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迪纳拉阿尔卑斯山北部岩溶地貌复杂地形中的植物物候模式

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

作者信息

Jakob Aljaž, Breg Valjavec Mateja, Čarni Andraž

机构信息

Jovan Hadži Institute of Biology, Research Centre of the Slovenian Academy of Sciences and Arts, Novi trg 2, 1000 Ljubljana, Slovenia.

Department of Biology, Biotechnical Faculty, University of Ljubljana, Večna pot 111, 1000 Ljubljana, Slovenia.

出版信息

Plants (Basel). 2025 Apr 1;14(7):1093. doi: 10.3390/plants14071093.

Abstract

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.

摘要

在研究人为引起的气候变化及其对陆地生态系统的影响的背景下,植被物候学最近受到了关注。它通常在各种区域和时间尺度上进行研究。这项研究聚焦于迪纳拉阿尔卑斯山脉最北端的漏斗状凹地的微观尺度。目的是确定开花开始的时间,并将其与地形和生态条件联系起来。我们研究了:(1)沿着从顶部斜坡到漏斗状凹地底部划分为2米×2米样地的西北走向样带的植物区系梯度,并确定与该梯度相关的离散组;(2)给出它们的诊断物种和群落。结果表明,漏斗状凹地底部和较低斜坡上地面植被早春开花受到春季高湿度、养分有效性以及中生落叶林开阔树冠层的刺激。较高斜坡和喀斯特高原上的开花开始较晚,这是由于5月/6月的降水高峰以及嗜热落叶林开阔树冠层较高的温度和光照可用性。岩石裂缝和岩石地带夏末开花开始延迟是由于恶劣立地条件刺激的特殊生理现象。沿着漏斗状凹地地形梯度的物候模式与植被物候的一般模式相反。应该对漏斗状凹地土壤的作用进行进一步研究,以探讨其对物候的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0348/11991487/2d36d7e01d7c/plants-14-01093-g001.jpg

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