4.5 Article

Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows

期刊

ECOSPHERE
卷 13, 期 8, 页码 -

出版社

WILEY
DOI: 10.1002/ecs2.4198

关键词

arrowleaf balsamroot; climate change; flower duration; flower onset; Greater Yellowstone Ecosystem; maximum floral display; montane meadows; phenology; snowpack manipulation; temperature manipulation

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资金

  1. Decagon Devices
  2. Xerces Society
  3. Center for Global and Regional Environmental Research
  4. Iowa State University Department of Ecology, Evolution, and Organismal Biology
  5. Iowa State University Graduate Program in Ecology and Evolutionary Biology
  6. Montana State University
  7. Disney Conservation Fund
  8. University of Wyoming NPS Research Station

向作者/读者索取更多资源

Climate change is altering species' response to environmental cues, potentially leading to phenological mismatches. This research shows that a combination of warming and earlier snowmelt can advance and extend flower blooming, providing more resources for pollinators. Short-term studies may underestimate the effects of climate change on plant phenology.
Climate change is shifting phenology globally, altering when and how species respond to environmental cues such as temperature and the timing of snowmelt. These shifts may result in phenological mismatches among interacting species, creating cascading effects on community and ecosystem dynamics. Using passive warming structures and snow removal, we examined how experimentally increased temperatures, earlier spring snowmelt, and the poorly understood interaction between warming and earlier spring snowmelt affected flower onset, flowering duration, and maximum floral display of the spring-flowering montane species, arrowleaf balsamroot (Balsamorhiza sagittata), over a 7-year period. Additionally, potential cumulative effects of treatments were evaluated over the study duration. The combination of heating with snow removal led to earlier flower onset, extended flowering duration, and increased maximum floral display. While there was year-to-year variation in floral phenology, the effect of heating with snow removal on earlier onset and maximum floral display strengthened over time. This suggests that short-term studies likely underestimate the potential for climate change to influence phenological plant traits. Overall, this research indicates that B. sagittata's flowering onset responded more strongly to snow removal than to heating, but the combination of heating with snow removal allowed plants to bloom earlier, longer, and more profusely, providing more pollinator resources in spring. If warming and early snowmelt cause similar responses in other plant species, these patterns could mitigate phenological mismatches with pollinators by providing a wider window of time for interaction and resiliency in the face of change. This example demonstrates that a detailed understanding of how spring-flowering plants respond to specific aspects of predicted climatic scenarios will improve our understanding of the effects of climate change on native plant-pollinator interactions in montane ecosystems. Studies like this help elucidate the long-term physiological effects of climate-induced stressors on plant phenology in long-lived forbs.

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