Benthic foraminiferal communities at DSDP Sites 94-609 to 94-611, supplement to: Murray, John W (1987): Benthic foraminifers and Neogene bottom-water masses at Deep Sea Drilling Project Leg 94 North Atlantic Sites. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 965-979

Benthic foraminiferal assemblages from northeast Atlantic DSDP Sites 609, 610, and 611 have been interpreted with reference to modern assemblages known to be linked with the overlying bottom-water masses. It is shown that the water masses in the late Miocene to Pleistocene were similar to those of t...

Full description

Bibliographic Details
Main Author: Murray, John W
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 1987
Subjects:
Deep Sea Drilling Project DSDP
Antarctic
Kidd
Antarc*
North Atlantic Deep Water
North Atlantic
Northeast Atlantic
Online Access:https://dx.doi.org/10.1594/pangaea.788704
https://doi.pangaea.de/10.1594/PANGAEA.788704
Description
Summary:Benthic foraminiferal assemblages from northeast Atlantic DSDP Sites 609, 610, and 611 have been interpreted with reference to modern assemblages known to be linked with the overlying bottom-water masses. It is shown that the water masses in the late Miocene to Pleistocene were similar to those of today. The distribution of the water masses changed with time, however. Antarctic Bottom Water ("AABW"), which at present is restricted to the area south of the Azores, reached as far north as the Gibbs Fracture Zone in the early Pliocene. Increased production of North Atlantic Deep Water in the late Pliocene displaced the AABW to the south

Similar Items