Middle to late Quaternary sediment fluxes in the Labrador Sea, ODP Leg 105, Site 646: a synthesis of rock-magnetic, oxygen-isotopic, carbonate, and planktonic foraminiferal data

F. R. Hall, J. Bloemendal, J. W. King, M. A. Arthur, A. E. Aksu

Research output: Contribution to journalArticle

6 Citations (Scopus)

Abstract

Examines rock-magnetic, carbonate, and planktonic foraminiferal fluxes to identify climatically controlled changes of terrigenous and pelagic sedimentation at Site 646 (the Labrador Sea). Terrigenous sediments are brought to the site principally by bottom currents. The shift observed in the lag times of parameters examined with respect to the SPECMAP record is attributed to a change in significance of orbital parameters. -from Authors

Original languageEnglish (US)
Pages (from-to)653-688
Number of pages36
JournalUnknown Journal
StatePublished - Jan 1 1989

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Ocean Drilling Program
carbonate
oxygen
bottom current
rock
sediment
sedimentation
parameter
sea

All Science Journal Classification (ASJC) codes

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

Cite this

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Middle to late Quaternary sediment fluxes in the Labrador Sea, ODP Leg 105, Site 646 : a synthesis of rock-magnetic, oxygen-isotopic, carbonate, and planktonic foraminiferal data. / Hall, F. R.; Bloemendal, J.; King, J. W.; Arthur, M. A.; Aksu, A. E.

In: Unknown Journal, 01.01.1989, p. 653-688.

Research output: Contribution to journalArticle

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T2 - a synthesis of rock-magnetic, oxygen-isotopic, carbonate, and planktonic foraminiferal data

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AU - Bloemendal, J.

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AU - Aksu, A. E.

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