Tracking the relationship between mountain uplift, silicate weathering, and long-term CO2 consumption with Ca isotopes: Southern Alps, New Zealand

Overview of attention for article published in Chemical Geology, March 2013

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Whether rapid upliftment of Greenland during Holocene - https://t.co/5Dh7YCseR8 - has resulted in the rapid erosion of carbonates as observed in the Southern Alps, New Zealand - https://t.co/oJaYFlLyvK

If silicate weathering is not responsible for long-term #Cenozoic cooling https://t.co/vgLL7lgyF6 then 1) rapid uplift of the mountains largely resulted in #carbonate #weathering, 2) and that has no influence on #alkalinity and #CO2 uptake of the oceans…

The Ca/Na and Ca/Mg is used to demarcate the regions of carbonate and silicate weathering (https://t.co/vgLL7lgyF6 and https://t.co/9heWLOJBuJ). During weathering of marine shales, Na replaces Ca and Mg https://t.co/KaRu8ScuT9. Thus, use of Ca/Na and C…

Whether enhanced carbonate weathering during rapid continental uplift https://t.co/vgLL7lgyF6 is responsible for extensive Cenozoic carbonate platforms in South East Asia - https://t.co/CGPIcJcJfk - especially around Borneo? - https://t.co/4JxNltaCUL

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