary:Lakes are a key feature of arctic landscapes and can be an important component of regional organic carbon (OC) budgets, but C burial rates are not well estimated. 210 Pb-dated sediment cores and carbon and organic matter (as loss-on-ignition) content were used to estimate OC burial for 16 lakes in SW Greenland. Burial rates were corrected for sediment focusing using the 210 Pb flux method. The study lakes span a range of water chemistries (conductivity range 25–3400 µS cm −1 ), areas (< 4–100 ha) and maximum depths (~ 10–50 m). The regional average focusing-corrected OC accumulation rate was ~ 2 g C m −2 y −1 prior to ~ 1950 and 3.6 g C m −2 y −1 after 1950. Among-lake variability in post-1950 OC AR was correlated with in-lake dissolved organic carbon concentration, conductivity, altitude and location along the fjord. Twelve lakes showed an increase in mean OC AR over the analyzed time period, ~ 1880–2000; as the study area was cooling until recently, this increase is probably attributable to other global change processes, for example, altered inputs of N or P. There are ~ 20,000 lakes in the study area ranging from ~ 1 ha to more than 130 km 2 , although over 83% of lakes are less than 10 ha. Extrapolating the mean post-1950 OC AR (3.6 g C m −2 y −1 ) to all lakes larger than 1000 ha and applying a lower rate of ~ 2 g C m −2 y −1 to large lakes (> 1000 ha) suggests a regional annual lake OC burial rate of ~ 10.14 × 10 9 g C y −1 post 1950. Given the low C content of soils in this area, lakes represent a substantial regional C store.

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