Very large release of mostly volcanic carbon during the Paleocene-Eocene Thermal Maximum
暂无分享,去创建一个
P. Pearson | A. Ridgwell | G. Foster | R. Norris | H. Pälike | P. Sexton | M. Gutjahr | E. Thomas | E. Anagnostou
[1] Atul K. Jain,et al. Global Carbon Budget 2019 , 2019, Earth System Science Data.
[2] G. Foster,et al. A new boron isotope-pH calibration for Orbulina universa, with implications for understanding and accounting for ‘vital effects’ , 2016 .
[3] J. Wright,et al. Impact ejecta at the Paleocene-Eocene boundary , 2016, Science.
[4] J. Zachos,et al. An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene-Eocene thermal maximum , 2016 .
[5] G. Foster,et al. Reconstructing Ocean pH with Boron Isotopes in Foraminifera , 2016 .
[6] P. Pearson,et al. Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate , 2016, Nature.
[7] A. Ridgwell,et al. Development of a novel empirical framework for interpreting geological carbon isotope excursions, with implications for the rate of carbon injection across the PETM , 2016 .
[8] D. Lunt,et al. An impulse response function for the “long tail” of excess atmospheric CO2 in an Earth system model , 2016 .
[9] S. Planke,et al. Thermogenic methane release as a cause for the long duration of the PETM , 2016, Proceedings of the National Academy of Sciences.
[10] J. Zachos,et al. Anthropogenic carbon release rate unprecedented during the past 66 million years , 2015 .
[11] D. Lunt,et al. The ‘long tail’ of anthropogenic CO2 decline in the atmosphere and its consequences for post-closure performance assessments for disposal of radioactive wastes , 2015, Mineralogical Magazine.
[12] L. Kump,et al. Global warming and the end-Permian extinction event: Proxy and modeling perspectives , 2015 .
[13] A. Saunders. Two LIPs and two Earth-system crises: the impact of the North Atlantic Igneous Province and the Siberian Traps on the Earth-surface carbon cycle , 2015, Geological Magazine.
[14] T. Lenton,et al. The time scale of the silicate weathering negative feedback on atmospheric CO2 , 2015 .
[15] P. Ziveri,et al. Boron isotope evidence for oceanic carbon dioxide leakage during the last deglaciation , 2015, Nature.
[16] R. Norris,et al. Persistence of carbon release events through the peak of early Eocene global warmth , 2014 .
[17] P. Pearson,et al. Drilling disturbance and constraints on the onset of the Paleocene–Eocene boundary carbon isotope excursion in New Jersey , 2014 .
[18] K. Farley,et al. Persistent environmental change after the Paleocene–Eocene Thermal Maximum in the eastern North Atlantic , 2014 .
[19] J. Zachos,et al. Carbon sequestration during the Palaeocene-Eocene Thermal Maximum by an efficient biological pump , 2014 .
[20] J. Zachos,et al. Rapid and sustained surface ocean acidification during the Paleocene-Eocene Thermal Maximum , 2014 .
[21] J. Wright,et al. Reply to Pearson and Nicholas, Stassen et al., and Zeebe et al.: Teasing out the missing piece of the PETM puzzle , 2014, Proceedings of the National Academy of Sciences.
[22] Ellen Thomas,et al. Unsettled puzzle of the Marlboro clays , 2014, Proceedings of the National Academy of Sciences.
[23] G. Dickens,et al. Onset of carbon isotope excursion at the Paleocene-Eocene thermal maximum took millennia, not 13 years , 2014, Proceedings of the National Academy of Sciences.
[24] P. Pearson,et al. Layering in the Paleocene/Eocene boundary of the Millville core is drilling disturbance , 2014, Proceedings of the National Academy of Sciences.
[25] A. Vengosh,et al. Interlaboratory Comparison of Boron Isotope Analyses of Boric Acid, Seawater and Marine CaCO3 by MC-ICPMS and NTIMS , 2013 .
[26] L. Kump,et al. Geochemical evidence for volcanic activity prior to and enhanced terrestrial weathering during the Paleocene Eocene Thermal Maximum , 2013 .
[27] G. Pagnoni,et al. The potential failure of Monte Nuovo at Ischia Island (Southern Italy): numerical assessment of a likely induced tsunami and its effects on a densely inhabited area , 2013, Bulletin of Volcanology.
[28] M. Maslin,et al. Climate model and proxy data constraints on ocean warming across the Paleocene-Eocene Thermal Maximum , 2013 .
[29] J. Wright,et al. Evidence for a rapid release of carbon at the Paleocene-Eocene thermal maximum , 2013, Proceedings of the National Academy of Sciences.
[30] B. Schubert,et al. Reconciliation of marine and terrestrial carbon isotope excursions based on changing atmospheric CO2 levels , 2013, Nature Communications.
[31] M. Kučera,et al. Calibration of the boron isotope proxy in the planktonic foraminifera Globigerinoides ruber for use in palaeo-CO2 reconstruction , 2013 .
[32] M. Rampino. Peraluminous igneous rocks as an indicator of thermogenic methane release from the North Atlantic Volcanic Province at the time of the Paleocene–Eocene Thermal Maximum (PETM) , 2013, Bulletin of Volcanology.
[33] W. Müller,et al. Deep time foraminifera Mg/Ca paleothermometry: Nonlinear correction for secular change in seawater Mg/Ca , 2012 .
[34] Eelco J. Rohling,et al. Making sense of palaeoclimate sensitivity , 2012, Nature.
[35] A. Coe,et al. Seawater oxygenation during the Paleocene-Eocene Thermal Maximum , 2012 .
[36] R. DeConto,et al. Past extreme warming events linked to massive carbon release from thawing permafrost , 2012, Nature.
[37] Stephen Barker,et al. The Geological Record of Ocean Acidification , 2011, Science.
[38] N. Urban,et al. Slow release of fossil carbon during the Palaeocene-Eocene Thermal Maximum , 2011 .
[39] J. Marshall,et al. Constraints on the numerical age of the Paleocene‐Eocene boundary , 2011 .
[40] F. A. McInerney,et al. The Paleocene-Eocene Thermal Maximum: A Perturbation of Carbon Cycle, Climate, and Biosphere with Implications for the Future , 2011 .
[41] J. Zachos,et al. Rapid carbon sequestration at the termination of the Palaeocene-Eocene Thermal Maximum , 2010 .
[42] A. Paytan,et al. Calcium isotope constraints on the end-Permian mass extinction , 2010, Proceedings of the National Academy of Sciences.
[43] S. Planke,et al. Zircon dating ties NE Atlantic sill emplacement to initial Eocene global warming , 2010, Journal of the Geological Society.
[44] P. Valdes,et al. Modelling the oxygen isotope distribution of ancient seawater using a coupled ocean–atmosphere GCM: Implications for reconstructing early Eocene climate , 2010 .
[45] A. Ridgwell,et al. Past constraints on the vulnerability of marine calcifiers to massive carbon dioxide release , 2010 .
[46] G. Dickens,et al. Carbon dioxide forcing alone insufficient to explain Palaeocene–Eocene Thermal Maximum warming , 2009 .
[47] F. Joos,et al. The role of ocean transport in the uptake of anthropogenic CO2 , 2009 .
[48] G. Foster. Erratum to “Seawater pH, pCO2 and [CO32−] variations in the Caribbean Sea over the last 130 kyr: A boron isotope and B/Ca study of planktic foraminifera” (doi: 10.1016/j.epsl.2008.04.015) , 2009 .
[49] G. Foster. Seawater pH, pCO2 and [CO2−3] variations in the Caribbean Sea over the last 130 kyr: A boron isotope and B/Ca study of planktic foraminifera , 2008 .
[50] J. Zachos,et al. On the duration of the Paleocene‐Eocene thermal maximum (PETM) , 2007 .
[51] Julia C. Hargreaves,et al. Regulation of atmospheric CO2 by deep‐sea sediments in an Earth system model , 2007 .
[52] M. Storey,et al. Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic , 2007, Science.
[53] F. Tateo,et al. Mode and tempo of the Paleocene-Eocene thermal maximum in an expanded section from the Venetian pre-Alps , 2007 .
[54] P. Pearson,et al. Microstructural and geochemical perspectives on planktic foraminiferal preservation: “Glassy” versus “Frosty” , 2006 .
[55] A. J. Kaufman,et al. Experimental measurement of boron isotope fractionation in seawater , 2006 .
[56] James D. Annan,et al. Marine geochemical data assimilation in an efficient Earth System Model of global biogeochemical cycling , 2006 .
[57] D. Schrag,et al. Beyond methane: Towards a theory for the Paleocene-Eocene Thermal Maximum , 2006 .
[58] R. Norris,et al. Abrupt reversal in ocean overturning during the Palaeocene/Eocene warm period , 2006, Nature.
[59] Robert Marsh,et al. Uncertainties due to transport-parameter sensitivity in an efficient 3-D ocean-climate model , 2005 .
[60] A. Malthe-Sørenssen,et al. Release of methane from a volcanic basin as a mechanism for initial Eocene global warming , 2004, Nature.
[61] H. Elderfield,et al. A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry , 2003 .
[62] B. Hönisch,et al. The influence of symbiont photosynthesis on the boron isotopic composition of foraminifera shells. , 2003 .
[63] D. Wolf-Gladrow,et al. Vital effects in foraminifera do not compromise the use of δ11B as a paleo‐pH indicator: Evidence from modeling , 2003 .
[64] K. Farley,et al. An alternative age model for the Paleocene–Eocene thermal maximum using extraterrestrial 3He , 2003 .
[65] C. Allègre,et al. Boron isotope systematics in large rivers: implications for the marine boron budget and paleo-pH reconstruction over the Cenozoic , 2002 .
[66] D. Lea,et al. Empirical relationship between pH and the boron isotopic composition of Globigerinoides sacculifer: Implications for the boron isotope paleo-pH proxy. , 2001 .
[67] G. Wefer,et al. New chronology for the late Paleocene thermal maximum and its environmental implications , 2000 .
[68] Sang-Tae Kim,et al. Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates , 1997 .
[69] Pascal Yiou,et al. Macintosh Program performs time‐series analysis , 1996 .
[70] R. M. Owen,et al. Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene , 1995 .
[71] Patrick V. Brady,et al. The effect of silicate weathering on global temperature and atmospheric CO2 , 1991 .
[72] J. Edmond,et al. Boron isotope exchange between seawater and the oceanic crust , 1987 .
[73] H. Jenkyns. Cretaceous anoxic events: from continents to oceans , 1980, Journal of the Geological Society.
[74] P. Bown,et al. Ocean warming, not acidification, controlled coccolithophore response during past greenhouse climate change , 2016 .
[75] S. Schiavon,et al. Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of IPCC the Intergovernmental Panel on Climate Change , 2014 .
[76] Hollis G. Potter,et al. Author Manuscript , 2013 .
[77] J. Hargreaves,et al. Regulation of atmospheric CO 2 by deep-sea sediments in an Earth system model , 2007 .
[78] A. Pardo,et al. Planktic foraminiferal turnover across the Paleocene-Eocene transition at DSDP Site 401, Bay of Biscay, North Atlantic , 1997 .