Lower Cambrian cavity-dwelling endolithic (boring) sponges
- 1 May 1981
- journal article
- research article
- Published by Canadian Science Publishing in Canadian Journal of Earth Sciences
- Vol. 18 (5) , 972-980
- https://doi.org/10.1139/e81-093
Abstract
In the Lower Cambrian Forteau Formation (middle Bonnia–Olenellus zone) of southern Labrador, cavities in archaeocyath patch reefs contain preserved coelobiontic endolithic sponges. Scallops and carbonate chips produced by sponge boring, spicules, and preserved endolithic sponge body fossils all point to the presence of endolithic sponges in Lower Cambrian reef cavities.The oldest previously described endolithic sponges are Early Ordovician in age and the oldest previously known reef interior bioerosion is Middle Ordovician in age. The presence of endolithic sponges in reef cavities of the Forteau Formation therefore extends both the record of endolithic sponges and of reef interior bioerosion from the Ordovician to the upper Lower Cambrian.This publication has 8 references indexed in Scilit:
- Upper Ordovician (Richmondian) cavity-dwelling (coelobiontic) organisms from southern OntarioCanadian Journal of Earth Sciences, 1980
- Cavity‐dwelling organisms in Lower Cambrian patch reefs from southern LabradorLethaia, 1979
- Lower Cambrian patch reefs and associated sediments: southern Labrador, CanadaSedimentology, 1978
- Boring Microorganisms and Microborings in Carbonate SubstratesPublished by Springer Nature ,1975
- 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