@Article{RossettiToleVale:2019:GeEvCo,
author = "Rossetti, Dilce de F{\'a}tima and Toledo, Peter Mann de and
Valeriano, M{\'a}rcio de Morisson",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "Neotectonics and tree mortality in a forest ecosystem of the Negro
basin: Geomorphic evidence of contemporary seismicity in the
intracratonic Brazilian Amazonia",
journal = "Geomorphology",
year = "2019",
volume = "329",
pages = "138--151",
month = "Mar.",
keywords = "Strike slip faults, Neotectonics, Forest structure, Amazonian
rainforest.",
abstract = "Neotectonic activity was increasingly recorded over the Amazonian
lowlands, even during historical times of a few tens of centuries.
However, detailed analyses linking structures and styles of
deformation are still few considering the large dimension of the
region. Such events in a relatively recent time are expected to
have caused conspicuous impacts on Amazonian ecosystems and forest
disturbance. Changes in topography and hydrology by fracturing,
faulting and folding during either subsidence or uplifting are
direct effects on landscape that leave marks on the structure of
the current forest, such as tree mortality and community
succession. Two rectangular elbow-like shaped wetlands from the
left margin of the middle Negro River valley in northwestern
Amazonia were attributed to neotectonics. Remote sensing imagery
was applied to test this hypothesis and also provide a tectonic
model that can explain deformation dynamics in this area. The
studied wetlands and adjacent river systems display various
morphostructural anomalies compatible with a tectonic control, as
well as lineaments paralleling main NW and NE-trending regional
structures. The geomorphic analysis led to suggest that the
wetlands are depressions formed by NW and NE-trending master
boundary faults of horizontal displacements intercepted by various
subsidiary faults. Transtensional strike slip regime is recorded
by both left and right-lateral faults, with the wetlands
corresponding to subsiding areas owned to conjugate strike slip
faults. Habitat fragmentation and other ecological processes
promoted by tectonic deformation would have impacted the overlying
forest canopy by changing its structure due to tree mortality. The
complex compartmentalization imposed by active tectonics would
have exposed the ground to contrasting hydrological conditions,
which controlled the rate of tree mortality within the wetlands.
We pose that the tectonic disturbance and associated tree
mortality documented in the middle Negro River evidence
contemporary seismicity within the intracratonic Brazilian
Amazonia.",
doi = "10.1016/j.geomorph.2018.12.028",
url = "http://dx.doi.org/10.1016/j.geomorph.2018.12.028",
issn = "0169-555X",
language = "en",
targetfile = "rossetti_neotectonics.pdf",
urlaccessdate = "27 abr. 2024"
}