(Q56527614)

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Nutrients as the dominant control on the spread of anoxia and euxinia across the Cenomanian-Turonian oceanic anoxic event (OAE2): Model-data comparison

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scholarly article

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Nutrients as the dominant control on the spread of anoxia and euxinia across the Cenomanian-Turonian oceanic anoxic event (OAE2): Model-data comparison (English)

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Cenomanian-Turonian boundary event

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object named as

A. Ridgwell

3

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author name string

F. M. Monteiro

1

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R. D. Pancost

2

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Y. Donnadieu

4

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publication date

December 2012

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Paleoceanography

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27

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4

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High sensitivity of the continental-weathering carbon dioxide sink to future climate change

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On the ages of flood basalt events

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Modelling the primary control of paleogeography on Cretaceous climate

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The co-evolution of the nitrogen, carbon and oxygen cycles in the Proterozoic ocean

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Convection of North Pacific deep water during the early Cenozoic

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Dominant eukaryotic export production during ocean anoxic events reflects the importance of recycled NH4+

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Black shale deposition, atmospheric CO2drawdown, and cooling during the Cenomanian-Turonian Oceanic Anoxic Event

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Evidence for rapid climate change in the Mesozoic–Palaeogene greenhouse world

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Geochemistry of oceanic anoxic events

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High temperatures in the Late Cretaceous Arctic Ocean

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The snowball Earth aftermath: Exploring the limits of continental weathering processes

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Oceanic Euxinia in Earth History: Causes and Consequences

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Further evidence for the development of photic-zone euxinic conditions during Mesozoic oceanic anoxic events

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Cretaceous oceanic anoxic event 2 triggered by a massive magmatic episode.

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Pyrite framboid diameter as a measure of oxygen deficiency in ancient mudrocks

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Warm tropical ocean surface and global anoxia during the mid-Cretaceous period

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Significant increases in global weathering during Oceanic Anoxic Events 1a and 2 indicated by calcium isotopes

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The role of ocean transport in the uptake of anthropogenic CO 2

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Stable organic carbon isotope stratigraphy across Oceanic Anoxic Event 2 of Demerara Rise, western tropical Atlantic

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Periodic mid-Cretaceous oceanic anoxic events linked by oscillations of the phosphorus and oxygen biogeochemical cycles

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Orbital forcing of organic carbon burial in the proto-North Atlantic during oceanic anoxic event 2

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Ocean anoxic events in the mid-Cretaceous simulated by a 3-D biogeochemical general circulation model

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Marine geochemical data assimilation in an efficient Earth System Model of global biogeochemical cycling

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The carbon isotopic response of algae, (cyano)bacteria, archaea and higher plants to the late Cenomanian perturbation of the global carbon cycle: Insights from biomarkers in black shales from the Cape Verde Basin (DSDP Site 367)

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Uncertainties due to transport-parameter sensitivity in an efficient 3-D ocean-climate model

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Phosphorus and the roles of productivity and nutrient recycling during oceanic anoxic event 2

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Cenomanian–Turonian palaeoceanographic change on the Kerguelen Plateau: a comparison with Northern Hemisphere records

1 reference

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Increased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period

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20My of nitrogen fixation during deposition of mid-Cretaceous black shales on the Demerara Rise, equatorial Atlantic Ocean

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A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2

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Evolution of organic matter degradation in Cretaceous black shales inferred from authigenic barite: A reaction-transport model

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The Cenomanian/Turonian oceanic anoxic event in the South Atlantic: New insights from a geochemical study of DSDP Site 530A

1 reference

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Paleo-redox conditions during OAE 2 reflected in Demerara Rise sediment geochemistry (ODP Leg 207)

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Black shale deposition on the northwest African Shelf during the Cenomanian/Turonian oceanic anoxic event: Climate coupling and global organic carbon burial

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Carbon sequestration activated by a volcanic CO2 pulse during Ocean Anoxic Event 2

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A multiple proxy and model study of Cretaceous upper ocean temperatures and atmospheric CO2concentrations

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Tropical warming and intermittent cooling during the Cenomanian/Turonian oceanic anoxic event 2: Sea surface temperature records from the equatorial Atlantic

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GEOCHEMICAL CHARACTERIZATION OF CENOMANIAN/TURONIAN BLACK SHALES FROM THE TARFAYA BASIN (SW MOROCCO). RELATIONSHIPS BETWEEN PALAEOENVIRONMENTAL CONDITIONS AND EARLY SULPHURIZATION OF SEDIMENTARY ORGANIC MATTER1

1 reference

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7 January 2021

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Enhanced productivity led to increased organic carbon burial in the euxinic North Atlantic basin during the late Cenomanian oceanic anoxic event

1 reference

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7 January 2021

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N2-fixing cyanobacteria supplied nutrient N for Cretaceous oceanic anoxic events

1 reference

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Oceanic anoxic events and plankton evolution: Biotic response to tectonic forcing during the mid-Cretaceous

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New biostratigraphic data from the Cretaceous Bolinxiala Formation in Zanda, southwestern Tibet of China, and their paleogeographic and paleoceanographic implications

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Orbital time scale and new C-isotope record for Cenomanian-Turonian boundary stratotype

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The radiolarian assemblages of the Bonarelli Horizon in the Umbria-Marche Apennines and Southern Alps, Italy

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Molecular isotopic evidence of environmental and ecological changes across the Cenomanian–Turonian boundary in the Levant Platform of central Jordan

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Evidence for gammacerane as an indicator of water column stratification

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Cretaceous Planktonic Foraminifers from Sites 865, 866, and 869: A Synthesis of Cretaceous Pelagic Sedimentation in the Central Pacific Ocean Basin

1 reference

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Carbon-isotope stratigraphy recorded by the Cenomanian–Turonian Oceanic Anoxic Event: correlation and implications based on three key localities

1 reference

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Benthic phosphorus regeneration, net primary production, and ocean anoxia: A model of the coupled marine biogeochemical cycles of carbon and phosphorus

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based on heuristic

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Identifiers

10.1029/2012PA002351

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