EarthRef.org Reference Database (ERR)
Development and Maintenance by the EarthRef.org Database Team

Detailed Reference Information
Broecker & Clark 2003
Broecker, W.S. and Clark, E. (2003). CaCO3 dissolution in the deep sea: Paced by insolation cycles. Geochemistry Geophysics Geosystems 4: doi: 10.1029/2002GC000450. issn: 1525-2027.

Three CaCO3 dissolution events have been documented in the western equatorial Atlantic, one associated with marine isotope stage 5d, one with stage 5b, and one with early stage 4. The intensity of these events appears to require a greatly expanded invasion of waters with a low carbonate ion concentration akin to that characterizing today's deep Pacific (and also the Antarctic Bottom Water). While evident in a core from a depth of 3.4 km, these three events appear to be much less intense in the western equatorial Pacific than in the western Atlantic. The Atlantic results appear to be telling us that the density difference between Southern Ocean and North Atlantic deep waters has been modulated by insolation changes associated with the 23,000-year precession cycle.

BACKGROUND DATA FILES

Abstract

Keywords
Geochemistry, Geochemical cycles, Geochemistry, Marine geochemistry (4835, 4850), Marine Geology and Geophysics, Marine sediments--processes and transport
Journal
Geochemistry Geophysics Geosystems
Publisher
American Geophysical Union
2000 Florida Avenue N.W.
Washington, D.C. 20009-1277
USA
1-202-462-6900
1-202-328-0566
service@agu.org
Click to clear formClick to return to previous pageClick to submit