Madison East
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View article: Decoupling Carbon and Calcification in Tropical Scleractinian Corals
Decoupling Carbon and Calcification in Tropical Scleractinian Corals Open
Coral calcification is known to depend on ocean pH, saturation state (Ω Arag ) and carbonate ion concentration [CO 32-].These
View article: The Influence of Carbonate Platforms on the Geomorphological Development of a Mixed Carbonate‐Siliciclastic Margin (Great Barrier Reef, Australia)
The Influence of Carbonate Platforms on the Geomorphological Development of a Mixed Carbonate‐Siliciclastic Margin (Great Barrier Reef, Australia) Open
Sedimentation regimes on the Great Barrier Reef margin often do not conform to more conventional sequence stratigraphic models, presenting difficulties when attempting to identify key processes that control the margin's geomorphological ev…
View article: Deep Carbon Cycling Over the Past 200 Million Years: A Review of Fluxes in Different Tectonic Settings
Deep Carbon Cycling Over the Past 200 Million Years: A Review of Fluxes in Different Tectonic Settings Open
Carbon is a key control on the surface chemistry and climate of Earth. Significant volumes of carbon are input to the oceans and atmosphere from deep Earth in the form of degassed CO2 and are returned to large carbon reservoirs in the mant…
View article: Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events: scripts and data
Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events: scripts and data Open
The files provided here supplement the following article which has been conditionally accepted to Gondwana Research: 'Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswel…
View article: Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events: scripts and data
Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events: scripts and data Open
The files provided here supplement the following article which has been conditionally accepted to Gondwana Research: 'Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswel…
View article: Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events
Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events Open
Subduction is a fundamental mechanism of material exchange between the planetary interior and the surface. Despite its significance, our current understanding of fluctuating subducting plate area and slab volume flux has been limited to a …