Stable isotopic study of Oligocene-Miocene sediments from DSDP Site 354, Equatorial Atlantic
References (71)
- et al.
Speculations about the upper Miocene change in abyssal Pacific dissolved bicarbonate C-13
Earth Planet. Sci. Lett.
(1979) Ecologic patterns of living planktonic Foraminifera
Deep-Sea Res.
(1969)- et al.
Stable isotope ratios of dissolved inorganic carbon in the Atlantic
Deep Sea Res.
(1969) - et al.
Oxygen isotopic evidence for the depth stratification of Tertiary and Cretaceous planktic foraminifera
Mar. Micropaleontol.
(1978) - et al.
Carbon isotope fractionation during the precipitation of calcium carbonate
Earth Planet. Sci. Lett.
(1970) - et al.
Oxygen and carbon isotopes of recent calcareous nannofossils as paleoceanographic indicators
Mar. Micropaleontol.
(1980) - et al.
Carbon and oxygen isotopic disequilibria of Recent Deep-Sea benthic foraminifera
Mar. Micropaleontol
(1981) The dissolved O2-CO2-13C system in the eastern Equatorial Pacific
Deep Sea Res.
(1974)The distribution of carbon-13 in the Atlantic Ocean
Earth Planet. Sci. Lett.
(1980)- et al.
Total CO2,13C, and dissolved oxygen18O at GEOSECS II in the North Atlantic
Earth Planet. Sci. Lett.
(1972)
Ocean basin and depth variability of oxygen isotopes in Cenozoic benthic foraminifera
Mar. Micropaleontol.
Miocene benthic foraminiferal isotope records: a synthesis
Mar. Micropaleontol.
Oxygen and carbon isotope studies in recent foraminifera from the southwest Indian Ocean
Mar. Micropaleontol.
Carbon isotopic compositions in Recent planktonic foraminifera of the Indian Ocean
Earth Planet. Sci. Lett.
Biological fractionation of oxygen and carbon isotopes by recent benthic foraminifera
Mar. Micropaleontol.
The stable isotope geochemistry of marinecoccoliths: a preliminary comparison with planktonic foraminifera
J. Foraminiferal Res.
Shell growth and structure of planktonic foraminifera
Science
Distribution and ecology of living planktonic Foraminifera in surface waters in the Atlantic and Indian Oceans
Stable isotopes in deep-sea carbonates: Bob Core ERDC-92, West Equatorial Pacific
Oceanol. Acta
The Oligocene/Miocene boundary in the Equatorial Atlantic DSDP Site 354. Results of studies on planktic foraminifera and calcareous nannofossils
Riv. Ital. Paleontol. Stratigr.
Late middle Eocene to Recent planktonic foraminiferal biostratigraphy
Tertiary oxygen and carbon isotope stratigraphy, Site 357 (mid latitude south Atlantic)
Oxygen and carbon isotope record through the Oligocene, DSDP Site 366, Equatorial Atlantic
Zonation of Cretaceous to Pliocene marine sediments based on planktonic Foraminifera
Boll. Inf. Assoc. Venez. Min. Petrol.
Ecology of Living Planktonic Foraminifera in the North and Euqatorial Pacific Ocean
Carbonate dissolution on the western flank of the east Pacific Rise
Oxygen isotope fractionation and algal symbiosis in benthic foraminifera from the Gulf of Elat, Israel
Bull. Geol. Soc. Den.
Oxygen isotope paleotemperature measurements on New Zealand Tertiary fossils
N.Z. J. Si.
Australian Tertiary paleotemperatures
J. Geol.
Oxygen and carbon isotope analyses of Cretaceous and Tertiary foraminifera from the central North Pacific
Differential isotopic fractionation in benthic foraminifera and paleotemperatures reassessed
Science
Depth habitats of some species of pelagic foraminifera as indicated by oxygen isotope ratios
Am. J. Sci.
Pleistocene temperatures
J. Geol.
Depth habitats of growth stages of pelagic foraminifera
Science
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Cenozoic coccolith size changes-Evolutionary and/or ecological controls?
2012, Palaeogeography, Palaeoclimatology, PalaeoecologyGeochemical assessment of the palaeoecology, ontogeny, morphotypic variability and palaeoceanographic utility of "Dentoglobigerina" venezuelana
2012, Marine MicropaleontologyCitation Excerpt :Most stable isotope studies of planktic foraminifera assign “D.” venezuelana to a sub-thermocline habitat (Barrera et al., 1985; Keller, 1985; Hodell and Vayavananda, 1993; Norris et al., 1993; Pearson and Shackleton, 1995; Pearson et al., 2001; Smart and Thomas, 2006; Spezzaferri and Pearson, 2009). However, data generated on samples of O/M boundary age (~ 23 Ma), from Ceara Rise and Trinidad, imply that “D.” venezuelana calcified higher in the water column, within the thermocline (Biolzi, 1983; Pearson et al., 1997; Pearson and Wade, 2009). Furthermore, results from analysis of Oligocene (~ 28 Ma) age samples from the Gulf of Mexico (Poore and Matthews, 1984) and the equatorial Pacific at ODP Site 1218 (Wade et al., 2007), imply that calcification took place within the mixed layer.