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. 2017 Feb 10;17(6):605–612. doi: 10.1002/elsc.201600183

Figure 3.

Figure 3

Thermogravimetric analysis of coccoliths. The decrease of weight (%) between 200°C and 600°C derives from the combustion of organic material (–5.0%). The decrease of weight (%) between 600°C and 780°C derives from the decomposition of CaCO3 (–39.7%).