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Contribution of river‐borne soil organic carbon to the Gulf of Lions (NW Mediterranean)
Author(s) -
Kim J.-H,
Zarzycka B.,
Buscail R.,
Peterse F.,
Bonnin J.,
Ludwig W.,
Schouten S.,
Sinninghe Damsté J. S.
Publication year - 2010
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.2010.55.2.0507
Subject(s) - mediterranean climate , environmental science , watershed , total organic carbon , mediterranean sea , hydrology (agriculture) , soil water , submarine pipeline , continental shelf , soil carbon , soil horizon , oceanography , soil science , geology , environmental chemistry , ecology , chemistry , biology , geotechnical engineering , machine learning , computer science
We determined the spatial distribution patterns of the Branched and Isoprenoid Tetraether (BIT) index, a specific proxy of riverborne soil organic carbon (OC) input from land to the ocean, by analyzing soils from the Têt watershed (France) and surface sediments from the Gulf of Lions (NW Mediterranean) into which the Têet and Rhône Rivers flow. The BIT index pattern in the Têt watershed is heterogeneously distributed, varying between 0.2 and 1.0, with an average BIT value of 0.84 ± 0.14 ( n = 58). Soil pH is the major factor controlling soil BIT values among the environmental factors considered on the basis of the statistical analysis of environmental parameters and glycerol dialkyl glycerol tetraether concentrations. In the Gulf of Lions, BIT values range from 0.01 to 0.85, with higher values along the coast compared with those offshore. The soil OC contributions to the total organic carbon (TOC), estimated on the basis of the BIT index, are > 10% along the coast, whereas those from the outer shelf and the continental slope are < 10%.