Hostname: page-component-5cf477f64f-xc2pj Total loading time: 0 Render date: 2025-04-06T06:16:46.556Z Has data issue: false hasContentIssue false
  • English
  • Français

Fluorescent tracers for observation of transport behavior of skeletal sediment particles

Published online by Cambridge University Press:  14 July 2015

Thomas W. Broadhead ,
Steven G. Driese  and
James L. Harvey
Thomas W. Broadhead
Affiliation:
Department of Geological Sciences, University of Tennessee, Knoxville 37996
Steven G. Driese
Affiliation:
Department of Geological Sciences, University of Tennessee, Knoxville 37996
James L. Harvey
Affiliation:
Department of Geological Sciences, University of Tennessee, Knoxville 37996
Get access Rights & Permissions [Opens in a new window]

Extract

Settling rates and behaviors of sediment grains are of particular interest as components in interpreting the hydrodynamics of skeletal carbonate sediments (Maiklem, 1968) and the deposition of skeletons of planktonic organisms (Bé, 1977; Casey and McMillen, 1977). Settling rates and behaviors also are important because even the disarticulated remains of benthic organisms may undergo repeated resuspension and differential settling prior to final burial.

Type
Paleontological Notes
Information
Journal of Paleontology , Volume 64 , Issue 5 , September 1990 , pp. 843 - 844
Copyright
Copyright © The Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bé, A. W. H. 1977. An ecological, zoogeographic and taxonomic review of recent planktonic foraminifera, p. 1–100. In Ramsay, A. T. S. (ed.), Oceanic Micropaleontology. Academic Press, London.Google Scholar
Casey, R. E., and McMillen, K. J. 1977. Cenozoic radiolarians of the Atlantic basin and margins, p. 521–544. In Swain, F. M. (ed.), Stratigraphic Micropaleontology of Atlantic Basin and Borderlands. Elsevier, Amsterdam.Google Scholar
Dingler, J. R., and Anima, R. J. 1989. Subaqueous grain flows at the head of Carmel submarine canyon, California. Journal of Sedimentary Petrology, 59:280–286.Google Scholar
Kennedy, V. C., and Kouba, D. L. 1970. Fluorescent sand as a tracer of fluvial sediment. U.S. Geological Survey Professional Paper 562-E, 13 p.Google Scholar
Maiklem, W. R. 1968. Some hydraulic properties of bioclastic carbonate grains. Sedimentology, 10:101–109.Google Scholar
Rathbun, R. E., Kennedy, V. C., and Culbertson, J. K. 1971. Transport and dispersion of fluorescent tracer particles for the flat-bed condition, Rio Grande Conveyance Channel, near Bernardo, New Mexico. U.S. Geological Survey Professional Paper 562-I, 56 p.Google Scholar