Basalt-sea water interaction, the Plenus cold event, enhanced weathering and geochemical change; deconstructing Oceanic Anoxic Event 2 (Cenomanian-Turonian, Late Cretaceous)

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doi: 10.1111/sed.12305
Author(s): Jenkyns, Hugh C.; Dickson, Alexander J.; Ruhl, Micha; van der Boorn, Sander H. J. M.
Author Affiliation(s): Primary:
University of Oxford, Department of Earth Sciences, Oxford, United Kingdom
Other:
Shell Global Solutions, Netherlands
Volume Title: Mesozoic climates and oceans
Volume Author(s): Robinson, Stuart A., editor; Heimhofer, Ulrich; Hesselbo, Stephen P.; Petrizzo, Maria Rose
Source: Sedimentology, 64(1), p.16-43; Workshop on Mesozoic climates and oceans, Ascona, Switzerland, July 2017, edited by Stuart A. Robinson, Ulrich Heimhofer, Stephen P. Hesselbo and Maria Rose Petrizzo. Publisher: Wiley-Blackwell, Oxford, United Kingdom. ISSN: 0037-0746 CODEN: SEDIAT
Note: In English. 130 refs.; illus., incl. sects., geol. sketch map
Summary: Oceanic Anoxic Event 2 (Cenomanian-Turonian: ca 94 Ma) represents a major palaeoceanographic phenomenon that took place during an interval of extreme global warmth when large amounts of organic matter entered the marine burial record, probably triggered by increased availability of nutrients for planktonic biota. Three sections (Eastbourne, Sussex, UK; Raia del Pedale, Campania, Italy; and Tarfaya, Morocco) recording this event illustrate the influence on marine geochemistry of mafic volcanic rock-seawater interaction, anoxia to euxinia, and re-oxygenation and cooling during the so-called 'Plenus Cold Event'. The Eastbourne section represents the organic-lean epicontinental pelagic deposits of the English Chalk; the Raia del Pedale section represents a shallow-water platform carbonate on the Tethyan continental margin, also largely devoid of organic matter; and the Tarfaya core represents an Atlantic margin site where cyclically bedded organic-rich sediments were well developed. Correlation between all three sections is readily achieved by biostratigraphy and carbon-isotope stratigraphy (δ13Ccarb and δ13Corg) over the Oceanic Anoxic Event 2 interval, represented by a characteristic broad positive carbon-isotope excursion. The stratigraphic range of the Plenus Cold Event, defined by the presence, in two discrete levels, of boreal fauna and an excursion to heavier oxygen-isotope values in the English Chalk, can be identified in Raia del Pedale and Tarfaya by using the carbon-isotope curve as a correlative tool. Similarly, a section in southern France allows its co-existing osmium-isotope excursion to relatively unradiogenic values to be placed in the context of the Oceanic Anoxic Event in all three analysed sections. A fall to lower osmium-isotope values clearly pre-dated the onset of Oceanic Anoxic Event 2, as defined by the initial rise in carbon-isotope values, allowing the putative magmatic/mafic event as a trigger for the Oceanic Anoxic Event. An initial drop in sulphur-isotope ratios (δ34SCAS) at Eastbourne correlates with the osmium-isotope curve, suggesting that isotopically light sulphur could have been derived from a mafic igneous source. Re-oxygenation of sediments of all three investigated sections during the Plenus Cold Event is variably illustrated by change in cerium:calcium, iodine:calcium, molybedenum:calcium and uranium:calcium ratios, according to the redox behaviour of the elements in question and whether controls on seawater chemistry were local or global in nature. Changes in molybdenum-isotope ratios from Tarfaya and portions of the sulphur-isotope curve from Eastbourne and Raia del Pedale also indicate the probable presence of more oxygen-rich bottom waters during the Plenus Cold Event. Oxidation by such waters of previously deposited organic-rich shales, as well as loss of anoxic/euxinic sinks, is credited with temporarily enriching global seawater in a range of other redox-sensitive trace metals (for example, V, Cr, Co, Ni, Cu, Zn and Cd) during ongoing basalt-seawater interaction indicated by persistent relatively non-radiogenic osmium-isotope seawater values. However, early diagenetic enrichment of manganese in the English Chalk over much of the Oceanic Anoxic Event interval is broadly correlative in time with relatively low osmium-isotope values in sections elsewhere: a relationship that may be due to the lack of affinity of manganese with carbon-rich shales, hence allowing relatively elevated concentrations of the element in marine waters to persist during leaching of mafic rocks, unlike other redox-sensitive species. The calcium-isotope and lithium-isotope ratios from Eastbourne and Raia del Pedale indicate an increase in global weathering during the initial phase of Oceanic Anoxic Event 2, and the shift in strontium isotopes and osmium isotopes to more unradiogenic values during the event suggests that not only construction but also destruction of one or more Large Igneous Provinces was probably a proximal cause of this major palaeoceanographic phenomenon by elevating nutrient levels and planktonic productivity in large tracts of the world ocean. Globally widespread carbon burial and silicate weathering are both identified as important mechanisms for drawing down atmospheric carbon dioxide that, in the absence of overwhelming volcanogenic replenishment of this greenhouse gas during the early phase of Oceanic Anoxic Event 2, caused the Plenus Cold Event. Abstract Copyright (2016), International Association of Sedimentologists.
Year of Publication: 2017
Research Program: ODP Ocean Drilling Program
Key Words: 02 Geochemistry; 12 Stratigraphy, Historical Geology and Paleoecology; Africa; Algae; Anaerobic environment; Aral region; Asia; Atlantic Ocean; Azov Sea; Biostratigraphy; Black Sea region; Boreal environment; C-13/C-12; Campania Italy; Carbon; Central Asia; Commonwealth of Independent States; Cretaceous; Demerara Rise; Depositional environment; Eastbourne England; England; Equatorial Atlantic; Europe; Foraminifera; Great Britain; Invertebrata; Isotope ratios; Isotopes; Italy; Leg 207; Leg 210; Lithofacies; Lithostratigraphy; Marine environment; Mesozoic; Microfossils; Morocco; Nannofossils; Newfoundland Basin; North Africa; North Atlantic; Northwest Atlantic; OAE 2; ODP Site 1260; ODP Site 1276; Ocean Drilling Program; Oceanic anoxic events; Paleoclimatology; Paleoecology; Paleoenvironment; Plantae; Plenus cold event; Protista; Raia del Pedale Italy; Reconstruction; S-34/S-32; Sedimentary rocks; Sedimentation; Southern Europe; Stable isotopes; Sulfur; Sussex England; Tarfaya Morocco; Terrestrial environment; Turonian; United Kingdom; Upper Cretaceous; West Atlantic; Western Europe
Coordinates: N410000 N460000 E0480000 E0420000
Record ID: 2017029936
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from John Wiley & Sons, Chichester, United Kingdom
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100 1 |a Jenkyns, Hugh C.  |u University of Oxford, Department of Earth Sciences, Oxford 
245 1 0 |a Basalt-sea water interaction, the Plenus cold event, enhanced weathering and geochemical change; deconstructing Oceanic Anoxic Event 2 (Cenomanian-Turonian, Late Cretaceous) 
300 |a p. 16-43 
500 |a In English. 130 refs. 
500 |a Research program: ODP Ocean Drilling Program 
500 |a Affiliation: University of Oxford, Department of Earth Sciences; Oxford; GBR; United Kingdom 
500 |a Affiliation: Shell Global Solutions; ; NLD; Netherlands 
500 |a Source note: Sedimentology, 64(1), p.16-43; Workshop on Mesozoic climates and oceans, Ascona, Switzerland, July 2017, edited by Stuart A. Robinson, Ulrich Heimhofer, Stephen P. Hesselbo and Maria Rose Petrizzo. Publisher: Wiley-Blackwell, Oxford, United Kingdom. ISSN: 0037-0746 
500 |a Publication type: conference paper or compendium article 
504 |b 130 refs. 
510 3 |a GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from John Wiley & Sons, Chichester, United Kingdom 
520 |a Oceanic Anoxic Event 2 (Cenomanian-Turonian: ca 94 Ma) represents a major palaeoceanographic phenomenon that took place during an interval of extreme global warmth when large amounts of organic matter entered the marine burial record, probably triggered by increased availability of nutrients for planktonic biota. Three sections (Eastbourne, Sussex, UK; Raia del Pedale, Campania, Italy; and Tarfaya, Morocco) recording this event illustrate the influence on marine geochemistry of mafic volcanic rock-seawater interaction, anoxia to euxinia, and re-oxygenation and cooling during the so-called 'Plenus Cold Event'. The Eastbourne section represents the organic-lean epicontinental pelagic deposits of the English Chalk; the Raia del Pedale section represents a shallow-water platform carbonate on the Tethyan continental margin, also largely devoid of organic matter; and the Tarfaya core represents an Atlantic margin site where cyclically bedded organic-rich sediments were well developed. Correlation between all three sections is readily achieved by biostratigraphy and carbon-isotope stratigraphy (δ>13`C<carb` and δ>13`C<org`) over the Oceanic Anoxic Event 2 interval, represented by a characteristic broad positive carbon-isotope excursion. The stratigraphic range of the Plenus Cold Event, defined by the presence, in two discrete levels, of boreal fauna and an excursion to heavier oxygen-isotope values in the English Chalk, can be identified in Raia del Pedale and Tarfaya by using the carbon-isotope curve as a correlative tool. Similarly, a section in southern France allows its co-existing osmium-isotope excursion to relatively unradiogenic values to be placed in the context of the Oceanic Anoxic Event in all three analysed sections. A fall to lower osmium-isotope values clearly pre-dated the onset of Oceanic Anoxic Event 2, as defined by the initial rise in carbon-isotope values, allowing the putative magmatic/mafic event as a trigger for the Oceanic Anoxic Event. An initial drop in sulphur-isotope ratios (δ>34`S<CAS`) at Eastbourne correlates with the osmium-isotope curve, suggesting that isotopically light sulphur could have been derived from a mafic igneous source. Re-oxygenation of sediments of all three investigated sections during the Plenus Cold Event is variably illustrated by change in cerium:calcium, iodine:calcium, molybedenum:calcium and uranium:calcium ratios, according to the redox behaviour of the elements in question and whether controls on seawater chemistry were local or global in nature. Changes in molybdenum-isotope ratios from Tarfaya and portions of the sulphur-isotope curve from Eastbourne and Raia del Pedale also indicate the probable presence of more oxygen-rich bottom waters during the Plenus Cold Event. Oxidation by such waters of previously deposited organic-rich shales, as well as loss of anoxic/euxinic sinks, is credited with temporarily enriching global seawater in a range of other redox-sensitive trace metals (for example, V, Cr, Co, Ni, Cu, Zn and Cd) during ongoing basalt-seawater interaction indicated by persistent relatively non-radiogenic osmium-isotope seawater values. However, early diagenetic enrichment of manganese in the English Chalk over much of the Oceanic Anoxic Event interval is broadly correlative in time with relatively low osmium-isotope values in sections elsewhere: a relationship that may be due to the lack of affinity of manganese with carbon-rich shales, hence allowing relatively elevated concentrations of the element in marine waters to persist during leaching of mafic rocks, unlike other redox-sensitive species. The calcium-isotope and lithium-isotope ratios from Eastbourne and Raia del Pedale indicate an increase in global weathering during the initial phase of Oceanic Anoxic Event 2, and the shift in strontium isotopes and osmium isotopes to more unradiogenic values during the event suggests that not only construction but also destruction of one or more Large Igneous Provinces was probably a proximal cause of this major palaeoceanographic phenomenon by elevating nutrient levels and planktonic productivity in large tracts of the world ocean. Globally widespread carbon burial and silicate weathering are both identified as important mechanisms for drawing down atmospheric carbon dioxide that, in the absence of overwhelming volcanogenic replenishment of this greenhouse gas during the early phase of Oceanic Anoxic Event 2, caused the Plenus Cold Event. Abstract Copyright (2016), International Association of Sedimentologists. 
650 7 |a Algae  |2 georeft 
650 7 |a Anaerobic environment  |2 georeft 
650 7 |a Biostratigraphy  |2 georeft 
650 7 |a Boreal environment  |2 georeft 
650 7 |a C-13/C-12  |2 georeft 
650 7 |a Carbon  |2 georeft 
650 7 |a Cretaceous  |2 georeft 
650 7 |a Depositional environment  |2 georeft 
650 7 |a Foraminifera  |2 georeft 
650 7 |a Isotope ratios  |2 georeft 
650 7 |a Isotopes  |2 georeft 
650 7 |a Lithofacies  |2 georeft 
650 7 |a Lithostratigraphy  |2 georeft 
650 7 |a Marine environment  |2 georeft 
650 7 |a Mesozoic  |2 georeft 
650 7 |a Microfossils  |2 georeft 
650 7 |a Nannofossils  |2 georeft 
650 7 |a OAE 2  |2 georeft 
650 7 |a Ocean Drilling Program  |2 georeft 
650 7 |a Oceanic anoxic events  |2 georeft 
650 7 |a Paleoclimatology  |2 georeft 
650 7 |a Paleoecology  |2 georeft 
650 7 |a Paleoenvironment  |2 georeft 
650 7 |a Plantae  |2 georeft 
650 7 |a Reconstruction  |2 georeft 
650 7 |a S-34/S-32  |2 georeft 
650 7 |a Sedimentary rocks  |2 georeft 
650 7 |a Sedimentation  |2 georeft 
650 7 |a Stable isotopes  |2 georeft 
650 7 |a Sulfur  |2 georeft 
650 7 |a Terrestrial environment  |2 georeft 
650 7 |a Turonian  |2 georeft 
650 7 |a Upper Cretaceous  |2 georeft 
651 7 |a Africa  |2 georeft 
651 7 |a Aral region  |2 georeft 
651 7 |a Asia  |2 georeft 
651 7 |a Atlantic Ocean  |2 georeft 
651 7 |a Azov Sea  |2 georeft 
651 7 |a Black Sea region  |2 georeft 
651 7 |a Campania Italy  |2 georeft 
651 7 |a Central Asia  |2 georeft 
651 7 |a Commonwealth of Independent States  |2 georeft 
651 7 |a Demerara Rise  |2 georeft 
651 7 |a England  |2 georeft 
651 7 |a Equatorial Atlantic  |2 georeft 
651 7 |a Europe  |2 georeft 
651 7 |a Great Britain  |2 georeft 
651 7 |a Italy  |2 georeft 
651 7 |a Leg 207  |2 georeft 
651 7 |a Leg 210  |2 georeft 
651 7 |a Morocco  |2 georeft 
651 7 |a Newfoundland Basin  |2 georeft 
651 7 |a North Africa  |2 georeft 
651 7 |a North Atlantic  |2 georeft 
651 7 |a Northwest Atlantic  |2 georeft 
651 7 |a ODP Site 1260  |2 georeft 
651 7 |a ODP Site 1276  |2 georeft 
651 7 |a Southern Europe  |2 georeft 
651 7 |a Sussex England  |2 georeft 
651 7 |a Tarfaya Morocco  |2 georeft 
651 7 |a United Kingdom  |2 georeft 
651 7 |a West Atlantic  |2 georeft 
651 7 |a Western Europe  |2 georeft 
653 |a Eastbourne England 
653 |a Invertebrata 
653 |a Plenus cold event 
653 |a Protista 
653 |a Raia del Pedale Italy 
700 1 |a Dickson, Alexander J., 
700 1 |a Ruhl, Micha, 
700 1 |a van der Boorn, Sander H. J. M., 
700 1 |a Heimhofer, Ulrich,  |e editor 
700 1 |a Hesselbo, Stephen P.,  |e editor 
700 1 |a Petrizzo, Maria Rose,  |e editor 
711 2 |a Workshop on Mesozoic climates and oceans  |d (2015 :  |c Ascona, Switzerland)  
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