浮游有孔虫,Planktonic foraminifera
1)Planktonic foraminifera浮游有孔虫
1.A preliminary study of living planktonic foraminifera distribution and its affecting factors in southern South China Sea;南海南部活体浮游有孔虫分布特征及其影响因素初探
2.Distribution of planktonic foraminifera in the surface sediment in the Northern South China Sea and its environmental significance;南海北部表层沉积物中浮游有孔虫分布特征与环境意义
3.Oxygen and Carbon isotope composition of planktonic foraminifera in surface sediments from South China Sea and its oceanography significance.;南海表层沉积物浮游有孔虫的氧碳同位素及其海洋学意义
英文短句/例句

1.Quaternary Planktonic Foraminiferal Assemblages in the Southern South China Sea and Paleoclimatic Variations;南海南部第四纪浮游有孔虫群与古气候变化
2.CHRONOSTRATIGRAPHY OF PLANKTONIC FORAMINIFERA IN THE YINGGEHAI-QIONGDONGNAN BASIN南海北部莺琼盆地浮游有孔虫年代地层研究
3.The influence of the size of marine planktonic foraminifers on the boron isotopic analysis浮游有孔虫个体大小对硼同位素分析的影响
4.PLANKTONIC FORAMINIFERA DURING LATE QUATERNARY IN THE BENGAL BAY AND THEIR PALEOCEANOGRAPHIC IMPLICATIONS孟加拉湾晚第四纪浮游有孔虫及其古海洋学意义
5.A Millennial Scale Mid-Pleistocene Paleoclimate Record of Planktonic Foraminifera from the Northern South China Sea Site 1144南海北部1144站中更新世浮游有孔虫的千年尺度古气候记录
6.Planktonic Foraminifer and Oxygen Isotopic Evidence of a Late Miocene Western Pacific Warm Pool晚中新世西太平洋暖池的浮游有孔虫和氧同位素证据
7.THE DISCOVERIES OF THE LATE EOCENE PLANKTONIC FORAMINIFERA INTHE PEARL RIVER MOUTH BASIN AND THEIR GEOLOGICAL IMPLICATIONS珠江口盆地晚始新世浮游有孔虫的发现及其地质意义
8.Measurement of Mg/Ca Ratios in Planktonic Foraminifera on ICP-OES and Application of Mg/Ca Ratios in Sea Surface Temperature;ICP-OES测定浮游有孔虫的Mg/Ca比值及其在SST分析中的应用
9.The Improvement in the Studies of Planktonic Foraminiferal Biostratigraphy in the Upper Cretaceous in Tingri, Tibet;西藏定日地区上白垩统浮游有孔虫生物地层研究新进展
10.Quaternary Planktonic Foraminiferal Fauna and Variations of the Warm Pool in the Western Equatorial Pacific;赤道西太平洋第四纪浮游有孔虫群与暖池的变动
11.THE EOCENE-PLIOCENE PLANKTONIC FORAMINIFERA FROM RAMREE ISLAND,BURMA缅甸英雄岛始新世—上新世浮游有孔虫及其古环境意义
12.PLANKTONIC FORAMINIFERA IN CORE 89PC FROM THE NORTHWESTERN SOUTH CHINA SEA AND THEIR PALEOENVIRONMENT SIGNIFICANCE南海西北部89PC柱样沉积物中浮游有孔虫特征及其古环境意义
13.Sea Ice Formation Rates Recorded in Planktonic Foraminiferal Oxygen and Carbon Isotopes in the Western Arctic Ocean during the Late Quaternary北冰洋西部晚第四纪浮游有孔虫氧碳同位素记录的海冰形成速率
14.A preliminary study of oxygen and carbon isotopic changes of planktonic foraminifera from surface sediments and plankton tow samples in southern South China Sea南海南部水体和沉积物中的浮游有孔虫氧碳同位素分析
15.RELATIONSHIP BETWEEN WATER PROPERTIES AND PLANKTONIC FORAMINIFERAL STABLE ISOTOPES FROM SURFACE SEDIMENTS IN WESTERN ARCTIC OCEAN北冰洋西部表层沉积物中的浮游有孔虫稳定氧、碳同位素与水团性质的关系
16.the free - swimming larva of the oyster.牡蛎的自由浮游幼虫
17.minute floating marine tunicate having a transparent body with an opening at each end.身体透明、两端有孔并且有背囊的微小的浮游海洋动物。
18.There are two main types of wormholes: Lorentzian wormholes and Euclidean wormholes.有二种主要类型的虫孔:洛伦兹虫孔和欧几里得虫孔。
相关短句/例句

planktonic foraminifer浮游有孔虫
1.A preliminary study of oxygen and carbon isotopic changes of planktonic foraminifera from surface sediments and plankton tow samples in southern South China Sea南海南部水体和沉积物中的浮游有孔虫氧碳同位素分析
2.The disappearance at ~10Ma of the deep dwelling planktonic foraminifer Globoquadrina dehiscens from the western Pacific including the South China Sea was about 3Ma earlier than its final extinction elsewhere.浮游有孔虫深水种Globoquadrinadehiscens于10Ma左右从西太平洋和南海绝灭,要比其他地区早大约3Ma。
3.The upmost 5 m of core MD01-2386 from the west Pacific warm pool was studied for determining the variability of the depth of thermocline(DOT) since the last glacial maximum at centennial scales based on high-resolution oxygen and carbon stable isotopes of planktonic foraminifers Globigerinoides ruber and Pulleniatina obliquiloculata with the AMS~(14)C age datings.对西太平洋暖池核心区MD01 2386柱状样最上部5m进行了高分辨率的浮游有孔虫Globigerinoidesruber和Pulleniatinaobliquiloculata的氧、碳稳定同位素分析,结合AMS14C测年,研究表明其属于末次盛冰期—全新世的沉积。
3)planktonic foraminiferal zone浮游有孔虫带
4)planktic foraminifera assemblages浮游有孔虫组合
5)foraminifera shell浮游有孔虫壳
6)planktonic foraminifers浮游的有孔虫
延伸阅读

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。