Abstract The Neoproterozoic interval (1000–540 Ma) contains ample evidence for a series of
glacial intervals. These include the 750–700 Ma Sturtian glaciation, the 625–580 Ma …

Paleomagnetic data for Neoproterozoic glacial deposits in South Australia and elsewhere
verify glaciomarine deposition near the paleoequator. Tidal rhythmites from such deposits in …

Of the many models that have been proposed to account for the enigmatically widespread
and apparently low-latitude Neoproterozoic glaciogenic deposits, three are widely …

The Neoproterozoic contains severe glacial intervals (750–580 Ma) including two extending
to low palaeomagnetic latitudes. Paucity of radiometric dates indicates the need for …

Earth's climate has alternated between warmer and cooler episodes. Warmer intervals of
sufficient duration (tens to hundreds of millions of years) are called “Greenhouse” episodes …

We examine the general conditions that must be satisfied by the configuration of the
continents in order that steady state solutions for Neoproterozoic climate exist that are …

New stratigraphic, geochronological and palaeomagnetic constraints allow updates to be
made to a synthesis of Neoproterozoic glacial palaeolatitudes, including modifications to …

The Neoproterozoic glacial intervals represent one of the most curious expressions of
Earth's climate. Despite the popularity of the hard “Snowball” hypothesis in the popular …

The main features of the low‐latitude Neoproterozoic glaciations remain the subject of
controversial debates concerning possible triggers. Here we use an AGCM coupled with a …

The IUGS-and UNESCO-funded International Geoscience Programme Project# 512
(Neoproterozoic Ice Ages) was conceived to contribute towards a global synthesis of current …