A quantitative analysis of the carbon cycle and comparison of carbon remineralization rates in marine Glacier Bay, Alaska

dc.contributor.authorLoughner, David Eric
dc.date.accessioned2008-08-12T22:55:08Z
dc.date.available2008-08-12T22:55:08Z
dc.date.issued2008-06-19
dc.description.abstractSediment cores were collected and analyzed for rates of carbon remineralization. It was hypothesized that the sediments beneath regions and areas of relatively high primary production rates would exhibit higher carbon remineralization rates and correspondingly, shallower oxygen penetration.en
dc.identifier.citationKeil R., Kelley D., D'Asaro E., Krembs C., and Collins R.E. [Eds.] 2008. Proceedings from the University of Washington School of Oceanography Undergraduate Thesis Research Expedition to Glacier Bay Alaska, March 2008. 296pp.en
dc.identifier.urihttp://hdl.handle.net/1773/3766
dc.language.isoen_USen
dc.publisherSchool of Oceanography, University of Washingtonen
dc.subjectMarine sediments--Alaska--Glacier Bay--analysisen
dc.subjectOxygen--Alaska--Glacier Bay--measurementen
dc.subjectCarbon cycle (Biogeochemistry)--Alaska--Glacier Bayen
dc.titleA quantitative analysis of the carbon cycle and comparison of carbon remineralization rates in marine Glacier Bay, Alaskaen
dc.typeOtheren

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