Glenn A. Jones

TL;DR: The Black Sea became a giant freshwater lake during the latest Quaternary glaciation and the surface of this lake drew down to levels more than 100 m below its outlet as mentioned in this paper.

TL;DR: In this article, a high-resolution reconstruction of Caribbean climate is presented based on O-18/O-16 ratios in ostracod shells from Lake Miragoane, Haiti.

TL;DR: In this paper, high-resolution paleogeochemical data from the North Atlantic Ocean indicate that in the interval 15,000 to 10,000 14C years before present (B.P.) North Atlantic Deep Water (NADW) production was decreased or eliminated four times: at about 14,500 (and probably older), 13,500, 12,000 and 10,500 years B.P. Each of these changes occurred at the same time as abrupt events of meltwater discharge to the surface ocean.

TL;DR: In this paper, the first oxygen isotope record from the Norwegian-Greenland Sea that is radiocarbon-dated directly by accelerator mass spectrometry was reported, which suggests that the marine-based Barents Shelf ice sheet disintegrated rapidly at approximately 15,000 years BP.

TL;DR: Two late Quaternary series of high resolution percent carbonate data from western North Atlantic sediment drifts (Bermuda Rise and Bahama Outer Ridge) show millennial-scale oscillations superimposed on the familiar, longer-period oscillations of orbital origin this paper.