Triassic inferno: Fires raged across Europe for millennia during past global warming. The end-Triassic mass extinction, 201 million years ago, is linked to volcanism that resulted from the break-up of Pangea and which pumped out vast amounts of CO2 into the atmosphere, causing extreme global warming of 5 to 10 degrees Celsius.
A apuração publicada por phys.org vira base para uma leitura editorial direta e contextualizada.
Trechos de apoio da pauta: The end-Triassic mass extinction, 201 million years ago, is linked to volcanism that resulted from the break-up of Pangea and which pumped out vast amounts of CO2 into the atmosphere, causing extreme global warming of 5 to 10 degrees Celsius. As a result, tree-dominated vegetation collapsed and the highly disturbed landscapes were colonized by ferns that formed savannahs across large swaths of what is now Northwest Europe.
- Ponto de atenção: triassic.
- Ponto de atenção: inferno.
- Ponto de atenção: fires.
Em resumo, a leitura editorial acompanha o impacto do tema no nicho Agro. Quando fizer sentido, a referência complementar pode ser acessada em agronegócio.
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