Phenological Plant Pattern in the Topographic Complex Karstic Landscape of the Northern Dinaric Alps

Vegetation phenology has lately gained attention in the context of studying human-induced climate change and its effects on terrestrial ecosystems. It is typically studied on various regional and temporal scales. This research focused on the microscale in dolines on the Northernmost part of the Dina...

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Main Authors: Aljaž Jakob, Mateja Breg Valjavec, Andraž Čarni
Format: Article
Language:English
Published: MDPI AG 2025-04-01
Series:Plants
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Online Access:https://www.mdpi.com/2223-7747/14/7/1093
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author Aljaž Jakob
Mateja Breg Valjavec
Andraž Čarni
author_facet Aljaž Jakob
Mateja Breg Valjavec
Andraž Čarni
author_sort Aljaž Jakob
collection DOAJ
description Vegetation phenology has lately gained attention in the context of studying human-induced climate change and its effects on terrestrial ecosystems. It is typically studied on various regional and temporal scales. This research focused on the microscale in dolines on the Northernmost part of the Dinaric Alps. The aim was to determine the timing of flowering onset and relate it to topographic and ecological conditions. We studied (1) the floristic gradient along N–W transects divided in 2 m × 2 m plots, from top slopes to the bottom of dolines, and identified discrete groups in relation to this gradient and (2) provided their diagnostic species and communities. The results indicate that the early spring onset of flowering of ground vegetation in the bottom and lower slopes of dolines is stimulated by high spring moisture and nutrient availability, as well as the open canopy of the mesophilous deciduous forests. The flowering onset on the upper slopes and karst plateau starts later, which is due to the precipitation peak in May/June and higher temperatures and light availability of the open canopy of thermophilous deciduous forests. The delayed onset of flowering in late summer in rocky crevices and rocky places is due to a particular physiology stimulated by the harsh site conditions. The phenology pattern along the doline topographic gradient is inverse to general patterns in vegetation phenology. Further study on the role of doline soils should be made to study their impact on phenology.
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spelling doaj-art-032ec96c22a9429bac871da5fb453eba2025-08-20T03:03:27ZengMDPI AGPlants2223-77472025-04-01147109310.3390/plants14071093Phenological Plant Pattern in the Topographic Complex Karstic Landscape of the Northern Dinaric AlpsAljaž Jakob0Mateja Breg Valjavec1Andraž Čarni2Jovan Hadži Institute of Biology, Research Centre of the Slovenian Academy of Sciences and Arts, Novi trg 2, 1000 Ljubljana, SloveniaAnton Melik Geographical Institute, Research Centre of the Slovenian Academy of Sciences and Arts, Novi trg 2, 1000 Ljubljana, SloveniaJovan Hadži Institute of Biology, Research Centre of the Slovenian Academy of Sciences and Arts, Novi trg 2, 1000 Ljubljana, SloveniaVegetation phenology has lately gained attention in the context of studying human-induced climate change and its effects on terrestrial ecosystems. It is typically studied on various regional and temporal scales. This research focused on the microscale in dolines on the Northernmost part of the Dinaric Alps. The aim was to determine the timing of flowering onset and relate it to topographic and ecological conditions. We studied (1) the floristic gradient along N–W transects divided in 2 m × 2 m plots, from top slopes to the bottom of dolines, and identified discrete groups in relation to this gradient and (2) provided their diagnostic species and communities. The results indicate that the early spring onset of flowering of ground vegetation in the bottom and lower slopes of dolines is stimulated by high spring moisture and nutrient availability, as well as the open canopy of the mesophilous deciduous forests. The flowering onset on the upper slopes and karst plateau starts later, which is due to the precipitation peak in May/June and higher temperatures and light availability of the open canopy of thermophilous deciduous forests. The delayed onset of flowering in late summer in rocky crevices and rocky places is due to a particular physiology stimulated by the harsh site conditions. The phenology pattern along the doline topographic gradient is inverse to general patterns in vegetation phenology. Further study on the role of doline soils should be made to study their impact on phenology.https://www.mdpi.com/2223-7747/14/7/1093climate changedolineecologyfloweringforestkarst
spellingShingle Aljaž Jakob
Mateja Breg Valjavec
Andraž Čarni
Phenological Plant Pattern in the Topographic Complex Karstic Landscape of the Northern Dinaric Alps
Plants
climate change
doline
ecology
flowering
forest
karst
title Phenological Plant Pattern in the Topographic Complex Karstic Landscape of the Northern Dinaric Alps
title_full Phenological Plant Pattern in the Topographic Complex Karstic Landscape of the Northern Dinaric Alps
title_fullStr Phenological Plant Pattern in the Topographic Complex Karstic Landscape of the Northern Dinaric Alps
title_full_unstemmed Phenological Plant Pattern in the Topographic Complex Karstic Landscape of the Northern Dinaric Alps
title_short Phenological Plant Pattern in the Topographic Complex Karstic Landscape of the Northern Dinaric Alps
title_sort phenological plant pattern in the topographic complex karstic landscape of the northern dinaric alps
topic climate change
doline
ecology
flowering
forest
karst
url https://www.mdpi.com/2223-7747/14/7/1093
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AT matejabregvaljavec phenologicalplantpatterninthetopographiccomplexkarsticlandscapeofthenortherndinaricalps
AT andrazcarni phenologicalplantpatterninthetopographiccomplexkarsticlandscapeofthenortherndinaricalps