By Moyano, Hugo
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Additional resources for Bryozoan Studies 2004: Proceedings of the 13th International Bryozoology Association conference, Concepción/Chile, 11-16 January 2004
J. F. Rawson (eds), Biotic response to global change. The last 145 million years: 195–206. Cambridge: The Natural History Museum and Cambridge University Press. qxd 04/01/2005 14:44 PM Page 25 Bryozoan Studies 2004 – Moyano, Cancino & Wyse Jackson (eds) © 2005 Taylor & Francis Group, London, ISBN 04 1537 293 3 Bryozoa of the Romaine and Mingan Formations (Lower and Middle Ordovician) of the Mingan Islands, Quebec, Canada Thomas E. Bolton (deceased) Geological Survey of Canada, Ottawa, Ontario, Canada Roger J.
Transverse and longitudinal sections; GSC 94780, 94779, ϫ32 and x16; GSC locality 96735, Île du Fantôme. 5, 8, 9: Phylloporina incepta (Hall). 4; GSC locality 96726, Île du Fantôme. 8: Weathered surface of a reticulate branching zoarium displaying both oval zooecial openings and long zooecial tubes; GSC 94768, ϫ8; same locality as Fig. 1. 9: Tangential peel displaying 3 to 4 rows of oval zooecia on reticulate branches and long zooecial tubes; GSC 94772, ϫ16; Desrochers’ locality 399A, Île du Fantôme.
1991), our data supports the assumption that the westward outflow of Mediterranean surface water, carrying bryozoan larvae into the Guadalquivir Basin, occurred through the Spanish corridors (Figure 2). Due to the exchange of species, and in contrast to the modern situation, a clear distinction between a late Tortonian eastern Atlantic and western Mediterranean shallow water bioprovince can thus not be made. The presence of numerous Mediterranean species on the Atlantic side of the corridors furthermore shows that, prior to the beginning of the MSC, environmental conditions in this region were sufficiently similar to the Mediterranean Sea.