@InProceedings{RossettiBGVAMTB:2010:LaPlRe,
author = "Rossetti, D and Bezerra, F H and G{\'o}es, A and Valeriano, M and
Andrades Filho, C and Millani, J and Tatumi, S and Brito Neves, B
B",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {} and USP,
S{\~a}o Paulo, Brazil and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and FATEC, S{\~a}o Paulo, Brazil and FATEC, S{\~a}o
Paulo, Brazil and USP, S{\~a}o Paulo, Brazil",
title = "The late Pleistocene-Holocene record of sea level in Northeastern
Brazil and its relation to climate, eustasy and tectonics",
booktitle = "Proceedings...",
year = "2010",
organization = "Meeting of the Americas.",
abstract = "AB: Late Quaternary deposits in Northeastern Brazil have been
scarcely investigated, despite their great relevance to discuss
the post-rift evolution of South American passive margin within
the context of landform, sea level and tectonic deformation.
Sedimentological, stratigraphic and morphological characterization
of these deposits led to their distinction from the underlying
Early/Middle Miocene Barreiras Formation. Two sedimentary units
(PB1 and PB2) were recognized and related, with basis on optically
stimulated luminescence (OSL) dating, to the time intervals
between 74.8±9.3 and 30.8±6.9 ka, and 8.8±0.9 and 1.8±0.2 ka,
respectively. Unit PB1 is exposed discontinuously in the highest
topography (usually between 100 m and 150 m), being mostly
composed of endured sandstones and breccias either with massive
bedding or an abundance of complex styles of ductile and brittle
soft sediment deformation structures related to contemporaneous
seismic activity. This unit also includes a large volume of
non-indured sharply bounded, fining upward massive or stratified
conglomerates and sandstones interbedded with mudstones,
attributed to fluvial, alluvial and aeolian dune environments.
These deposits might include nearshore marine-influenced strata in
areas located nearby the modern coastline, as suggested by
presence of burrows as Skolithos, Thalassinoides, Planolites,
Diplocraterion, and Teichichnus. Unit PB2, composed of sands with
massive or dissipation dune structures, occurs continuously,
mostly on northeastward dipping tablelands located at altitudes
lower than 100 m. The present work focusing on units PB1 and PB2,
together referred as Post-Barreiras Sediments, opens a new
opportunity to discuss landform, sea level and tectonic history of
eastern South American passive margin during the latest
Quaternary. Hence, following the Miocene transgression, there was
a prolonged period of non-deposition and sub-aerial exposure,
which is related to combination of a worldwide low sea level in
the Tortonian and tectonic quiescence. Sediment deposition was
reactivated during the latest Pleistocene due to tectonic
deformation, which created space to accommodate unit PB1 in
downthrown faulted blocks and, perhaps, also synclines produced by
extension and compression associated with strike-slip tectonic
deformation. Although deposition of this unit was simultaneous to
the eustatic fall that followed the Penultimate Transgression,
punctuated rises superimposed on the overall fall, added to
subsidence, would have favored marine deposition in areas located
nearby the modern coastline. A renewed phase of deformation would
have resulted in newly subsiding areas in the Holocene, promoting
deposition of unit PB2 over unit PB1. Although unit PB2 formed
during most of the last transgression, except along coastal areas,
it has no records of marine sedimentation, suggesting a
non-significant rise or reworking of thin transgressive sands by
aeolian process. The data presented herein leads to review the
evolution of South American passive margin based on assumptions of
uniform sedimentation and undeformed planation surfaces over a
wide coastal area of Northeastern Brazil.",
conference-location = "Foz Igua{\c{c}}u",
conference-year = "8-12 Aug. 2010",
language = "en",
targetfile = "cintra.pdf",
urlaccessdate = "27 abr. 2024"
}