Carbon is one of the key elements in organisms and non-living compounds on Earth.
Carbon dioxide and methane are important greenhouse gases in the atmosphere, dissolved …

Reconstructions of past changes in dissolved oxygen concentrations in the abyssal ocean
are of interest to paleoceanographers because of their potential to help characterize and …

The dominant feature of large-scale mass transfer in the modern ocean is the Atlantic
meridional overturning circulation (AMOC). The geometry and vigour of this circulation …

Geologic intervals of sustained warmth such as the mid-Pliocene Warm Period can inform
our understanding of future climate change, including the long-term consequences of …

Several modelling and observational studies suggest deep water formation in the subpolar
North Pacific as a possible alternative mode of thermohaline circulation that occurred in the …

Circulation changes have been suggested to play an important role in the sequestration of
atmospheric CO 2 in the glacial ocean. However, previous studies have resulted in …

Abstract The Southern Ocean is an important regulator of global CO2 levels and likely had a
key role in lowering atmospheric CO2 levels during the Last Glacial Maximum (LGM) and …

Increased carbon sequestration in the ocean subsurface is commonly assumed to have
been one of the main causes responsible for lower glacial atmospheric CO2 concentrations …

Despite its importance for climate and the carbon cycle, the deep ocean circulation during
the Last Glacial Maximum (LGM) remains poorly understood. Whereas most studies suggest …

The chemical composition of benthic foraminifera from marine sediment cores provides
information on how glacial subsurface water properties differed from modern, but separating …