Rs. Ganeshram et Tf. Pedersen, Glacial-interglacial variability in upwelling and bioproductivity off NW Mexico: Implications for quaternary paleoclimate, PALEOCEANOG, 13(6), 1998, pp. 634-645
Sedimentary accumulation of biogenic components (organic carbon, opal, and
biogenic barium) on the northwestern Mexican margin declined during every g
lacial interval of the past 140 kyr, indicating decreases in upwelling-indu
ced productivity during cold periods. The glacial-interglacial contrasts in
upwelling on this margin are attributed to reversals in land-ocean thermal
contrast, the waxing and waning of the Laurentide Ice Sheet, and consequen
t responses of the western hemisphere wind fields. This scenario is consist
ent with three independent lines of evidence: terrestrial paleoclimatic dat
a, general circulation model results, and our marine records. This pattern
of glacial interglacial variability in upwelling off NW Mexico is opposite
to that observed in other low-latitude and midlatitude upwelling areas, suc
h as the eastern equatorial Pacific. These results add to a growing pool of
observations that the response of oceanic upwelling to glacial climatic fo
rcing has been regionally variable.