Margaretta sp.

Zágoršek, Kamil & Gordon, Dennis P., 2013, Late Tortonian bryozoans from Mut Basin, Central Anatolian Plateau, southern Turkey, Acta Palaeontologica Polonica 58 (3), pp. 595-607 : 602

publication ID

https://doi.org/ 10.4202/app.2011.0100

persistent identifier

https://treatment.plazi.org/id/03D07132-FFBB-5357-323D-90A2FA38FD37

treatment provided by

Felipe

scientific name

Margaretta sp.
status

 

Margaretta sp.

Fig. 1F–J View Fig .

Referred material.—Altogether eight specimens were studied

(three of them illustrated ( Fig. 1F–H View Fig ) PM2−T1130 to PM2− T1132), mainly with highly developed secondary calcification. Description.—Colony columnar with branches of circular cross−section ( Fig. 1F View Fig ). Autozooecia arranged in 4–8 longitudinal rows, of indistinct shape owing to densely perforated slightly convex frontal wall ( Fig. 1F View Fig ). Secondary orifice circular to oval, no external peristome observed. Ascopore not observable from exterior. Ovicell deeply immersed, peristomial ( Fig. 1F View Fig ). Interior view shows regular small frontal pores ( Fig. 1G View Fig ) and median, circular, slightly larger ascopore ( Fig. 1G View Fig ); peristome consisting of 5–8 longitudinal bands separated by narrow, but distinct furrows ( Fig. 1G, H View Fig ). Ovicell not observed in interior view.

Remarks.— Margaretta cereoides ( Ellis and Solander, 1786) as described from the Miocene of Moravia by Zágoršek (2010b: 154, pl. 109: 1–4) does not have furrows in the peristomial wall fabric (visible in our Fig. 1J View Fig ), which may be considered a species−specific feature. However, a revision of the Margarettidae would be needed for a definite conclusion.

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