Clay Mineral Assemblages in Flysch from the Campo de Gibraltar Area (Spain)

Following the latest Permian extinction ∼252 million years ago, normal marine and terrestrial ecosystems did not recover for another 5-9 million years. The driver(s) for the Early Triassic biotic crisis, marked by high atmospheric CO2 concentration, extreme ocean warming, and marine anoxia, remains unclear. Here we constrain the timing of authigenic K-bearing mineral formation extracted from supergene weathering profiles of NW-Pangea by Argon geochronology, to demonstrate that an accelerated hydrological cycle causing intense chemical alteration of the continents occurred between ∼254 and 248 Ma, and continued throughout the Triassic period. We show that enhanced ocean nutrient supply from this intense continental weathering did not trigger increased ocean productivity during the Early Triassic biotic crisis, due to strong thermal ocean stratification off NW Pangea. Nitrogen isotope constraints suggest, instead, that full recovery from ocean nutrient stress, despite some brief amelioration ∼1.5 million years after the latest Permian extinction, did not commence until climate cooling revitalized the global upwelling systems and ocean mixing ∼10 million years after the mass extinction.

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Clay Mineral Assemblages in Flysch from the Campo de Gibraltar Area (Spain)

Cited by 4 publications

References 19 publications

Swelling damage in clay-rich sandstones used in the church of San Mateo in Tarifa (Spain)

Swelling damage in clay-rich sandstones used in the church of San Mateo in Tarifa (Spain)

Chapter 14 Genesis of Clay Minerals

Continental weathering and recovery from ocean nutrient stress during the Early Triassic Biotic Crisis

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