Chapter Six Planktonic Foraminifera as Tracers of Past Oceanic Environments

作者: Michal Kucera

DOI: 10.1016/S1572-5480(07)01011-1

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摘要: … Relationship between shell size and temperature in planktonic foraminifera. Individual species achieve maximum size where they are most abundant (A), indicating that large …

参考文章(163)
N. Dittert, K.-H. Baumann, T. Bickert, R. Henrich, R. Huber, H. Kinkel, H. Meggers, Carbonate Dissolution in the Deep-Sea: Methods, Quantification and Paleoceanographic Application Springer Berlin Heidelberg. pp. 255- 284 ,(1999) , 10.1007/978-3-642-58646-0_10
Wh Berger, Mc Bonneau, Fl Parker, Foraminifera on the deep-sea floor - lysocline and dissolution rate Oceanologica Acta. ,vol. 5, pp. 249- 258 ,(1982)
Eelco J Rohling, Steve Cooke, None, Stable oxygen and carbon isotopes in foraminiferal carbonate shells Springer, Dordrecht. pp. 239- 258 ,(1999) , 10.1007/0-306-48104-9_14
David W. Lea, Trace elements in foraminiferal calcite Springer, Dordrecht. pp. 259- 277 ,(1999) , 10.1007/0-306-48104-9_15
Cesare Emiliani, The oceanic lithosphere Wiley. ,(1981)
Peter R. Thompson, Tsunemasa Saitō, Dee Breger, Systematic index of recent and pleistocene planktonic foraminifera University of Tokyo Press. ,(1981)
Jeremy R. Young, Hans R. Thierstein, Coccolithophores : from molecular processes to global impact Springer. ,(2004)
Karl K. Turekian, The Late Cenozoic glacial ages Yale University Press. ,(1971)
Colomban de Vargas, Alberto G. Sáez, Linda K. Medlin, Hans R. Thierstein, Super-Species in the calcareous plankton Coccolithophores. pp. 271- 298 ,(2004) , 10.1007/978-3-662-06278-4_11