Constraining the volatile content of magmas is critical to our understanding of eruptive
processes and their deep Earth cycling essential to planetary habitability [R. Dasgupta, MM …

Abstract Upper Cretaceous–Miocene alkaline SiO2-undersaturated volcanic rocks in the
southern Central European Volcanic Province (CEVP) comprise two distinct rock series:(i) …

Determining the evolutionary history of mantle oxygen fugacity (f o2) is crucial, as it controls
the f o2 of mantle-derived melts and regulates atmospheric composition through volcanic …

The convecting mantle is the Earth's largest carbon reservoir that controls the carbon outflux
from the interior to surface, but its carbon content remains largely uncertain due to limited …

A number of possible hypotheses have been proposed to explain the origin of mid-
lithospheric discontinuities (MLDs), typically characterized by∼ 2-6% reductions in seismic …

The goal of this study is to constrain the origins of layering in the seismic velocity structure
within the cratonic mantle lithosphere (ie mid‐lithospheric discontinuities [MLDs]). For long …

The nuclei of continents, manifested as cratons, are the most long-lived parts of Earth's
lithosphere. However, ancient cratons in some areas can be substantially destroyed through …

Some of the most CO 2-rich magmas on Earth are erupted by intraplate ocean island
volcanoes. Here, we characterise olivine-hosted melt inclusions from recent (< 10 ky) …

Recent advances indicate that the amount of carbon released by gradual degassing from
the mantle needs to be revised upwards, whereas the carbon supplied by plumes may have …

The evolution of Earth's atmospheric O 2 levels on long timescales is modulated in part by
the composition of magmatic gases, specifically their oxidation state and speciation. Here …