Depositional Processes of Organic Matter in the Rhone River Delta (Gulf of Lion, France) Traced by Density Fractionation Coupled with ∆14C and δ13C
Bibliographic Data
| ID | 20972286 |
|---|---|
| Authors | Flora Toussaint (Université de Versailles Saint-Quentin-en-Yvelines, corresponding author) |
| Year | 2013 |
| Volume | 55 |
| Issue | 3–4 |
| Publication date | 2013-01-01 |
| Open Access | No |
| Type | ARTICLE |
| Venue | Radiocarbon (JOURNAL) |
| Journal identifiers | ISSN: 0033-8222 • E-ISSN: 1945-5755 |
| Publisher | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.2458/azu_js_rc.55.16287 |
| OpenAlex | W4229980646 |
| Language | EN |
| References cited | 2 |
As a main source of freshwater and particles, the Rhône River plays a major role in the biogeochemical cycle of organic carbon (OC) in the Mediterranean Sea. To better understand the origin of organic matter and the processes leading to its export to the coastal sea near the Rhône River, we measured radiocarbon (Δ14C) and stable carbon isotopes (δ13C) in the sediments of the delta, after density fractionation. In April 2007, 3 sites located along an offshore transect (A, C, and E) were sampled for surface sediments, and bulk sediment was separated into 4 fractions of different densities ( 2.5 g cm−3). In order to better understand the evolution of the OC along the transect, we investigated the OC sources and their evolution for each density fraction. Bulk OC shows a large increase in δ13C from −27.2′ nearshore to −24.5′ at offshore stations while Δ14C decreased from 59′ to −320′. The distribution of δ13C with density displayed a convex pattern at all stations. Except for fraction >2.5 g cm−3, δ13C increases by 2.5′ between stations A and E, indicating a loss of terrestrial signature. The distribution of Δ14C versus density had a concave pattern at all stations: at a single station, it showed a large heterogeneity with a difference of 500–600′ between the 2.5 g cm−3 had less variability, with an average δ13C of −24.6 ± 0.4′ and Δ14C of −370 ± 115′. Several processes may explain this distribution: retention in the prodelta of large particles; mineralization of all fractions during the transport and deposition in the delta and shelf sediments; and dilution of terrestrial particles in continental shelf pool
Biogeochemical cycle · Delta · Fractionation · Geomorphology · Isotopes of carbon · Mediterranean climate · Mediterranean sea · Organic matter · Radiocarbon dating · Sediment · Sedimentary depositional environment · Spatial distribution · Stable isotope ratio · Structural basin · Total organic carbon · Transect · δ13C · Chemistry · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Marine and coastal ecosystems · Ecology · Environmental Chemistry · Geology · Oceanography · Paleontology
| Highly cited | No |
|---|