机译:全新世期间黑海东北和西南陆架的古环境变化
Shrshov Institute of Oceanology, RAS, 36 Nakhimovsky Prosp., Moscow 117997, Russia;
Shrshov Institute of Oceanology, RAS, 36 Nakhimovsky Prosp., Moscow 117997, Russia;
Geological Faculty, Lomonosov Moscow State University, Vorobyevy Cory, Moscow 119992, Russia;
AV. Zhirmunsky Institute of Marine Biology, Far East Division RAS, 17 Pal'chevsky Street, Vladivostok 690041, Russia;
School of Environmental Sciences, University of Liverpool, Liverpool 169 7ZT, UK;
National 926A Center US Geological Survey, Reston, VA 20191, USA;
Department of Earth and Environmental Science, Temple University, 313 Beury Hall, 1901 N. 13th Street, Philadelphia, PA 19122, USA;
Geological Faculty, Lomonosov Moscow State University, Vorobyevy Cory, Moscow 119992, Russia;
机译:晚熟到全新的古环境变化的黑海
机译:黑海从晚冰期到全新世的古环境演化,并通过在rac骨壳上获得的稳定的氧同位素记录进行了重建
机译:西南黑海陆架(土耳其)全新世沉积物的矿物学与物源,海平面和当前状况的关系
机译:全新世和晚期黑海沿海地区东北海洋沿海地区的环境变化
机译:与丹麦海峡(冰岛)相邻的大陆架的全新世古环境重建。
机译:黑海流出物对全新世融水事件的响应
机译:基于钙质Nannoplankton的黑海中全新世生物近视和古环境变化
机译:蒙大拿州西南部黑尾山脉东北侧晚白垩世断裂和矿化的地质和裂变径迹证据