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. 2018 May 25;9:997. doi: 10.3389/fmicb.2018.00997

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Copyright © 2018 Kraus, Beeler, Mors, Floyd, GeoBiology 2016, Stamps, Nunn, Stevenson, Johnson, Shapiro, Loyd, Spear and Corsetti.

This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

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Model results for the evolution of calcite saturation state (Ω) and δ¹³C_DIC for degassing of LHC waters. The measured isotopic values from the precipitates (δ¹³C_CARB) occur at the greatest slope in the modeled increase of calcite saturation state.