Application of secondary ion mass spectrometry to the determination of Mg/Ca in rare, delicate, or altered planktonic foraminifera: Examples from the Holocene, Paleogene, and Cretaceous
- 23 December 2005
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 6 (12)
- https://doi.org/10.1029/2005gc000974
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Data Report: Stable Isotope Ratios of Foraminifers from ODP Leg 207 Sites 1257, 1258, and 1260 and a Cleaning Procedure for Foraminifers in Organic-Rich ShalesPublished by International Ocean Discovery Program (IODP) ,2005
- Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time seriesPaleoceanography and Paleoclimatology, 2003
- The potential of ion microprobe analysis in detecting geochemical variations across individual foraminifera testsGeochemistry, Geophysics, Geosystems, 2003
- Adaptation of a flow‐through leaching procedure for Mg/Ca paleothermometryGeochemistry, Geophysics, Geosystems, 2003
- Kinetic control of skeletal Sr/Ca in a symbiotic coral: Implications for the paleotemperature proxyPaleoceanography and Paleoclimatology, 2001
- Past temperature and δ18O of surface ocean waters inferred from foraminiferal Mg/Ca ratiosNature, 2000
- Variations in Mg/Ca and Sr/Ca ratios of planktonic foraminifera caused by postdepositional dissolution: Evidence of shallow Mg‐dependent dissolutionPaleoceanography and Paleoclimatology, 1996
- Comparative determinations of trace and minor elements in coral aragonite by ion microprobe analysis, with preliminary results from Phuket, southern ThailandGeochimica et Cosmochimica Acta, 1996
- Chemical Hydrography of the South Atlantic During the Last Glacial Maximum: Cd vs. δ13CPublished by Springer Nature ,1996
- Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: changes in deep ocean circulation and chemical inventoriesEarth and Planetary Science Letters, 1985