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Research Highlights Reviews & Environment | https://doi.org/10.1038/s43017-020-0031-4 | Published online 13 February 2020

TECTONICS weakening and plume-induced density variations. Plume-driven can even occur in Plume-induced subduction cases where no prior lithospheric represents one of the of the Earth’s rigid outer shell weaknesses are present. However, key factors that separate the Earth (the ) 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 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 tecto­nics 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 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- 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