Plume-Induced Subduction Cases Where No Prior Lithospheric Plate Tectonics Represents One of the of the Earth’S Rigid Outer Shell Weaknesses Are Present

Plume-Induced Subduction Cases Where No Prior Lithospheric Plate Tectonics Represents One of the of the Earth’S Rigid Outer Shell Weaknesses Are Present

RESEARCH HIGHLIGHTS Nature Reviews Earth & Environment | https://doi.org/10.1038/s43017-020-0031-4 | Published online 13 February 2020 TECTONICS weakening and plume-induced density variations. Plume-driven subduction can even occur in Plume-induced subduction cases where no prior lithospheric Plate tectonics represents one of the of the Earth’s rigid outer shell weaknesses are present. However, key factors that separate the Earth (the lithosphere) remains poorly further numerical simulations from other planetary bodies in the constrained. demonstrate that pre-existing Solar System. Formation of new crust Marzieh Baes from GFZ German extensional stresses, and/or the at mid-ocean ridges, and recycling Research Center for Geosciences, presence of a high-temperature of this crust into the Earth’s mantle Germany, and colleagues, used plume ‘tail’ beneath the plume head, at subduction zones, are important 3-dimensional thermo-mechanical increase the likelihood of plate tectonic processes that control vital models to investigate the origin of subduction regardless of lithospheric geochemical cycles, thus maintaining subduction on present-day Earth. age or crustal thickness. Simulations the Earth’s climate and habitability They found that a high-temperature run with higher mantle temperatures over geological timescales. However, mantle plume impinging on the base and thicker crust also indicate that whilst the importance of plate of relatively young (<50 Myr) oceanic plume-driven subduction might be tecto nics is widely appreciated, the lithosphere may cause it to fracture feasible in the Archean (>2.5 Ga). mechanism that initiates subduction and subduct due to magmatic Verifying that plume presence may initiate subduction could explain the formation of several modern-day subduction zones (such as the Caribbean) and, impor- tantly, how the Earth transitioned from a stagnant-lid regime to a plate- tectonic regime during the Archean. Further modelling is required to assess the precise conditions that can lead to plume-induced subduction on the early Earth, and identify why plate-tectonics dominates on Earth yet is absent on Mars and Venus where mantle plumes are expected to be present. Matthew Gleeson ORIGINAL ARTICLE Baes, M. et al. Plume- induced subduction initiation: single- or multi- slab subduction? Geochem. Geophys. Geosyst. https://doi.org/10.1029/2019GC008663 (2020) Credit: MARK GARLICK/SCIENCE PHOTO LIBRARY/getty PHOTO GARLICK/SCIENCE MARK Credit: NATURE REVIEWS | EARTH & ENVIRONMENT VOLUME 1 | MARCH 2020 | 139.

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