2018 ESA Annual Meeting (August 5 -- 10)

OOS 35-5 - Will plant communities change more quickly in refugia? A biogeographic and landscape perspective

Thursday, August 9, 2018: 2:50 PM
343, New Orleans Ernest N. Morial Convention Center
David Ackerly, Integrative Biology & Environmental Science, Policy, and Management, UC Berkeley, Berkeley, CA, Matthew Kling, Integrative Biology, UC Berkeley, Meagan F. Oldfather, Integrative Biology, UC Berkeley, Berkeley, CA and Prahlada D. Papper, Department of Integrative Biology, University of California, Berkeley
Background/Question/Methods

Species distributions within local landscapes often mirror broader scale biogeographic patterns. For example, species restricted to cool and/or moist locations in a local landscape (potential refugia) will usually occur in cooler/moister geographies at a regional scale. In addition, restriction to refugial sites within landscapes may indicate that the species are at the hot/dry edge of their range, and thus represent trailing edge populations that would be susceptible to a warming climate. We test the hypothesis that refugial sites may be particularly sensitive to climate change because 1) they are preferentially occupied by trailing edge populations, and 2) because warmer-adapted immigrants will be located nearby on the landscape, reducing dispersal limitation to these sites.

Results/Conclusions

At a local scale (Pepperwood Preserve, California, USA), we found that tree communities on cooler topographic positions have greater potential for shifts in community composition due to predominance of cool-adapted species near their warm/dry climatic limits, and presence of hotter adapted species at low abundance, coupled with abundant seed sources from nearby hotter sites. Similarly, at a regional scale, minimum dispersal distances for arrival of new, hotter adapted species are lower for communities in cool and moist regions. These analyses suggest that communities occupying cool and/or moist landscape locations may exhibit more rapid biotic change in response to a warming climate.