foraminiferal
foraminiferal
1. 46 Spivack A J ,You C F , Smith HJ . Foraminiferal boron isotope ratios as a proxy for surface ocean pH over the past 21 - Myr. Nature ,
45刘卫国,肖应凯,孙大鹏,等.马海盐湖区卤水和盐类矿物的氯同位素特征及意义.盐湖研究,1995,3(2).
2. However, although marine planktonic foraminiferal boron isotope has great potential to be a proxy for atmospheric pCO2, further studies on calibrations are required.
不过，尽管海洋浮游有孔虫中的硼同位素作为大气二氧化碳浓度的替代指标很具有潜力，但还需要进行更加深入地研究。
3. The natural thermoluminescence (NTL) of foraminiferal shells from piston cores MD81349 and MD77181 from the Ninetyeast Ridge and the Bengal Fan of the Indian Ocean were studied for the climate changes during the past 300 ka.
东北印度洋赤道90°E海岭和孟加拉扇MD81349,MD77181岩心记录了30万a来气候变化的历史.
4. LATE CRETACEOUS DEEP-WATER BENTHIC FORAMINIFERAL BIOFACIES AND LITHOFACIES OF THE WESTERN AND EASTERN TETHYS
东西特提斯晚白垩世深水底栖有孔虫生物相和岩相
5. Benthic foraminiferal distribution in surface sediment along the continental slope of the southern Okinawa Trough: dependance on water masses and food supply
冲绳海槽南部表层沉积中底栖有孔虫分布:水团和食物供应的共同制约
6. 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
7. Paleoclimatic Instability During the Mid-Pleistocene Transition: Implications from Foraminiferal Stable Isotope at ODP Site 1144, Northern South China Sea
南海北部ODP 1144站中更新世气候转型期有孔虫稳定同位素古气候意义
8. THE NEOGENE FORAMINIFERAL STRATIGRAPHY OF THE LH-19-4-1 BORE HOLE, PEARL RIVER MOUTH BASIN, SOUTH CHINA SEA
南海珠江口盆地LH-19-4-1井新近纪有孔虫生物地层研究
9. Ningbo Formation has long been considered to belong to a terrestrial one, but recently a large number of foraminiferal, ostracoda and mollusca fossils have been discovered in it.
在以往一直认为属于陆相地层的宁波组中,发现了大量有孔虫、介形虫和软体动物化石。
10. Cretaceous Paleocene Foraminiferal Communities from the Western Tarim Basin and Their Environmental Significance
塔里木盆地西部白垩纪－古新世有孔虫群落的划分及其环境意义
11. THE FORAMINIFERAL FAUNA AND THE CARBONIFEROUS - PERMIAN BOUNDARY IN THE TAIYUAN FORMATION OF THE XINWEN COALFIELD, SHANDONG
山东新汶煤田太原组小有孔虫动物群及石炭-二叠系界线的探讨
12. ON THE FORAMINIFERAL BIOSTRATIGRAPHY IN THE TAIYUAN FORMATION OF JINING COALFIELD (EAST AREA), SHANDONG
山东济宁煤田(东区)太原组小有孔虫生物地层
13. All counts were made between 1969 to 1990 of the planktonic foraminiferal population larger than 149 microns.The majority counts are larger than 300 individuals;some range as low as 100.
所有的数据测量都是在1969年至1990年进行的，浮游的有孔虫大多长于149微米，主要的计算都多于300个个体，有一些在100个个体左右。
14. foraminiferal zonation
有孔虫成带现象
15. foraminiferal ooze
有孔虫软泥
16. and finally, suggests that the free specimen materials should be used as much as possible in the Paleozoic foraminiferal study.
本文最后建议，古生代的有孔虫研究应该尽可能地利用实体化石来进行。
17. Characteristics of Foraminiferal Fauna in the Surficial Sediments of Tidal Flat in North Coast of Hangzhou Bay
杭州湾北岸潮滩表层沉积物中的有孔虫群特征
18. 3 assemblages and 5 subassemblages of benthic foraminifera are divided on the basis of the characters of abundance and distribution of benthic foraminiferal fauna in the area of study.
根据有孔虫动物群的数量及分布特点,研究区的底栖有孔虫可分为3个组合和5个亚组合。
19. REVIEW OF PLANKTONIC FORAMINIFERAL ASSEMBLAGES FOR SEA SURFACE TEMPERATURE ESTIMATE
浅谈浮游有孔虫群落海水古温度估算
20. LATEST PERMIAN SMALL FORAMINIFERAL FAUNA AT THE MEISHAN SECTION, ZHEJIANG PROVINCE
浙江煤山剖面二叠纪末的小有孔虫动物群
21. planktonic foraminiferal zone
浮游有孔虫带
22. DISCOVERY OF THE CARBONIFEROUS-PERMIAN FORAMINIFERAL MIXED FAUNA FROM THE BOTTOM OF CHIHSIA FORMATION IN SOUTHEASTERN HUNAN
湘东南栖霞组底部石炭-二叠纪有孔虫混生动物群的发现
23. Environmental Significance of Holocene Foraminiferal Assemblages in Shanggang, Yancheng
盐城上岗全新世有孔虫组合的环境意义
24. FORAMINIFERAL FAUNA DISTRIBUTION IN REEF-FACIES BEDS SINCE LATE MIOCENE IN XISHA ISLANDS AND ITS SIGNIFICANCE
西沙晚中新世以来礁相地层中有孔虫动物群的分布及其意义
25. This abundant foraminiferal fauna provides new data for a better understanding on the mass extinction pattern at the end of the Permian.
这一丰富的有孔虫动物群，不仅进一步完善了长兴阶标准剖面的化石资料，而且也为研究二叠纪末的生物灭绝形式提供了新的依据。
26. The results show the foraminiferal taphocoenoses are mixed from the indigenous with allochthonous compositions.
这些特点反映出埋葬群在形成过程中辐射沙洲区强大潮流的搬运作用。
27. Huang, T.-Y.(1977) Late Neogene planktonic foraminiferal biostratigraphy of the Tainan foothills region, Tainan, Taiwan. Petroleum Geology of Taiwan, 14, 121-145.
黄敦友(1977)台湾台南麓山带新第三纪浮游性有孔虫之生物地层。台湾石油地质，第14号，第121-145页。
28. Huang, T.-Y.(1978) Foraminiferal biostratigraphy of the Hunghuatzu section, southern Taiwan. Petroleum Geology of Taiwan, 15, 35-48.
黄敦友(1978)台湾南部红花仔剖面之有孔虫生物地层学研究。台湾石油地质，第15号，第35-48页。
