Direct correlation of sea surface paleotemperatures, deep circulation, and terrestrial paleoclimates: Foraminiferal and palynological evidence from two cores off Chesapeake Bay
- 1 June 1976
- journal article
- Published by Elsevier in Marine Geology
- Vol. 21 (2) , 121-147
- https://doi.org/10.1016/0025-3227(76)90053-0
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Correlation of Marine and Continental Quaternary Pollen Records from the Northeast Pacific and Western WashingtonQuaternary Research, 1973
- Deep-sea carbonates; Pleistocene dissolution cyclesJournal of Foraminiferal Research, 1973
- Paleoclimatic Investigation of a Late Pleistocene Caribbean Deep-Sea Core: Comparison of Isotopic and Faunal MethodsQuaternary Research, 1973
- Palynology of the Great Lakes: The Surface Sediments of Lake OntarioCanadian Journal of Earth Sciences, 1973
- Pollen Evidence of Pleistocene and Holocene Vegetation on the Allegheny Plateau, MarylandQuaternary Research, 1972
- SEASONAL INTERACTIONS BETWEEN THE NORTH PACIFIC OCEAN AND THE ATMOSPHERE DURING THE 1960'sMonthly Weather Review, 1969
- ATMOSPHERIC TELECONNECTIONS FROM THE EQUATORIAL PACIFIC1Monthly Weather Review, 1969
- Source and distribution of palynomorphs in bottom sediments, southern part of Gulf of CaliforniaMarine Geology, 1966
- Possible Late Pleistocene Uplift Chesapeake Bay EntranceThe Journal of Geology, 1965
- Palynology of Recent Orinoco Delta and Shelf Sediments: Reports of the Orinoco Shelf Expedition; Volume 5Micropaleontology, 1959