Changes in redox conditions in deep-sea sediments of the subarctic North Pacific Ocean: Possible evidence for the presence of North Pacific Deep Water
- 1 December 1989
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 4 (6) , 639-653
- https://doi.org/10.1029/pa004i006p00639
Abstract
No abstract availableKeywords
This publication has 49 references indexed in Scilit:
- Recurrent uranium relocations in distal turbidites emplaced in pelagic conditionsPublished by Elsevier ,2003
- Data on the geochemistry of pelagic clay of the subarctic North Pacific OceanOpen-File Report, 1989
- Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulationPaleoceanography and Paleoclimatology, 1988
- Late Quaternary deep-ocean circulationGSA Bulletin, 1986
- Major Asian aeolian inputs indicated by the mineralogy of aerosols and sediments in the western North PacificNature, 1985
- Post-depositional migration of elements during diagenesis in brown clay and turbidite sequences in the North East AtlanticGeochimica et Cosmochimica Acta, 1984
- Identification of the Holocene‐Pleistocene boundary in the Bering Sea by diatomsBoreas, 1982
- A Pleistocene Sand Sea on the Alaskan Arctic Coastal PlainScience, 1981
- Eolian sand and interbedded organic horizons at Kealok Creek on the Arctic Coastal Plain of Alaska: possible regional implicationsOpen-File Report, 1978
- Postdepositional mobility of some transition elements, phosphorus, uranium and thorium in deep sea sedimentsGeochimica et Cosmochimica Acta, 1971