Rapid changes from arid to humid conditions during the onset of the Paraná-Etendeka Igneous Provinces: can volcanic gas emissions from Continental Flood Basalts affect the precipitation regime?
Posted on 09.07.2021 - 15:51
Despite the intriguing correlation between Continental Flood Basalt (CFB) provinces and environmental crises, little is known about how the local/regional sedimentary systems and environment respond to flood basalt volcanism. Active sedimentary systems, and their interaction with volcanism, provide an important rock record to understand palaeoenvironments in volcanic settings. The Paraná-Etendeka Igneous Province is a well-known example of a CFB emplaced on a dry desert environment, but evidence has also shown the existence of humid conditions during the volcanic episode. This work describes and interprets non-volcanic sedimentary and volcaniclastic rocks interbedded with Paraná-Etendeka Igneous Province lavas in southernmost Brazil to better understand palaeoenvironmental process and changes during the onset of volcanism. Non-volcanic sedimentary rocks record the existence of ephemeral sheet-like flows and ponds/lakes while volcaniclastic rocks document hydromagmatic activity, supporting a change to more humid conditions. Stratigraphic constraints indicate that this change started with the onset of volcanism and affected the whole province. We suggest that SO2 degassing from the Paraná-Etendeka province may have caused a net global surface cooling, resulting in precipitation redistribution and a local increase in rainfall. This hypothesis may help in explaining the cooling and increased humidity that is observed elsewhere to be closely related with the Paraná-Etendeka emplacement.
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Cruz, V.G.P.; Lima, E.F.; Rossetti, L.M.M.; Pasqualon, N.G. (2021): Rapid changes from arid to humid conditions during the onset of the Paraná-Etendeka Igneous Provinces: can volcanic gas emissions from Continental Flood Basalts affect the precipitation regime?. Geological Society of London. Collection. https://doi.org/10.6084/m9.figshare.c.5505710.v1
Paran á-Etendeka Igneous Provincesdesert environment2 degassingParan á-Etendeka provincerock recordStratigraphic constraintsParan á-Etendeka Igneous Province lavaspalaeoenvironmental processParan á-Etendeka Igneous ProvinceRapid changesrocks recordParan á-Etendeka emplacementvolcaniclastic rocks interbeddedContinental Flood Basaltsprecipitation redistributionflood basalt volcanismvolcaniclastic rocks document hydro...CFB emplacedprecipitation regimeContinental Flood Basaltsurface coolingonsetsheet-like flowsgas emissions