Dynamics of Mid-latitude/ Mediterranean climate during the last 150 ka: Black Sea /Northern Anatolian Paleoenvironmental Reconstructions (DynNAP)

在第一阶段，研究了黑海南部的海相/湖沼沉积物以及Sofular洞穴的石笋。它们提供了安纳托利亚腹地过去植被动态和降水变化的古环境记录，以及全新世、Eem和最后两个冰期终止期间海洋/湖泊黑海系统本身环境变化的古海洋学/古湖泊学数据。在第二阶段，我们计划将我们的研究扩展到额外的海洋沉积物岩心，来自黑海邻近地区的一组新的表面样本和石笋，以便更好地了解观察到的区域尺度上的环境变化。我们还计划介绍在研究期间环境变化的建模方面。这将使我们更全面地了解北大西洋气候和印度季风系统的远场影响、1期和2期冰川终止期黑海的水文动态以及全新世的人为/气候影响。

During the first phase marine/limnic sediments from the southern part of the Black Sea as well as stalagmites from Sofular Cave were investigated. They provided excellent paleoenvironmental records of past vegetation dynamics and changing precipitation regimes in the Anatolian hinterland as well as paleoceanographic / paleolimnologic data of environmental changes in the marine / limnic Black Sea system itself during the Holocene, Eem and the last two glacial terminations. In a second phase, we plan to extend our study to additional marine sediment cores, a new set of surface samples from neighboring regions of the Black Sea, and stalagmites in order to get a better understanding of the observed environmental changes on the regional scale. We also plan to introduce modeling aspects on the environmental changes during the studied periods. This will provide a more comprehensive understanding of the far-field effects of North Atlantic climate and Indian monsoon system, the hydrological dynamics in the Black Sea during the glacial terminations 1 and 2 and the anthropogenic / climatic impacts during the Holocene.