Palaeogeography, Palaeoclimatology, Palaeoecology
Deep circulation in the Late Cretaceous: Oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores
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Cited by (74)
Climate paleogeography knowledge graph and deep time paleoclimate classifications
2023, Geoscience FrontiersCitation Excerpt :The nearest living relatives of fossil plants are also unambiguous (Bowman et al., 2014). In addition, a lot of paleoclimatic studies had been conducted both based on the geological proxies and paleoclimate modeling (Saltzman and Barron, 1982; Upchurch et al., 1998; de Bar et al., 2019; Schlanser et al., 2019; Zhang et al., 2019), which provide abundant quantitative paleoclimatic data. For Boucot’s classification, a total of 397 climatically sensitive deposits during the Coniacian-Maastrichtian are used (Boucot et al., 2013).
The giant inoceramid Platyceramus platinus as a high-resolution paleoclimate archive for the Late Cretaceous of the Western Interior Seaway
2018, Cretaceous ResearchCitation Excerpt :Inoceramids were marine benthic bivalves that occurred worldwide and were one of the most abundant bivalve taxon among Late Cretaceous macrofaunas (Saltzman and Barron, 1982; Dhondt, 1992; Voigt, 1995; MacLeod and Huber, 1996).
Extinction, dissolution, and possible ocean acidification prior to the Cretaceous/Paleogene (K/Pg) boundary in the tropical Pacific
2017, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :During the Cretaceous, inoceramids were common in many benthic marine communities. They were found globally at all latitudes and wide paleodepths (Saltzman and Barron, 1982; MacLeod et al., 1996). Their extinction was diachronous over a 3–4 Myr time span first at high latitudes at ~ 72 Ma, followed by low latitude regions ~ 68–69 Ma (MacLeod, 1994a; MacLeod et al., 1996; MacLeod and Huber, 1996; Crame and Luther, 1997; Chauris et al., 1998; this study).
Greenhouse Climates
2013, Treatise on Geochemistry: Second Edition<sup>87</sup>Sr/<sup>86</sup>Sr ratios in inoceramids (Bivalvia) and carbonate matrix as indicators of differential diagenesis during burial. Early Maastrichtian Bay of Biscay sections (Spain and France). Potential use for chemostratigraphy?
2008, Cretaceous ResearchCitation Excerpt :The most accepted scenario to explain this extinction is a change in ocean circulation. The sluggish circulation of dense, warm, deep-ocean waters changed to vigorous, deep, cold, and oxygen-rich Antarctic waters (Saltzmann et al., 1982; Barron et al., 1984; Barrera and Huber, 1990; Huber, 1990; Thomas, 1990). Both inoceramid and carbonate matrix oxygen isotope records from Member II of the Sopelana II, Sopelana I, and Zumaya sections (Basque-Cantabrian Basin) indicate that inoceramid disappearance is associated with a positive shift in the δ18O values (Gómez-Alday, 2002; Gómez-Alday and Elorza, 2003).
Can biomass burning produce a globally significant carbon-isotope excursion in the sedimentary record?
2006, Earth and Planetary Science Letters