Pacific deep circulation: A velocity increase at the end of the interglacial stage 5?
- 1 December 1982
- journal article
- research article
- Published by Elsevier in Deep Sea Research Part A. Oceanographic Research Papers
- Vol. 29 (12) , 1517-1530
- https://doi.org/10.1016/0198-0149(82)90040-1
Abstract
No abstract availableFunding Information
- Deutsche Forschungsgemeinschaft
This publication has 8 references indexed in Scilit:
- Organic carbon decomposition rates in sediments of the pacific manganese nodule belt dated by 230Th and 231PaEarth and Planetary Science Letters, 1980
- Uranium and thorium series nuclides in oriented ferromanganese nodules: growth rates, turnover times and nuclide behaviorEarth and Planetary Science Letters, 1978
- ratios in Pacific deep-sea sediments: Effect of inorganic ammonium and organic nitrogen compounds sorbed by claysGeochimica et Cosmochimica Acta, 1977
- Deep Pacific circulation: Intensification during the Early CenozoicMarine Geology, 1974
- Ocean-Floor Erosion in the Equatorial PacificGSA Bulletin, 1972
- Antarctic Bottom Water: Major Change in Velocity during the Late Cenozoic between Australia and AntarcticaScience, 1971
- The Last Interglacial: Paleotemperatures and ChronologyScience, 1971
- Insolation changes, ice volumes, and the O18 record in deep‐sea coresReviews of Geophysics, 1970