[5] Elliott specialises in developing analytical approaches to yield novel isotopic means to reconstruct planetary histories.

[1] In particular, he has assessed elemental fluxes from descending plates and has highlighted how the rise of atmospheric oxygen has been remarkably recorded in the isotopic composition of the deep, solid Earth.

[1] His recent focus on planetary growth has identified the rapid formation of metallic cores, how bulk chemistry is notably modified during early accretion and distinctively embellished in its terminal stages.

[1] “All text published under the heading 'Biography' on Fellow profile pages is available under Creative Commons Attribution 4.0 International License.” --"Royal Society Terms, conditions and policies".

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