Quaternary deposits in six sediment cores from the Scotia Sea, Antarctica,
were examined for the presence of volcanic ash layers. The cores were recovered
from water depths of 3369-4025 m. Altogether, 23 ash layers were found, 18 of
which have been investigated by electron-probe microanalysis. Deception Island is
identified as the source of all the ash layers analyzed. The upper ash layer in
each core can be correlated across all six cores, over a distance of -100 km, on
the basis of its unusual bimodal composition, major oxide geochemistry and
stratigraphie position. Two other ash layers can also be correlated between
several of the cores.
Reconstructing 7000 years of North Atlantic hurricane variability using deep-sea sediment cores from the western Great Bahama Bank
