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Middle to Late Pleistocene evolution of the Bengal Fan : Integrating core and seismic observations for chronostratigraphic modeling of the IODP Expedition 354 8° North transect

Reilly, B.T. ; Bergmann, F. ; Weber, M.E. ; Stoner, J.S. ; Selkin, P. ; Meynadier, L. ; Schwenk, T. ; Spiess, V. ; France-Lanord, C., G3

Middle to Late Pleistocene evolution of the Bengal Fan : Integrating core and seismic observations for chronostratigraphic modeling of the IODP Expedition 354 8° North transect

Reilly, B.T. ; Bergmann, F. ; Weber, M.E. ; Stoner, J.S. ; Selkin, P. ; Meynadier, L. ; Schwenk, T. ; Spiess, V. ; France-Lanord, C.

Geochemistry, Geophysics, Geosystems, 2020, 21, e2019GC008878

Abstract :

We investigate chronology and age uncertainty for the middle to upper Pleistocene lower Bengal Fan using a novel age‐depth modeling approach that factors lithostratigraphic, magnetostratigraphic, biostratigraphic, cyclostratigraphic, and seismic stratigraphic constraints, based on results from the International Ocean Discovery Program Expedition 354 Bengal Fan and analysis of the GeoB97‐020/027 seismic line. The initial chronostratigraphic framework is established using regionally extensive hemipelagic sediment units, and only age‐depth models of fan deposits that respect the superposition of channel‐levee systems between sites are accepted. In doing so, we reconstruct signals of regional sediment accumulation rate and lithogenic sediment input through the perspective of a two‐dimensional 320 km transect at 8°N that are consistent with more distal and more ambiguous regional records. This chronology allows us to discuss the depositional history of the middle to upper Pleistocene lower Bengal Fan within the context of sea level, climate, and tectonic controls. We hypothesize, based on the timing of accumulation rate changes, that progradation and intensification of the Bengal Fan’s channel‐levee system at 8°N was largely driven by increases in sea level amplitude during this time. However, it is also possible this progradation was influenced by changes in Pleistocene climate and increased Himalayan erosion rates, driving greater sediment flux to the fan.

Voir en ligne : https://doi.org/10.1029/2019GC008878




publié mercredi 9 septembre 2020