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International audience; We tested the applicability of the BIT (branched and isoprenoid tetraether) index as a proxy for palaeoflood events in the river-dominated continental margin of the Gulf of Lions (NW Mediterranean). We compared the concentrations of branched glycerol dialkyl glycerol tetraethers (br GDGTs) and crenarchaeol in suspended particulate matter (SPM) collected downstream in the Rhône River, as well as in surface sediments and a ca. 8m piston core from the Rhône prodelta. The core covered the last 400 yr, with four distinct intervals recording the river influence under natural and man-induced shifts in four main channels of the river mouth (Bras de Fer, Grand Rhône, Pégoulier,and Roustan). The results indicate that there are mixed sources of br GDGTs and crenarchaeol in the prodelta, complicating applicationof the BIT index as an indicator of continental organic carbon input and thus as a palaeoflood proxy. However, the sedimentary BIT record for the period when continental material was delivered by the river more directly to the core site (Roustan phase;1892 to present) mimics the historical palaeoflood record. This shows the potential of the BIT index as a palaeoflood proxy, provided that the delivery route of the continental material by rivers to the core sites remains constant over time. The study also highlights the idea that shifts in river channels should be taken into account for the use of the BIT index as a palaeoflood proxy.

This paper is focused on carbohydrates, an abundant chemical class in marine organic matter, mostly found as polysaccharides. An experiment showed that the use of H2SO4 1 M (95 °C, 4 h) yielded a good compromise between recovery and degradation of all neutral monosaccharides from two kinds of organic material: surface sediments and trapped particles. Twenty samples of surface sediments (0–0.5 cm) were collected in various physiographic and bathymetric locations on the Northwestern Mediterranean margin. Neutral monosaccharides were determined by an ionic chromatography system with electrochemical detection (HPAEC–PAD). Differences between total neutral monosaccharides (NMTOT) and total carbohydrates, determined by a spectrophotometric method on the same samples, brought further assumptions on the nature of the carbohydrate pool. Total neutral monosaccharides contents varied from 0.46 to 1.04 mg g−1 and their proportions donated to the organic carbon pool (NMTOT–C/OC) barely reached 5%. The spatial distribution of NMTOT and organic carbon (OC) clearly showed that organic inputs, originating from the shallower epicontinental area, spread along canyon axis while undergoing dilution processes. In spite of the high physiographic and bathymetric diversity, surface sediments from most stations were characterized markedly by the homogeneity in the neutral monosaccharide compositions. Two stations, E21 (Ebro prodelta) and EC36 (Balearic slope) showed, however, distinct signatures with high relative abundances of glucose and galactose, respectively. Glucose was found to trace the continental inputs, whereas galactose characterized the marine inputs. The relative “freshness” of the organic material at station EC36, assumed by the high proportion of hexose neutral monosaccharides, confirms the dominance of phytoplankton remains at this station. This work showed that the use of monosaccharides as tracers of the biological source and fate of organic compounds is deeply linked to the quality of the organic material. The monosaccharide signature is only preserved in samples of surface sediments where inputs of fresh organic material are higher than the refractory one.

The study of biogeochemical processes at the water-sediment interface must be able to explain the relatively small content of organic carbon in the sediment, compared to the calculated carbon flux in the oceans. The input of an organic molecule at the marine sediment surface (Gulf of Lion, France) was simulated by the injection of a 14C labelled molecule in the water of a preserved interface. A glutamic acid [14C(U)] simulated marine organic matter, whereas a catechol [14C(U)] represented continental organic material. The separation by successive acid and basic extractions of the remaining initial compounds and the resulting products showed the relative importance of biological (respiration, assimilation) and geochemical (adsorption on argillaceous particles and condensation in geopolymers) processes occurring at the water-sediment interface. The evaluation was supported by the determination of the geochemical (humic substances), hydrological (conditions of temperature and degree of oxygenation) and sedimentological characteristics of the environment studied and by the estimation of the benthic activity.