Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6441553 | Marine Geology | 2015 | 15 Pages |
Abstract
Based on the radiocarbon and tephra-integrated age model the marine transgression at 12.55 ± 0.35 cal ka BP was followed by the deposition of the main lower Holocene sapropel between ca. 12.3 and 5.7 cal ka BP, and in the shallow shelf areas (<~100 m depth) such as the Gemlik Gulf, by the formation of the upper Holocene sapropel between ca. 5.4 and 2.7 cal ka BP.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
M. Namık ÃaÄatay, Sabine Wulf, Ãmmühan Sancar, Aslı Ãzmaral, Laurence Vidal, Pierre Henry, Oona Appelt, Luca Gasperini,