Interglacials, including the present (Holocene) period, are warm, low land ice extent (high
sea level), end‐members of glacial cycles. Based on a sea level definition, we identify …

The future impacts of anthropogenic global change on marine ecosystems are highly
uncertain, but insights can be gained from past intervals of high atmospheric carbon dioxide …

Ice volume (and hence sea level) and deep-sea temperature are key measures of global
climate change. Sea level has been documented using several independent methods over …

Cenozoic temperature, sea level and CO2 covariations provide insights into climate
sensitivity to external forcings and sea-level sensitivity to climate change. Climate sensitivity …

Research on global ice-volume changes during Pleistocene glacial cycles is hindered by a
lack of detailed sea-level records for time intervals older than the last interglacial. Here we …

Contentious observations of Pleistocene shoreline features on the tectonically stable islands
of Bermuda and the Bahamas have suggested that sea level about 400,000 years ago was …

Early Levallois core technology is usually dated in Europe to the end of Marine Isotope
Stage (MIS) 9 and particularly from the beginning of MIS 8 to MIS 6. This technology is …

The hydrological balance of the Black Sea is governed by riverine input and by the
exchange with the Mediterranean Sea through the shallow Bosporus Strait. These sources …

Although the role that P leistocene glacial cycles have played in shaping the present biota of
oceanic islands world‐wide has long been recognized, their geographical, biogeographical …

No glacial inception is projected to occur at the current atmospheric CO2 concentrations of
390 ppmv (ref.). Indeed, model experiments suggest that in the current orbital configuration …