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AGU: Journal of Geophysical Research, Earth Surface

 

Keywords

  • Gulf of Papua
  • 210Pb
  • inventory
  • fluxes
  • Ashmore
  • Pandora
  • Moresby
  • PANASH
  • MARGINS

Index Terms

  • Marine Geology and Geophysics: Marine sediments: processes and transport
  • Oceanography: General: Continental shelf and slope processes
  • Oceanography: Biological and Chemical: Sedimentation
Abstract
Cited By (2)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, F01S17, 14 PP., 2008
doi:10.1029/2006JF000676

Excess 210Pb inventories and fluxes along the continental slope and basins of the Gulf of Papua

Zahid Muhammad

Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, Louisiana, USA

Samuel J. Bentley

Earth Sciences Department, Memorial University of Newfoundland, St. John's, Newfoundland and Labrador, Canada

Lawrence A. Febo

Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana, USA

André W. Droxler

Department of Earth Science, Rice University, Houston, Texas, USA

Gerald R. Dickens

Department of Earth Science, Rice University, Houston, Texas, USA

Larry C. Peterson

Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, USA

Bradley N. Opdyke

Department of Earth and Marine Science, Australian National University, Canberra, Australia

Sediment samples were collected from continental slopes and marginal basins in the Gulf of Papua and analyzed for excess 210Pb to elucidate transport processes of fine- grained particles to this region. Estimated excess 210Pb fluxes of 1.0–12.8 dpm cm−2 a−1 were derived from measured seabed inventories. Highest sediment accumulation rates (0.28–0.35 cm a−1) were measured along the northeastern shelf edge, and they decrease in seaward directions and along isobaths to the southwest. The excess 210Pb flux could result from either focused deposition of high-210Pb activity sediments from the continental shelf and upper slope or scavenging of 210Pb brought landward from deep-sea waters. This sediment flux is concentrated in the northeastern Gulf of Papua, where the shelf is narrow and calcium carbonate contents are lowest. Analysis of sedimentary fabric and 210Pb distributions in cores suggests sediment delivery to the slope occurs on a 100-year timescale as both diffuse hemipelagic deposition as well as turbidity flows. The flux of sediment in turbidity flows is not well constrained but may be producing additional deep-sea accumulation in the Moresby Trough, as well as export from the study area.

Received 31 August 2006; accepted 20 December 2007; published 19 March 2008.

Citation: Muhammad, Z., S. J. Bentley, L. A. Febo, A. W. Droxler, G. R. Dickens, L. C. Peterson, and B. N. Opdyke (2008), Excess 210Pb inventories and fluxes along the continental slope and basins of the Gulf of Papua, J. Geophys. Res., 113, F01S17, doi:10.1029/2006JF000676.

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