The ecohydrology of ecosystem transitions: a meta‐analysis
A vast body of literature demonstrated that anthropogenic disturbances such as overgrazing and fire are key drivers of abrupt transition between vegetation types in ecosystems. In this study, we propose that the hydrological context (described in terms of rainfall, evapotranspiration and water yield) is a first‐order, primordial determinant of the propensity of ecosystems to undergo transition. This implies that the anthropogenic disturbance is a second‐order determinant that is strongly conditioned by the first one. Through the meta‐analysis of existing studies, a collection of 685 geo‐referenced study cases was organized to study the hydrological characteristics of three climatic regions and three ecosystems that vary in their relation between woody and grassy plants. Thus, humid, sub‐humid and dry climatic regions, respectively, receiving >1000, 500–1000 and <500 mm year−1, were studied, and possible transition mechanisms among grasslands/savannas, shrublands and forests were analysed. The results showed that the ecohydrological context determines the probabilities of ecosystems transitions in different climatic regions and the prevalence of alternative transition mechanisms. We showed that transition of forests into other ecosystems is highly improbable in high‐precipitation regions, more probable and likely subject to a bi‐stable and reversible regime in sub‐humid regions, and highly probable and irreversible in dry regions. Factors such as runoff, deep‐water drainage, fire, flammable/nonflammable biomass and overgrazing were considered as hypothetical transition mechanisms. As a novel finding, we demonstrate that ecohydrology, as a determinant of transition, is a factor that operates at a hierarchical level higher than that of the human‐driven disturbance. A synthetic graphical model was proposed to characterize resilience (the capacity of ecosystems to withstand transition) in the three study climatic regions.
| Main Authors: | , , , , |
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| Format: | info:ar-repo/semantics/artículo biblioteca |
| Language: | eng |
| Published: |
Wiley
2015-07
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| Subjects: | Hydrology, Ecosystems, Evapotranspiration, Resilience, Anthropogenic Factors, Woody Plants, Hidrología, Ecosistema, Evapotranspiración, Resiliencia Frente a Impactos y Crisis, Factores Antropogénicos, Plantas Leñosas, Ecosystems Conversion, |
| Online Access: | http://hdl.handle.net/20.500.12123/4943 https://onlinelibrary.wiley.com/doi/full/10.1002/eco.1540 https://doi.org/10.1002/eco.1540 |
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| Summary: | A vast body of literature demonstrated that anthropogenic disturbances such as overgrazing and fire are key drivers of abrupt transition between vegetation types in ecosystems. In this study, we propose that the hydrological context (described in terms of rainfall, evapotranspiration and water yield) is a first‐order, primordial determinant of the propensity of ecosystems to undergo transition. This implies that the anthropogenic disturbance is a second‐order determinant that is strongly conditioned by the first one. Through the meta‐analysis of existing studies, a collection of 685 geo‐referenced study cases was organized to study the hydrological characteristics of three climatic regions and three ecosystems that vary in their relation between woody and grassy plants. Thus, humid, sub‐humid and dry climatic regions, respectively, receiving >1000, 500–1000 and <500 mm year−1, were studied, and possible transition mechanisms among grasslands/savannas, shrublands and forests were analysed. The results showed that the ecohydrological context determines the probabilities of ecosystems transitions in different climatic regions and the prevalence of alternative transition mechanisms. We showed that transition of forests into other ecosystems is highly improbable in high‐precipitation regions, more probable and likely subject to a bi‐stable and reversible regime in sub‐humid regions, and highly probable and irreversible in dry regions. Factors such as runoff, deep‐water drainage, fire, flammable/nonflammable biomass and overgrazing were considered as hypothetical transition mechanisms. As a novel finding, we demonstrate that ecohydrology, as a determinant of transition, is a factor that operates at a hierarchical level higher than that of the human‐driven disturbance. A synthetic graphical model was proposed to characterize resilience (the capacity of ecosystems to withstand transition) in the three study climatic regions. |
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