Past sea surface temperature (SST) evolution in the Alboran Sea (western Me
diterranean) during the last 50,000 years has been inferred from the study
of C-37 alkenones in International Marine Global Change Studies MD952043 co
re. This record has a time resolution of similar to 200 years allowing the
study of millennial-scale and even shorter climatic changes. The observed S
ST curve displays characteristic sequences of extremely rapid warming and c
ooling events along the glacial period. Comparison of this Alboran record w
ith delta(18)O from Greenland ice (Greenland Ice Sheet Project 2 core) show
s a strong parallelism between these SST oscillations and the Dansgaard-Oes
chger events. Five prominent cooling episodes standing out in the SST profi
le are accompanied by an anomalous high abundance of Neogloboquadrina pachy
derma sinistral which is confined to the duration of these cold intervals.
These features and the isotopic record reflect drastic changes in the surfa
ce hydrography of the Alboran Sea in association with Heinrich events H1-5.