Middle Ordovician (Chazy Group) cavity-dwelling boring sponges
- 1 June 1981
- journal article
- research article
- Published by Canadian Science Publishing in Canadian Journal of Earth Sciences
- Vol. 18 (6) , 1101-1108
- https://doi.org/10.1139/e81-105
Abstract
Microcavities in lower Middle Ordovician bryozoan mounds from the Laval Formation (Chazy Group) near Montreal, Quebec [Canada] contain evidence that endolithic (boring) sponges were present. Ramose borings with scalloped walls and swellings resembling endolithic sponge galleries, faceted carbonate grains similar to modern sponge chips and siliceous spicules both in situ on the cavity wall or roof and in the sediment, all point to the activities of endolithic sponges in the hard substrate of the wall and roof. Coelobiontic (cavity-dwelling) endolithic sponges infested cavities in skeletal mounds and reefs in the Middle Ordovician and appear to have exploited the cavity habitat very soon after the appearance of metazoan skeletal reefs in the Ordovician.This publication has 8 references indexed in Scilit:
- Lower Cambrian cavity-dwelling endolithic (boring) spongesCanadian Journal of Earth Sciences, 1981
- Cavity-dwelling biota in Middle Ordovician (Chazy) bryozoan mounds from QuebecCanadian Journal of Earth Sciences, 1981
- Upper Ordovician (Richmondian) cavity-dwelling (coelobiontic) organisms from southern OntarioCanadian Journal of Earth Sciences, 1980
- Lower Cambrian patch reefs and associated sediments: southern Labrador, CanadaSedimentology, 1978
- Borings As Trace Fossils, and the Processes of Marine BioerosionPublished by Springer Nature ,1975
- Growth and submarine fossilization of algal cup reefs, Bermuda*Sedimentology, 1973
- Ferromanganese nodules from the devonian of the montagne noire (S. France) and West GermanyInternational Journal of Earth Sciences, 1973
- OBSERVATIONS ON COASTAL EROSION IN BERMUDA AND MEASUREMENTS OF THE BORING RATE OF THE SPONGE, CLIONA LAMPA1,2Limnology and Oceanography, 1966