1) deep-water agglutinated foraminifera
深水胶结有孔虫
1.
Cretaceous deep-water paleoceanography is still in an early stage, since stable isotope analysis and geochemical data from calcitic benthic foraminifera are generally unavailable owing to an unusually high calcite compensation depth, and since the use of organically cemented deep-water agglutinated foraminifera as tracers is still insufficiently exploited.
深海环境深水胶结有孔虫的分布主要取决于碳酸盐可利用状况、原始生产的输入通量、深水交换、环境波动(深海洋流、浊流和快速沉积事件)和底层沉积类型,因此对于重建深海环境具有非常巨大的潜力。
2) Brackish water foraminifers
半咸水有孔虫群
3) depth stratification of planktonic foraminifera
浮游有孔虫深度分层
1.
According to the classification model of depth stratification of planktonic foraminifera in Miocene Indo Pacific Ocean (Keller,1985;Gasperi & Kennett,1993),Late Tertiary planktonic foraminiferal species from Ya 13 1 4 oil well in Qiongdongnan basin of the northern part of South China Sea could be grouped into the shallow,intermidiate and deep water dwelling groups.
依据Ｋｅｌｅｒ１９８５年、Ｇａｓｐｅｒｉ等１９９３年有关中新世印度洋和太平洋浅层水、中层水和深层水浮游有孔虫深度分层组合的划分模式，对南海琼东南盆地崖１３－１－４井晚第三纪浮游有孔虫作了定量研究，并分析了陆架海区浮游有孔虫不同深度分层组合含量的变化与古地理环境变迁的关系。
2.
According to the classification model of depth stratification of planktonic foraminifera in Miocene Indo-Pacific Ocean (Keller,1985;Gasperi & Kennett,1993), Later Tertiary planktonic foraminiferal species from Ya19-1-1 oil well in Qiongdongnan basin of the northern part of South China Sea could be grouped into the shallow,intermidiate and deep water dwelling groups.
依据ＧｅｒｔａＫｅｌｅｒ和Ｇａｓｐｅｒｉ，Ｋｅｎｎｅｔｔ有关中新世印度洋和太平洋浅层水、中层水和深层水浮游有孔虫深度分层组合的划分模式，对南海琼东南盆地崖１９－１－１井晚第三纪浮游有孔虫作了定量研究，并分析了陆架海区浮游有孔虫不同深度分层组合含量的变化与古地理环境变迁的关系。
4) deep worm hole
深虫孔
5) shellac,bond
虫胶胶结
6) Foraminifera
[英][fə,ræmi'nifərə] [美][fə,ræmə'nɪfərə]
有孔虫
1.
Separation and Isotopic Measurement of Boron in Foraminifera;
有孔虫中硼的分离及其正热电离质谱法测定
2.
Boron isotopic analyses on marine planktonic foraminifera;
海洋浮游有孔虫中硼同位素的测定和分析
3.
Foraminifera assemblages and it s sediment environment in Qianhu Bay of Zhangpu,Fujian;
福建漳浦前湖湾有孔虫群落及其沉积环境
补充资料：有孔虫
1.单细胞动物。有石灰质壳﹐壳上多小孔﹐由此溢出许多丝状的假足。生活在海洋中﹐遗壳堆积海底﹐形成岩石。有孔虫化石可用来测定岩石的地质年龄。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条