Shells of small (micromorphic)
brachiopods are not so attractive as other fossils preserved in the white
chalk facies, for instance the
belemnite rostra or
echinoid tests. Despite this, they are important for the Late
Cretaceous stratigraphy and palaeoecology. We describe brachiopods from the Maastrichtian chalk at
Chełm, eastern Poland. The studied assemblage is dominated by small forms and allows for precise
dating of the succession and determination of its
depositional environment.
Figure: location of the Chełm site, an example of a micromorphic brachiopod shell (Terebratulina longicollis), and the chalk succession with ranges of identified taxa.