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Mg/Ca Variation in Planktonic Foraminiferal Tests:Assessing Influence of Salinity and Diagenetic Carbonate Dissolution for Reconstruction of Palaeo-seawater Temperature

Mg/Ca Variation in Planktonic Foraminiferal Tests:Assessing Influence of Salinity and Diagenetic Carbonate Dissolution for Reconstruction of Palaeo-seawater Temperature

作     者:Anna Sabbatini Frank Bassinot Alessandra Negri 

作者机构:Department of Marine SciencePolytechnic University of Marche Laboratoire des Sciences du Climat et de l'Environnement(CNRS/CEAAJVSQ) 

出 版 物:《地学前缘》 (Earth Science Frontiers)

年 卷 期:2009年第16卷第S1期

页      面:223-223页

核心收录:

学科分类:0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 

主  题:planktonic foraminiferal Mg/Ca paleotemperature salinity diagenesis Mediterranean Basin 

摘      要:Over the past decade,the Mg/Ca ratio in foraminiferal tests has emerged as a valuable paleotemperature *** this study we describe the application of the Mg/Ca paleothermometer with the aim of illustrate its use in the Mediterranean *** value the influence of the salinity and diagenetic carbonate processes besides temperature as an important environmental factor controlling the foraminiferal Mg/*** this purpose 3 species of

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