Understanding the fate of terrestrial organic carbon (C org) delivered to oceans by rivers is
critical for constraining models of biogeochemical cycling and Earth surface evolution. C org …

The eastern Levantine basin (ELB) is an ultra-oligotrophic, warm and saline marine system,
significantly affected by climate change during the past several decades. The deployment of …

Microbial-driven organic matter (OM) degradation is a cornerstone of benthic community
functioning, but little is known about the relation between OM and community composition …

A significant fraction of the global carbon flux to the ocean occurs in River-dominated Ocean
Margins (RiOMar) although large uncertainties remain in the cycle of organic matter (OM) in …

Estuarine regions are generally considered a major source of atmospheric CO 2, as a result
of the high organic carbon (OC) mineralization rates in their water column and sediments …

Observations indicate that resuspension and associated fluxes of organic material and
porewater between the seabed and overlying water can alter biogeochemical dynamics in …

We used field observations, laboratory measurements and a reactive transport model (RTM)
to investigate temporal and spatial variations in benthic nitrogen (N) cycling in the eutrophic …

The north-western Mediterranean deep convection plays a crucial role in the general
circulation and biogeochemical cycles of the Mediterranean Sea. The DEWEX (DEnse …

Sources and pathways of the Hg accumulated in the sediments of the Gulf of Lion (GoL) and
its adjacent marine areas (Northwestern Mediterranean) have been explored using …

Measurements of diffusive (DOU) and total (TOU) sediment oxygen uptakes, oxygen
penetration depth, porosity, OC, TN, carbohydrate, lipid, amino acid, chlorophyll a and …