An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska

dc.contributor.authorPeterson, Marcus
dc.date.accessioned2008-08-12T23:31:35Z
dc.date.available2008-08-12T23:31:35Z
dc.date.issued2008-06-19
dc.description.abstractIron in seawater is biologically significant for its contribution to primary productivity. This study showed a high livel of iron in Glacier Bay, as well as higher values for the metal in water beneath the mixed layer. This suggests that sediments are the source for iron in the bay.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/1773/3767
dc.language.isoen_USen
dc.publisherSchool of Oceanography, University of Washingtonen
dc.subjectCarbon cycle (biogeochemistry)--Alaska--Glacier Bayen
dc.subjectTrace elementsen
dc.subjectSeawater--Iron content--analysisen
dc.titleAn investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaskaen
dc.typeOtheren

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