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Le Guerroué, Erwan (2010) Duration and synchroneity of the largest negative carbon isotope excursion on Earth: The Shuram/Wonoka anomaly. Comptes Rendus Geoscience, 342 (3). 204-214 doi:10.1016/j.crte.2009.12.008

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Reference TypeJournal (article/letter/editorial)
TitleDuration and synchroneity of the largest negative carbon isotope excursion on Earth: The Shuram/Wonoka anomaly
JournalComptes Rendus Geoscience
AuthorsLe Guerroué, ErwanAuthor
Year2010 (March)Volume342
Issue3
PublisherElsevier BV
DOIdoi:10.1016/j.crte.2009.12.008Search in ResearchGate
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Mindat Ref. ID3802000Long-form Identifiermindat:1:5:3802000:1
GUID0
Full ReferenceLe Guerroué, Erwan (2010) Duration and synchroneity of the largest negative carbon isotope excursion on Earth: The Shuram/Wonoka anomaly. Comptes Rendus Geoscience, 342 (3). 204-214 doi:10.1016/j.crte.2009.12.008
Plain TextLe Guerroué, Erwan (2010) Duration and synchroneity of the largest negative carbon isotope excursion on Earth: The Shuram/Wonoka anomaly. Comptes Rendus Geoscience, 342 (3). 204-214 doi:10.1016/j.crte.2009.12.008
In(2010, March) Comptes Rendus Geoscience Vol. 342 (3) Elsevier BV

See Also

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Le Guerroué, Erwan, Cozzi, Andrea (2010) Veracity of Neoproterozoic negative C-isotope values: The termination of the Shuram negative excursion. Gondwana Research, 17 (4) 653-661 doi:10.1016/j.gr.2009.11.002
Le Guerroué, Erwan, Allen, Philip A., Cozzi, Andrea (2006) Chemostratigraphic and sedimentological framework of the largest negative carbon isotopic excursion in Earth history: The Neoproterozoic Shuram Formation (Nafun Group, Oman) Precambrian Research, 146 (1) 68-92 doi:10.1016/j.precamres.2006.01.007
Le Guerroué, Erwan, Allen, Philip A., Cozzi, Andrea (2007) Erratum to “Chemostratigraphic and sedimentological framework of the largest negative carbon isotopic excursion in Earth history: The Neoproterozoic Shuram Formation (Nafun Group, Oman)” [J. Precam. Res. 146 (2006) 68–92]. Precambrian Research, 153 (3) 262-265 doi:10.1016/j.precamres.2006.12.002
Derry, Louis A. (2010) A burial diagenesis origin for the Ediacaran Shuram–Wonoka carbon isotope anomaly. Earth and Planetary Science Letters, 294 (1) 152-162 doi:10.1016/j.epsl.2010.03.022
Paillard, Didier (2010) Climate and the orbital parameters of the Earth. Comptes Rendus Geoscience, 342 (4). 273-285 doi:10.1016/j.crte.2009.12.006
Minguez, D., Kodama, K.P., Hillhouse, J.W. (2015) Paleomagnetic and cyclostratigraphic constraints on the synchroneity and duration of the Shuram carbon isotope excursion, Johnnie Formation, Death Valley Region, CA. Precambrian Research, 266. 395-408 doi:10.1016/j.precamres.2015.05.033
Williams, George E., Schmidt, Phillip W. (2018) Shuram–Wonoka carbon isotope excursion: Ediacaran revolution in the world ocean's meridional overturning circulation. Geoscience Frontiers, 9 (2) 391-402 doi:10.1016/j.gsf.2017.11.006
Cui, Huan (2017) Rock magnetic chronostratigraphy of the Shuram carbon isotope excursion: Wonoka Formation, Australia: COMMENT. Geology, 45 (10) doi:10.1130/g39593c.1
Wostbrock, Jordan A.G.; Planavsky, Noah (2026) The Shuram carbon isotope excursion in the Wonoka Formation, South Australia, does not record open ocean conditions. Earth and Planetary Science Letters, 684. doi:10.1016/j.epsl.2026.120005
Petit, Michel, Dercourt, Jean (2010) Éditorial. Comptes Rendus Geoscience, 342 (9). 685-686 doi:10.1016/j.crte.2010.04.004
Dabas, Alain (2010) Observing the atmospheric wind from space. Comptes Rendus Geoscience, 342 (4). 370-379 doi:10.1016/j.crte.2009.09.014
 
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