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paleoceanography相关的网络例句

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与 paleoceanography 相关的网络例句 [注:此内容来源于网络,仅供参考]

This finding is of great significance not only to the reconstruction of paleoceanography, paleoenvironment, paleotectonics, and paleoclimate, but also to deepwater petroleum exploration in the South China Sea.

根据最新的地震资料分析发现,该牵引体实际上由一系列逆陆坡向上倾方向迁移的沉积物波组成,这一发现对于南海北部大陆边缘古海洋、古环境和古气候研究,以及南海深水油气勘探具有重要意义。

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。

Particularly the Cretaceous time period is a time of major changes in the Earth Systems demonstrated by major plate tectonic processes, as is the dispersal of Pangea supercontinent, plaeoclimate and paleoceanography changes.

Berriasian~Albian早期,延续时间超过30Ma;而在Thakkhola地区时代为Hauterivian晚期-Albian早期,延续时间约20Ma,在Zanskar地区火山岩屑砂岩仅仅出现在Albian期,延续时间小于10Ma。

The relative ratio of 〓 over 〓 diols , defined as the diol index, serves as a good indicator for changes in paleoceanography and paleoclimate in southern South China during the last 30.0 ka.

长链烷基二醇的稳定碳同位素值在-30.17~-38.98‰之间,反映出其先质为水生生物——海洋黄绿藻Eustigmatophytes。

It utilized factor analysis and regression analysis ofthe multi-statistics to make the quantitative analysis on a great deal of core proxies in the North Indian Ocean and Indonesian Archipelago areas, and acquiredthe exact conversion relations of paleoceanic environment parameters (sea surface temperatureand salinity) and proxies. Then it made the change curve which can show the changes of paleo-ceanic environment parameters (sea surface temperature and salinity) which followed the changesof depth and provided the contrast between paleoceanic environment parameters of different coreson the landscape orientation. This paper supplied a more scientific and exact method for resumingthe paleoceanic environment on paleoceanography research.

本文阐述了以古海洋学数据库系统数据为基础的古海洋学多元统计分析模型,利用多元统计学中的因子分析和回归分析技术对北印度洋以及印尼多岛海地区大量岩芯的替代指标做定量分析,求出古环境参数与替代指标的精确转换关系,从而做出各岩芯处古环境参数随深度的变化曲线,提供不同岩芯在横向上的古环境参数对比,为古海洋学研究中恢复古环境提供了一种更科学更精确的方法。

Each unitis of different biotic characters and displays different features of seawater composition during the time. 2 The black unit including a biotic extinction was caused by oceanic anoxic event. Crisis that deepwater keeled foraminifera encountered represents a ferocious anoxia in deep marine environment . Biotic recovery in gray unit reflects gradually improved marine circumstance. What the biotic extinction at the C/T boundary in black unit reflects an environmental mutation, whereas the gradual biotic change characterize the recovery of marine dissolved oxygen environment in a stepwise process. The red unit is the result of oxic deposition and characterized by extremely abundance of foraminiferal faunas, which reflects a high-oxidized marine circumstance. 3 As the most ordinary biotic index in paleoceanography researches, foraminifera represent anexcellent environmental indicator in this paper.

三套岩层表现出不同的生物特征,并指示出当时海水的不同性质。2黑层段是大洋缺氧造成的结果,生物大量灭绝,深层水具旋脊有孔虫的所遭受的危机反映出当时海洋深层水体严重缺氧的特征;灰层段中生物的恢复反映出海洋环境自缺氧事件之后的逐步改善过程,与黑层段反映的C/T 界线处生物绝灭反映的环境突变不同,灰层段生物特征的渐变指示出当时海洋溶解氧环境的恢复也是一个逐步的过程;红层段属于富氧沉积的产物,特征是有孔虫生物的极度繁盛,反映的是一种高氧化性的海洋环境。3有孔虫作为古海洋研究中最常用的生物指标,在本文研究中显示了良好的环境指示性。

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