机译:最后350年内鄂霍次克海的轨道和千年尺度环境和沉积学变化
V.I. II'ichev Pacific Oceanological Institute (POI), Far East Branch Russian Academy of Science, Vladivostok, Russia;
rnJapan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan;
rnNorth-Eastern Interdisciplinary Scientific Research Institute Far East Branch, Russian Academy of Science, Magadan, Russia;
rnV.I. II'ichev Pacific Oceanological Institute (POI), Far East Branch Russian Academy of Science, Vladivostok, Russia;
rnV.I. II'ichev Pacific Oceanological Institute (POI), Far East Branch Russian Academy of Science, Vladivostok, Russia;
rnLimnological Institute of Siberian Branch of Russian Academy of Science, Irkutsk, Russia;
the okhotsk sea; geochemical and lithophysical sediment; properties; orbital and millennial-scale climate changes; last 350 kyr;
机译:中央Okhotsk Sea的轨道和千禧年环境和水文变化,从微孔(放射性术和底栖菌),地球化学和岩性代理和负责它们的机制
机译:过去350kyr鄂霍次克海深水沉积物的冰川和冰川间相的地球化学多元素标志:对轨道和千年尺度全球气候变化的反应
机译:在过去的350年里,鄂霍次克海环境和沉积学对轨道和千年尺度上全球气候变化的响应
机译:过去140 kyrs Zoige盆地Zoige盆地的古环境重建
机译:350米以下墨西哥湾深海底鱼类调查
机译:90 kyr之前的北欧海域的海冰和千年尺度的气候变化
机译:在鄂霍次克海的海冰条件在过去550 kyr从环境磁力推导出来