234Th/238U disequilibrium as an indicator of the seasonal export flux of particulate organic carbon in the North Water
- 31 December 2002
- journal article
- Published by Elsevier in Deep Sea Research Part II: Topical Studies in Oceanography
- Vol. 49 (22-23) , 5191-5209
- https://doi.org/10.1016/s0967-0645(02)00185-6
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Water column structure and circulation under the North Water during spring transition: April–July 1998Deep Sea Research Part II: Topical Studies in Oceanography, 2002
- 238U,234U and232Th in seawaterPublished by Elsevier ,2002
- Dynamics of Chaetoceros socialis blooms in the North WaterDeep Sea Research Part II: Topical Studies in Oceanography, 2002
- Upper ocean export of particulate organic carbon and biogenic silica in the Southern Ocean along 170°WDeep Sea Research Part II: Topical Studies in Oceanography, 2001
- Upper ocean export of particulate organic carbon in the Arabian Sea derived from thorium-234Deep Sea Research Part II: Topical Studies in Oceanography, 1998
- Export flux of carbon at the equator during the EqPac time-series cruises estimated from 234Th measurementsDeep Sea Research Part II: Topical Studies in Oceanography, 1996
- Carbon and nitrogen export during the JGOFS North Atlantic Bloom experiment estimated from 234Th: 238U disequilibriaDeep Sea Research Part A. Oceanographic Research Papers, 1992
- Do upper-ocean sediment traps provide an accurate record of particle flux?Nature, 1991
- The chemistry, biology, and vertical flux of particulate matter from the upper 400 m of the equatorial Atlantic OceanDeep Sea Research, 1977
- 234Th/238U ratios in the oceanEarth and Planetary Science Letters, 1968