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    Academic Journal
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    وصف الملف: text/tab-separated-values, 35 data points

    Relation: Kozdon, Reinhard; Kelly, Daniel Clay (in review): Hot tropical temperatures during the Paleocene-Eocene thermal maximum revealed by paired in-situ d13C and Mg/Ca measurements on individual planktic foraminifer shells.; Kozdon, Reinhard; Kelly, Daniel Clay; Kita, Noriko T; Fournelle, John H; Valley, John W (2011): Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical sea surface temperatures during the Early Paleogene. Paleoceanography, 26(3), PA3206, https://doi.org/10.1029/2010PA002056; Kozdon, Reinhard; Kelly, Daniel Clay; Kitajima, K; Strickland, A; Fournelle, John H; Valley, John W (2013): In situ d18O and Mg/Ca analyses of diagenetic and planktic foraminiferal calcite preserved in a deep-sea record of the Paleocene-Eocene thermal maximum%7C. Paleoceanography, 28(3), 517-528, https://doi.org/10.1002/palo.20048; Kozdon, Reinhard; Kelly, Daniel Clay; Valley, John W (2018): Diagenetic Attenuation of Carbon Isotope Excursion Recorded by Planktic Foraminifers During the Paleocene‐Eocene Thermal Maximum. Paleoceanography and Paleoclimatology, 33(4), 367-380, https://doi.org/10.1002/2017PA003314; Kozdon, Reinhard; Ushikubo, Takayuki; Kita, Noriko T; Spicuzza, Michael J; Valley, John W (2009): Intratest oxygen isotope variability in the planktonic foraminifer N. pachyderma: Real vs. apparent vital effects by ion microprobe. Chemical Geology, 258(3-4), 327-337, https://doi.org/10.1016/j.chemgeo.2008.10.032; https://doi.pangaea.de/10.1594/PANGAEA.967641; https://doi.org/10.1594/PANGAEA.967641

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    وصف الملف: text/tab-separated-values, 434 data points

    Relation: Kozdon, Reinhard; Kelly, Daniel Clay (in review): Hot tropical temperatures during the Paleocene-Eocene thermal maximum revealed by paired in-situ d13C and Mg/Ca measurements on individual planktic foraminifer shells.; Kozdon, Reinhard; Kelly, Daniel Clay; Kita, Noriko T; Fournelle, John H; Valley, John W (2011): Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical sea surface temperatures during the Early Paleogene. Paleoceanography, 26(3), PA3206, https://doi.org/10.1029/2010PA002056; Kozdon, Reinhard; Kelly, Daniel Clay; Kitajima, K; Strickland, A; Fournelle, John H; Valley, John W (2013): In situ d18O and Mg/Ca analyses of diagenetic and planktic foraminiferal calcite preserved in a deep-sea record of the Paleocene-Eocene thermal maximum%7C. Paleoceanography, 28(3), 517-528, https://doi.org/10.1002/palo.20048; Kozdon, Reinhard; Kelly, Daniel Clay; Valley, John W (2018): Diagenetic Attenuation of Carbon Isotope Excursion Recorded by Planktic Foraminifers During the Paleocene‐Eocene Thermal Maximum. Paleoceanography and Paleoclimatology, 33(4), 367-380, https://doi.org/10.1002/2017PA003314; Kozdon, Reinhard; Ushikubo, Takayuki; Kita, Noriko T; Spicuzza, Michael J; Valley, John W (2009): Intratest oxygen isotope variability in the planktonic foraminifer N. pachyderma: Real vs. apparent vital effects by ion microprobe. Chemical Geology, 258(3-4), 327-337, https://doi.org/10.1016/j.chemgeo.2008.10.032; https://doi.pangaea.de/10.1594/PANGAEA.967640; https://doi.org/10.1594/PANGAEA.967640

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    Periodical

    المصدر: Euroweek. 4/15/2005, Issue 899, p62-63. 2p.

    مصطلحات موضوعية: *FINANCIAL leverage

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