A global compilation of deep-sea isotopic records suggests that Maastrichtian
ocean-climate evolution was tectonically driven. During the early
Maastrichtian, the Atlantic intermediate-deep ocean ...
Geochemical and sedimentological evidence suggest that the rapid climate
warming oscillations of the last ice age, the Dansgaard-Oeschger cycles, were
coupled to fluctuations in North Atlantic meridional ...
Evidence from a North Atlantic deep-sea sediment core reveals that the largest
climatic perturbation in our present interglacial, the 8200-year event, is
marked by two distinct cooling events in ...
The recent efforts of the paleoceanographic community have
resulted in a unique set of reconstructed sea-surface temperature
for the Atlantic Ocean during the Last Glacial Maximum, plus estimates ...
Late Holocene (2200-present) spring water temperatures from Chesapeake
Bay in the eastern United States determined from magnesium/calcium
(Mg/Ca) ratios in the ostracode Loxoconcha. The file provides ...
This data consists of reconstructed changes of paleotemperature,
-salinity, and -productivity within the southern Peru-Chile Current
during the last 8,000 years from a high-resolution sediment core ...
Variations in the strength of North Atlantic Ocean thermohaline circulation
have been linked to rapid climate changes during the last glacial cycle
through oscillations in North Atlantic Deep Water ...
