Broecker, Wallace S; Bond, Gerard C; Klas, Mieczyslawa; Bonani, Georges; Wolfli, Willy (1990): Age determination and stable isotope ratios of planktonic foraminifera from DSDP Hole 94-609. PANGAEA, https://doi.org/10.1594/PANGAEA.727183, Supplement to: Broecker, WS et al. (1990): A salt oscillator in the glacial Atlantic? 1. the concept. Paleoceanography, 5(4), 469-477, https://doi.org/10.1029/PA005i004p00469
Always quote above citation when using data! You can download the citation in several formats below.
As shown by the work of Dansgaard and his colleagues, climate oscillations of one or so millennia duration punctuate much of glacial section of the Greenland ice cores. These oscillations are characterized by 5°C air temperature changes, severalfold dust content changes and 50 ppm CO2 changes. Both the temperature and CO2 change are best explained by changes in the mode of operation of the ocean. In this paper we provide evidence which suggests that oscillations in surface water conditions of similar duration are present in the record from a deep sea core at 50°N. Based on this finding, we suggest that the Greenland climate changes are driven by oscillations in the salinity of the Atlantic Ocean which modulate the strength of the Atlantic's conveyor circulation.
Latitude: 49.877800 * Longitude: -24.238200
Date/Time Start: 1983-07-22T00:00:00 * Date/Time End: 1983-07-22T00:00:00
94-609 * Latitude: 49.877800 * Longitude: -24.238200 * Date/Time: 1983-07-22T00:00:00 * Elevation: -3884.0 m * Penetration: 399.4 m * Recovery: 301.4 m * Location: North Atlantic/FLANK * Campaign: Leg94 * Basis: Glomar Challenger * Device: Drilling/drill rig (DRILL) * Comment: 40 cores; 380.2 m cored; 19.2 m drilled; 79.3 % recovery