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] 07[理学] 070901[理学-矿物学、岩石学、矿床学]
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 proxy.In this study we describe the application of the Mg/Ca paleothermometer with the aim of illustrate its use in the Mediterranean Basin.We value the influence of the salinity and diagenetic carbonate processes besides temperature as an important environmental factor controlling the foraminiferal Mg/Ca.For this purpose 3 species of