Carbonate Ion Effect on Foraminifera Stable Isotopes: Readme file --------------------------------------------------------------------- NOAA Paleoclimatology Program and World Data Center A - for Paleoclimatology --------------------------------------------------------------------- NOTE: PLEASE CITE ORIGINAL REFERENCE WHEN USING THIS DATA!!!!! NAME OF DATA SET: Carbonate Ion Effect on Foraminifera Stable Isotopes LAST UPDATE: 10/1999 (Original Receipt by WDCA Paleo) CONTRIBUTOR: Ann Russell, University of California, Davis IGBP PAGES/WDCA CONTRIBUTION SERIES NUMBER: 1999-054 SUGGESTED DATA CITATION: Russell, A. D. and H. J. Spero, 1999, Carbonate Ion Effect on Foraminifera Stable Isotopes, IGBP PAGES/World Data Center A for Paleoclimatology Data Contribution Series #1999-054. NOAA/NGDC Paleoclimatology Program, Boulder CO, USA. ORIGINAL REFERENCE: Russell, A. D. and H. J. Spero, 2000, Field examination of the oceanic carbonate ion effect on stable isotopes in planktonic foraminifera, Paleoceanography, v.15, No.1, pp.43-52, February 2000. FUNDING SOURCE: National Science Foundation, USA This material is based upon work supported by the National Science Foundation under Grant No. OCE-9726821. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the National Science Foundation. GEOGRAPHIC REGION: Eastern Tropical Pacific PERIOD OF RECORD: Modern LIST OF FILES: Readme.Russell1999.txt (this file), Russell1999data.doc (Microsoft Word format), Russell1999.table1.txt, Russell1999.table2.txt, Russell1999.table3.txt (Tab delimited ASCII text format) DESCRIPTION: This study looks for evidence of the carbonate ion effect (identified in laboratory experiments) on stable isotopes in foraminifera spanning a natural carbonate ion gradient at the equatorial Pacific. The data set comprises size, weight, d18O and d13C data for two species of planktonic foraminifera (G. ruber and P. obliquiloculata) collected in sediment traps along a transect spanning the equator along 140°W, from 5°N to 12°S (135°W).