Discovery of davemaoite, CaSiO 3 -perovskite, as a mineral from the lower mantle

Author:

Tschauner Oliver1ORCID,Huang Shichun1ORCID,Yang Shuying2ORCID,Humayun Munir2ORCID,Liu Wenjun3,Gilbert Corder Stephanie N4ORCID,Bechtel Hans A.4ORCID,Tischler Jon3ORCID,Rossman George R.5ORCID

Affiliation:

1. Department of Geoscience, University of Nevada, Las Vegas, NV 89154, USA.

2. National High Magnetic Field Laboratory and Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL 32310, USA.

3. Advanced Photon Source, Argonne National Laboratory, Lemont, IL 60439, USA.

4. Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA.

5. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91105, USA.

Abstract

Lower mantle “garbage can” Calcium silicate perovskite has finally been identified in a natural sample and now has the mineral name davemaoite. Tschauner et al . discovered the type mineral trapped at high pressure and temperature as a diamond inclusion (see the Perspective by Fei). Structural and chemical analysis of the mineral showed that it is able to host a wide variety of elements, not unlike fitting bulky objects into garbage can. Specifically, it has a large amount of trapped potassium. Davemaoite can thus host three of the major heat-producing elements (uranium and thorium were previously shown experimentally) affecting heat generation in Earth’s lower mantle. —BG

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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