Patterns and processes in a seasonally flooded tropical plain: The Apure Llanos, Venezuela

Aim: The factors and processes determining the ecology and distribution of ecosystems in the Apure lowlands, Venezuela, are critically discussed. Location: The Middle Apure region, an alluvial Quaternary plain built by the Arauca and Apure rivers, occupies a subsidence area caused by faulting of the...

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Autores principales: Sarmiento, G., Pinillos, M.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_03050270_v28_n8_p985_Sarmiento
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spelling todo:paper_03050270_v28_n8_p985_Sarmiento2023-10-03T15:21:10Z Patterns and processes in a seasonally flooded tropical plain: The Apure Llanos, Venezuela Sarmiento, G. Pinillos, M. Landscape evolution Soil genesis Tropical forests Tropical savannas Venezuelan Llanos Water regime Wetlands ecosystem structure floodplain landscape ecology landscape evolution pedogenesis Quaternary savanna water budget Venezuela Aim: The factors and processes determining the ecology and distribution of ecosystems in the Apure lowlands, Venezuela, are critically discussed. Location: The Middle Apure region, an alluvial Quaternary plain built by the Arauca and Apure rivers, occupies a subsidence area caused by faulting of the geological basement during the last and most active phases of the Andean uplift. Methods: To assess the determinants of the hydrological and ecological variability in this region, we used remote imagery and field surveys. Results: The hydrological and ecological variability responds to a set of interconnected processes of different nature: geological, climatic and paleoclimatic and hydrographic, which together have conditioned the geomorphological history of the regional landscape. This evolution, in turn, has guided the soil forming processes and the functional behaviour of the different types of savanna, forest and wetland ecosystems. The continuously subsiding trend of the Llanos that accompanied the Andean Orogeny, together with the Quaternary climatic oscillations, settled the framework in which successive depositional and erosional events took place. Five Quaternary depositional events, gave rise to the actual landscape pattern. The youngest, Q0a is the actual flood plain, Q0b is the Holocene flood plain, Q1 is from Upper Pleistocene, Q2 from Middle Pleistocene, while Q3 the oldest sedimentary material in this area, is of Lower Pleistocene age. Within each sedimentary unit, we analysed the pattern of land forms, soils and natural ecosystems. The Q0 and Q1 land units show a characteristic unstable drainage system, with frequent changes in the course of rivers and their affluents and diffluents. Soil genesis mainly correlates with the contrasting characteristics of the wet and dry tropical climate, and with the water regime of each land form on each sedimentary unit. So, a sequence from entisols, through inceptisols and alfisols, to ultisols, correlates with the sequence of land units from Q0 to Q3. Different vegetation types predominate on each land form/soil unit. Gallery forest (evergreen and semi-evergreen) exclusively occurs on Q0a entisols, semi-deciduous forest characterizes Q0b and Q1 inceptisols, semiseasonal savanna is almost entirely restricted to Q0 and Q1 units, hyperseasonal savanna widely dominates on Q2 and Q3 alfisols and ultisols, while seasonal savanna just occurs on the well-drained Q1 and Q2 alfisols, and on dunes. Main conclusions: The genesis and dynamics of the various land forms and soils throughout the Quaternary, provide the key to their particular hydrology, and determines the kind of plant formation able to occupy each habitat, thus explaining the complex pattern of quite different ecosystems found in the region. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_03050270_v28_n8_p985_Sarmiento
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Landscape evolution
Soil genesis
Tropical forests
Tropical savannas
Venezuelan Llanos
Water regime
Wetlands
ecosystem structure
floodplain
landscape ecology
landscape evolution
pedogenesis
Quaternary
savanna
water budget
Venezuela
spellingShingle Landscape evolution
Soil genesis
Tropical forests
Tropical savannas
Venezuelan Llanos
Water regime
Wetlands
ecosystem structure
floodplain
landscape ecology
landscape evolution
pedogenesis
Quaternary
savanna
water budget
Venezuela
Sarmiento, G.
Pinillos, M.
Patterns and processes in a seasonally flooded tropical plain: The Apure Llanos, Venezuela
topic_facet Landscape evolution
Soil genesis
Tropical forests
Tropical savannas
Venezuelan Llanos
Water regime
Wetlands
ecosystem structure
floodplain
landscape ecology
landscape evolution
pedogenesis
Quaternary
savanna
water budget
Venezuela
description Aim: The factors and processes determining the ecology and distribution of ecosystems in the Apure lowlands, Venezuela, are critically discussed. Location: The Middle Apure region, an alluvial Quaternary plain built by the Arauca and Apure rivers, occupies a subsidence area caused by faulting of the geological basement during the last and most active phases of the Andean uplift. Methods: To assess the determinants of the hydrological and ecological variability in this region, we used remote imagery and field surveys. Results: The hydrological and ecological variability responds to a set of interconnected processes of different nature: geological, climatic and paleoclimatic and hydrographic, which together have conditioned the geomorphological history of the regional landscape. This evolution, in turn, has guided the soil forming processes and the functional behaviour of the different types of savanna, forest and wetland ecosystems. The continuously subsiding trend of the Llanos that accompanied the Andean Orogeny, together with the Quaternary climatic oscillations, settled the framework in which successive depositional and erosional events took place. Five Quaternary depositional events, gave rise to the actual landscape pattern. The youngest, Q0a is the actual flood plain, Q0b is the Holocene flood plain, Q1 is from Upper Pleistocene, Q2 from Middle Pleistocene, while Q3 the oldest sedimentary material in this area, is of Lower Pleistocene age. Within each sedimentary unit, we analysed the pattern of land forms, soils and natural ecosystems. The Q0 and Q1 land units show a characteristic unstable drainage system, with frequent changes in the course of rivers and their affluents and diffluents. Soil genesis mainly correlates with the contrasting characteristics of the wet and dry tropical climate, and with the water regime of each land form on each sedimentary unit. So, a sequence from entisols, through inceptisols and alfisols, to ultisols, correlates with the sequence of land units from Q0 to Q3. Different vegetation types predominate on each land form/soil unit. Gallery forest (evergreen and semi-evergreen) exclusively occurs on Q0a entisols, semi-deciduous forest characterizes Q0b and Q1 inceptisols, semiseasonal savanna is almost entirely restricted to Q0 and Q1 units, hyperseasonal savanna widely dominates on Q2 and Q3 alfisols and ultisols, while seasonal savanna just occurs on the well-drained Q1 and Q2 alfisols, and on dunes. Main conclusions: The genesis and dynamics of the various land forms and soils throughout the Quaternary, provide the key to their particular hydrology, and determines the kind of plant formation able to occupy each habitat, thus explaining the complex pattern of quite different ecosystems found in the region.
format JOUR
author Sarmiento, G.
Pinillos, M.
author_facet Sarmiento, G.
Pinillos, M.
author_sort Sarmiento, G.
title Patterns and processes in a seasonally flooded tropical plain: The Apure Llanos, Venezuela
title_short Patterns and processes in a seasonally flooded tropical plain: The Apure Llanos, Venezuela
title_full Patterns and processes in a seasonally flooded tropical plain: The Apure Llanos, Venezuela
title_fullStr Patterns and processes in a seasonally flooded tropical plain: The Apure Llanos, Venezuela
title_full_unstemmed Patterns and processes in a seasonally flooded tropical plain: The Apure Llanos, Venezuela
title_sort patterns and processes in a seasonally flooded tropical plain: the apure llanos, venezuela
url http://hdl.handle.net/20.500.12110/paper_03050270_v28_n8_p985_Sarmiento
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