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The mantle structure below petit-spot volcanoes
The compositional fingerprint of petit-spot magmas represents an enriched mantle source and carbonatitic or carbonated silicate melts below the oceanic lithosphere, suggests a synthesis of geochemical analyses on petit-spot volcanism.
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Influences on Antarctic Ice
The floating ice shelves around Antarctica are vulnerable to warming of the atmosphere as well as the ocean. Because they already float on the ocean, sea level is not directly affected if they are lost. Nevertheless, sea level can rise when they no longer hold back land-based ice on its journey to the ocean, and the ocean circulation is altered when large amounts of hitherto frozen freshwater melt. In this Collection we present articles that explore the mechanisms that determine where and when the Antarctic ice shelves may disintegrate.
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Transient variation in seismic wave speed points to fast fluid movement in the Earth's outer core
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Post-publication careers: follow-up expeditions reveal avalanches at Dyatlov Pass
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Lead removal at trace concentrations from water by inactive yeast cells
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Recent marine heatwaves in the North Pacific warming pool can be attributed to rising atmospheric levels of greenhouse gases