Atmospheric carbon dioxide concentrations and climate are regulated on geological timescales by the balance between carbon input from volcanic and metamorphic outgassing and its removal by weathering feedbacks; these feedbacks involve the erosion of silicate rocks and organic-carbon-bearing rocks. The integrated effect of these processes is reflected in the calcium carbonate compensation depth, which is the oceanic depth at which calcium carbonate is dissolved.
Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/cenozoic-record-equatorial-pacific-carbonate-compensation-depth
[2] http://admin.indiaenvironmentportal.org.in/category/author/heiko-p%C3%A4
[3] http://admin.indiaenvironmentportal.org.in/category/author/mitchell-w-lyle
[4] http://admin.indiaenvironmentportal.org.in/category/author/hiroshi-nishi-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/journal/nature
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/oceans-and-seas
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/sediment-transport
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/carbon-dioxide
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/north-pacific-ocean