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Reply to ‘Unfeasible subduction?’

David Rowley
Miquela Ingalls
Correspondence01 Dec 2017
Nature Geoscience

Volume: 10, P: 879-880
Large-scale subduction of continental crust implied by India–Asia mass-balance calculation

Buoyant continental crust is thought to resist subduction. Calculation of the crustal mass balance during the collision between India and Eurasia indicates that about 50% of pre-collisional continental crust has been subducted into the mantle.

Miquela Ingalls
David B. Rowley
Albert S. Colman
Research19 Sept 2016
Nature Geoscience

Volume: 9, P: 848-853
Addendum: Large-scale subduction of continental crust implied by India–Asia mass-balance calculation

Miquela Ingalls
David B. Rowley
Albert S. Colman
Amendments and Corrections02 May 2017
Nature Geoscience

Volume: 10, P: 393
Millennial-timescale thermogenic CO₂ release preceding the Paleocene-Eocene Thermal Maximum

A short-lived carbon release preceded the PETM. Here the global nature of this is confirmed, effects on the surface ocean carbon cycle are resolved, and a thermogenic CO₂ source is inferred.

Shijun Jiang
Ying Cui
Andy Ridgwell
ResearchOpen Access30 Jun 2025
Nature Communications

Volume: 16, P: 1-12

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Reply to ‘Unfeasible subduction?’

Large-scale subduction of continental crust implied by India–Asia mass-balance calculation

Addendum: Large-scale subduction of continental crust implied by India–Asia mass-balance calculation

Millennial-timescale thermogenic CO2 release preceding the Paleocene-Eocene Thermal Maximum

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Millennial-timescale thermogenic CO₂ release preceding the Paleocene-Eocene Thermal Maximum