Evidence of sediment transport in the Quaternary of Campos Basin lower slope, based on allochthonous ostracodes
Keywords:
ostracods |, mixed assemblages, sedimentary transportation, deep-water, Quaternary, Campos Basin, BrazilAbstract
The susceptibility of ostracoda from different habitats to environmental and climatic change, form distinct assemblages that are useful both in continental and marine paleoenvironmental reconstructions. Ostracod assemblages recovered from late Pleistocene-Holocene carbonatic mud, of piston core GL-451 in the Campos Basin, contains mixed assemblages featuring autochthonous (Krithe, Poseidonamicus, Australoecia, Cytheropteron, Bythocypris, Bradleya) and allochthonous (Brasilicythere, Caudites, Cyprideis, Eucythere, Loxoconcha, Meridionalicythere, Paracytheridea, Xestoleberis) taxa. These studies report that, the autochthonous taxa predominate within the assemblages, indicating that the muds were deposited in a deep water environment (lower bathyal). The occurrence of mixed assemblages is most common during glacial phases, with evidence to support a higher sediment transport from the continental-platform to slope areas, which took place during the ice age. The greater abundance peak of allochthonous ostracodes lies in the upper portion of the planktonic foraminifer Subzone Y1 (upper Pleistocene), which is related to the colder period and consequently a reduction in the relative sea level (RSL).
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