Bryozoan Studies 2004 : Proceedings of the 13th by G. Hugo I. Moyano, Juan M. Cancino, Patrick M. Wyse Jackson

By G. Hugo I. Moyano, Juan M. Cancino, Patrick M. Wyse Jackson

A variety of papers provided on the thirteenth overseas convention of the overseas Bryozoology organization held in Concepci?n Chile in January 2004 and hosted via the Universidad de Concepci?n and Universidad Cat?lica de los angeles Sant?sima Concepci?n. the themes provided during this quantity mirror the range of reports on bryozoa with authors from 18 nations. They contain investigations in seven thematic components: ecology and existence ideas; contemporary and fossil faunas of Australia and New Zealand; prior and current bryozoans from either Antarctic and Arctic seas; geology and palaeontology of bryozoans from Eurasia and North the US; clean water bryozoans around the globe; fossil bryozoans of the Mediterranean and Tethyan geographical regions and evolution and variety of contemporary species. This quantity represents the latest advances made in bryozoological reviews over the last 3 years, and makes an important contribution to the literature.

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In well-oriented tangential sections, zooecial apertures tend toward diamond-shaped, with their walls locally arranged in a distinctly rhombic grid. In many zooecia, proximal walls are slightly thickened (lunarium, which does not project much above the colony surface), and in a few the proximal zooecial angle is somewhat rounded. Local small interruptions in a few zooecial walls may represent occasional interzooecial or communication pores (but could instead be diagenetic defects). Neither exilazooecia nor acanthorods are developed.

Tangential section displaying diamond-shaped zooecia; holotype, GSC 94757, ϫ32; Desrochers’ locality 369B, Île du Fantôme; (also see Fig. 3 (2)). 6–8. Phylloporina incepta (Hall). Surfaces of reticulate branches sufficiently weathered in places to display both aligned oval zooecial openings and long zooecial tubes; GSC 94765, 94766, ϫ4 and x8; GSC locality 95785, Île Nue de Mingan; and GSC 94767, ϫ4; GSC locality 96732, Île à Calculot. qxd 04/01/2005 14:44 PM Page 35 Figure 7. Bryozoa, Mingan Formation.

The Appendix at the end of this paper gives details of the exact collecting localities (also see Fig. 1). In the systematic descriptions and figure captions, only the locality number and its island name are given, to avoid unnecessary repetition. 2 Bioherms and biostromes The upper limestones, the Mingan Formation, contain a number of reefs or build-ups, some mounded bioherms, others tabular biostromes (Desrochers & James 1989). These were constructed in part by bryozoans, accompanied by tabulate corals, lithistid sponges, and solenoporacean algae.

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