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Transport and Destruction of Pelecypod Valves in the Minas Basin, Bay of Fundy

dc.contributor.advisorRisk, M. J.
dc.contributor.authorSzczuczko, Robert Bolek
dc.contributor.departmentGeologyen_US
dc.date.accessioned2016-09-14T17:11:22Z
dc.date.available2016-09-14T17:11:22Z
dc.date.issued1975-05
dc.description.abstract<p> Processes affecting the transportation and destruction of empty valves of the pelecypods Mya arenaria and Macoma balthica, were examined within the intertidal zone off Portapique Beach in the Minas Basin(Bay of Fundy). It was found that valve transport was away from shore within channels and eastward alongshore on the flats. It was observed that the rate of transport of left valves and small valves was greater than right valves large valves respectively. Transported valves are preferential oriented by currents of the flood and ebb tides and those within intertidal channels. Channel migration does not appear to be of significance in removing empty valves from these intertidal sediments. The loss valves from within the sediment is attributed to an unknown 'escape' mechanism. Once free of the sediment, valves are transported, weakened by boring thallophytes and mechanically destroyed during transport.</p>en_US
dc.description.degreeBachelor of Science (BSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/20355
dc.language.isoen_USen_US
dc.subjecttransport, destruction, pelecypod valves, Bay of Fundy, intertidal channels, sedimenten_US
dc.titleTransport and Destruction of Pelecypod Valves in the Minas Basin, Bay of Fundyen_US
dc.typeThesisen_US

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