Oceanographic and Climatic Change in the Bering Sea, Last Glacial Maximum to Holocene-Reference-Cited by-同舟云学术

Oceanographic and Climatic Change in the Bering Sea, Last Glacial Maximum to Holocene

Published:2018-01 Issue:1 Volume:33 Page:93-111
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanography and Paleoclimatology

Author:

Pelto Ben M.¹²^ORCID,Caissie Beth E.³^ORCID,Petsch Steven T.²,Brigham‐Grette Julie²

Affiliation:

1. Natural Resources and Environmental Studies Institute and Geography Program University of Northern British Columbia Prince George British Columbia Canada

2. Department of Geosciences University of Massachusetts Amherst Amherst MA USA

3. Department of Geological and Atmospheric Sciences Iowa State University Ames IA USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017PA003265

Reference143 articles.

1. Productivity and sedimentaryδ15N variability for the last 17,000 years along the northern Gulf of Alaska continental slope

2. Evolution of marine sedimentation in the Bering Sea since the Pliocene

3. Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilization

4. Provenance of terrigenous detritus of the surface sediments in the Bering and Chukchi Seas as derived from Sr and Nd isotopes: Implications for recent climate change in the Arctic regions

5. Deglacial Meltwater Pulse 1B and Younger Dryas Sea Levels Revisited with Boreholes at Tahiti

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3. The People;Culture and Archaeology of the Ancestral Unangax̂/Aleut of the Aleutian Islands, Alaska;2023

4. Evaluating the paleoenvironmental significance of sediment grain size in Bering Sea sediments during Marine Isotope Stage 11;Stratigraphy;2022-06

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