Abrupt episode of mid-Cretaceous ocean acidification triggered by massive volcanism
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A. Jacobson | R. Hobbs | B. Sageman | Matthew M. Jones | J. Kuroda | L. Riquier | K. Macleod | M. Tejada | D. Selby | K. Bogus | B. Huber | S. Batenburg | K. MacLeod
[1] A. Jacobson,et al. Calcium isotope ratios of malformed foraminifera reveal biocalcification stress preceded Oceanic Anoxic Event 2 , 2022, Communications Earth & Environment.
[2] M. Petrizzo,et al. Enhanced hydrological cycle during Oceanic Anoxic Event 2 at southern high latitudes: New insights from IODP Site U1516 , 2022, Global and Planetary Change.
[3] Zhonghui Liu,et al. Enhanced ocean connectivity and volcanism instigated global onset of Cretaceous Oceanic Anoxic Event 2 (OAE2) ∼94.5 million years ago , 2022, Earth and Planetary Science Letters.
[4] M. Petrizzo,et al. Exploring the paleoceanographic changes registered by planktonic foraminifera across the Cenomanian-Turonian boundary interval and Oceanic Anoxic Event 2 at southern high latitudes in the Mentelle Basin (SE Indian Ocean) , 2021 .
[5] J. Curtis,et al. Assessing the contribution of the La Luna Sea to the global sink of organic carbon during the Cenomanian-Turonian Oceanic Anoxic Event 2 (OAE2) , 2021 .
[6] C. Holmden,et al. Changing inputs of continental and submarine weathering sources of Sr to the oceans during OAE 2 , 2021, Geochimica et Cosmochimica Acta.
[7] M. Petrizzo,et al. Early Cretaceous subsidence of the Naturaliste Plateau defined by a new record of volcaniclastic-rich sequence at IODP Site U1513 , 2020, Gondwana Research.
[8] S. Wright,et al. High resolution osmium data record three distinct pulses of magmatic activity during cretaceous Oceanic Anoxic Event 2 (OAE-2) , 2020 .
[9] R. Zeebe,et al. History of carbonate ion concentration over the last 100 million years II: Revised calculations and new data , 2019, Geochimica et Cosmochimica Acta.
[10] D. Selby,et al. Influence of the High Arctic Igneous Province on the Cenomanian/Turonian boundary interval, Sverdrup Basin, High Canadian Arctic , 2019, Earth and Planetary Science Letters.
[11] S. Self,et al. The eruptive tempo of Deccan volcanism in relation to the Cretaceous-Paleogene boundary , 2019, Science.
[12] J. Middelburg,et al. The role of calcification in carbonate compensation , 2018, Nature Geoscience.
[13] B. Arbic,et al. Current CaCO3 dissolution at the seafloor caused by anthropogenic CO2 , 2018, Proceedings of the National Academy of Sciences.
[14] S. Flögel,et al. New insights into Cenomanian paleoceanography and climate evolution from the Tarfaya Basin, southern Morocco , 2018 .
[15] S. Nielsen,et al. Constraining the rate of oceanic deoxygenation leading up to a Cretaceous Oceanic Anoxic Event (OAE-2: ~94 Ma) , 2017, Science Advances.
[16] A. Turchyn,et al. Remobilization of crustal carbon may dominate volcanic arc emissions , 2017, Science.
[17] R. Zeebe,et al. Quantifying the volcanic emissions which triggered Oceanic Anoxic Event 1a and their effect on ocean acidification , 2017 .
[18] R. Pancost,et al. A Southern Hemisphere record of global trace‐metal drawdown and orbital modulation of organic‐matter burial across the Cenomanian–Turonian boundary (Ocean Drilling Program Site 1138, Kerguelen Plateau) , 2017 .
[19] R. Pancost,et al. Gradual and sustained carbon dioxide release during Aptian Oceanic Anoxic Event 1a , 2016 .
[20] H. Nishi,et al. Pacific 187 Os/ 188 Os isotope chemistry and U-Pb geochronology: Synchroneity of global Os isotope change across OAE 2 , 2015 .
[21] A. Jacobson,et al. Ca isotope stratigraphy across the Cenomanian–Turonian OAE 2: Links between volcanism, seawater geochemistry, and the carbonate fractionation factor , 2015 .
[22] K. Farley,et al. Impact of dissolution on the sedimentary record of the Paleocene–Eocene thermal maximum , 2014 .
[23] B. Sageman,et al. Cenomanian To Campanian Carbon Isotope Chemostratigraphy from the Western Interior Basin, U.S.A , 2014 .
[24] I. Jarvis,et al. Marine 187Os/188Os isotope stratigraphy reveals the interaction of volcanism and ocean circulation during Oceanic Anoxic Event 2 , 2014 .
[25] A. Sluijs,et al. A middle Eocene carbon cycle conundrum , 2013 .
[26] A. A. Tantawy,et al. The expression of the Cenomanian–Turonian oceanic anoxic event in Tibet , 2013 .
[27] D. P. Murphy,et al. A Cenozoic record of the equatorial Pacific carbonate compensation depth , 2012, Nature.
[28] D. Bottjer,et al. Recognising ocean acidification in deep time: An evaluation of the evidence for acidification across the Triassic-Jurassic boundary , 2012 .
[29] Stephen Barker,et al. The Geological Record of Ocean Acidification , 2011, Science.
[30] J. Mutterlose,et al. Late Cretaceous (Cenomanian–Maastrichtian) calcareous nannofossils from Goban Spur (DSDP Sites 549, 551): Implications for the palaeoceanography of the proto North Atlantic , 2011 .
[31] E. Erba,et al. Calcareous Nannoplankton Response to Surface-Water Acidification Around Oceanic Anoxic Event 1a , 2010, Science.
[32] A. Paytan,et al. Calcium isotope constraints on the end-Permian mass extinction , 2010, Proceedings of the National Academy of Sciences.
[33] Stefan Schouten,et al. A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2 , 2010 .
[34] P. Meyers,et al. Origins and maturity of organic matter in mid-Cretaceous black shales from ODP Site 1138 on the Kerguelen Plateau , 2009 .
[35] M. Böttcher,et al. Paleo-redox conditions during OAE 2 reflected in Demerara Rise sediment geochemistry (ODP Leg 207) , 2009 .
[36] T. Yamanaka,et al. Litho-, bio- and chemostratigraphy across the Cenomanian/Turonian boundary (OAE 2) in the Vocontian Basin of southeastern France , 2009 .
[37] R. Duncan,et al. C-isotope stratigraphy and paleoenvironmental changes across OAE2 (mid-Cretaceous) from shallow-water platform carbonates of southern Mexico , 2009 .
[38] M. Petrizzo,et al. The Cenomanian/Turonian oceanic anoxic event in the South Atlantic: New insights from a geochemical study of DSDP Site 530A , 2008 .
[39] M. Wagreich,et al. Calcareous nannoplankton, planktonic foraminiferal, and carbonate carbon isotope stratigraphy of the Cenomanian–Turonian boundary section in the Ultrahelvetic Zone (Eastern Alps, Upper Austria) , 2008 .
[40] S. Turgeon,et al. Cretaceous oceanic anoxic event 2 triggered by a massive magmatic episode , 2008, Nature.
[41] F. Rodríguez-Tovar,et al. Ichnological record of deep-sea palaeoenvironmental changes around the Oceanic Anoxic Event 2 (Cenomanian–Turonian boundary): An example from the Barnasiówka section, Polish Outer Carpathians , 2008 .
[42] H. Tokuyama,et al. Contemporaneous massive subaerial volcanism and late cretaceous Oceanic Anoxic Event 2 , 2007 .
[43] A. Gale,et al. Sea-level change, carbon cycling and palaeoclimate during the Late Cenomanian of northwest Europe; an integrated palaeoenvironmental analysis , 2006 .
[44] H. Brumsack,et al. Anoxic vs dysoxic events reflected in sediment geochemistry during the Cenomanian-Turonian Boundary Event (Cretaceous) in the Umbria-Marche Basin of central Italy , 2006 .
[45] A. Bellanca,et al. Comparative high-resolution chemostratigraphy of the Bonarelli Level from the reference Bottaccione section (Umbria–Marche Apennines) and from an equivalent section in NW Sicily: Consistent and contrasting responses to the OAE2 , 2006 .
[46] H. Brumsack. The trace metal content of recent organic carbon-rich sediments; implications for Cretaceous black shale formation , 2006 .
[47] T. Bralower,et al. Paleoceanographic significance of high-resolution carbon isotope records across the Cenomanian–Turonian boundary in the Western Interior and New Jersey coastal plain, USA , 2005 .
[48] J. Zachos,et al. Rapid Acidification of the Ocean During the Paleocene-Eocene Thermal Maximum , 2005, Science.
[49] R. Coccioni,et al. PLANKTONIC FORAMINIFERA AND ENVIRONMENTAL CHANGES ACROSS THE BONARELLI EVENT (OAE2, LATEST CENOMANIAN) IN ITS TYPE AREA: A HIGH-RESOLUTION STUDY FROM THE TETHYAN REFERENCE BOTTACCIONE SECTION (GUBBIO, CENTRAL ITALY) , 2004 .
[50] B. Peucker‐Ehrenbrink,et al. The marine osmium isotope record , 2000 .
[51] A. Nederbragt,et al. Stratigraphy and palaeoceanography of the Cenomanian-Turonian Boundary Event in Oued Mellegue, north-western Tunisia , 1999 .
[52] A. Kerr. Oceanic plateau formation: a cause of mass extinction and black shale deposition around the Cenomanian–Turonian boundary? , 1998, Journal of the Geological Society.
[53] J. Morgan,et al. Re-Os Ages of Group IIA, IIIA, IVA, and IVB Iron Meteorites , 1996, Science.
[54] C. Müller,et al. Ocean-wide stagnation episode in the late Cretaceous , 1984, Nature.
[55] P. Vogt,et al. Initial Reports of the Deep Sea Drilling Project, 43 , 1979 .