Mercury anomalies in upper Aptian-lower Albian sediments from the Tethys realm
暂无分享,去创建一个
M. Sprovieri | Nadia Sabatino | R. Coccioni | M. Bonsignore | S. Ferraro | Vincenzo Tancredi | M. Core | N. Sabatino
[1] P. Bown,et al. The Global Boundary Stratotype Section and Point (GSSP) for the base of the Albian Stage, of the Cretaceous, the Col de Pré-Guittard section, Arnayon, Drôme, France , 2017 .
[2] S. Grasby,et al. On the causes of mass extinctions , 2017 .
[3] T. Mather,et al. Mercury evidence for pulsed volcanism during the end-Triassic mass extinction , 2017, Proceedings of the National Academy of Sciences.
[4] K. Föllmi,et al. Mercury enrichment indicates volcanic triggering of Valanginian environmental change , 2017, Scientific Reports.
[5] J. Barbosa,et al. Mercury enrichment and Hg isotopes in Cretaceous–Paleogene boundary successions: Links to volcanism and palaeoenvironmental impacts , 2016 .
[6] D. Bottjer,et al. Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction , 2016, Nature Communications.
[7] L. D. Lacerda,et al. Mercury anomaly, Deccan volcanism and the end-Cretaceous Mass Extinction: REPLY , 2016 .
[8] 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 .
[9] B. Beauchamp,et al. Progressive environmental deterioration in northwestern Pangea leading to the latest Permian extinction , 2015 .
[10] H. Sanei,et al. Mercury anomalies associated with three extinction events (Capitanian Crisis, Latest Permian Extinction and the Smithian/Spathian Extinction) in NW Pangea , 2015, Geological Magazine.
[11] M. Sprovieri,et al. High-resolution chemostratigraphy of the late Aptian–early Albian oceanic anoxic event (OAE 1b) from the Poggio le Guaine section (Umbria–Marche Basin, central Italy) , 2015 .
[12] A. Malinverno,et al. Environmental consequences of Ontong Java Plateau and Kerguelen Plateau volcanism , 2015 .
[13] T. Tomiyasu,et al. Distribution of mercury in sediments from Kagoshima Bay, Japan, and its relationship with physical and chemical factors , 2015, Environmental Earth Sciences.
[14] J. Barbosa,et al. High-resolution Hg chemostratigraphy: A contribution to the distinction of chemical fingerprints of the Deccan volcanism and Cretaceous–Paleogene Boundary impact event , 2014 .
[15] P. Bown,et al. Integrated stratigraphy across the Aptian/Albian boundary at Col de Pré-Guittard (southeast France): A candidate Global Boundary Stratotype Section , 2014 .
[16] P. Wignall,et al. Large igneous provinces and mass extinctions: An update , 2014 .
[17] G. Avard,et al. Mercury fluxes from volcanic and geothermal sources: an update , 2014 .
[18] J. Barbosa,et al. Mercury as a proxy for volcanic activity during extreme environmental turnover: The Cretaceous–Paleogene transition , 2013 .
[19] H. Sanei,et al. Mercury deposition through the Permo–Triassic Biotic Crisis , 2013 .
[20] R. S. Martin,et al. Bioindication of volcanic mercury (Hg) deposition around Mt. Etna (Sicily). , 2012 .
[21] K. Föllmi. Early Cretaceous life, climate and anoxia , 2012 .
[22] A. Gale,et al. Abrupt planktic foraminiferal turnover across the Niveau Kilian at Col de Pré-Guittard (Vocontian Basin, southeast France): new criteria for defining the Aptian/Albian boundary , 2012 .
[23] Guangliang Liu,et al. Adsorption of Mercury on Solids in the Aquatic Environment , 2011 .
[24] M. Kučera,et al. Paleotemperature and paleosalinity inferences and chemostratigraphy across the Aptian/Albian boundary in the subtropical North Atlantic. , 2011 .
[25] Roeland van Gilst,et al. The sedimentary expression of oceanic anoxic event 1b in the North Atlantic , 2011 .
[26] R. S. Martin,et al. Rapid oxidation of mercury (Hg) at volcanic vents: insights from high temperature thermodynamic models of Mt Etna's emissions , 2011 .
[27] T. Herbert,et al. Astronomical tuning of the Aptian Stage from Italian reference sections , 2010 .
[28] Roland von Glasow,et al. Atmospheric chemistry in volcanic plumes , 2010 .
[29] D. Watkins,et al. Elevated primary productivity of calcareous nannoplankton associated with ocean anoxic event 1b during the Aptian/Albian transition (Early Cretaceous) , 2008 .
[30] P. Hamilton,et al. Evidence for control of mercury accumulation rates in Canadian High Arctic lake sediments by variations of aquatic primary productivity. , 2007, Environmental science & technology.
[31] Nicola Pirrone,et al. A Synthesis of Progress and Uncertainties in Attributing the Sources of Mercury in Deposition , 2007, Ambio.
[32] A. Saunders. Large Igneous Provinces: Origin and Environmental Consequences , 2005 .
[33] G. Schmiedl,et al. Millennial- to Centennial-Scale Interruptions of the Oceanic Anoxic Event 1b (Early Albian, mid-Cretaceous) Inferred from Benthic Foraminiferal Repopulation Events , 2005 .
[34] P. Wallace. Volatiles in subduction zone magmas: concentrations and fluxes based on melt inclusion and volcanic gas data , 2005 .
[35] C. Hemleben,et al. High-resolution carbon isotope records of the Aptian to Lower Albian from SE France and the Mazagan Plateau (DSDP Site 545): a stratigraphic tool for paleoceanographic and paleobiologic reconstruction , 2004 .
[36] C. Spötl,et al. Continuous-flow isotope ratio mass spectrometric analysis of carbonate minerals. , 2003, Rapid communications in mass spectrometry : RCM.
[37] J. Fischer,et al. Influence of sulphur cycle on mercury methylation in estuarine sediment (Seine estuary, France) , 2003 .
[38] J. Herrle. Calcareous nannofossils from the Aptian–Lower Albian of southeast France: palaeoecological and biostratigraphic implications , 2003 .
[39] C. Hemleben,et al. Forcing mechanisms for mid-Cretaceous black shale formation: evidence from the Upper Aptian and Lower Albian of the Vocontian Basin (SE France) , 2003 .
[40] T. Ishikawa,et al. Boninitic volcanism in the Oman ophiolite: Implications for thermal condition during transition from spreading ridge to arc , 2002 .
[41] R. Leckie,et al. Oceanic anoxic events and plankton evolution: Biotic response to tectonic forcing during the mid-Cretaceous , 2002 .
[42] Pringle,et al. Kerguelen Hotspot Magma Output since 130 Ma , 2002 .
[43] R. Duncan. A Time Frame for Construction of the Kerguelen Plateau and Broken Ridge , 2002 .
[44] Robert P. Mason,et al. Constants for mercury binding by dissolved organic matter isolates from the Florida Everglades , 2001 .
[45] D. Sayers,et al. Bonding of Hg(II) to reduced organic sulfur in humic acid as affected by S/Hg ratio. , 2001, Environmental science & technology.
[46] R. Norris,et al. Increased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period , 2001, Nature.
[47] C. Hemleben,et al. Correlating environmental changes during early Albian oceanic anoxic event 1B using benthic foraminiferal paleoecology , 1999 .
[48] Andrew Heyes,et al. Sulfide Controls on Mercury Speciation and Bioavailability to Methylating Bacteria in Sediment Pore Waters , 1999 .
[49] P. Bloom,et al. X-ray absorption spectroscopic evidence for the complexation of HG(II) by reduced sulfur in soil humic substances , 1999 .
[50] John Munthe,et al. Atmospheric mercury—An overview , 1998 .
[51] K. Föllmi,et al. Correlation of Early Cretaceous carbon isotope stratigraphy and platform drowning events: a possible link? , 1998 .
[52] J. Zachos,et al. High-resolution records of the late Paleocene thermal maximum and circum-Caribbean volcanism: is there a causal link? , 1997 .
[53] R. T. Powell,et al. Mercury associated with colloidal material in an estuarine and an open-ocean environment , 1996 .
[54] O. Eldholm,et al. Large igneous provinces: crustal structure, dimensions, and external consequences , 1994 .
[55] R. White. Melt production rates in mantle plumes , 1993, Philosophical Transactions of the Royal Society of London. Series A: Physical and Engineering Sciences.
[56] M. Rampino,et al. Flood Basalt Volcanism During the Past 250 Million Years , 1988, Science.
[57] R. Leckie. Mid-Cretaceous Planktonic Foraminiferal Biostratigraphy off Central Morocco, Deep Sea Drilling Project Leg 79, Sites 545 and 547 , 1984 .
[58] F. Horváth,et al. Adria, the African promontory, in mesozoic Mediterranean palaeogeography , 1979 .
[59] K. Föllmi,et al. Mercury enrichments in lower Aptian sediments support the link between Ontong Java large igneous province activity and oceanic anoxic episode 1a , 2017 .
[60] B. Beauchamp,et al. Isotopic signatures of mercury contamination in latest Permian oceans , 2017 .
[61] H. Sanei,et al. Latest Permian mercury anomalies , 2012 .
[62] R. Leckie,et al. PLANKTIC FORAMINIFERAL SPECIES TURNOVER ACROSS DEEP-SEA APTIAN/ ALBIAN BOUNDARY SECTIONS , 2011 .
[63] H. Skov,et al. Chapter 4 Gaseous Elemental Mercury in the Ambient Atmosphere: Review of the Application of Theoretical Calculations and Experimental Studies for Determination of Reaction Coefficients and Mechanisms with Halogens and Other Reactants , 2008 .
[64] Alan Robock,et al. Volcanism and the Earth's Atmosphere , 2003 .
[65] D. Weis,et al. Leg 183 synthesis: Kerguelen plateau-broken ridge-a large igneous province , 2003 .
[66] P. Renne,et al. On the ages of flood basalt events , 2003 .
[67] W. Kuhnt,et al. No extinctions during Oceanic Anoxic Event 1b: the Aptian-Albian benthic foraminiferal record of ODP Leg 171 , 2001, Geological Society, London, Special Publications.
[68] I. P. Silva,et al. Cretaceous paleoceanography: Evidence from planktonic foraminiferal evolution , 1999 .
[69] M. Meili. Mercury in lakes and rivers , 1997 .
[70] J. Royer,et al. Jurassic to Eocene plate tectonic reconstructions in the Kerguelen Plateau region , 1992 .