Bryozoan–serpulid–algal–thrombolite bioherms of up to 50 cm size are described from the
Sarmatian (upper Middle Miocene) of the Central Paratethys. They occur on top of lower …

Trepostome bryozoans, with their thick calcitic skeletons, formed the largest number of
symbiotic associations with endobionts in the Phanerozoic. Such associations were also …

Background Placentation has evolved multiple times among both chordates and
invertebrates. Although they are structurally less complex, invertebrate placentae are much …

Ctenostome bryozoans are a small group of bryozoans whose soft‐tissue morphology has
received only little attention. The present study represents the third in a series of articles …

Trepostome bryozoan skeletalisation did not passively respond to changes in seawater
chemistry associated with calcite-aragonite seas. According to Stanley and others …

The post-impact fauna of the Dalby Limestone of Tvären Bay has been extensively
examined, with the exception of the Palaeostomate bryozoan taxa present. Here, we report …

Sessile epibenthos were diverse and played important part in the process of energy flow in
the Cambrian marine ecosystem. Based on new specimens from the Gaoloufang Section of …

Bryostromatolites are found in stressed environments from the Paleozoic to the Recent. They
are formed by alternating layers of bryozoans and microbes. This study investigates recent …

Calcitic skeletons of trepostome bryozoans from the Upper Ordovician (Katian) of the
Cincinnati region (Kentucky and Indiana, USA) record diverse interactions with encrusting …

Sclerobionts are organisms that encrust onto or bore into a hard substrate. They are
valuable sources of palaeoecological data as they often preserve the skeletonized portion of …