Other Scholarly Content

 

KlinkhammerGaryCEOASLinking8.2KAEvent.pdf Public Deposited

Analytics

Downloadable Content

Download PDF
https://ir.library.oregonstate.edu/concern/defaults/9880vs48x

Descriptions

Attribute NameValues
Creator
Abstract
  • The 8.2 ka event was the last deglacial abrupt climate event. A reduction in the Atlantic meridional overturning circulation (AMOC) attributed to the drainage of glacial Lake Agassiz may have caused the event, but the freshwater signature of Lake Agassiz discharge has yet to be identified in δ¹⁸O of foraminiferal calcite records from the Labrador Sea, calling into question the connection between freshwater discharge to the North Atlantic and AMOC strength. Using Mg/Ca-paleothermometry, we demonstrate that ∼3°C of near-surface ocean cooling masked an ∼1.0‰ decrease in western Labrador Sea δ¹⁸O of seawater concurrent with Lake Agassiz drainage. Comparison with North Atlantic δ¹⁸O of seawater records shows that the freshwater discharge was transported to regions of deep-water formation where it could perturb AMOC and force the 8.2 ka event.
Rights Statement
Additional Information
  • description.provenance : Submitted by Deanne Bruner (deanne.bruner@oregonstate.edu) on 2012-11-20T00:44:58Z No. of bitstreams: 1 KlinkhammerGaryCEOASLinking8.2KAEvent.pdf: 842719 bytes, checksum: 12ce90332df0dd5ddabcd6d80caa9f98 (MD5)
  • description.provenance : Made available in DSpace on 2012-11-20T00:44:58Z (GMT). No. of bitstreams: 1 KlinkhammerGaryCEOASLinking8.2KAEvent.pdf: 842719 bytes, checksum: 12ce90332df0dd5ddabcd6d80caa9f98 (MD5) Previous issue date: 2012-09-20

Relationships

Parents:

Items

Thumbnail Title Date Uploaded Visibility Actions
8c97kr967?file=thumbnail KlinkhammerGaryCEOASLinking8.2KAEvent.pdf 2017-07-25 Public