海洋学

The results are published in the American journal Paleoceanography.

其结果发表在美国古海洋学杂志。

The current advances of the studies of geochemistry and paleoceanography of the Co rich crust are reviewed in this paper.

本文综述了近年来国内外富钴结壳地球化学与古海洋学研究的新进展。

The evolvement of climate environment in the geological history is one important contents ofthe paleoceanography research and has an important significance.

地质历史时期古海洋气候环境的演变也是古海洋学研究中的一项重要内容，具有十分重要的意义。

As the extremely low growth rate and stable forming environment,Fe-Mn crust is the ideal fossil of Paleoceanography and global change.

由于铁锰结壳极低的生长速率和较稳定的形成环境，使它成为古海洋学和全球变化研究的理想&化石&。

Biogenic silica content was determined in 25 surface sediment samples from the southern South China Sea to study its distribution and its modern oceanic environmental significance, which may provide further scientific evidence for paleoceanography explaination.

对南海南部25个表层沉积样进行了生物硅的测定分析，试图揭示南海南部表层沉积生物硅的分布及其对现代海洋环境的指示意义，以便为古海洋学研究提供进一步的科学依据。

South China Sea ; late Quaternary ; paleoceanography ; high-resolution stratigraphy

南海；晚第四纪；古海洋学；高分辨率地层学

Deeply study on changes of marine environment, provenance and flux of the sediments during the glaciation-interglaciation climatic cycle is a highlight field of the paleoceanography studies in the Okinawa Trough .

深入揭示冰期/间冰期气候旋回中冲绳海槽沉积物记录的海洋环境、物质来源和通量变化及其对古气候和海平面变化的响应信息，是该区古海洋学研究的前沿课题。

Center for Ecology and Conservation Biology is primarily dedicated to education and research in ecology and conservation biology including paleoceanography, ecological economics, sensory biology, behavioral ecology of birds, behavioral ecology and insect sociobiology, evolutionary biology, ichthyology, forest ecology and biogeochemistry, mammalian population genetics, etc.

生态学与保护生物学中心致力于生态学与保护生物学的教学与研究，其研究领域包括古海洋学，生态经济学，感官生物学，鸟？？？？？行为生态学，行为生态学和昆虫社会生物学，进化生物学，鱼类学，森林生态学和生物地理化学，哺乳动物遗传学等。

Keywords: Indonesian Archipelago; foraminifera assemblage; last glacial; paleoceanography

中文关键词：印度尼西亚多岛海；有孔虫组合；末次冰期；古海洋学

Comparing and analyzing of the paleoceanography characters from the SST, SSS, paleoproductivity, carbonate dissolution, paleo-monsoon and throughflow actions, we find it is obvious that the ocean currents system difference between the glacial and deglacial.

通过不同洋流区的岩芯末次冰期以来的古水温、古盐度、古生产力、碳酸盐溶解作用、古季风、穿越流活动等古海洋学特点的对比分析，可看出研究区冰期与冰后期海洋环流特点存在着明显的差异。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。