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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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The Arctic has warmed nearly four times faster than the globe since 1979
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Past megadroughts in central Europe were longer, more severe and less warm than modern droughts
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Rapid 20th century warming reverses 900-year cooling in the Gulf of Maine
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Influence and prediction value of Arctic sea ice for spring Eurasian extreme heat events