CaSiO3 perovskite in diamond indicates the recycling of oceanic crust into the lower mantle

Journal: Nature

Published: 2018-03-08

DOI: 10.1038/nature25972

Affiliations: 11

Authors: 11

Go to article

Research Highlight

Sparkling secrets from the Earth’s interior

© brainmaster/Getty

© brainmaster/Getty

Peering into a priceless diamond shines light on the inner workings of the Earth.

Calcium silicate perovskite is thought to be Earth’s fourth most abundant mineral, but it has never been observed in nature because it is unstable at the Earth’s surface.

A team that included University of Cape Town researchers have used X-ray and infrared imaging to peer inside a diamond found in the same South African mine as two of the British crown jewels. They discovered a pocket of calcium silicate perovskite preserved inside the diamond.

The mineral’s structure suggests it started out as oceanic crust, which gradually sank deep into the Earth until it reached the immense pressures required to form calcium silicate perovskite, which resurfaced millions of years later encased in a diamond.

This is the strongest evidence yet that oceanic crust, and hence surface carbon, is recycled deep within the Earth.

Supported content

  1. Nature 555, 237–241 (2018). doi: 10.1038/nature25972
Institutions FC
Department of Earth, Ocean and Atmospheric Sciences (EOS), UBC, Canada 0.14
Department of Geosciences, UNIPD, Italy 0.09
Department of Earth Sciences "Ardito Desio", UNIMI, Italy 0.09
Department of Earth and Atmospheric Sciences, U of A, Canada 0.09
UCL Department of Earth Sciences, United Kingdom (UK) 0.09
Department of Earth and Environmental Sciences, UNIPV, Italy 0.09
Institute of Geosciences and Earth Resources (IGG), CNR, Italy 0.09
University of Cape Town (UCT), South Africa 0.09
Rhodes University (RU), South Africa 0.09
SKA South Africa, South Africa 0.09
Institute of Precambrian Geology and Geochronology, RAS, Russia 0.05

Return