Reconstructing paleoceanographic oxygen conditions in the Soledad Basin, Mexico

dc.contributor.author	Anderson, Chloe
dc.date.accessioned	2012-08-24T15:57:35Z
dc.date.available	2012-08-24T15:57:35Z
dc.date.issued	2012-06
dc.description	Senior thesis written for Oceanography 444	en_US
dc.description.abstract	[Author's Abstract] The global oceans contain relevant information about past environment. Oceanic sediments retain signatures from variations in productivity, water conditions and temperature making it possible to recreate past environmental conditions in the context of climate change. In Oxygen Deficient Zones (ODZs), oceanic regions with low oxygen concentration, the sediment record is mostly undisturbed creating ideal study sites for paleoceanographic reconstructions. This project seeks to reconstruct the oxygen conditions back approximately 600 years in Soledad Basin, a semi-enclosed basin on the continental shelf off Baja California, Mexico from a sediment core collected March 19, 2012.	en_US
dc.identifier.uri	http://hdl.handle.net/1773/20472
dc.language.iso	en_US	en_US
dc.relation.ispartofseries	Proceedings from the University of Washington School of Oceanography Senior Thesis, Academic Year 2011-2012;
dc.subject	Marine sediments--Mexico--Pacific Coast Analysis	en_US
dc.subject	Oceanography--Soledad Basin	en_US
dc.title	Reconstructing paleoceanographic oxygen conditions in the Soledad Basin, Mexico	en_US
dc.type	Other	en_US

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