1978
DOI: 10.1111/j.1502-3885.1978.tb00051.x
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Planktonic foraminiferal and oxygen isotopic stratigraphy and paleoclimatology of Norwegian Sea deep‐sea cores

Abstract: BOREAS Kellogg, T. B., Duplessy, J. C. & Shackleton, N. J. 1978 03 01: Planktonic foraminiferal and oxygen isotopic stratigraphy and paleoclimatology of Norwegian Sea deep‐sea cores. Boreas. Vol. 7, pp. 61–73. Oslo. ISSN 0300–9483. Three Norwegian Sea deep‐sea cores, which penetrate to sediments at least 200,000 years old, were analyzed for oxygen isotope content, total calcium carbonate, and planktonic foraminifera. The oxygen isotopic stratigraphy was used to refine the time control for paleoclimatic and pal… Show more

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Cited by 185 publications
(85 citation statements)
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“…Oxygen isotope studies (KELLOGG et al, 1978;KELLOGG, 1980;LABEYRIE & DUPLESSY, 1985;HENRICH et al, 1988) have successfully been used to establish a chronostratigraphic framework for Quater-nary sediment series in the Norwegian and Greenland seas. They typically result in sedimentation rates of, on average, several cm per thousand years for this period and mostly indicate a pronounced variability in accumulation through time .…”
Section: Introductionmentioning
confidence: 99%
“…Oxygen isotope studies (KELLOGG et al, 1978;KELLOGG, 1980;LABEYRIE & DUPLESSY, 1985;HENRICH et al, 1988) have successfully been used to establish a chronostratigraphic framework for Quater-nary sediment series in the Norwegian and Greenland seas. They typically result in sedimentation rates of, on average, several cm per thousand years for this period and mostly indicate a pronounced variability in accumulation through time .…”
Section: Introductionmentioning
confidence: 99%
“…In the Norwegian Sea, at the northernmost stretches of the North Atlantic, numerous oscillations of the Arctic Polar Front during the late Quaternary have been documented through quantitative studies of foraminifers and calcareous nannofossils and oxygen isotope data (Kellogg et al, 1978;Belanger, 1982;Gard and Backman, in press). Detailed correlations between the oxygen isotope stratigraphy and nannofossils in the Norwegian Sea show that nannofossil abundance and assemblage variations reflect climatic changes.…”
Section: Background and Objectivesmentioning
confidence: 99%
“…Therefore, δ 18 O values of fossil planktic foraminiferal shells have been widely used to estimate sea surface temperatures (e.g. Kellogg et al, 1978;Erez and Luz, 1983), salinity (e.g. Duplessy et al, 1992) and ocean stratification (Simstich et al, 2003).…”
Section: Introductionmentioning
confidence: 99%