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Van Schöll, L., Kuyper, Th.W., Smits, M.M., Landeweert, R., Hoffland, E. and Van Bremen, N. (2008) Rock-Eating Mycorrhizas: Their Role in Plant Nutrition and Biogeochemical Cycles. Plant and Soil, 303, 35-47.
https://doi.org/10.1007/s11104-007-9513-0

has been cited by the following article:

• TITLE: Olivine Weathering against Climate Change

  AUTHORS: Roelof Dirk Schuiling

  KEYWORDS: Climatic Change, Olivine, Rate of Weathering, Biotic Effects

  JOURNAL NAME: Natural Science, Vol.9 No.1, January 17, 2017

  ABSTRACT: One natural process has since the origin of the Earth removed almost all the CO2 that was ever produced by volcanism. That process is the reaction of CO2 and water with rocks, a process known as weathering. It is a logical choice to see if we can use the same process to remove also the vastly higher CO2 emissions caused by burning in a few hundred years the fossil fuels that have taken hundreds of millions of years for their formation. Many people claim that the rate of weathering of olivine is too slow to counter climate change, but they base this on experimental data in sterile laboratories, under exclusion of biotic and other environmental factors. As many conditions determine the weathering rate at each specific location, these laboratory conditions are irrelevant for the real world. Weathering models based on these laboratory data are off by orders of magnitude. Weathering experiments that use conditions closer to nature [1] show already much higher weathering rates. In this note I provide some data on the weathering of olivine in nature, which make clear that the weathering of olivine is fast enough to play an important role in the cycle of CO2 capture and its safe and sustainable storage as carbonate rocks. The CO2 released by volcanism has always been captured by the weathering of rocks since the origin of the Earth. Without this mechanism the Earth would be a lifeless planet with a CO2 atmosphere in the order of 100 bar, as our neighbor planet Venus demonstrates.