Abstract
Drought occurrence is increasing due to anthropogenic climate change. Drought can negatively affect plants via reduced water below-ground and increased evaporative demand or vapour pressure deficit (VPD) above-ground. Past work has shown that plant diversity can ameliorate the negative effects of drought in plant communities, but these results are inconsistent between experimental and natural drought studies. Furthermore, while studies on the negative effects of reduced soil moisture on plant growth in drought experiments are abundant, the effects of predicted increases in atmospheric VPD have been neglected. We directly manipulated atmospheric relative humidity in a biodiversity and drought experiment at the California State University, Los Angeles (CA, USA) under three atmospheric conditions (ambient, dehumidified and humidified), two treatments of native perennial grass diversity (monoculture and eight species polyculture) and two soil drought treatments (control and drought). We assessed both polyculture plant community and individual species (Poa secunda) responses to atmospheric drought and soil drought. We found that soil drought only limits above-ground biomass production when atmospheric conditions are also dry. We also found that P. secunda was limited by increased competition in polyculture when ambient atmospheric conditions were humid but was facilitated by diversity when atmospheric conditions were dry. Synthesis. Higher diversity ecosystems may be capable of protecting individual species from the negative effects of drought (facilitation). Without careful experimental manipulation of atmospheric drought, this important mechanism will be missed.
Original language | English (US) |
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Pages (from-to) | 1986-1999 |
Number of pages | 14 |
Journal | Journal of Ecology |
Volume | 109 |
Issue number | 5 |
DOIs | |
State | Published - May 2021 |
Externally published | Yes |
Bibliographical note
Publisher Copyright:© 2021 British Ecological Society
Keywords
- biodiversity
- climate change
- facilitation
- soil drought
- stress gradient hypothesis
- vapour pressure deficit