Show simple item record

dc.identifier.urihttp://hdl.handle.net/1951/60233
dc.identifier.urihttp://hdl.handle.net/11401/71054
dc.description.sponsorshipThis work is sponsored by the Stony Brook University Graduate School in compliance with the requirements for completion of degree.en_US
dc.formatMonograph
dc.format.mediumElectronic Resourceen_US
dc.language.isoen_US
dc.publisherThe Graduate School, Stony Brook University: Stony Brook, NY.
dc.typeDissertation
dcterms.abstractThis study of the relict `Oyster Terrain' in the Peconic Estuary of Long Island, NY using multibeam bathymetry, chirp sonar and sample analysis provides a history of estuarine evolution over thousands of years. More than 10,000 relict oyster reefs are exposed as mounds on the seabed within the Peconic Estuary, with more mounds imaged below the sediment surface. The tops of these relict oyster reefs are at water depths of ~6 m - 18 m and reef thicknesses of up to 6 m suggest active reef building over a few thousand years. At 28 psu, the present estuary is too saline for natural populations of the Eastern Oyster, Crassostrea virginica, to survive although transplanted oysters will grow. Morphological and shell data tell of a time when crowded oyster reefs once dominated the area; however, there has been a natural evolution in the Holocene to an environment where oysters are rare. Shells from relict oyster reefs provide the opportunity for a more detailed environmental reconstruction of this important transition through <super>14<super>C dating and geochemical proxies such as <super>87<super>Sr/<super>86<super>Sr (salinity) and <super>226<super>226 (submarine groundwater discharge). Reefs persisted in the Peconic Estuary despite rising salinities until ~1,350 years ago. Relict shells were compared to modern aquaculture shells grown in Peconic oyster farms. Submarine groundwater discharge seems to have dramatically decreased over time within the estuary according to concentrations of <super>226<super>Ra recorded in several sample shells. Sr isotope measurements indicate past variability in salinity was also captured in the relict shells. The era of abundant oyster reefs ended gradually suggesting that there was a gradual evolution to conditions that did not favor oyster survival. Surprisingly, the oyster reefs were growing in slightly deeper water than we anticipated before dying off. The youngest reefs were in only ~2.5 m of water 1,350 years ago; however, the oldest exposed reef tops we dated would have been active in ~10 m of water some 2,350 years ago. Our results suggest that oysters may have thrived in deeper waters more abundantly in the past than in modern stressed estuaries.
dcterms.available2013-05-24T16:38:16Z
dcterms.available2015-04-24T14:45:43Z
dcterms.contributorFlood, Roger D.en_US
dcterms.contributorCochran, J. Kirken_US
dcterms.contributorVarekamp, Johan C.Black, David E.Cerrato, Robert M.en_US
dcterms.creatorKinney, Juliet Kinney West
dcterms.dateAccepted2013-05-24T16:38:16Z
dcterms.dateAccepted2015-04-24T14:45:43Z
dcterms.dateSubmitted2013-05-24T16:38:16Z
dcterms.dateSubmitted2015-04-24T14:45:43Z
dcterms.descriptionDepartment of Marine and Atmospheric Scienceen_US
dcterms.extent369 pg.en_US
dcterms.formatMonograph
dcterms.formatApplication/PDFen_US
dcterms.identifierhttp://hdl.handle.net/1951/60233
dcterms.identifierhttp://hdl.handle.net/11401/71054
dcterms.issued2012-05-01
dcterms.languageen_US
dcterms.provenanceMade available in DSpace on 2013-05-24T16:38:16Z (GMT). No. of bitstreams: 1 StonyBrookUniversityETDPageEmbargo_20130517082608_116839.pdf: 41286 bytes, checksum: 425a156df10bbe213bfdf4d175026e82 (MD5) Previous issue date: 1en
dcterms.provenanceMade available in DSpace on 2015-04-24T14:45:43Z (GMT). No. of bitstreams: 3 StonyBrookUniversityETDPageEmbargo_20130517082608_116839.pdf.jpg: 1934 bytes, checksum: c116f0e1e7be19420106a88253e31f2e (MD5) StonyBrookUniversityETDPageEmbargo_20130517082608_116839.pdf.txt: 336 bytes, checksum: 84c0f8f99f2b4ae66b3cc3ade09ad2e9 (MD5) StonyBrookUniversityETDPageEmbargo_20130517082608_116839.pdf: 41286 bytes, checksum: 425a156df10bbe213bfdf4d175026e82 (MD5) Previous issue date: 1en
dcterms.publisherThe Graduate School, Stony Brook University: Stony Brook, NY.
dcterms.subjectmultibeam echosounder, oyster reef, paleoceanography, sediment, sub-bottom seismic profile, submarine groundwater discharge
dcterms.subjectMarine geology--Geomorphology--Paleoclimate science
dcterms.titleEvolution of the Peconic Estuary `Oyster Terrain' Long Island, NY
dcterms.typeDissertation


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record