Abstract
The climatic and environmental impact of exclusively volcanic CO2 emissions is assessed during the main effusive phase of the Central Atlantic Magmatic Province (CAMP), which is synchronous with the end-Triassic mass extinction. CAMP volcanism occurred in brief and intense eruptive pulses each producing extensive basaltic lava flows. Here, CAMP volcanic CO2 injections into the surface system are modelled using a biogeochemical box model for the carbon cycle. Our modelling shows that, even if positive feedback phenomena may be invoked to explain the carbon isotope excursions preserved in end-Triassic sedimentary records, intense and pulsed volcanic activity alone may have caused repeated temperature increases and pH drops, up to 5 °C and about 0.2 log units respectively. Hence, rapid and massive volcanic CO2 emissions from CAMP, on a similar scale to current anthropogenic emissions, severely impacted on climate and environment at a global scale, leading to catastrophic biotic consequences.
Original language | English |
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Article number | 103731 |
Number of pages | 10 |
Journal | Global and Planetary Change |
Volume | 209 |
Early online date | 27 Dec 2021 |
DOIs | |
Publication status | Published - Feb 2022 |
Bibliographical note
Funding:This study was supported by the following collaborative research projects: NERC Large Grant NE/N018559/1 (United Kingdom) to Robert J. Newton and PRIN 20178LPCP (Italy) to Andrea Marzoli.
Keywords
- CO2
- Global warming
- Ocean acidification
- Mass extinction
- Large Igneous Provinces
- End-Triassic
- Biogeochemical modelling