The deglacial transition on the southeastern Alaska Margin: Meltwater input, sea level rise, marine productivity, and sedimentary anoxia-Reference-Cited by-同舟云学术

The deglacial transition on the southeastern Alaska Margin: Meltwater input, sea level rise, marine productivity, and sedimentary anoxia

Author:

Davies M. H.¹,Mix A. C.¹,Stoner J. S.¹,Addison J. A.²,Jaeger J.³,Finney B.⁴,Wiest J.⁵

Affiliation:

1. College of Oceanic and Atmospheric Sciences; Oregon State University; Corvallis Oregon USA

2. Department of Geology and Geophysics; University of Alaska Fairbanks; Fairbanks Alaska USA

3. Department of Geological Sciences; University of Florida; Gainesville Florida USA

4. Department of Biological Sciences; Idaho State University; Pocatello Idaho USA

5. College of Veterinary Medicine; Oregon State University; Corvallis Oregon USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

Reference134 articles.

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