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Climatic Legacies Drive Spatial Aggregation of Plants in Drylands
Benoît Pichon1, Sonia Kéfi1,2, Isabelle Gounand3
1ISEM, Univ Montpellier, CNRS, IRD, Montpellier, France.
Past climates significantly influence dryland vegetation patterns, impacting both cover and spatial aggregation. These climate legacies, potentially linked to soil properties, are as important as current climate conditions for understanding ecosystem resilience.
Area of Science:
- Ecology
- Paleoclimatology
- Dryland Ecosystems
Background:
- Dryland vegetation typically forms spatial patches separated by bare soil.
- Research has primarily focused on current climate and herbivory's impact on these patterns.
- Past climate conditions (climate legacies) may also influence present-day vegetation patterns.
Purpose of the Study:
- To investigate the effects of past and current climates on plant spatial patterns in drylands.
- To compare the magnitude of past versus current climate influences on vegetation cover and aggregation.
- To explore potential mechanisms, such as soil properties, linking climate legacies to vegetation patterns.
Main Methods:
- Integrated datasets on plant spatial patterns with paleoclimate data (mid-Holocene, last glacial maximum).
- Analyzed the influence of past and current climate variables on vegetation cover and spatial aggregation.
- Examined relationships between climate legacies, soil multifunctionality, and soil sand content.
Main Results:
- Past climates exert influences on vegetation cover comparable to current climates.
- Climate legacies have a stronger effect on the spatial aggregation of dryland vegetation than current climates.
- Long-lasting effects of past climates on soil properties (multifunctionality, sand content) may mediate vegetation pattern legacies.
Conclusions:
- Climate legacies play a crucial role in shaping current dryland vegetation patterns, particularly spatial aggregation.
- Understanding these legacies is essential for accurately assessing dryland functioning and resilience.
- This research highlights the importance of considering long-term climate dynamics and their effects on soil when studying ecosystems.
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