39. SYNTHESIS OF STRATIGRAPHIC CORRELATIONS OF THE AMAZON FAN1David J.W. Piper,2
Roger D. Flood,3 Stan
Cisowski,4 Frank Hall,5 Patricia L. Manley,6
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The older part of the Amazon Fan sequence penetrated on Leg 155 predates the last interglacial but is probably no older than oxygen isotopic Stage 8. The presence or absence of the zonal fossil E. huxleyi in sediments interpreted as isotopic Stage 7 appears variable, as the result of ecologic changes, dissolution, or reworking. Last interglacial highstand deposits are identified at Sites 942 and 946 from a microfossil assemblage, isotopic character, and the paleomagnetic Blake Event. They may have been removed by erosion by mass-transport deposits at other deep sites. The available data do not allow a consistent stratigraphy to be developed for the late Pleistocene (Stages 4 and 3) prior to the paleomagnetic Lake Mungo Excursion (32 ka). A consistent correlation is developed for sequences younger than the Lake Mungo Excursion using oxygen isotopes of planktonic foraminifers, magnetic susceptibility, and paleomagnetic intensity and inclination. This correlation confirms that there is considerable variability in oxygen isotopic variations across the fan. The last glacial maximum is represented by the middle part of the Brown Channel-levee System. Shipboard seismic correlations are shown to be generally correct and confirm that major channel-levee systems formed sequentially. Several levees continued to accumulate mud with silt laminae, derived from flow-stripping of turbidity currents, after shifting of the active channel. A tentative age model is based on sparse 14C dates and the correlation of paleomagnetic intensity events with the global stack. |
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