Meso-scale phytophysiognomic units in the Northern Pantanal and their relations with geomorphology
Keywords:
flood intensity and duration, topography, floodplain vegetation, remote sensing, Cuiabá River, ecohydrologyAbstract
The purpose of this work was to characterize and quantify phytophysiognomic units at mesoscale and evaluate their relationships with flood intensity, flood duration and topography. The study was conducted at a 25 km² Long-Term Sampling Site (LTSS), located within the floodplain of the Cuiabá River in the Pantanal of Mato Grosso. The phytophysiognomic units were determined from the supervised classification of CBERS 2B sensor CCD satellite images. The maps of flood intensity, flood duration and of topography were generated from the spatial interpolation of planialtimetric field surveys. Four phytophysiognomic units were identified; Campo inundável (flooded grassland) was the unit with the largest area of occurrence, followed by Cordilheiras (dense arboreal savanna), Landizal (seasonally flooded evergreen forest), and Cambarazal (monodominant Vochysia divergens Pohl. forest), respectively. Campo inundável is distributed mainly in areas of high flood intensity and duration and low topographic positions. Cambarazal predominates in areas of medium flood intensity and duration and intermediate elevation, Landizal in areas of high flood intensity and duration and low topographic position, whereas Cordilheiras are characterized by low flood intensity and duration and location in higher elevations. Statistical tests indicated that flood intensity is the main factor responsible for the mesoscale distribution of phytophysiognomic units in the northern Pantanal.Published
2010-06-01
How to Cite
Fantin-Cruz, I., Girard, P., Zeilhofer, P., Collischonn, W., & Cunha, C. N. da. (2010). Meso-scale phytophysiognomic units in the Northern Pantanal and their relations with geomorphology. Biota Neotropica, 10(2). Retrieved from //www.biotaneotropica.org.br/BN/article/view/672
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