Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering
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DOI: 10.1038/ngeo2931
Abstract: The onset of the late Palaeozoic ice age about 340 million years ago has been attributed to a decrease in atmospheric CO2 concentrations associated with expansion of land plants, as plants both enhance silicate rock… read more here.
Keywords: palaeozoic ice; late palaeozoic; palaeozoic; ice age ... See more keywords