Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadow

dc.contributor.authorDurney, J. Simone
dc.contributor.authorEngel, Arden
dc.contributor.authorDebinski, Diane M.
dc.contributor.authorBurkle, Laura A.
dc.date.accessioned2022-12-06T23:38:07Z
dc.date.available2022-12-06T23:38:07Z
dc.date.issued2022-08
dc.description.abstractClimate 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.en_US
dc.identifier.citationDurney, J. Simone,Arden Engel, Diane M. Debinski, and LauraA. Burkle. 2022.“Earlier Spring Snowmelt DrivesArrowleaf Balsamroot Phenology in MontaneMeadows.”Ecosphere13(8): e4198.https://doi.org/10.1002/ecs2.4198en_US
dc.identifier.issn2150-8925
dc.identifier.urihttps://scholarworks.montana.edu/handle/1/17456
dc.language.isoen_USen_US
dc.publisherWileyen_US
dc.rightscc-byen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.subjectarrowleaf balsamrooten_US
dc.subjectclimate changeen_US
dc.subjectflower durationen_US
dc.subjectflower onseten_US
dc.subjectGreater YellowstoneEcosystemen_US
dc.subjectmaximum floral displayen_US
dc.subjectmontane meadowsen_US
dc.subjectphenologyen_US
dc.subjectsnowpackmanipulationen_US
dc.subjecttemperature manipulationen_US
dc.titleEarlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadowen_US
dc.typeArticleen_US
mus.citation.extentfirstpage1en_US
mus.citation.extentlastpage14en_US
mus.citation.issue8en_US
mus.citation.journaltitleEcosphereen_US
mus.citation.volume13en_US
mus.data.thumbpage6en_US
mus.identifier.doi10.1002/ecs2.4198en_US
mus.relation.collegeCollege of Letters & Scienceen_US
mus.relation.departmentEcology.en_US
mus.relation.universityMontana State University - Bozemanen_US

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