Understanding the causes of the~ 90 ppmv atmospheric CO2 swings between glacial and
interglacial climates is an important open challenge in paleoclimate research. Although the …

Abstract Changes in water mass distribution are considered to be a significant contributor to
the atmospheric CO 2 concentration drop to around 186 ppm recorded during the Last …

Three time-slice carbon cycle simulations for the last glacial maximum (LGM) constrained by
the CO 2 concentration in the atmosphere and the increase in the mean concentration of …

In this paper we describe the implementation of the carbon isotopes 13 C and 14 C
(radiocarbon) into the marine biogeochemistry model REcoM3. The implementation is tested …

Representing glacial‐interglacial changes in ocean carbon sequestration remains a major
challenge for Earth System Models (ESMs). Uncertainties in ocean circulation and biological …

Abstract Model intercomparison studies of coupled carbon‐climate simulations have the
potential to improve our understanding of the processes explaining the drawdown at the …

We present results of simulations performed with a physical–biogeochemical ocean model
of the Mediterranean Sea for the Last Glacial Maximum (LGM) and analyse the differences …

We combine consistently dated benthic carbon isotopic records distributed over the entire
Atlantic Ocean with numerical simulations performed by a glacial configuration of the …

We present results of simulations performed with a physical–biogeochemical ocean model
of the Mediterranean Sea for the Last Glacial Maximum (LGM) and analyse the differences …

Atmospheric CO 2 concentrations changed over ice age cycles due to net exchange fluxes
between land, ocean, ocean sediments, atmosphere, and the lithosphere. Marine sediment …