The Glanderud section has been studied for quantitative changes in agglutinated benthic foraminifera.Twenty-five species were recognized in the uppermost Maastrichtian Marl and in the K-P boundary clay layer. Three types ...

High resolution sampling across the Cretaceous/Paleogene boundary (K/Pg) at the Galanderud section in northern Iran provides the most expanded and continuous section for us to consider biostratigraphy and the mass extinction pattern of Cretaceous...