Lake Van is the fourth largest terminal lake in the world (38.5° N, 43° E, volume 607 km 3, area 3570 km 2, maximum water depth 460 m), extending for 130 km WSW–ENE on the …
A new sediment core from Padul, Padul-15-05, provides a long and continuous sedimentary and paleoenvironmental record of the last∼ 200 kyr. Here we present a detailed …
Sedimentary, geochemical and mineralogical analyses of the ICDP cores recovered from the Northern Basin (NB) of Lake Van provide evidence of lake level and climatic changes …
Millennial to orbital-scale rainfall changes in the Mediterranean region and corresponding variations in vegetation patterns were the result of large-scale atmospheric reorganizations …
Hydrogen production from the electrolysis of water by sea or lake waters used as electrolyte plays a crucial role in providing sustainable hydrogen production. Production of hydrogen …
M Stockhecke, M Sturm, I Brunner… - …, 2014 - Wiley Online Library
The lithostratigraphic framework of L ake V an, eastern T urkey, has been systematically analysed to document the sedimentary evolution and the environmental history of the lake …
Fossil long-chain alkenones have been used for several decades to reconstruct past ocean surface water temperatures and gained recent interest as a paleotemperature proxy for …
Even though some individual studies on natural lakes spread around Turkey over time have been conducted to analyze their preceding characteristics and to monitor their temporal …