Geochronological constraints on post-extinction recovery of the ammonoids and carbon cycle perturbations during the Early Jurassic

[1]  L. Cocchi,et al.  Birth of an ocean in the Red Sea: Initial pangs , 2012 .

[2]  V. Atudorei,et al.  Disentangling the Hettangian carbon isotope record: Implications for the aftermath of the end‐Triassic mass extinction , 2012 .

[3]  J. Bowring,et al.  An algorithm for U‐Pb isotope dilution data reduction and uncertainty propagation , 2011 .

[4]  N. Evans,et al.  Acigöl rhyolite field, Central Anatolia (part 1): high-resolution dating of eruption episodes and zircon growth rates , 2011 .

[5]  Â. Min,et al.  Timing and duration of the Central Atlantic magmatic province in the Newark and Culpeper basins, eastern U.S.A. , 2011 .

[6]  D. Günther,et al.  A new method integrating high-precision U–Pb geochronology with zircon trace element analysis (U–Pb TIMS-TEA) , 2010 .

[7]  S. Bowring,et al.  Isotopic composition (238U/235U) of some commonly used uranium reference materials , 2010 .

[8]  G. Paris,et al.  Bentho-planktonic evidence from the Austrian Alps for a decline in sea-surface carbonate production at the end of the Triassic , 2010 .

[9]  K. Priestley,et al.  Rayleigh wave phase velocity maps of Tibet and the surrounding regions from ambient seismic noise tomography , 2010 .

[10]  O. Bachmann,et al.  The 40Ar/39Ar and U/Pb dating of young rhyolites in the Kos‐Nisyros volcanic complex, Eastern Aegean Arc, Greece: Age discordance due to excess 40Ar in biotite , 2010 .

[11]  D. Stockli,et al.  Episodic growth and homogenization of plutonic roots in arc volcanoes from combined U-Th and (U-Th)/He zircon dating , 2010 .

[12]  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 .

[13]  P. Harries,et al.  Effect of nutrient availability on marine origination rates throughout the Phanerozoic eon , 2010 .

[14]  U. Schaltegger,et al.  Correlating the end-Triassic mass extinction and flood basalt volcanism at the 100 ka level , 2010 .

[15]  R. Sambrotto,et al.  Compound-specific carbon isotopes from Earth’s largest flood basalt eruptions directly linked to the end-Triassic mass extinction , 2010, Proceedings of the National Academy of Sciences.

[16]  V. Davydov,et al.  High‐precision U‐Pb zircon age calibration of the global Carboniferous time scale and Milankovitch band cyclicity in the Donets Basin, eastern Ukraine , 2010 .

[17]  L. Tanner,et al.  Latest Triassic onset of the Central Atlantic Magmatic Province (CAMP) volcanism in the Fundy Basin (Nova Scotia): New stratigraphic constraints , 2009 .

[18]  U. Schaltegger,et al.  Tectonomagmatic evolution of Western Amazonia: Geochemical characterization and zircon U-Pb geochronologic constraints from the Peruvian Eastern Cordilleran granitoids , 2009 .

[19]  P. Brack,et al.  Zircon and titanite recording 1.5 million years of magma accretion, crystallization and initial cooling in a composite pluton (southern Adamello batholith, northern Italy) , 2009 .

[20]  P. Wagner,et al.  Fossil Plant Relative Abundances Indicate Sudden Loss of Late Triassic Biodiversity in East Greenland , 2009, Science.

[21]  Colin J. N. Wilson,et al.  Rapid Rates of Magma Generation at Contemporaneous Magma Systems, Taupo Volcano, New Zealand: Insights from U–Th Model-age Spectra in Zircons , 2009 .

[22]  U. Schaltegger,et al.  Crustal growth along a non-collisional cratonic margin: A Lu–Hf isotopic survey of the Eastern Cordilleran granitoids of Peru , 2009 .

[23]  P. Renne,et al.  Synchronizing Rock Clocks of Earth History , 2008, Science.

[24]  M. Whitehouse,et al.  Plesovice zircon : A new natural reference material for U-Pb and Hf isotopic microanalysis , 2008 .

[25]  U. Schaltegger,et al.  Precise U–Pb age constraints for end-Triassic mass extinction, its correlation to volcanism and Hettangian post-extinction recovery , 2008 .

[26]  P. Renne,et al.  Implications of pre-eruptive magmatic histories of zircons for U–Pb geochronology of silicic extrusions , 2008 .

[27]  S. Bowring,et al.  U-Pb dating of zircon in the Bishop Tuff at the millennial scale , 2007 .

[28]  R. Miller,et al.  Zircon growth and recycling during the assembly of large, composite arc plutons , 2007 .

[29]  L. Tanner,et al.  Stomatal response of swordfern to volcanogenic CO2 and SO2 from Kilauea volcano , 2007 .

[30]  M. Schmitz,et al.  Derivation of isotope ratios, errors, and error correlations for U‐Pb geochronology using 205Pb‐235U‐(233U)‐spiked isotope dilution thermal ionization mass spectrometric data , 2007 .

[31]  A. Tankard,et al.  Tectonic evolution and paleogeography of the Mesozoic Pucará Basin, central Peru , 2007 .

[32]  W. Snyder,et al.  High-precision U–Pb zircon age constraints on the Carboniferous–Permian boundary in the southern Urals stratotype , 2007 .

[33]  D. Fornari,et al.  Submarine volcanic morphology of the western Galápagos based on EM300 bathymetry and MR1 side‐scan sonar , 2007 .

[34]  A. Coe,et al.  The impact of the Central Atlantic Magmatic Province on climate and on the Sr- and Os-isotope evolution of seawater , 2007 .

[35]  S. Bernasconi,et al.  Stratigraphy and palaeoenvironmental analysis of the Triassic–Jurassic transition in the western Southern Alps (Northern Italy) , 2007 .

[36]  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 .

[37]  M. Bill,et al.  Carbon–isotope stratigraphy and ammonite faunal turnover for the Middle Jurassic in the Southern Iberian palaeomargin , 2006 .

[38]  U. Schaltegger,et al.  New Early to Middle Triassic U–Pb ages from South China: Calibration with ammonoid biochronozones and implications for the timing of the Triassic biotic recovery , 2006 .

[39]  J. Guex Reinitialization of evolutionary clocks during sublethal environmental stress in some invertebrates , 2006 .

[40]  J. Mattinson Zircon U–Pb chemical abrasion (“CA-TIMS”) method: Combined annealing and multi-step partial dissolution analysis for improved precision and accuracy of zircon ages , 2005 .

[41]  M. Reid,et al.  The pace of rhyolite differentiation and storage in an 'archetypical' silicic magma system, Long Valley, California [rapid communication] , 2005 .

[42]  J. Lowenstern,et al.  Late Pleistocene granodiorite source for recycled zircon and phenocrysts in rhyodacite lava at Crater Lake, Oregon [rapid communication] , 2005 .

[43]  P. Renne,et al.  Age and Timing of the Permian Mass Extinctions: U/Pb Dating of Closed-System Zircons , 2004, Science.

[44]  V. Atudorei,et al.  High-resolution ammonite and carbon isotope stratigraphy across the Triassic-Jurassic boundary at New York Canyon (Nevada) , 2004 .

[45]  L. Tanner,et al.  Assessing the record and causes of Late Triassic extinctions , 2004 .

[46]  J. Guex A generalization of Cope’s rule , 2003 .

[47]  K. Page,et al.  Global Stratotype Section and Point for base of the Sinemurian Stage (Lower Jurassic) , 2002 .

[48]  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 .

[49]  D. Wilbur,et al.  Sudden Productivity Collapse Associated with the Triassic-Jurassic Boundary Mass Extinction , 2001, Science.

[50]  Â. Min,et al.  Extensive 200-million-year-Old continental flood basalts of the central atlantic magmatic province , 1999, Science.

[51]  P. Tapponnier,et al.  On causal links between flood basalts and continental breakup , 1999 .

[52]  A. Coe,et al.  Strontium isotopic variations in Jurassic and Cretaceous seawater , 1994 .

[53]  Von H. K. Errben,et al.  ÜBER DEN URSPRUNG DER AMMONOIDEA , 1966 .

[54]  O. Haas Recurrence of morphologic types and evolutionary cycles in Mesozoic ammonites , 1942 .

[55]  O. Bachmann The 40 Ar / 39 Ar and U / Pb dating of young rhyolites in the Kos-Nisyros volcanic complex , Eastern Aegean Arc , Greece : Age discordance due to excess 40 Ar in biotite , 2010 .

[56]  J. Lowenstern,et al.  Zircon crystallization and recycling in the magma chamber of the rhyolitic Kos Plateau Tuff (Aegean arc) , 2007 .

[57]  J. Lowenstern,et al.  Magma Generation at a Large, Hyperactive Silicic Volcano (Taupo, New Zealand) Revealed by U–Th and U–Pb Systematics in Zircons , 2005 .

[58]  J. Guex,et al.  The Triassic Jurassic System boundary in the John Day Inlier, East-Central Oregon. , 2002 .

[59]  P. Renne,et al.  A test for systematic errors in 40Ar/39Ar geochronology through comparison with U/Pb analysis of a 1.1-Ga rhyolite , 2000 .

[60]  J. Guex Ammonites hettangiennes de la Gabbs Valley Range (Nevada, USA) , 1995 .

[61]  S. Lucas Triassic Tetrapod Extinctions and the Compiled Correlation Effect , 1994 .

[62]  D. Jablonski Mass extinctions: Persistent problems and new directions , 1994 .

[63]  J. Guex Contradictory Biochronologic Correlations , 1991 .

[64]  Jean Guex,et al.  Unitary associations method: use of graph theory and computer algorithm , 1984 .

[65]  L. Spath The ammonites of the blue lias , 1924 .

[66]  A. Hyatt Genesis of the Arietidae , 1889 .