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

doi:10.2973/odp.proc.sr.105.177.1989

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

Geosciences

Research output: Contribution to journal › Article › peer-review

7 Scopus citations

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 language	English (US)
Pages (from-to)	653-688
Number of pages	36
Journal	Unknown Journal
DOIs	https://doi.org/10.2973/odp.proc.sr.105.177.1989
State	Published - 1989

All Science Journal Classification (ASJC) codes

General Environmental Science
General Earth and Planetary Sciences

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10.2973/odp.proc.sr.105.177.1989

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author = "Hall, {F. R.} and J. Bloemendal and King, {J. W.} and Arthur, {M. A.} and Aksu, {A. E.}",

year = "1989",

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language = "English (US)",

pages = "653--688",

journal = "Unknown Journal",

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T1 - Middle to late Quaternary sediment fluxes in the Labrador Sea, ODP Leg 105, Site 646

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

AU - Hall, F. R.

AU - Bloemendal, J.

AU - King, J. W.

AU - Arthur, M. A.

AU - Aksu, A. E.

PY - 1989

Y1 - 1989

N2 - 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

AB - 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

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JO - Unknown Journal

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ER -

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

Abstract

All Science Journal Classification (ASJC) codes

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