Duration of and decoupling between carbon isotope excursions during the end-Triassic mass extinction and Central Atlantic Magmatic Province emplacement
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D. Bottjer | A. West | F. Corsetti | W. Berelson | N. Rollins | S. Rosas | J. Yager | A. J. West
[1] C. Bjerrum,et al. A new correlation of Triassic–Jurassic boundary successions in NW Europe, Nevada and Peru, and the Central Atlantic Magmatic Province: A time-line for the end-Triassic mass extinction , 2017 .
[2] D. Bottjer,et al. Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction , 2016, Nature Communications.
[3] J. Spangenberg,et al. Thermal erosion of cratonic lithosphere as a potential trigger for mass-extinction , 2016, Scientific Reports.
[4] J. Erez,et al. A novel determination of calcite dissolution kinetics in seawater , 2015 .
[5] J. Payne,et al. Modelling the impact of pulsed CAMP volcanism on pCO2 and δ13C across the Triassic–Jurassic transition , 2015, Geological Magazine.
[6] P. Ehrlich,et al. Accelerated modern human–induced species losses: Entering the sixth mass extinction , 2015, Science Advances.
[7] J. Wright,et al. A 30 Myr record of Late Triassic atmospheric pCO2 variation reflects a fundamental control of the carbon cycle by changes in continental weathering , 2015 .
[8] D. Bottjer,et al. Andean sponges reveal long-term benthic ecosystem shifts following the end-Triassic mass extinction , 2015 .
[9] D. Bottjer,et al. NEW EVIDENCE ON THE ROLE OF SILICEOUS SPONGES IN ECOLOGY AND SEDIMENTARY FACIES DEVELOPMENT IN EASTERN PANTHALASSA FOLLOWING THE TRIASSIC–JURASSIC MASS EXTINCTION , 2014 .
[10] J. Pálfy,et al. Volcanism of the Central Atlantic magmatic province as the trigger of environmental and biotic changes around the Triassic-Jurassic boundary , 2014 .
[11] L. Krystyn,et al. Towards accurate numerical calibration of the Late Triassic: High- precision U-Pb geochronology constraints on the duration of the Rhaetian , 2014 .
[12] N. Youbi,et al. The dawn of CAMP volcanism and its bearing on the end-Triassic carbon cycle disruption , 2014, Journal of the Geological Society.
[13] J. Payne,et al. Microbes, mud and methane: cause and consequence of recurrent Early Jurassic anoxia following the end‐Triassic mass extinction , 2013 .
[14] D. Kent,et al. Zircon U-Pb Geochronology Links the End-Triassic Extinction with the Central Atlantic Magmatic Province , 2013, Science.
[15] J. Payne,et al. Carbon cycle dynamics following the end‐Triassic mass extinction: Constraints from paired δ13Ccarb and δ13Corg records , 2012 .
[16] V. Atudorei,et al. Geochronological constraints on post-extinction recovery of the ammonoids and carbon cycle perturbations during the Early Jurassic , 2012 .
[17] G. Pedersen,et al. No causal link between terrestrial ecosystem change and methane release during the end-Triassic mass extinction , 2012 .
[18] D. Bottjer,et al. Recognising ocean acidification in deep time: An evaluation of the evidence for acidification across the Triassic-Jurassic boundary , 2012 .
[19] M. Chiaradia,et al. Latest Triassic marine Sr isotopic variations, possible causes and implications , 2012 .
[20] F. Corsetti,et al. Constraining pathways of microbial mediation for carbonate concretions of the Miocene Monterey Formation using carbonate-associated sulfate , 2012 .
[21] M. Leng,et al. Evidence for bias in C and N concentrations and δ13C composition of terrestrial and aquatic organic materials due to pre-analysis acid preparation methods , 2011 .
[22] Â. Min,et al. Timing and duration of the Central Atlantic magmatic province in the Newark and Culpeper basins, eastern U.S.A. , 2011 .
[23] R. Hori,et al. Marine osmium isotope record across the Triassic-Jurassic boundary from a Pacific pelagic site , 2010 .
[24] G. Paris,et al. Early Hettangian benthic-planktonic coupling at Doniford (SW England) Palaeoenvironmental implications for the aftermath of the end-Triassic crisis , 2010 .
[25] W. Krijgsman,et al. Astronomical constraints on the duration of the early Jurassic Hettangian stage and recovery rates following the end-Triassic mass extinction (St Audrie's Bay/East Quantoxhead, UK) , 2010 .
[26] U. Schaltegger,et al. Correlating the end-Triassic mass extinction and flood basalt volcanism at the 100 ka level , 2010 .
[27] C. Spötl,et al. Palaeoenvironmental significance of carbon- and oxygen-isotope stratigraphy of marine Triassic–Jurassic boundary sections in SW Britain , 2009, Journal of the Geological Society.
[28] T. McConnaughey,et al. Carbon isotopes in mollusk shell carbonates , 2008 .
[29] A. Tomašových,et al. Carbon cycle perturbation and stabilization in the wake of the Triassic‐Jurassic boundary mass‐extinction event , 2008 .
[30] U. Schaltegger,et al. Precise U–Pb age constraints for end-Triassic mass extinction, its correlation to volcanism and Hettangian post-extinction recovery , 2008 .
[31] A. Tankard,et al. Tectonic evolution and paleogeography of the Mesozoic Pucará Basin, central Peru , 2007 .
[32] K. Williford,et al. An extended organic carbon-isotope record across the Triassic–Jurassic boundary in the Queen Charlotte Islands, British Columbia, Canada , 2007 .
[33] P. Falkowski,et al. End-Triassic calcification crisis and blooms of organic-walled 'disaster species' , 2007 .
[34] H. Westphal. Limestone–marl alternations as environmental archives and the role of early diagenesis: a critical review , 2006 .
[35] L. Zaninetti,et al. Synchrony of the Central Atlantic magmatic province and the Triassic-Jurassic boundary climatic and biotic crisis , 2004 .
[36] V. Atudorei,et al. High-resolution ammonite and carbon isotope stratigraphy across the Triassic-Jurassic boundary at New York Canyon (Nevada) , 2004 .
[37] S. Hesselbo,et al. Sea-level change and facies development across potential Triassic–Jurassic boundary horizons, SW Britain , 2004, Journal of the Geological Society.
[38] D. Beerling,et al. Biogeochemical constraints on the Triassic‐Jurassic boundary carbon cycle event , 2002 .
[39] S. Piasecki,et al. Terrestrial and marine extinction at the Triassic-Jurassic boundary synchronized with major carbon-cycle perturbation: A link to initiation of massive volcanism? , 2002 .
[40] J. Pálfy,et al. Carbon isotope anomaly and other geochemical changes at the Triassic-Jurassic boundary from a marine section in Hungary , 2001 .
[41] D. Wilbur,et al. Sudden Productivity Collapse Associated with the Triassic-Jurassic Boundary Mass Extinction , 2001, Science.
[42] Michael J. Whiticar,et al. Carbon and hydrogen isotope systematics of bacterial formation and oxidation of methane , 1999 .
[43] Michael A. Arthur,et al. Interpreting carbon-isotope excursions: carbonates and organic matter , 1999 .
[44] A. J. Kaufman,et al. Neoproterozoic variations in the C-isotopic composition of seawater: stratigraphic and biogeochemical implications. , 1995, Precambrian research.
[45] P. Meyers. Preservation of elemental and isotopic source identification of sedimentary organic matter , 1994 .
[46] M. Katz,et al. The Norian/Rhaetian boundary interval at Pignola-Abriola section (southern Apennines, Italy) as a GSSP candidate for the Rhaetian stage: an update , 2016 .
[47] G. Paris,et al. Geochemical consequences of intense pulse-like degassing during the onset of the Central Atlantic Magmatic Province , 2016 .
[48] U. Schacht,et al. Chapter 9 - Early diagenesis of deep-sea sediments , 2011 .
[49] F. Hu,et al. Sedimentary organic matter preservation : A test for selective degradation under oxic conditions , 1999 .
[50] S. Burns,et al. Oxygen and carbon isotopic composition of marine carbonate concretions; an overview , 1993 .
[51] P. Kroopnick. The distribution of 13C of ΣCO2 in the world oceans , 1985 .