MN Çağatay, N Görür, O Algan, C Eastoe… - Marine Geology, 2000 - Elsevier
Stratigraphic analysis of Late Quaternary sediments of the Sea of Marmara Basin (SMB) indicates that it was a freshwater lake during the late glacial to ca 12,000 yr BP, depositing …
PJM Van Santvoort, GJ De Lange, J Thomson… - … et Cosmochimica Acta, 1996 - Elsevier
Over a wide area of the eastern Mediterranean basin, two Mn-rich layers have been observed above the most recent sapropel (S1), one immediately above the sapropel top and …
Throughout its geologic history, the Black Sea experienced major sea level changes accompanied by severe environmental modifications, including geomorphologic reshaping …
The enhanced accumulation of organic matter in Eastern Mediterranean sapropels and their unusually low δ 15 N values have been attributed to either enhanced nutrient availability …
Quantitative analyses of coccolithophores, planktonic foraminifers, dinoflagellate cysts and pollen assemblages were carried out on shallow (NS-14) and deeper (NS-40) sediment …
Abstract The Jurassic to Holocene record of black shale deposition in the Tethys‐ Mediterranean region is unrivalled by that of any other ocean basin, either in land sections …
M Rossignol‐Strick - Paleoceanography, 1987 - Wiley Online Library
A working hypothesis is proposed to account for the present accumulation of brines in isolated pockets of the ocean floor and for the formation of the underlying organic and metal …
IA Nijenhuis, GJ de Lange - Marine Geology, 2000 - Elsevier
Seventeen eastern Mediterranean Pliocene sapropels from ODP Sites 964, 966, 967 and 969, some of which are coeval, have been analysed for their geochemistry. The sapropels …
Not only the occurrence of distinct organic-rich intervals (sapropels), but also the relative contents of key major and minor elements and isotopes in the sediments of the eastern …