Research paperStable isotope fractionation in benthic foraminifera from the Peruvian continental margin
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Fundamental questions and applications of sclerochronology: Community-defined research priorities
2020, Estuarine, Coastal and Shelf ScienceCitation Excerpt :Other limitations of clumped isotope paleothermometry are its time-consuming and demanding analytical methods and its sensitivity to diagenetic overprint (Leutert et al., 2019). Offsets between the δ18Oc-derived temperatures and measured in situ temperatures have been reported for different archives and locations (e.g., Weber, 1970; McConnaughey, 1989; Bonitz et al., 2017; Dunbar and Wefer, 1984; Kelemen et al., 2017). In response to this issue, species-specific or site-specific calibrations are often formulated [Q17, 18].
The application of molluscs for investigating tsunami deposits
2020, Geological Records of Tsunamis and Other Extreme WavesOxygen and carbon isotope records of Upper Cretaceous foraminifera from Poland: vital and microhabitat effects
2018, Palaeogeography, Palaeoclimatology, PalaeoecologyVariability of foraminiferal stable isotope ratios in Caribbean shallow waters of Panama: A modern framework for Neogene studies
2016, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :We analyzed the benthic foraminifera Uvigerina peregrina Cushman (sensu Poag, 1981) and Cibicides pachyderma Rzehak (sensu van Morkhoven et al., 1986) to determine bottom stable isotopic values. The former has been demonstrated to be relatively free of “vital effects” (Shackleton, 1973; Grossman, 1984, 1987), depositing its test in isotopic equilibrium with ambient conditions for δ18O, and with a 1‰ offset for δ13C (Smith and Emiliani, 1968; Shackleton, 1977; Woodruff et al., 1980; Graham et al., 1981; Ganssen, 1983; Dunbar and Wefer, 1984). Graham et al. (1981) show that the oxygen isotope equilibrium fractionation of this taxon has remained constant through time.