Remobilization of crustal carbon may dominate volcanic arc emissions.

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Volcanic ash as a driver of enhanced organic carbon burial in the Cretaceous.

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Q55079202-76268DBF-3184-4E29-AA7E-C2C736833323

P2860

Remobilization of crustal carbon may dominate volcanic arc emissions.

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2017 nî lūn-bûn

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Remobilization of crustal carbon may dominate volcanic arc emissions.

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Remobilization of crustal carbon may dominate volcanic arc emissions.

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Remobilization of crustal carbon may dominate volcanic arc emissions.

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P1476

Remobilization of crustal carbon may dominate volcanic arc emissions

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P2093

Emily Mason

http://www.w3.org/2001/XMLSchema#string

Marie Edmonds

http://www.w3.org/2001/XMLSchema#string

P2860

Reevaluating carbon fluxes in subduction zones, what goes down, mostly comes up

The carbon cycle and associated redox processes through time

Continental arc volcanism as the principal driver of icehouse-greenhouse variability.

Isotope fractionation and atmospheric oxygen: implications for phanerozoic O(2) evolution

A neoproterozoic snowball earth

The rise of oxygen over the past 205 million years and the evolution of large placental mammals.

Authigenic carbonate and the history of the global carbon cycle.

The fate of terrestrial organic carbon in the marine environment.

Metamorphic devolatilization of subducted marine sediments and the transport of volatiles into the Earth's mantle.

Transition of Mount Etna lavas from a mantle-plume to an island-arc magmatic source.

P304

290-294

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scholarly article

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10.1126/SCIENCE.AAN5049

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P407

English

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6348

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357

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P50

Alexandra V Turchyn

Marie Edmonds

Emily Mason

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2017-07-01T00:00:00Z

http://www.w3.org/2001/XMLSchema#dateTime

P698

28729507

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Remobilization of crustal carbon may dominate volcanic arc emissions.

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P2860

P2860

Remobilization of crustal carbon may dominate volcanic arc emissions.

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P1476

P2093

P2860

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P2093

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P698