Ae. Aksu et al., Oscillating Quaternary water levels of the Marmara Sea and vigorous outflow into the Aegean Sea from the Marmara Sea Black Sea drainage corridor, MARINE GEOL, 153(1-4), 1999, pp. 275-302
Detailed interpretation of single-channel air-gun and deep-tow boomer profi
les demonstrates that the Marmara Sea, Turkey, experienced small-amplitude
(similar to 70 m) fluctuations in sea level during the later Quaternary, li
mited in magnitude by the sill depth of the Strait of Dardanelles. Moderate
subsidence along the southern shelf and Quaternary glacio-eustatic sea-lev
el variations created several stacked deltaic successions, separated by maj
or shelf-crossing unconformities, which developed during the transitions fr
om global glacial to integlacial periods. Near the Strait of Dardanelles, a
series of sand-prone deposits are identified beneath an uppermost (Holocen
e) transparent mud drape. The sandy deposits thicken into mounds with the m
orphology and cross-sectional geometries of barrier islands, sand waves, an
d current-generated marine bars. All cross-stratification indicates unidire
ctional flow towards the Dardanelles prior to the deposition of the transpa
rent drape which began similar to 7000 years BP, in strong support: of the
notion that the Marmara Sea flowed westwards into the Aegean Sea through th
e Dardanelles at times of deglaciation in northern Europe. The global sea-l
evel curve shows that, at similar to 11,000 and similar to 9500 years BP, s
ea level rose to the sill depths of the Straits of Dardanelles and Bosphoru
s, respectively. The effect from similar to 11,000 to similar to 9500 years
BP was seawater incursion into the Marmara Sea, drowning and formation of
algal-serpulid bioherms atop lowstand barrier islands, and transgression of
shelves and lowstand deltas. At similar to 9500 years BP, glacial meltwate
r temporarily stored in the Black Sea lake, developed into a vigorous south
ward flow toward the Aegean Sea, forming west-directed sandy bedforms in th
e western Marmara Sea and initiating deposition of sapropel S1 in the Aegea
n Sea. This strong outflow persisted until similar to 7000 years BP, after
which a mud drape began to accumulate in the Marmara Sea and euryhaline Med
iterranean mollusks successfully migrated into a progressively more saline
Black Sea where sapropel deposition began. Most eastern Mediterranean sapro
pels from S1 to S11 appear to correlate with periods of rising sea level an
d breaching, or near-breaching, of the Bosphorus sill. These events are bel
ieved to coincide with times of vigorous outflow of low-salinity (?fresh) s
urface waters transiting the Black Sea-Marmara Sea corridor, and ultimately
derived from melting of northern European ice sheets. (C) 1999 Elsevier Sc
ience B.V. All rights reserved.