Article ID Journal Published Year Pages File Type
7449049 Quaternary International 2018 13 Pages PDF
Abstract
Based on the ascidian spicules and nannofossil records of the coring/drilled muds of Lake Ä°znik was marine, as an inlet or lagoon connected to the modern Gulf of Gemlik, during the Pleistocene to Upper Holocene. It was likely separated from the Marmara Sea and turned into a freshwater lake after the upper Holocene.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Authors
, , ,