Stable isotopic fractionation among particles in Quaternary coccolith‐sized deep‐sea sediments
- 1 August 1987
- journal article
- research article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 2 (4) , 423-429
- https://doi.org/10.1029/pa002i004p00423
Abstract
Oxygen and carbon isotopic ratios of individual grain size splits of the 18O and ∂13C values of individual splits are linearly related to each other with a slope of 1.5 ∂13C/∂18O in all Holocene and Glacial samples analyzed. Although the observed variability is less than predicted from culture experiments of individual components, compositional variations can significantly influence the stable isotopic stratigraphies measured on the nannofossil fraction.This publication has 21 references indexed in Scilit:
- Carbon isotope fractionation during the precipitation of calcium carbonatePublished by Elsevier ,2002
- Stable isotopic composition of coccolithsMarine Micropaleontology, 1986
- Isotopic and biostratigraphical records of calcareous nannofossils in a Pleistocene coreNature, 1981
- Coccoliths in Pleistocene–Holocene nannofossil assemblagesNature, 1980
- Oxygen and carbon isotopes of Recent calcareous nannofossils as paleoceanographic indicatorsMarine Micropaleontology, 1980
- Oxygen isotope content of coccoliths grown in cultureDeep Sea Research Part A. Oceanographic Research Papers, 1979
- Oxygen and Carbon Isotope Analyses of Tertiary and Cretaceous Microfossils from Shatsky Rise and Other Sites in the North Pacific OceanPublished by International Ocean Discovery Program (IODP) ,1975
- The stable isotope geochemistry of marine coccoliths; a preliminary comparison with planktonic foraminiferaJournal of Foraminiferal Research, 1975
- A kinetic approach to the effect of temperature on algal growth1Limnology and Oceanography, 1974
- REVISED CARBONATE-WATER ISOTOPIC TEMPERATURE SCALEGSA Bulletin, 1953