The concept of stability in connection with the gallery forests of the Chaco region

This paper discusses the concept of stability in a concrete natural situation: the gallery forests in the Chaco region. On the basis of Pickett's definition of minimal structure, stability is considered as the response which enables a system to keep its (minimal and configurational) structure o...

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Autor principal: Sennhauser, E.B.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00423106_v94_n1_p1_Sennhauser
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spelling todo:paper_00423106_v94_n1_p1_Sennhauser2023-10-03T14:51:23Z The concept of stability in connection with the gallery forests of the Chaco region Sennhauser, E.B. Chaco Gallery forest dynamics Resilience River dynamic Stability gallery forest resilience stability Argentina, Chaco, Lower Bermejo Basin This paper discusses the concept of stability in a concrete natural situation: the gallery forests in the Chaco region. On the basis of Pickett's definition of minimal structure, stability is considered as the response which enables a system to keep its (minimal and configurational) structure once an alteration has taken place (Pickett et al. 1989). Resilience is, instead, another kind of response which enables the system to keep its minimal structure intact regardless of what might happen to its configurational structure. The system to be analysed is that of the gallery forests in the Lower Bermejo Basin, in Argentina, which is subject to intense river bed migrations and floods caused by this allochthonous watercourse. The effect of this alteration is analysed on different space-time scales. Locally floods behave as a completely unpredictable phenomena, starting a complex floristic changes mechanism that would eventually enable the system to recover its structure once the alteration is over. These forests appear to be resilient but little adaptable, with low resistence and low elasticity. The latter, when combined with the alternation's return interval, which is under the ecosystem's generation time, upset the theoretical stability conditions, thus making the system seem 'apparently unstable'. Regionally, instead, migrations act as regular and permanent phenomena (highly predictable) always affecting some part of the area. The autochthonous system river side forests have become adapted through evolution to this new situation, so much so that this phenomenon has become a part of the system's internal dynamics. Chaco physiognomy, were it not due to the allochthonous phenomena affecting it today, would certainly be very different from the present one. © 1991 Kluwer Academic Publishers. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00423106_v94_n1_p1_Sennhauser
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Chaco
Gallery forest dynamics
Resilience
River dynamic
Stability
gallery forest
resilience
stability
Argentina, Chaco, Lower Bermejo Basin
spellingShingle Chaco
Gallery forest dynamics
Resilience
River dynamic
Stability
gallery forest
resilience
stability
Argentina, Chaco, Lower Bermejo Basin
Sennhauser, E.B.
The concept of stability in connection with the gallery forests of the Chaco region
topic_facet Chaco
Gallery forest dynamics
Resilience
River dynamic
Stability
gallery forest
resilience
stability
Argentina, Chaco, Lower Bermejo Basin
description This paper discusses the concept of stability in a concrete natural situation: the gallery forests in the Chaco region. On the basis of Pickett's definition of minimal structure, stability is considered as the response which enables a system to keep its (minimal and configurational) structure once an alteration has taken place (Pickett et al. 1989). Resilience is, instead, another kind of response which enables the system to keep its minimal structure intact regardless of what might happen to its configurational structure. The system to be analysed is that of the gallery forests in the Lower Bermejo Basin, in Argentina, which is subject to intense river bed migrations and floods caused by this allochthonous watercourse. The effect of this alteration is analysed on different space-time scales. Locally floods behave as a completely unpredictable phenomena, starting a complex floristic changes mechanism that would eventually enable the system to recover its structure once the alteration is over. These forests appear to be resilient but little adaptable, with low resistence and low elasticity. The latter, when combined with the alternation's return interval, which is under the ecosystem's generation time, upset the theoretical stability conditions, thus making the system seem 'apparently unstable'. Regionally, instead, migrations act as regular and permanent phenomena (highly predictable) always affecting some part of the area. The autochthonous system river side forests have become adapted through evolution to this new situation, so much so that this phenomenon has become a part of the system's internal dynamics. Chaco physiognomy, were it not due to the allochthonous phenomena affecting it today, would certainly be very different from the present one. © 1991 Kluwer Academic Publishers.
format JOUR
author Sennhauser, E.B.
author_facet Sennhauser, E.B.
author_sort Sennhauser, E.B.
title The concept of stability in connection with the gallery forests of the Chaco region
title_short The concept of stability in connection with the gallery forests of the Chaco region
title_full The concept of stability in connection with the gallery forests of the Chaco region
title_fullStr The concept of stability in connection with the gallery forests of the Chaco region
title_full_unstemmed The concept of stability in connection with the gallery forests of the Chaco region
title_sort concept of stability in connection with the gallery forests of the chaco region
url http://hdl.handle.net/20.500.12110/paper_00423106_v94_n1_p1_Sennhauser
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