Abstract. Rivers transport dissolved and solid loads from
terrestrial realms to the oceans and between inland reservoirs, representing
major mass fluxes on Earth's surface. The composition of river water and
sediment provides clues to a plethora of Earth and environmental processes,
including weathering, erosion, nutrient and carbon cycling, environmental
pollution, reservoir exchange, and tectonic cycles. While there are
documented, publicly available databases for riverine dissolved and
suspended nutrients, there is no openly accessible, georeferenced database
for riverine suspended sediment composition. Here, we present a globally
representative set of 2828 suspended and bed sediment compositional
measurements from 1683 locations around the globe. This database, named
Global River Sediments (GloRiSe) version 1.1, includes major, minor and trace
elements, along with mineralogical data, and provides time series for some
sites. Each observation is complemented by metadata describing geographic
location, sampling date and time, sample treatment, and measurement details,
which allows for grouping and selection of observations, as well as for
interoperability with external data sources, and improves interpretability.
Information on references, unit conversion and references makes the database
comprehensible. Notably, the close to globe-spanning extent of this
compilation allows the derivation of data-driven, spatially resolved global-scale
conclusions about the role of rivers and processes related to them within
the Earth system. GloRiSe version 1.1 can be downloaded from Zenodo
(https://doi.org/10.5281/zenodo.4485795, Müller et al.,
2021) and GitHub (https://github.com/GerritMuller/GloRiSe, last access: 26 May 2021),
where updates with adapted version numbers will become available, along
with a technical documentation and an example calculation in the form of
MATLAB scripts, which calculate the sediment-flux-weighted major element
composition of the annual riverine suspended sediment export to the ocean
and related uncertainties.