The Arctic Ocean has experienced rapid warming and sea ice loss in recent decades,
becoming the first open-ocean basin to experience widespread aragonite undersaturation …

Stable isotopes in water (oxygen-18 and deuterium) are hydrologic tracers, which have
been embedded into both analytical mass balance and physically based continuous …

The melting of marine terminating glaciers in Northeast Greenland is a visible sign that our
climate is changing. This melt has been partly attributed to changes in oceanic heat fluxes …

The cyclic growth and decay of continental ice sheets can be reconstructed from the history
of global sea level. Sea level is relatively well constrained for the Last Glacial Maximum …

Accurate ocean environment perception is crucial for weather and climate prediction.
Environmental limitations and deployment costs constrain satellite and buoy real-time …

As calcareous foraminifera precipitate their shells from the surrounding water mass, they are
the basis of most marine radiocarbon chronologies and paleo-proxies. Nevertheless, post …

Abstract The western Fram Strait is the only deep-water gateway connecting the Arctic
Ocean and North Atlantic. Consequently, today, the western Fram Strait and the Northeast …

The Northeast Greenland shelf is highly sensitive to climate and ocean variability because it
is swept by the East Greenland Current, which, through the western Fram Strait, forms the …

Fossil‐bound organic material holds great potential for the reconstruction of past changes in
nitrogen (N) cycling. Here, with a series of laboratory experiments, we assess the potential …

The origin of life on Earth required myriads of chemical and physical processes. These
include the formation of the planet and its geological structures, the formation of the first …