Evolution of the Toarcian (Early Jurassic) carbon-cycle and global climatic controls on local sedimentary processes (Cardigan Bay Basin, UK)

[1]  R. Pancost,et al.  Carbon sequestration in an expanded lake system during the Toarcian oceanic anoxic event , 2017 .

[2]  Paul L. Smith,et al.  High-resolution carbon isotope records of the Toarcian Oceanic Anoxic Event (Early Jurassic) from North America and implications for the global drivers of the Toarcian carbon cycle , 2017 .

[3]  M. Leng,et al.  Astronomical constraints on the duration of the Early Jurassic Pliensbachian Stage and global climatic fluctuations , 2016 .

[4]  X. Fu,et al.  Early Jurassic carbon-isotope excursion in the Qiangtang Basin (Tibet), the eastern Tethys: Implications for the Toarcian Oceanic anoxic event , 2016 .

[5]  M. Leng,et al.  Osmium isotope evidence for two pulses of increased continental weathering linked to Early Jurassic volcanism and climate change , 2016 .

[6]  R. Hoffmann,et al.  Perturbation of the carbon cycle during the late Pliensbachian – early Toarcian: New insight from high-resolution carbon isotope records in Morocco , 2016 .

[7]  H. Jenkyns,et al.  The Toarcian Oceanic Anoxic Event (Early Jurassic) in the Neuquén Basin, Argentina: A Reassessment of Age and Carbon Isotope Stratigraphy , 2016, The Journal of Geology.

[8]  C. Korte,et al.  Jurassic climate mode governed by ocean gateway , 2015, Nature Communications.

[9]  T. Mather,et al.  Globally enhanced mercury deposition during the end-Pliensbachian extinction and Toarcian OAE: A link to the Karoo–Ferrar Large Igneous Province , 2015 .

[10]  G. Suan,et al.  Toarcian extreme warmth led to tropical cyclone intensification , 2015 .

[11]  T. Adatte,et al.  Calibrating the magnitude of the Toarcian carbon cycle perturbation , 2015 .

[12]  S. Bowring,et al.  High-precision geochronology links the Ferrar large igneous province with early-Jurassic ocean anoxia and biotic crisis , 2015 .

[13]  C. Little,et al.  Environmental controls on Jurassic marine ecosystems during global warming , 2015 .

[14]  L. Simon,et al.  Calcium isotope evidence for dramatic increase of continental weathering during the Toarcian oceanic anoxic event (Early Jurassic) , 2015 .

[15]  D. Kemp,et al.  Multiproxy geochemical analysis of a Panthalassic margin record of the early Toarcian oceanic anoxic event (Toyora area, Japan) , 2014 .

[16]  C. Korte,et al.  Effect of a Jurassic oceanic anoxic event on belemnite ecology and evolution , 2014, Proceedings of the National Academy of Sciences.

[17]  E. Mattioli,et al.  Carbon isotope evidence for sedimentary discontinuities in the lower Toarcian of the Lusitanian Basin (Portugal): Sea level change at the onset of the Oceanic Anoxic Event , 2014 .

[18]  P. Pellenard,et al.  Continental weathering and climatic changes inferred from clay mineralogy and paired carbon isotopes across the early to middle Toarcian in the Paris Basin , 2014 .

[19]  R. Summons,et al.  Organic geochemistry of the early Toarcian oceanic anoxic event in Hawsker Bottoms, Yorkshire, England , 2014 .

[20]  P. Pellenard,et al.  Black shale deposition during Toarcian super-greenhouse driven by sea level , 2013 .

[21]  K. Miller,et al.  Mochras borehole revisited: a new global standard for Early Jurassic earth history , 2013 .

[22]  A. Coe,et al.  Primary productivity controls on opportunistic bivalves during Early Jurassic oceanic deoxygenation , 2013 .

[23]  Paul L. Smith,et al.  The Pliensbachian-Toarcian (Early Jurassic) extinction, a global multi-phased event , 2013 .

[24]  H. Chamley North Atlantic Clay Sedimentation and Paleoenvironment Since the Late Jurassic. , 2013 .

[25]  Ben Johnson,et al.  Lower Jurassic Foraminifera from the Llanbedr (Mochras Farm) Borehole, North Wales, UK , 2013 .

[26]  K. Föllmi,et al.  Palaeoenvironmental significance of Toarcian black shales and event deposits from southern Beaujolais, France , 2013, Geological Magazine.

[27]  E. Tohver,et al.  Phanerozoic polar wander, palaeogeography and dynamics , 2012 .

[28]  F. Hilgen,et al.  On the Geologic Time Scale , 2012, Newsletters on Stratigraphy.

[29]  S. Planke,et al.  Rapid magma emplacement in the Karoo Large Igneous Province , 2012 .

[30]  T. Lyons,et al.  A global perturbation to the sulfur cycle during the Toarcian Oceanic Anoxic Event , 2011 .

[31]  Stephen Barker,et al.  The Geological Record of Ocean Acidification , 2011, Science.

[32]  A. Coe,et al.  Astronomical forcing and chronology of the early Toarcian (Early Jurassic) oceanic anoxic event in Yorkshire, UK , 2011 .

[33]  P. Neige,et al.  Ammonite paleobiogeography during the Pliensbachian-Toarcian crisis (Early Jurassic) reflecting paleoclimate, eustasy, and extinctions , 2011 .

[34]  J. Damsté,et al.  Warm Middle Jurassic–Early Cretaceous high-latitude sea-surface temperatures from the Southern Ocean , 2011 .

[35]  M. Joachimski,et al.  Climatic ups and downs in a disturbed Jurassic world , 2011 .

[36]  S. Hesselbo,et al.  Stepwise atmospheric carbon-isotope excursion during the Toarcian Oceanic Anoxic Event (Early Jurassic, Polish Basin) , 2011 .

[37]  Stefan Schouten,et al.  TEX86 and stable δ18O paleothermometry of early Cretaceous sediments: Implications for belemnite ecology and paleotemperature proxy application , 2010 .

[38]  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.

[39]  P. Brański Kaolinite peaks in early Toarcian profiles from the Polish Basin-an inferred record of global warming , 2010 .

[40]  P. Louvat,et al.  The fundamental role of island arc weathering in the oceanic Sr isotope budget , 2010 .

[41]  H. Jenkyns Geochemistry of oceanic anoxic events , 2010 .

[42]  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 .

[43]  J. Huggett,et al.  Late Jurassic palaeoclimatic change from clay mineralogy and gamma-ray spectrometry of the Kimmeridge Clay, Dorset, UK , 2009, Journal of the Geological Society.

[44]  H. Jenkyns,et al.  A carbon-isotope perturbation at the Pliensbachian–Toarcian boundary: evidence from the Lias Group, NE England , 2009, Geological Magazine.

[45]  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.

[46]  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 .

[47]  E. Mattioli,et al.  Dramatic decrease of pelagic carbonate production by nannoplankton across the Early Toarcian anoxic event (T-OAE) , 2009 .

[48]  M. Renard,et al.  Expression of the Early Toarcian negative carbon-isotope excursion in separated carbonate microfractions (Jurassic, Paris Basin) , 2009 .

[49]  H. Jenkyns,et al.  The response of two Tethyan carbonate platforms to the early Toarcian (Jurassic) oceanic anoxic event: environmental change and differential subsidence , 2008 .

[50]  A. Varga,et al.  Climato-environmental controls on clay mineralogy of the Hettangian–Bajocian successions of the Mecsek Mountains, Hungary , 2008 .

[51]  C. Lécuyer,et al.  Evidence for major environmental perturbation prior to and during the Toarcian (Early Jurassic) oceanic anoxic event from the Lusitanian Basin, Portugal , 2008 .

[52]  Anders Malthe-Sørenssen,et al.  Hydrothermal venting of greenhouse gases triggering Early Jurassic global warming , 2007 .

[53]  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 .

[54]  P. Falkowski,et al.  Early Jurassic climate change and the radiation of organic-walled phytoplankton in the Tethys Ocean , 2005, Paleobiology.

[55]  I. Davison Central Atlantic margin basins of North West Africa: Geology and hydrocarbon potential (Morocco to Guinea) , 2005 .

[56]  A. Coe,et al.  Astronomical pacing of methane release in the Early Jurassic period , 2005, Nature.

[57]  P. Falkowski,et al.  Biological overprint of the geological carbon cycle , 2005 .

[58]  S. Hesselbo,et al.  Changes in carbon dioxide during an oceanic anoxic event linked to intrusion into Gondwana coals , 2005, Nature.

[59]  F. Cecca,et al.  The two Early Toarcian (Early Jurassic) extinction events in ammonoids , 2004 .

[60]  A. Coe,et al.  Osmium isotope evidence for the regulation of atmospheric CO2 by continental weathering , 2004 .

[61]  K. Page The Lower Jurassic of Europe: its subdivision and correlation , 2003 .

[62]  H. Jenkyns Evidence for rapid climate change in the Mesozoic–Palaeogene greenhouse world , 2003, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

[63]  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 .

[64]  C. E. Jones,et al.  Chemostratigraphy of the Jurassic System: applications, limitations and implications for palaeoceanography , 2002, Journal of the Geological Society.

[65]  I. Poole,et al.  Stable carbon isotopes of wood: a clue to palaeoclimate? , 2002 .

[66]  H. Jenkyns,et al.  Nitrogen isotope evidence for water mass denitrification during the Early Toarcian (Jurassic) oceanic anoxic event , 2001 .

[67]  R. Tyson,et al.  Contrasting watermass conditions during deposition of the Whitby Mudstone (Lower Jurassic) and Kimmeridge Clay (Upper Jurassic) formations, UK , 2000 .

[68]  A. Gale,et al.  Geochemistry of Early Siderite Cements from the Eocene Succession of Whitecliff Bay, Hampshire Basin, U.K. , 2000 .

[69]  Paul L. Smith,et al.  Synchrony between Early Jurassic extinction, oceanic anoxic event, and the Karoo-Ferrar flood basalt volcanism , 2000 .

[70]  C. Bjerrum,et al.  Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event , 2000, Nature.

[71]  D. Donovan,et al.  Strontium isotope profile of the early Toarcian (Jurassic) oceanic anoxic event, the duration of ammonite biozones, and belemnite palaeotemperatures , 2000 .

[72]  M. Thiry Palaeoclimatic interprétation of clay minerals in marine deposits : an outlook from the continental origin. , 2000 .

[73]  R. Duncan,et al.  The timing and duration of the Karoo igneous event, southern Gondwana , 1997 .

[74]  H. Jenkyns,et al.  Lower Jurassic epicontinental carbonates and mudstones from England and Wales: chemostratigraphic signals and the early Toarcian anoxic event , 1997 .

[75]  Stefan Schouten,et al.  Diagenetic and catagenetic products of isorenieratene: Molecular indicators for photic zone anoxia , 1996 .

[76]  H. Barnes,et al.  THE SIZE DISTRIBUTION OF FRAMBOIDAL PYRITE IN MODERN SEDIMENTS : AN INDICATOR OF REDOX CONDITIONS , 1996 .

[77]  M. Benton,et al.  Early Jurassic mass extinction: A global long-term event: Geol-ogy , 1995 .

[78]  J. Hayes,et al.  Evidence for gammacerane as an indicator of water column stratification. , 1995, Geochimica et cosmochimica acta.

[79]  J. Kennett,et al.  Antarctic subtropical humid episode at the Paleocene-Eocene boundary: Clay-mineral evidence , 1994 .

[80]  C. E. Jones,et al.  Strontium isotopes in Early Jurassic seawater , 1994 .

[81]  P. Rawson,et al.  Atlas of Palaeogeography and Lithofacies , 1992 .

[82]  R. Ruedy,et al.  Pangaean climate during the Early Jurassic: GCM simulations and the sedimentary record of paleoclimate , 1992 .

[83]  J. Edmond,et al.  Controls over the strontium isotope composition of river water , 1992 .

[84]  D. Bernoulli,et al.  Clay mineral assemblages of Mesozoic pelagic and flysch sediments of the Lombardian Basin (Southern Alps): implications for palaeotectonics, palaeoclimate and diagenesis , 1991 .

[85]  Robert C. Reynolds,et al.  X-Ray Diffraction and the Identification and Analysis of Clay Minerals , 1989 .

[86]  B. Tucholke,et al.  Upper Triassic—Lower Jurassic salt basin southeast of the Grand Banks , 1989 .

[87]  J. Edmond,et al.  The strontium isotope budget of the modern ocean , 1989 .

[88]  H. Jenkyns The early Toarcian (Jurassic) anoxic event; stratigraphic, sedimentary and geochemical evidence , 1988 .

[89]  H. Jenkyns,et al.  Black shales and carbon isotopes in pelagic sediments from the Tethyan Lower Jurassic , 1986 .

[90]  H. Jenkyns The early Toarcian and Cenomanian-Turonian anoxic events in Europe: comparisons and contrasts , 1985 .

[91]  E. J. Gallegos,et al.  Relationship Between Petroleum Composition and Depositional Environment of Petroleum Source Rocks , 1985 .

[92]  B. Sellwood,et al.  Basins and swells and the evolution of an epeiric sea , 1975, Journal of the Geological Society.

[93]  B. Sellwood The genesis of some sideritic beds in the Yorkshire Lias (England) , 1971 .

[94]  W. Farrand,et al.  Geology of Clays: Weathering · Sedimentology · Geochemistry , 1970 .

[95]  D. Spears,et al.  The formation of sedimentary iron minerals , 1968 .

[96]  D. H. Porrenga Glauconite and chamosite as depth indicators in the marine environment , 1967 .

[97]  D. Kemp,et al.  Sedimentary evidence for enhanced hydrological cycling in response to rapid carbon release during the early Toarcian oceanic anoxic event , 2018 .

[98]  D. Canfield,et al.  The Iron Biogeochemical Cycle Past and Present , 2012 .

[99]  S. Bottrell,et al.  Low marine sulfate concentrations and the isolation of the European epicontinental sea during the Early Jurassic , 2011 .

[100]  P. Neige,et al.  Distribution of clay minerals in Early Jurassic Peritethyan seas: Palaeoclimatic significance inferred from multiproxy comparisons , 2009 .

[101]  S. Calvert,et al.  Chapter Fourteen Elemental Proxies for Palaeoclimatic and Palaeoceanographic Variability in Marine Sediments: Interpretation and Application , 2007 .

[102]  Sue McQueen,et al.  JOINT NATURE CONSERVATION COMMITTEE , 2006 .

[103]  Stefan Schouten,et al.  Effects of an oceanic anoxic event on the stable carbon isotopic composition of Early Toarcian carbon , 2000 .

[104]  L. V. Duarte Clay minerals and geochemical evolution in the Toarcian-lower Aalenian of the Lusitanian Basin (Portugal) = Minerales de arcilla y evolución geoquímica durante el Toarciense-Aaleniense inferior en la cuenca lusitaniense (Portugal) , 1998 .

[105]  R. A. Chadwick,et al.  Geology of Cardigan Bay and the Bristol Channel. United Kingdom offshore regional report , 1995 .

[106]  D. Tappin The geology of Cardigan Bay and the Bristol Channel , 1994 .

[107]  M. Dobson,et al.  The geology of Cardigan Bay , 1987 .

[108]  R. Aller,et al.  Diagenesis of Fe and S in Amazon inner shelf muds: apparent dominance of Fe reduction and implications for the genesis of ironstones , 1986 .

[109]  J. Cope The Mesozoic history of Wales , 1984 .

[110]  W. Küspert Environmental Changes During Oil Shale Deposition as Deduced from Stable Isotope Ratios , 1982 .

[111]  J. Moldowan,et al.  The effect of thermal stress on source-rock quality as measured by hopane stereochemistry , 1980 .