The grit principle and the morphology of oyster reefs.

dc.acquisition-srcen_US
dc.call-noAcc# 4527en_US
dc.call-noShelved with Journal of Shellfish Researchen_US
dc.contract-noen_US
dc.contributor.authorGunter, G.en_US
dc.contributor.otherProceedings of the National Shellfisheries Associationen_US
dc.date.accessioned2010-02-15T17:09:22Z
dc.date.available2010-02-15T17:09:22Z
dc.date.issued1979en_US
dc.degreeen_US
dc.descriptionp. 1-5.en_US
dc.description-otheren_US
dc.description.abstractOld oyster reefs of the genus Crassostrea from barren central ridges consisting of dead shell that may reach to the water surface and above. Some of the reef shell is as fine as flour and it varies upward in size to recently dead valves, but most of this material is of small size and is called grit. It is in constant motion on windy days and this scour prevents the settling of fouling organisms so that large areas of old shell remain bare except in deeper water on the flanks, where the effects of waves usually are not felt on the bottom. There live oysters grow. The grit principle explains the general structure of oyster reefs and their long existence as piles of dead shell until covered by sediment. Recognition of the grit principle explains many previously puzzling facts of live oyster and dead shell distribution. Examples are given.en_US
dc.description.urihttp://gbic.tamug.edu/request.htmen_US
dc.geo-codeGalveston Bayen_US
dc.geo-codeSmith Pointen_US
dc.geo-codeEagle Pointen_US
dc.historyen_US
dc.identifier.urihttp://hdl.handle.net/1969.3/22333
dc.latitudeen_US
dc.locationGalveston Bay Collection; TAMUG periodical collection.en_US
dc.longitudeen_US
dc.notesen_US
dc.publisheren_US
dc.relation.ispartofseries4527.00en_US
dc.relation.urien_US
dc.scaleen_US
dc.seriesen_US
dc.subjectanimal morphologyen_US
dc.subjectoyster reefsen_US
dc.subjectCrassostreaen_US
dc.subjectlife historyen_US
dc.titleThe grit principle and the morphology of oyster reefs.en_US
dc.typeArticleen_US
dc.universityen_US
dc.vol-issue69en_US

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