Quantifying Degradative Loss of Terrigenous Organic Carbon in Surface Sediments Across the Laptev and East Siberian Sea

Lisa Bröder, August Andersson, Tommaso Tesi, Igor Semiletov, Örjan Gustafsson

Research output: Contribution to journalArticle

Abstract

Ongoing permafrost thaw in the Arctic may remobilize large amounts of old organic matter. Upon transport to the Siberian shelf seas, this material may be degraded and released to the atmosphere, exported off-shelf, or buried in the sediments. While our understanding of the fate of permafrost-derived organic matter in shelf waters is improving, poor constraints remain regarding degradation in sediments. Here we use an extensive data set of organic carbon concentrations and isotopes (n = 109) to inventory terrigenous organic carbon (terrOC) in surficial sediments of the Laptev and East Siberian Seas (LS + ESS). Of these ~2.7 Tg terrOC about 55% appear resistant to degradation on a millennial timescale. A first-order degradation rate constant of 1.5 kyr−1 is derived by combining a previously established relationship between water depth and cross-shelf sediment-terrOC transport time with mineral-associated terrOC loadings. This yields a terrOC degradation flux of ~1.7 Gg/year from surficial sediments during cross-shelf transport, which is orders of magnitude lower than earlier estimates for degradation fluxes of dissolved and particulate terrOC in the water column of the LS + ESS. The difference is mainly due to the low degradation rate constant of sedimentary terrOC, likely caused by a combination of factors: (i) the lower availability of oxygen in the sediments compared to fully oxygenated waters, (ii) the stabilizing role of terrOC-mineral associations, and (iii) the higher proportion of material that is intrinsically recalcitrant due to its chemical/molecular structure in sediments. Sequestration of permafrost-released terrOC in shelf sediments may thereby attenuate the otherwise expected permafrost carbon-climate feedback.

Original languageEnglish
JournalGlobal Biogeochemical Cycles
DOIs
Publication statusPublished - 1 Jan 2019

Fingerprint

Organic carbon
Sediments
organic carbon
Permafrost
sediment
Degradation
permafrost
degradation
Surficial sediments
evolutionarily stable strategy
shelf sediment
Water
surficial sediment
Biological materials
Minerals
Rate constants
sea
loss
Carbon Isotopes
Fluxes

Keywords

  • Arctic shelves
  • carbon fluxes
  • degradation
  • marine sediments
  • permafrost

ASJC Scopus subject areas

  • Global and Planetary Change
  • Environmental Chemistry
  • Environmental Science(all)
  • Atmospheric Science

Cite this

Quantifying Degradative Loss of Terrigenous Organic Carbon in Surface Sediments Across the Laptev and East Siberian Sea. / Bröder, Lisa; Andersson, August; Tesi, Tommaso; Semiletov, Igor; Gustafsson, Örjan.

In: Global Biogeochemical Cycles, 01.01.2019.

Research output: Contribution to journalArticle

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