Biological and climatic consequences of a cold, stratified, high latitude ocean

The flux from deep- and shallow-living radiolarian assemblages provides evidence of a glacial, high latitude, cold ocean stratification that increased biological pump efficiency and promoted ocean carbon sequestration. Greater deep (>200 m) than shallow-living (45° N) sediments with the deep-livi...

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Veröffentlicht in:	Quaternary science reviews 2013-12, Vol.82, p.78-92
Hauptverfasser:	Hays, James D., Martinson, Douglas G., Morley, Joseph J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Biological pump Deep sea cores Flux Glacial ocean Holocene Marine North Pacific Ocean carbon sequestration Pleistocene Radiolaria Sea of Okhotsk Stratification
Online-Zugang:	Volltext
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