Hydrological impact of heinrich events in the subtropical northeast atlantic

By R. Meyer, J. Sloan, R. Dunin‐Borkowski, A. Kirkland, Miles C. Novotny, Sam R. Bailey, J. Hutchison. Science, 2000

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Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciation (2013, methodology): “available proxy data and maximum ice sheet volume (Duplessy et al., 1988; Bard et al., 2000; Adkins et al., 2002; Pflaumann, 2003; Peltier, 2004; Gersonde et al., 2005; LynchStieglitz et al., 2007; Clark et al., 2009; Gutjahr and Lippold, 2011; Hesse et al., 2011), the Last Glacial Maximum (LGM, abo”
The late Pleistocene desiccation of Lake Victoria and the origin of its endemic biota (2007, background): “It also coincided with ice-rafting events in the North Atlantic (Bard et al., 2000), disturbances in the atmospheric (14)C record (Kitagawa & van der Plicht, 1998), and with cooling cycles associated with solar weakening in Greenland’s GISP2 ice core record (Mayewski et al.”
Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings (2011, methodology): “The simulated cooling off the Iberian margin is overestimated compared to the estimated SST anomaly (Bard et al., 2000; Bard, 2002; Martrat et al., 2004, 2007), while it is in agreement with a reconstructed 3 C cooling in the Western Mediterranean Sea (Cacho et al.”
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes (2004, background): “5 kyr ago coincides with the timing of Heinrich event H”