Structure and timing of the last deglaciation: Oxygen-isotope evidence☆
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Cited by (103)
High latitude regulation of low latitude thermocline ventilation and planktic foraminifer populations across glacial-interglacial cycles
2011, Earth and Planetary Science LettersCitation Excerpt :Age models for all sites apart from five (those numbered 2, 4, 5, 11 and 23 in Figs. 8 and 9) are based on radiocarbon analyses. These analyses are primarily of bulk calcium carbonate and were generated in the late 1970s and early-mid 1980s using classic decay counting methodologies (Bé et al., 1976; Jones and Ruddiman, 1982; Mix and Ruddiman, 1985; Ruddiman and Mix, 1993). However, the radiocarbon age model for our new faunal data (site no. 1 in Figs. 8 and 9) (Came et al., 2003), in addition to that for site no. 20 (Huls and Zahn, 2000), was produced using new Accelerator Mass Spectrometry (AMS) technologies.
Latest Pleistocene and Holocene alpine glacier fluctuations in Scandinavia
2009, Quaternary Science ReviewsInfluences on the fractionation of calcium isotopes in planktonic foraminifera
2008, Earth and Planetary Science LettersCitation Excerpt :Samples were collected in subarctic, subtropical, and tropical Atlantic to represent a range of calcification temperatures (Fig. 1b). Ages of samples determined using radiocarbon dating were found to be within the Holocene (Mix and Ruddiman, 1985; Ravelo and Andreason, 1999; Simstich, 1999; Simstich et al., 2003). The calcification temperature range of each species varies according to its environmental preferences (Table 3).
Changes Deduced from Foraminiferal Assemblages, their Isotopic Composition and from Alkenones
2008, Developments in Quaternary ScienceCitation Excerpt :upper slope off the Niger River (Pastouret et al., 1978), lower slope of Gabon and Guyana (Mix and Ruddiman, 1985), may be, in the Benguela system and subtropical gyre margin where slow rates of sedimentation are recorded (Wefer et al., 1996).
Sediment Accumulation Rates and Fluxes
2008, Developments in Quaternary ScienceCitation Excerpt :The lowered sea level may have given rise to turbidity currents originating from the outer shelf and the uppermost slope when the coastal currents and waves were active erosion agents. Tropical Atlantic sediments were especially studied because high pelagic sedimentation rates in this area typically 3–5 cm/kyr allow high-resolution analyses (Mix and Ruddiman, 1985). During the last 30 kyr, the rate of sedimentation is essentially constant in the shallower cores with higher sedimentation rates.
Deglacial ocean and climate seasonality in laminated diatom sediments, Mac.Robertson Shelf, Antarctica
2005, Palaeogeography, Palaeoclimatology, Palaeoecology
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Lamont Doherty Geological Observatory Contribution No. 3895.
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Present address: College of Oceanography, Oregon State University, Corvallis, OR 97331, U.S.A.