View of Benthic foraminifera from the Lower Jurassic transgressive mudstones of the south-western Barents Sea - a possible high-latitude expression of the global Pliensbachian-Toarcian turnover?

Return to Article Details Benthic foraminifera from the Lower Jurassic transgressive mudstones of the south-western Barents Sea - a possible high-latitude expression of the global Pliensbachian-Toarcian turnover? Download Download PDF