Climate-driven compositional modifications of arc volcanoes along the East Equatorial Pacific Margin — The magmatic response to a cooling planet

Nota bibliográfica

Funding Information:
This work is part of C. Errázuriz-Henao Ph.D dissertation thesis supported by Consejo Nacional de Ciencias y Tecnología (CONACyT, Mexico) . We are grateful to Ofelia Pérez-Arvizu, Liliana Corona and Manuel Albarrán, for their assistance during sample preparation and analysis; and to Carolina Henao for drafting Fig. 11. We acknowledge the use of imagery from the Ocean Biology Processing Group (OBPG) ( https://wvs.earthdata.nasa.gov ), part of the Earth Observing System Data and Information System (EOSDIS). We thank the Lamont-Doherty Earth Observatory Core Repository (New York, USA) and the International Ocean Discovery Program Gulf Coast Repository (Texas, USA) for kindly providing deep-sea sediment samples from the Mexican margin. The manuscript benefited greatly from the careful reviews of Maarten de Moor and an anonymous reviewer. Editorial handling by Christina Yan Wang is highly appreciated. This work was partially supported by CONACyT grant 239494 to A. Gómez-Tuena.

Funding Information:
This work is part of C. Errázuriz-Henao Ph.D dissertation thesis supported by Consejo Nacional de Ciencias y Tecnología (CONACyT, Mexico). We are grateful to Ofelia Pérez-Arvizu, Liliana Corona and Manuel Albarrán, for their assistance during sample preparation and analysis; and to Carolina Henao for drafting Fig. 11. We acknowledge the use of imagery from the Ocean Biology Processing Group (OBPG) (https://wvs.earthdata.nasa.gov), part of the Earth Observing System Data and Information System (EOSDIS). We thank the Lamont-Doherty Earth Observatory Core Repository (New York, USA) and the International Ocean Discovery Program Gulf Coast Repository (Texas, USA) for kindly providing deep-sea sediment samples from the Mexican margin. The manuscript benefited greatly from the careful reviews of Maarten de Moor and an anonymous reviewer. Editorial handling by Christina Yan Wang is highly appreciated. This work was partially supported by CONACyT grant 239494 to A. Gómez-Tuena.

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