| Literature DB >> 31788223 |
Rebecca Lee Molinari1, Tara B B Bishop1, Matthew F Bekker2, Stanley G Kitchen3, Loreen Allphin1, Samuel B St Clair1.
Abstract
Human activities are changing patterns of ecological disturbance globally. In North American deserts, wildfire is increasing in size and frequency due to fuel characteristics of invasive annual grasses. Fire reduces the abundance and cover of native vegetation in desert ecosystems. In this study, we sought to characterize stem growth and reproductive output of a dominant native shrub in the Mojave Desert, creosote bush (Larrea tridentata (DC.) Coville) following wildfires that occurred in 2005. We sampled 55 shrubs along burned and unburned transects 12 years after the fires (2017) and quantified age, stem diameter, stem number, radial and vertical growth rates, and fruit production for each shrub. The shrubs on the burn transects were most likely postfire resprouts based on stem age while stems from unburn transects dated from before the fire. Stem and vertical growth rates for shrubs on burned transects were 2.6 and 1.7 times higher than that observed for shrubs on unburned transects. Fruit production of shrubs along burned transects was 4.7-fold more than shrubs along paired unburned transects. Growth rates and fruit production of shrubs in burned areas did not differ with increasing distance from the burn perimeter. Positive growth and reproduction responses of creosote following wildfires could be critical for soil stabilization and re-establishment of native plant communities in this desert system. Additional research is needed to assess if repeat fires that are characteristic of invasive grass-fire cycles may limit these benefits.Entities:
Keywords: Larrea tridentata; Mojave Desert; creosote bush; dendrochronology; fire ecology
Year: 2019 PMID: 31788223 PMCID: PMC6875574 DOI: 10.1002/ece3.5771
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
Figure 1The burned and unburned side of a fire boundary in the northeastern Mojave Desert 14‐year postfire
Figure 2Map of the fire extents and transect locations in the northeastern Mojave Desert study site near the Beaver Dam Wash (Latitude 37.0837 N, Longitude 114.0119 W, and elevation 1,216 m)
The average creosote stem age for each transect type from the study site is shown with ± SE
| Fire | Average stem age (years) |
|---|---|
| Unburned (U) | 16.6 ± 0.5 |
| Burn edge (E) | 12.1 ± 0.6 |
| Burn interior (I) | 11.1 ± 0.3 |
| U × E | 32.1** |
| E × I | 2.9 |
The lower portion of the table shows the F values from the mixed models.
Abbreviations: E, burn edge; I, burn interior; U, unburned.
Significance is denoted with asterisks: ** p < .01
Figure 3Cross sections from creosote stem samples collected from unburned (top), burn edge (bottom left), and burn interior transects (bottom right)
Figure 4(a) Mean stem radial growth and (b) vertical growth rates ± SE of creosote by burn condition and burn location. Significant differences (p < .05) are denoted by different letters
Figure 5Average fruit number per creosote by burn condition and location for each observed year ± SE. Unburned transects compared to burn edge transects (burn condition) had F = 18 and p = .0007, Year had an F = 2.0 and p = .2, and Burn condition*Year effect F = 0.3 and p = .7. Burn edge compared to burn interior (burn location) had F = 0.1 and p = .7, Year had F = 2.1 and p = .2, and Burn location*Year had F = 0.09 and p = .9
Figure 6Average number of fruits per unit creosote shrub volume by burn condition and location ± SE. Significant differences (p < .05) are indicated with differences in letters