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