http://alliance.la.asu.edu/dorn/Dorn_Ants_Geology2014_Online.pdf


The biotic enhancement of Ca-Mg silicate weathering has helped maintain Earth’s 
habit-
ability over geological time scales by assisting in the gradual drawdown of 
atmospheric CO2. 25 years of in-situ measurements of Ca-Mg silicate mineral 
dissolution by ants, termites, root mats, bare ground, and a control reveals 
ants to be one of the most powerful biotic weathering agents yet recognized. 
Six sites in Arizona and Texas (USA) indicate that eight different ant species 
enhance mineral dissolution by ~50×–300× over controls. A comparison of 
extracted soil at a 50 cm depth in ant colonies and adjacent bare ground shows 
a gradual accumulation of CaCO3 content for all eight ant species over 25 yr. 
Ants, thus, have potential to provide clues on how to enhance contemporary 
carbon sequestration efforts to transform Ca-Mg sili- cates and CO2 into 
carbonate. Given that ants underwent a great diversification and biomass 
expansion over the Cenozoic, a speculative implication of this research is that 
ant enhance- ment of Ca-Mg silicate dissolution
 might have been an influence on Cenozoic cooling.


How about an ant colony in every home to promote Anthropocene cooling? So much 
for $600/tonne CO2 DAC.

Greg

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