Home
About
Advanced Search
Browse by Discipline
Scientific Societies
E-print Alerts
Add E-prints
FAQ
•
HELP
•
SITE MAP
•
CONTACT US
Search
Advanced Search
Lea, David - Department of Geological Sciences, University of California at Santa Barbara
2170 VOLUME 17J O U R N A L O F C L I M A T E 2004 American Meteorological Society
Core top calibration of Mg/Ca in tropical foraminifera: Refining paleotemperature estimation
Quaternary deep sea temperature histories derived from benthic foraminiferal Mg/Ca
Role of deep sea temperature in the carbon cycle during the last glacial
Nevertheless, the presence of previously un-known, higher order lineages of fungi in tundra
Supplemental Online Materials for Lea et al. Materials and methods
Climate Impact of Late Quaternary Equatorial Pacific
3Geochemistry Published by AGU and the Geochemical Society
Quaternary Science Reviews 25 (2006) 11521167 Paleoclimate history of Gala pagos surface waters
Influence of volcanic shards on foraminiferal Mg/Ca in a core from the Galapagos region
doi:10.1016/j.gca.2004.03.013 Effects of seawater carbonate ion concentration and temperature on shell U, Mg, and Sr in
1 LEA ET AL. SST IN THE WESTERN EQUATORIAL PACIFIC DURING MIS 11 Sea Surface Temperatures in the Western Equatorial Pacific During
Quaternary Science Reviews 21 (2002) 283293 Reconstructing a 350 ky history of sea level using planktonic Mg/Ca
References and Notes 1. E. Coronado, J. R. Galan-Mascaros, C. J. Gomez-Gar-
Uranium-series and radiocarbon geochronology of deep-sea corals: implications for Southern Ocean ventilation rates and
PII S0016-7037(99)00197-0 Controls on magnesium and strontium uptake in planktonic foraminifera determined by
ELSEVIER Earth and Planetary Science Letters 170 (1999) 417432 www.elsevier.com/locate/epsl
A simple evaluation of cleaning procedures on fossil benthic foraminiferal Mg/Ca
Effects of temperature on Mg/Ca in neogloboquadrinid shells determined by live culturing
ELSEVIER Marine Micropaleontology 38 (2000) 213228 www.elsevier.com/locate/marmicro
Variability in the El Nin~o Southern Oscillation Through a
A9000 Elemental and Isotopic Proxies of Past Ocean Temperatures