Abstract
A variety of patterns observed in ecosystems can
be explained by resource–concentration mechanisms. A
resource–concentration mechanism occurs when organisms
increase the lateral flow of a resource toward them, leading
to a local concentration of this resource and to its depletion
from areas farther away. In resource–concentration systems,
it has been proposed that certain spatial patterns could
indicate proximity to discontinuous transitions where an
ecosystem abruptly shifts from one stable state to another.
Here, we test this hypothesis using a model of vegetation
dynamics in arid ecosystems. In this model, a resource–
concentration mechanism drives a positive feedback between
vegetation and soil water availability. We derived the
conditions leading to bistability and pattern formation. Our
analysis revealed that bistability and regular pattern
formation are linked in our model. This means that, when
regular vegetation patterns occur, they indicate that the
system is along a discontinuous transition to desertification.
Yet, in real systems, only observing regular vegetation
patterns without identifying the pattern-driving mechanism
might not be enough to conclude that an ecosystem is along
a discontinuous transition because similar patterns can
emerge from different ecological mechanisms.
Original language | English |
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Pages (from-to) | 257-269 |
Number of pages | 13 |
Journal | Theoretical Ecology |
Volume | 3 |
Issue number | 4 |
DOIs | |
Publication status | Published - 2010 |
Keywords
- Resource-concentration
- Scale-dependent feedback
- Desertification
- Spatial organization