“…In the Klettgau area and from there in a south-western direction to the Frick area (canton Aargau), the basal layers of the Beggingen Member contain iron-ooids (Figs. 7, 10; see Jordan 1983;Schlatter 1989). In contrast, the upper layers (Bucklandi to Obtusum zone) occur over a larger area in northern Switzerland and consist mainly of locally strongly phosphoritic arenitic limestone which are rich in fossils; the bivalve Gryphaea arcuata LAM.…”