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Department of Earth and Planetary Sciences, Harvard University, 20 Oxford St., Cambridge, MA 02138, USA
Department of Earth and Planetary Sciences, Harvard University, 20 Oxford St., Cambridge, MA, 02138, USA
A dynamic magnesium cycle during the Cenozoic? Insights from the magnesium isotopic composition of pelagic carbonates
Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous?
Beyond methane: Towards a theory for the Paleocene-Eocene Thermal Maximum
Magnesium isotope profiles in deep-sea sediments
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