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
Document Type
Article
Date of Original Version
1-1-1989
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
Publication Title, e.g., Journal
Proc., scientific results, ODP, Leg 105, Baffin Bay and Labrador Sea
Citation/Publisher Attribution
Hall, F. R., J. Bloemendal, J. W. King, M. A. Arthur, and A. E. Aksu. "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." Proc., scientific results, ODP, Leg 105, Baffin Bay and Labrador Sea (1989). doi: 10.2973/odp.proc.sr.105.177.1989.