M. Rossignol-strick et M. Paterne, A synthetic pollen record of the eastern Mediterranean sapropels of the last 1 Ma: implications for the time-scale and formation of sapropels, MARINE GEOL, 153(1-4), 1999, pp. 221-237
The Quaternary climate of southern Europe (south Italy and Greece) is inves
tigated by pollen analysis of the sapropels which were deposited in the dee
p eastern Mediterranean Sea during the last I million year (Ma). The time-s
cale of core KC01b in the Ionian Sea has been established by tuning its oxy
gen isotopic record to the ice volume model of Imbrie and Imbrie (1980). Fo
r the last 250,000 year (250 ka), the previous pollen studies and astronomi
cal tuning have been confirmed. Sapropels were deposited under a large rang
e of Mediterranean climates: fully interglacial, fully glacial, and interme
diary, as revealed mainly by the balance between the respective pollen abun
dances of oak (Quercus) and sage-brush (Artemisia). The high value of the o
ak reveals the warm and wet climate of an Interglacial, and the high value
of the sage-brush, the dry and cold climate of a Glacial. Whereas the Medit
erranean climate is directly related to the variation of the high-latitude
ice sheets, the deposition of sapropels is not so. In contrast with the wid
e climatic range, sapropels were deposited only when summer insolation in t
he low latitudes reached its highest peaks. However, between 250 ka and 1 M
a, that stable pattern is not yet established. Only six sapropels are obser
ved, many expected ones do not appear, even as ghosts signalled by peaks of
barium abundance, that remain after the post-deposition oxidation of organ
ic matter. The pattern of sapropel formation in stable and direct relations
hip to highest insolation does not seem to apply. For five of those saprope
ls, neither climate extremes are observed; they mainly formed during interm
ediary types of Mediterranean climate. In contrast, one sapropel (and one g
host) relates to a relatively low peak of insolation, and its climate is of
a unique, composite type not seen later. This might suggest an unsuspected
, more complex pattern linking the formation of Mediterranean sapropels to
the astronomical configuration. (C) 1999 Elsevier Science B.V. All rights r
eserved.