The deglacial transition on the southeastern Alaska Margin: Meltwater input, sea level rise, marine productivity, and sedimentary anoxia
about
Mid-Pleistocene climate transition drives net mass loss from rapidly uplifting St. Elias Mountains, Alaska.Paleoceanographic insights on recent oxygen minimum zone expansion: lessons for modern oceanographyClimate change decouples oceanic primary and export productivity and organic carbon burialDeglacial rapid sea level rises caused by ice-sheet saddle collapses.North Pacific deglacial hypoxic events linked to abrupt ocean warming.Cordilleran Ice Sheet mass loss preceded climate reversals near the Pleistocene Termination.Productivity and sedimentaryδ15N variability for the last 17,000 years along the northern Gulf of Alaska continental slopeTransient stratification as the cause of the North Pacific productivity spike during deglaciationMegathrust splay faults at the focus of the Prince William Sound asperity, Alaska
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P2860
The deglacial transition on the southeastern Alaska Margin: Meltwater input, sea level rise, marine productivity, and sedimentary anoxia
description
im Juni 2011 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в червні 2011
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name
The deglacial transition on th ...... tivity, and sedimentary anoxia
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The deglacial transition on th ...... tivity, and sedimentary anoxia
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type
label
The deglacial transition on th ...... tivity, and sedimentary anoxia
@en
The deglacial transition on th ...... tivity, and sedimentary anoxia
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prefLabel
The deglacial transition on th ...... tivity, and sedimentary anoxia
@en
The deglacial transition on th ...... tivity, and sedimentary anoxia
@nl
P2093
P2860
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P356
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The deglacial transition on th ...... tivity, and sedimentary anoxia
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P2093
J. A. Addison
J. S. Stoner
M. H. Davies
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P356
10.1029/2010PA002051
P577
2011-06-01T00:00:00Z