High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity

Published version. Source at http://dx.doi.org/10.1088/1748-9326/11/12/125006 The duration of specific periods within a plant’s life cycle are critical for plant growth and performance. In the High Arctic, the start of many of these phenological periods is determined by snowmelt date, which may chan...

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Published in:Environmental Research Letters
Main Authors: Semenchuk, Philipp, Gillespie, Mark, Rumpf, Sabine Bettina, Baggesen, Nanna Schrøder, Cooper, Elisabeth J.
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2016
Subjects:
Online Access:https://hdl.handle.net/10037/10430
https://doi.org/10.1088/1748-9326/11/12/125006
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/10430 2023-05-15T14:26:10+02:00 High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity Semenchuk, Philipp Gillespie, Mark Rumpf, Sabine Bettina Baggesen, Nanna Schrøder Cooper, Elisabeth J. 2016-11-29 https://hdl.handle.net/10037/10430 https://doi.org/10.1088/1748-9326/11/12/125006 eng eng IOP Publishing Environmental Research Letters Semenchuk P, Gillespie M, Rumpf SB, Baggesen NS, Elberling B, Cooper E.J. High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity. Environmental Research Letters. 2016;11(12) FRIDAID 1435117 doi:10.1088/1748-9326/11/12/125006 1748-9326 https://hdl.handle.net/10037/10430 openAccess Spitsbergen Svalbard phenology phenophase phenoperiod growing-season length flowering VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480 VDP::Mathematics and natural science: 400::Zoology and botany: 480 Journal article Tidsskriftartikkel Peer reviewed 2016 ftunivtroemsoe https://doi.org/10.1088/1748-9326/11/12/125006 2021-06-25T17:55:03Z Published version. Source at http://dx.doi.org/10.1088/1748-9326/11/12/125006 The duration of specific periods within a plant’s life cycle are critical for plant growth and performance. In the High Arctic, the start of many of these phenological periods is determined by snowmelt date, which may change in a changing climate. It has been suggested that the end of these periods during late-season are triggered by external cues, such as day length, light quality or temperature, leading to the hypothesis that earlier or later snowmelt dates will lengthen or shorten the duration of these periods, respectively, and thereby affect plant performance.Wetested whether snowmelt date controls phenology and phenological period duration in High Arctic Svalbard using a melt timing gradient from natural and experimentally altered snow depths.Weinvestigated the response of early- and late-season phenophases from both vegetative and reproductive phenological periods of eight common species.Wefound that all phenophases follow snowmelt patterns, irrespective of timing of occurrence, vegetative or reproductive nature. Three of four phenological period durations based on these phenophases were fixed for most species, defining the studied species as periodic. Periodicity can thus be considered an evolutionary trait leading to disadvantages compared with aperiodic species and we conclude that the mesic and heath vegetation types in Svalbard are at risk of being outcompeted by invading, aperiodic species from milder biomes. Article in Journal/Newspaper Arctic Arctic Svalbard Spitsbergen University of Tromsø: Munin Open Research Archive Arctic Svalbard Environmental Research Letters 11 12 125006
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
topic Spitsbergen
Svalbard
phenology
phenophase
phenoperiod
growing-season length
flowering
VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480
VDP::Mathematics and natural science: 400::Zoology and botany: 480
spellingShingle Spitsbergen
Svalbard
phenology
phenophase
phenoperiod
growing-season length
flowering
VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480
VDP::Mathematics and natural science: 400::Zoology and botany: 480
Semenchuk, Philipp
Gillespie, Mark
Rumpf, Sabine Bettina
Baggesen, Nanna Schrøder
Cooper, Elisabeth J.
High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity
topic_facet Spitsbergen
Svalbard
phenology
phenophase
phenoperiod
growing-season length
flowering
VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480
VDP::Mathematics and natural science: 400::Zoology and botany: 480
description Published version. Source at http://dx.doi.org/10.1088/1748-9326/11/12/125006 The duration of specific periods within a plant’s life cycle are critical for plant growth and performance. In the High Arctic, the start of many of these phenological periods is determined by snowmelt date, which may change in a changing climate. It has been suggested that the end of these periods during late-season are triggered by external cues, such as day length, light quality or temperature, leading to the hypothesis that earlier or later snowmelt dates will lengthen or shorten the duration of these periods, respectively, and thereby affect plant performance.Wetested whether snowmelt date controls phenology and phenological period duration in High Arctic Svalbard using a melt timing gradient from natural and experimentally altered snow depths.Weinvestigated the response of early- and late-season phenophases from both vegetative and reproductive phenological periods of eight common species.Wefound that all phenophases follow snowmelt patterns, irrespective of timing of occurrence, vegetative or reproductive nature. Three of four phenological period durations based on these phenophases were fixed for most species, defining the studied species as periodic. Periodicity can thus be considered an evolutionary trait leading to disadvantages compared with aperiodic species and we conclude that the mesic and heath vegetation types in Svalbard are at risk of being outcompeted by invading, aperiodic species from milder biomes.
format Article in Journal/Newspaper
author Semenchuk, Philipp
Gillespie, Mark
Rumpf, Sabine Bettina
Baggesen, Nanna Schrøder
Cooper, Elisabeth J.
author_facet Semenchuk, Philipp
Gillespie, Mark
Rumpf, Sabine Bettina
Baggesen, Nanna Schrøder
Cooper, Elisabeth J.
author_sort Semenchuk, Philipp
title High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity
title_short High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity
title_full High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity
title_fullStr High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity
title_full_unstemmed High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity
title_sort high arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity
publisher IOP Publishing
publishDate 2016
url https://hdl.handle.net/10037/10430
https://doi.org/10.1088/1748-9326/11/12/125006
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Arctic
Svalbard
Spitsbergen
genre_facet Arctic
Arctic
Svalbard
Spitsbergen
op_relation Environmental Research Letters
Semenchuk P, Gillespie M, Rumpf SB, Baggesen NS, Elberling B, Cooper E.J. High Arctic plant phenology is determined by snowmelt patterns but duration of phenological periods is fixed: an example of periodicity. Environmental Research Letters. 2016;11(12)
FRIDAID 1435117
doi:10.1088/1748-9326/11/12/125006
1748-9326
https://hdl.handle.net/10037/10430
op_rights openAccess
op_doi https://doi.org/10.1088/1748-9326/11/12/125006
container_title Environmental Research Letters
container_volume 11
container_issue 12
container_start_page 125006
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