Polar record of Early Jurassic massive carbon injection
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M. Rogov | K. Föllmi | C. Lécuyer | J. Spangenberg | T. Adatte | F. Baudin | E. Mattioli | G. Suan | B. Pittet | J. Riding | B. Nikitenko | A. Goryacheva | L. Glinskikh | V. G. Knyazev | Boris L. Nikitenko | 3. JorgeE. | Spangenberg | 4. Thierry | Adatte | B. L. Nikitenko
[1] A. Hannenberg,et al. A GLOBAL EVENT , 2013 .
[2] M. Floquet,et al. Drowning of a carbonate platform as a precursor stage of the Early Toarcian global anoxic event (Southern Provence sub‐Basin, South‐east France) , 2012 .
[3] Paul L. Smith,et al. The significance of an Early Jurassic (Toarcian) carbon-isotope excursion in Haida Gwaii (Queen Charlotte Islands), British Columbia, Canada , 2011 .
[4] J. J. Gómez,et al. Warming-driven mass extinction in the Early Toarcian (Early Jurassic) of northern and central Spain. Correlation with other time-equivalent European sections , 2011 .
[5] M. Joachimski,et al. Climatic ups and downs in a disturbed Jurassic world , 2011 .
[6] H. Jenkyns,et al. A global event with a regional character: the Early Toarcian Oceanic Anoxic Event in the Pindos Ocean (northern Peloponnese, Greece) , 2011, Geological Magazine.
[7] S. Hesselbo,et al. Stepwise atmospheric carbon-isotope excursion during the Toarcian Oceanic Anoxic Event (Early Jurassic, Polish Basin) , 2011 .
[8] E. Mattioli,et al. Toarcian carbon isotope shifts and nutrient changes from the Northern margin of Gondwana (High Atlas, Morocco, Jurassic): Palaeoenvironmental implications , 2010 .
[9] F. Venturi,et al. Ammonite faunas, OAE and the Pliensbachian–Toarcian boundary (Early Jurassic) in the Apennines , 2010 .
[10] H. Jenkyns,et al. First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquén Basin, Argentina , 2010, Journal of the Geological Society.
[11] Y. Rosenthal,et al. The enigmatic ichnofossil Tisoa siphonalis and widespread authigenic seep carbonate formation during the Late Pliensbachian in southern France , 2010 .
[12] S. Planke,et al. Early Jurassic shale chemostratigraphy and U-Pb ages from the Neuquén Basin (Argentina): Implications for the Toarcian Oceanic Anoxic Event , 2010 .
[13] P. Wignall,et al. An 80 million year oceanic redox history from Permian to Jurassic pelagic sediments of the Mino-Tamba terrane, SW Japan, and the origin of four mass extinctions , 2010 .
[14] H. Jenkyns. Geochemistry of oceanic anoxic events , 2010 .
[15] M. Philippe,et al. Secular environmental precursors to Early Toarcian (Jurassic) extreme climate changes , 2010 .
[16] A. Coe,et al. New range data for marine invertebrate species across the early Toarcian (Early Jurassic) mass extinction , 2009, Journal of the Geological Society.
[17] A. Bellanca,et al. Carbon‐isotope records of the Early Jurassic (Toarcian) oceanic anoxic event from the Valdorbia (Umbria–Marche Apennines) and Monte Mangart (Julian Alps) sections: palaeoceanographic and stratigraphic implications , 2009 .
[18] J. Hunen,et al. No evidence for thermogenic methane release in coal from the Karoo-Ferrar large igneous province , 2009 .
[19] R. Howarth,et al. Basinal restriction, black shales, Re‐Os dating, and the Early Toarcian (Jurassic) oceanic anoxic event , 2008 .
[20] I. Boomer,et al. The extinction of the Metacopina (Ostracoda) , 2008 .
[21] P. Renne,et al. The 40Ar/39Ar ages of the sill complex of the Karoo large igneous province: Implications for the Pliensbachian‐Toarcian climate change , 2008 .
[22] L. Kump,et al. Oceanic Euxinia in Earth History: Causes and Consequences , 2008 .
[23] E. Mattioli,et al. Duration of the Early Toarcian carbon isotope excursion deduced from spectral analysis: Consequence for its possible causes , 2008 .
[24] B. Nikitenko. The Early Jurassic to Aalenian paleobiogeography of the Arctic realm: Implication of microbenthos (Foraminifers and Ostracodes) , 2008 .
[25] J. J. Gómez,et al. Seawater temperature and carbon isotope variations in belemnites linked to mass extinction during the Toarcian (Early Jurassic) in Central and Northern Spain. Comparison with other European sections , 2008 .
[26] B. Jones,et al. A Review and Synthesis of Glendonites (Pseudomorphs after Ikaite) with New Data: Assessing Applicability as Recorders of Ancient Coldwater Conditions , 2007 .
[27] A. Coe,et al. The Late Palaeocene–Early Eocene and Toarcian (Early Jurassic) carbon isotope excursions: a comparison of their time scales, associated environmental changes, causes and consequences , 2007, Journal of the Geological Society.
[28] Anders Malthe-Sørenssen,et al. Hydrothermal venting of greenhouse gases triggering Early Jurassic global warming , 2007 .
[29] H. Jenkyns,et al. Carbon-isotope record of the Early Jurassic (Toarcian) Oceanic Anoxic Event from fossil wood and marine carbonate (Lusitanian Basin, Portugal) , 2007 .
[30] J. Damsté,et al. Isorenieratane record in black shales from the Paris Basin, France: Constraints on recycling of respired CO2 as a mechanism for negative carbon isotope shifts during the Toarcian oceanic anoxic event , 2006 .
[31] E. Mattioli,et al. The Early Toarcian anoxia, a synchronous event in the Western Tethys? An approach by quantitative biochronology (Unitary Associations), applied on calcareous nannofossils , 2006 .
[32] S. Robles,et al. Geochemical arguments for identifying second‐order sea‐level changes in hemipelagic carbonate ramp deposits , 2006 .
[33] B. Nikitenko,et al. Pliensbachian-Toarcian biotic turnover in north Siberia and the Arctic region , 2006 .
[34] C. Little,et al. The timing of paleoenvironmental change and cause-and-effect relationships during the early Jurassic mass extinction in Europe , 2005 .
[35] A. Coe,et al. Astronomical pacing of methane release in the Early Jurassic period , 2005, Nature.
[36] K. Miller,et al. Toarcian oceanic anoxic event: An assessment of global causes using belemnite C isotope records , 2005 .
[37] E. Mattioli,et al. Phytoplankton evidence for the timing and correlation of palaeoceanographical changes during the early Toarcian oceanic anoxic event (Early Jurassic) , 2004, Journal of the Geological Society.
[38] A. Coe,et al. Osmium isotope evidence for the regulation of atmospheric CO2 by continental weathering , 2004 .
[39] Y. Rosenthal,et al. Paleoceanographic changes of the Late Pliensbachian-Early Toarcian interval: a possible link to the genesis of an Oceanic Anoxic Event , 2003 .
[40] F. Behar,et al. Rock-Eval 6 Technology: Performances and Developments , 2001 .
[41] C. Bjerrum,et al. Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event , 2000, Nature.
[42] P. Wignall,et al. Pyrite framboid diameter as a measure of oxygen deficiency in ancient mudrocks , 1998 .
[43] A. Kontorovich,et al. Main oil source formations of the West Siberian Basin , 1997, Petroleum Geoscience.
[44] A. Hallam. Estimates of the amount and rate of sea-level change across the Rhaetian—Hettangian and Pliensbachian—Toarcian boundaries (latest Triassic to early Jurassic) , 1997, Journal of the Geological Society.
[45] R. Steel,et al. Dunlin group sequence stratigraphy in the northern North Sea: A model for Cook sandstone deposition , 1997 .
[46] H. Barnes,et al. THE SIZE DISTRIBUTION OF FRAMBOIDAL PYRITE IN MODERN SEDIMENTS : AN INDICATOR OF REDOX CONDITIONS , 1996 .
[47] M. Bennett,et al. Global cooling inferred from dropstones in the Cretaceous: fact or wishful thinking? , 1996 .
[48] R. Rosenbauer,et al. The Solubility and Stabilization of Ikaite (CaCO3·6H2O) from 0° to 25°C: Environmental and Paleoclimatic Implications for Thinolite Tufa , 1993, The Journal of Geology.
[49] P. Wignall. Model for transgressive black shales , 1991 .
[50] H. Jenkyns. The early Toarcian (Jurassic) anoxic event; stratigraphic, sedimentary and geochemical evidence , 1988 .
[51] A. Seilacher,et al. Cyclic and Event Stratification , 1982 .
[52] P. Neige,et al. Distribution of clay minerals in Early Jurassic Peritethyan seas: Palaeoclimatic significance inferred from multiproxy comparisons , 2009 .
[53] A. Schmid-Röhl,et al. Lower Toarcian (Upper Liassic) Black Shales of the Central European Epicontinental Basin: A Sequence Stratigraphic Case Study from the Sw German Posidonia Shale , 2005 .
[54] B. Nikitenko,et al. Foraminifera and ostracodes across the Pliensbachian-Toarcian boundary in the Arctice Realm (stratigraphy, palaeobiogeography and biofacies) , 2004, Geological Society, London, Special Publications.
[55] J. Guex,et al. Découverte d'une importante lacune stratigraphique à la limite Domérien-Toarcien : implications paléo-océanographiques , 2001 .
[56] L. Schwark,et al. The Posidonia Shale (Lower Toarcian) of SW-Germany: an oxygen-depleted ecosystem controlled by sea level and palaeoclimate , 2001 .
[57] Stefan Schouten,et al. Effects of an oceanic anoxic event on the stable carbon isotopic composition of Early Toarcian carbon , 2000 .
[58] J. Riding,et al. Jurassic and lowermost Cretaceous dinoflagellate cyst biostratigraphy of the Russian Platform and northern Siberia, Russia , 1999 .
[59] G. Parisi,et al. Stratigraphy and geochemical anomalies of the early Toarcian oxygen-poor interval in the Umbria-Marche Apennines (Italy) , 1996 .
[60] N. Hughes,et al. Jurassic and Cretaceous floras and climates of the Earth , 1994 .
[61] B. Ligouis,et al. Organic matter and palynomorphs in the ‘Posidonienschiefer’ (Toarcian, Lower Jurassic) of southern Germany , 1991, Geological Society, London, Special Publications.
[62] M. Vandenbroucke,et al. Mapping and geochemical characterization of the Toarcian organic matter in the Mediterranean Tethys and Middle East , 1990 .
[63] W. Küspert. Environmental Changes During Oil Shale Deposition as Deduced from Stable Isotope Ratios , 1982 .