Ocean thermohaline circulation and sedimentary 231Pa/230Th ratio
- 1 December 2000
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 15 (6), 625-641
- https://doi.org/10.1029/2000pa000496
Abstract
No abstract availableKeywords
This publication has 52 references indexed in Scilit:
- Variations of biogenic particle flux in the southern Atlantic section of the Subantarctic Zone during the late Quaternary: Evidence from sedimentary
Pa ex andTh ex Marine Geology, 1999 - Last-glacial-maximum North Atlantic deep water: on, off or somewhere in-between?Philosophical Transactions Of The Royal Society B-Biological Sciences, 1995
- Anomalous boundary scavenging in the Middle Atlantic Bight: evidence from 230Th, 231Pa, 10Be and 210PbDeep Sea Research Part II: Topical Studies in Oceanography, 1994
- What Controls Opal Preservation in Tropical Deep‐Sea Sediments?Paleoceanography and Paleoclimatology, 1993
- CADMIUM AND δ13C PALEOCHEMICAL OCEAN DISTRIBUTIONS DURING THE STAGE 2 GLACIAL MAXIMUMAnnual Review of Earth and Planetary Sciences, 1992
- Tracers of chemical scavenging in the ocean: boundary effects and large-scale chemical fractionationPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1988
- Removal of 230Th and 231Pa at ocean marginsEarth and Planetary Science Letters, 1983
- Removal of230Th and231Pa from the open oceanEarth and Planetary Science Letters, 1983
- Accumulation rates of Th-230, Pa-231, and some transition metals on the Bermuda RiseGeochimica et Cosmochimica Acta, 1982
- Distribution of thorium isotopes between dissolved and particulate forms in the deep seaJournal of Geophysical Research: Oceans, 1982