Source to sink sedimentary systems are important settings of carbon cycling, serving as sites
of carbon transfer between terrestrial and marine reservoirs, and as the primary locations for …

Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …

Rivers transfer terrestrial organic carbon (OC) from mountains to ocean basins, playing a
key role in the global carbon cycle. During fluvial transit, OC may be oxidized and emitted to …

Residual solid products of erosion display a wide range of size, density, shape, mineralogy,
and chemical composition and are hydrodynamically sorted in large river channels during …

We present an extensive river sediment dataset covering the Ganga basin from the
Himalayan front downstream to the Ganga mainstream in Bangladesh. These sediments …

Although the proxies based on elemental geochemistry of siliciclastic sediments have been
well developed to indicate the intensity of chemical weathering in various catchments, their …

Large rivers connect the continents and the oceans, and corresponding material fluxes have
a global impact on marine biogeochemistry. The Yellow River transports vast quantities of …

Total organic carbon (TOC), total nitrogen (TN) and their δ13C and δ15N values were
determined from 110 sediment samples from the Ayeyarwady (Irrawaddy) continental shelf …

At geological time scales, the role of continental erosion in the organic carbon (OC) cycle is
determined by the balance between recent OC burial and petrogenic OC oxidation …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …