Aspects of bioerosion of modern Caribbean reefs
Boring organisms are ubiquitous and destructive on modern reefs, and have an extensive fossil record. In modern reefs, representatives of at least eight different phyla are capable of boring into the reef framework. Cellular-grade Monera (bacteria) and tissue-grade Protista (algae and fungí) erode v...
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Universidad de Costa Rica
1978
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RBT607862024-07-01T19:41:23Z Aspects of bioerosion of modern Caribbean reefs Aspects of bioerosion of modern Caribbean reefs Risk, Michael J. MacGeachy, Kirk No reporta No reporta Boring organisms are ubiquitous and destructive on modern reefs, and have an extensive fossil record. In modern reefs, representatives of at least eight different phyla are capable of boring into the reef framework. Cellular-grade Monera (bacteria) and tissue-grade Protista (algae and fungí) erode via chemical secretions. Tissue-grade Metazoa (the sponges) use a unique combination of chemical weakening combined with physical removal. Organ-grade Metazoa (polychaetes, bivalves, barnacles, crustaceans, sipunculids) employ a variety of techniques, ranging from the chemicalIy-assisted physical to the purely physical. Boring organisms are ubiquitous and destructive on modern reefs, and have an extensive fossil record. In modern reefs, representatives of at least eight different phyla are capable of boring into the reef framework. Cellular-grade Monera (bacteria) and tissue-grade Protista (algae and fungí) erode via chemical secretions. Tissue-grade Metazoa (the sponges) use a unique combination of chemical weakening combined with physical removal. Organ-grade Metazoa (polychaetes, bivalves, barnacles, crustaceans, sipunculids) employ a variety of techniques, ranging from the chemicalIy-assisted physical to the purely physical. Universidad de Costa Rica 1978-11-01 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion https://revistas.ucr.ac.cr/index.php/rbt/article/view/60786 Revista de Biología Tropical; Vol. 26 No. S1 (1978): SIMPOSIO SOBRE CIENCIAS MARINAS EN LAS AMERICAS; 85-105 Revista de Biología Tropical; Vol. 26 Núm. S1 (1978): SIMPOSIO SOBRE CIENCIAS MARINAS EN LAS AMERICAS; 85-105 Revista Biología Tropical; Vol. 26 N.º S1 (1978): SIMPOSIO SOBRE CIENCIAS MARINAS EN LAS AMERICAS; 85-105 2215-2075 0034-7744 10.15517/rev.biol.trop..v26iS1.1978 http://creativecommons.org/licenses/by/4.0 |
institution |
Universidad de Costa Rica |
collection |
Revista de Biología Tropical |
format |
Online |
author |
Risk, Michael J. MacGeachy, Kirk |
spellingShingle |
Risk, Michael J. MacGeachy, Kirk Aspects of bioerosion of modern Caribbean reefs |
author_facet |
Risk, Michael J. MacGeachy, Kirk |
author_sort |
Risk, Michael J. |
description |
Boring organisms are ubiquitous and destructive on modern reefs, and have an extensive fossil record. In modern reefs, representatives of at least eight different phyla are capable of boring into the reef framework. Cellular-grade Monera (bacteria) and tissue-grade Protista (algae and fungí) erode via chemical secretions. Tissue-grade Metazoa (the sponges) use a unique combination of chemical weakening combined with physical removal. Organ-grade Metazoa (polychaetes, bivalves, barnacles, crustaceans, sipunculids) employ a variety of techniques, ranging from the chemicalIy-assisted physical to the purely physical. |
title |
Aspects of bioerosion of modern Caribbean reefs |
title_short |
Aspects of bioerosion of modern Caribbean reefs |
title_full |
Aspects of bioerosion of modern Caribbean reefs |
title_fullStr |
Aspects of bioerosion of modern Caribbean reefs |
title_full_unstemmed |
Aspects of bioerosion of modern Caribbean reefs |
title_sort |
aspects of bioerosion of modern caribbean reefs |
title_alt |
Aspects of bioerosion of modern Caribbean reefs |
publisher |
Universidad de Costa Rica |
publishDate |
1978 |
url |
https://revistas.ucr.ac.cr/index.php/rbt/article/view/60786 |
work_keys_str_mv |
AT riskmichaelj aspectsofbioerosionofmoderncaribbeanreefs AT macgeachykirk aspectsofbioerosionofmoderncaribbeanreefs |
_version_ |
1810115373031227392 |