Estimating the impact of the cryptic degassing of Large Igneous Provinces: A mid-Miocene case-study

•We estimate the range of cryptic degassing possible from the Columbia River Basalt.•We model the carbon emissions necessary to match the palaeorecords around 16.0 Ma.•We find additional cryptic degassing can explain some mid-Miocene climate change.•Other climate drivers are required before and after the Columbia River Basalt.•We propose that cryptic degassing also amplified the emissions of other LIPs.

Large Igneous Provinces (LIPs) have been emplaced throughout Earth's history, erupting great quantities (>104 km3) of lava in long-lived (>105 y) events that have been linked to major environmental disruptions. The largest LIP eruptions (e.g. Siberian Traps) are widely considered to have had an impact on global climate through basalt CO2 degassing but the impact of the more numerous smaller LIPs is debated. Here we test the hypothesis that LIPs had a greater impact on Earth's climate history than previously estimated because of the 'cryptic degassing' of intruded and crust-contaminated magma, injecting extra CO2 over and above that coming from sub-aerial basalts. We use biogeochemical box models to investigate the potential impact of the Columbia River Basalts (CRB) during the mid-Miocene where multiple palaeorecords for this geologically relatively recent event enable more rigorous data-model comparison. We find that the effect on the long-term carbon cycle of basalt degassing from the CRB alone is negligible, but that a total CRB emission of 4090-5670 Pg of carbon with 3000-4000 Pg of this carbon emitted during the Grande Ronde Basalt eruptions, a flux within the acceptable estimated range when cryptic degassing is included, does well in reproducing the record of benthic δ13C and atmospheric CO2 change during the core of the Miocene Climatic Optimum. Nevertheless, mechanisms other than degassing are required to drive observed warmth before 16.3 Ma and to match observed calcite compensation depth behaviour after ∼15.4 Ma. Hence, our findings rule out the possibility that CRB emplacement alone can fully explain the mid-Miocene record but they demonstrate the enhanced climate impact that occurs when substantial cryptic degassing accompanies LIP emplacement.