
Mg/Ca temperature calibration for the benthic foraminifer Cibicidoides pachyderma
Author(s) -
Marchitto T. M.,
Bryan S. P.,
Curry W. B.,
McCorkle D. C.
Publication year - 2007
Publication title -
paleoceanography
Language(s) - English
Resource type - Journals
eISSN - 1944-9186
pISSN - 0883-8305
DOI - 10.1029/2006pa001287
Subject(s) - authigenic , geology , benthic zone , oceanography , salinity , temperature salinity diagrams , paleoceanography , foraminifera , paleontology , sedimentary rock
The recent development of foraminiferal Mg/Ca as a paleotemperature proxy has enabled the extraction of global ice volume and local salinity from the more traditional paleotemperature proxy δ 18 O. The benthic foraminiferal genus Cibicidoides is widely used in paleoceanographic reconstructions because of its epifaunal habitat and cosmopolitan distribution, and it has received early attention in Mg/Ca work. However, existing temperature calibrations for Cibicidoides rely heavily on C. pachyderma core top data from one location, Little Bahamas Bank, where authigenic processes and/or reworking may result in elevated warm water Mg/Ca values. Here we present new C. pachyderma Mg/Ca data from a series of 29 high‐quality multicore tops collected in the Florida Straits, spanning a temperature range of 5.8–18.6°C. In contrast to previous calibrations, we find no evidence for a strongly exponential response to temperature. The data are best explained by a linear relationship, with a sensitivity of 0.12 mmol mol −1 per °C.