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Swart, P.K., Kennedy, M.J. (2012) Does the global stratigraphic reproducibility of δ13C in Neoproterozoic carbonates require a marine origin? A Pliocene–Pleistocene comparison. Geology, 40 (1) 87-90 doi:10.1130/g32538.1

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Reference TypeJournal (article/letter/editorial)
TitleDoes the global stratigraphic reproducibility of δ13C in Neoproterozoic carbonates require a marine origin? A Pliocene–Pleistocene comparison
JournalGeology
AuthorsSwart, P.K.Author
Kennedy, M.J.Author
Year2012 (January)Volume40
Issue1
PublisherGeological Society of America
DOIdoi:10.1130/g32538.1Search in ResearchGate
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Mindat Ref. ID141540Long-form Identifiermindat:1:5:141540:1
GUID0
Full ReferenceSwart, P.K., Kennedy, M.J. (2012) Does the global stratigraphic reproducibility of δ13C in Neoproterozoic carbonates require a marine origin? A Pliocene–Pleistocene comparison. Geology, 40 (1) 87-90 doi:10.1130/g32538.1
Plain TextSwart, P.K., Kennedy, M.J. (2012) Does the global stratigraphic reproducibility of δ13C in Neoproterozoic carbonates require a marine origin? A Pliocene–Pleistocene comparison. Geology, 40 (1) 87-90 doi:10.1130/g32538.1
In(2012, January) Geology Vol. 40 (1) Geological Society of America

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Kennedy, Martin J., Christie-Blick, Nicholas (2012) Condensation origin for Neoproterozoic cap carbonates during deglaciation: REPLY. Geology, 40 (4) doi:10.1130/g33214y.1
Kula, Joseph, Metcalf, James R., Wilkinson, Bruce H. (2012) Condensation origin for Neoproterozoic cap carbonates during deglaciation: COMMENT. Geology, 40 (4) doi:10.1130/g32688c.1
Kennedy, M. J., Christie-Blick, N. (2011) Condensation origin for Neoproterozoic cap carbonates during deglaciation. Geology, 39 (4) 319-322 doi:10.1130/g31348.1
Prave, A. R. (1999) Two diamictites, two cap carbonates, two δ13C excursions, two rifts: The Neoproterozoic Kingston Peak Formation, Death Valley, California. Geology, 27 (4) 339 doi:10.1130/0091-7613(1999)027<0339:tdtcct>2.3.co;2
Kennedy, Martin J., Droser, Mary L. (2012) Early Cambrian metazoans in fluvial environments, evidence of the non-marine Cambrian radiation: REPLY. Geology, 40 (6) doi:10.1130/g33346y.1
Tiwari, R.K (1987) A Walsh spectral comparison of oxygen (δ18O) and carbon isotope (δ13C) variations of the Pleistocene bore hole (Eureka 67–135) from the Gulf of Mexico and their orbital significance. Marine Geology, 78 (1) 167-174 doi:10.1016/0025-3227(87)90076-4
Artoni, Andrea (2013) The Pliocene-Pleistocene stratigraphic and tectonic evolution of the Central sector of the Western Periadriatic Basin of Italy. Marine and Petroleum Geology, 42. 82-106 doi:10.1016/j.marpetgeo.2012.10.005
Bouloubassi, Ioanna, Rullkötter, Jürgen, Meyers, Philip A (1999) Origin and transformation of organic matter in Pliocene–Pleistocene Mediterranean sapropels: organic geochemical evidence reviewed. Marine Geology, 153 (1) 177-197 doi:10.1016/s0025-3227(98)00082-6
Prave, Anthony R. (2000) Two diamictites, two cap carbonates, two δ13C excursions, two rifts: The Neoproterozoic Kingston Peak Formation, Death Valley, California: Comment and Reply. Geology, 28 (2) 192 doi:10.1130/0091-7613(2000)28<192:tdtcct>2.0.co;2
Fujioka, Toshiyuki, Chappell, John, Fifield, L. Keith, Rhodes, Edward J. (2009) Australian desert dune fields initiated with Pliocene–Pleistocene global climatic shift. Geology, 37 (1) 51-54 doi:10.1130/g25042a.1
Swart, P.K., Wortmann, U.G., Mitterer, R.M., Malone, M.J., Smart, P.L., Feary, D.A., Hine, A.C. (2000) Hydrogen sulfide–hydrates and saline fluids in the continental margin of South Australia. Geology, 28 (11) 1039-1042 doi:10.1130/0091-7613(2000)028<1039:hshasf>2.3.co;2
 
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