Quantitative evaluation of bioturbation rates in deep ocean sediments. II. Comparison of rates determined by 210Pb and 239,240Pu
Authors:
- N.L GuinassoNGN.L Guinasso
- 1 September 1985
- journal article
- research article
- Published by Elsevier in Marine Chemistry
- Vol. 17 (2) , 99-114
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Laboratory and field studies of the relative mobility of 239,240Pu and 241Am from lake sediments under oxic and anoxic conditionsGeochimica et Cosmochimica Acta, 1981
- Plutonium and americium in anoxic marine sediments: Evidence against remobitizationGeochimica et Cosmochimica Acta, 1981
- 210Pb activities in and fluxes to sediments of the Washington continental slope and shelfGeochimica et Cosmochimica Acta, 1981
- Sedimentary processes in the inner New York Bight: Evidence from excess210Pb and239,240PuEarth and Planetary Science Letters, 1981
- Radium, thorium, uranium, and 210 Pb in deep-sea sediments and sediment pore waters from the North Equatorial PacificAmerican Journal of Science, 1980
- Effects of biological sediment mixing on the210Pb chronology and trace metal distribution in a Long Island Sound sediment coreEarth and Planetary Science Letters, 1979
- Experimental studies of changes produced by deposit feeders on pore water, sediment, and overlying water chemistryAmerican Journal of Science, 1978
- 210Pb/226Ra and 210Po/210Pb disequilibria in seawater and suspended particulate matterEarth and Planetary Science Letters, 1976
- 234Th/238U disequilibrium in near-shore sediment: Particle reworking and diagenetic time scalesEarth and Planetary Science Letters, 1976
- Stratigraphic effects of tubificids in profundal lake sediments1Limnology and Oceanography, 1974