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Carbonate Mineralization Related to Weathering of Mafic and Ultramafic Rocks in the Pali Aike Volcanic Field, Extra-Andean Patagonia, Chile

On geological timescales, the volume of CO2 in the atmosphere is influenced by processes such as silicate weathering. In particular, the weathering of basaltic rocks increase the availability of divalent cations such as Mg2+ and Ca2+ in natural waters enabling carbonate formation under atmospheric conditions.
Carolina Henriquez   +4 more
openaire   +1 more source

The role of physicochemical and biochemical processes on carbonate precipitation within the Laguna Timone maar in the Pali Aike Volcanic Field, southernmost extra-Andean Patagonia

Sedimentary Geology, 2022
Carolina Henríquez   +6 more
openaire   +1 more source

Linked canopy, climate, and faunal change in the Cenozoic of Patagonia

Science, 2015
Regan E Dunn   +2 more
exaly  

High Plant Diversity in Eocene South America: Evidence from Patagonia

Science, 2003
Peter Wilf, Kirk R Johnson, Scott L Wing
exaly  

Techno-economic analysis of a potential energy trading link between Patagonia and Japan based on CO2 free hydrogen

International Journal of Hydrogen Energy, 2019
David Severin Ryberg   +2 more
exaly  

Southern Annular Mode-like changes in southwestern Patagonia at centennial timescales over the last three millennia

Nature Communications, 2014
Patricio I Moreno   +2 more
exaly  

Ancient genomes in South Patagonia reveal population movements associated with technological shifts and geography

Nature Communications, 2020
Nathan Nakatsuka   +2 more
exaly  

Gondwanide continental collision and the origin of Patagonia

Earth-Science Reviews, 2006
Christopher Mark Fanning
exaly  

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