4.7 Article

The hadal zone is an important and heterogeneous sink of black carbon in the ocean

Journal

COMMUNICATIONS EARTH & ENVIRONMENT
Volume 3, Issue 1, Pages -

Publisher

SPRINGERNATURE
DOI: 10.1038/s43247-022-00351-7

Keywords

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Funding

  1. National Natural Science Foundation of China [41976030, 42076029, 91951210]
  2. Open Research Fund of State Key Laboratory of Estuarine and Coastal Research [SKLEC-KF202108]
  3. China Post-doctoral Science Foundation [2020M682768]
  4. Danish National Research Foundation via the Danish Center for Hadal Research [DNRF145]
  5. SUSTech Presidential Postdoctoral Fellowship
  6. Shanghai Sheshan National Geophysical Observatory [2020Z01]
  7. HADES-ERC Advanced grant [669947]

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Black carbon accumulation rates in hadal trenches in the deepest regions of the oceans could be seven-fold higher than the global ocean average, according to geochemical and isotopic analyses of sediments from six trenches in the Pacific Ocean.
Black carbon is ubiquitous in the marine environment. However, whether it accumulates in the deepest ocean region, the hadal zone, is unknown. Here we measure the concentration and carbon isotopes (delta C-13 and Delta C-14) of black carbon and total organic carbon in sediments from six hadal trenches. Black carbon constituted 10% of trench total organic carbon, and its delta C-13 and Delta C-14 were more negative than those of total organic carbon, suggesting that the black carbon was predominantly derived from terrestrial C3 plants and fossil fuels. The contribution of fossil carbon to the black carbon pool was spatially heterogeneous, which could be related to differences in the distance to landmass, land cover and socioeconomic development. Globally, we estimate a black carbon burial rate of 1.0 +/- 0.5 Tg yr(-1) in the hadal zone, which is seven-fold higher than the global ocean average per unit area. We propose that the hadal zone is an important, but overlooked, sink of black carbon in the ocean. Black carbon accumulation rates in hadal trenches in the deepest regions of the oceans could be seven-fold higher than the global ocean average, according to geochemical and isotopic analyses of sediments from six trenches in the Pacific Ocean.

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