Using a simple 3‐box model of the ocean‐atmosphere system, we simulate the cycling of
carbon and strontium in the aftermath of a global glaciation. Model simulations include the …

The gradual discovery that late Neoproterozoic ice sheets extended to sea level near the
equator poses a palaeoenvironmental conundrum. Was the Earth's orbital obliquity> …

Carbonates capping Neoproterozoic glacial deposits contain peculiar sedimentological
features and geochemical anomalies ascribed to extraordinary environmental conditions in …

Geologic evidence suggests that in the Late Neoproterozoic (∼ 600 Ma) almost all land
masses were glaciated, with sea‐level glaciation existing even at the equator. A recent …

We use an Earth system model of intermediate complexity, CLIMBER‐2, to investigate what
recent improvements in the representation of the physics and biology of the glacial ocean …

The snowball Earth theory, initially proposed by JL Kirschvink to explain the Neoproterozoic
glacial episodes, suggests that the Earth was globally ice covered at 720 Ma (Sturtian …

In spite of significant progress in paleoclimate reconstructions and modelling of different
aspects of the past glacial cycles, the mechanisms which transform regional and seasonal …

During the cold period of the Last Glacial Maximum (LGM, about 21 000 years ago)
atmospheric CO 2 was around 190 ppm, much lower than the pre-industrial concentration of …

Geochemical data from cap carbonates deposited above Cryogenian glacial deposits have
been widely used to infer the conditions that prevailed in the aftermath of snowball Earth …

The Snowball Earth hypothesis explains the development of glaciation at low latitudes in the
Neoproterozoic, as well as the associated iron formations and cap carbonates, in terms of a …