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Influences of 20th-century warming at the upper tree line contingent on local-scale interactions: evidence from a latitudinal gradient in the Rocky Mountains, USA

机译:20世纪上层树线变暖对局部尺度相互作用的影响:来自美国落基山脉的纬度梯度的证据

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AimsTwentieth-century climate, the spatial pattern of tree establishment and positive feedback influence upper tree line ecotones. Here, I investigate how these factors interact to gain a more holistic understanding of how broad-scale abiotic and local-scale site conditions regulate tree establishment within upper tree line ecotones.LocationA latitudinal gradient (c. 35-45 degrees N) in the US Rocky Mountains. Study sites (n = 22) were located in the Bighorn (BH), Medicine Bow (MB), Front Range (FR) and Sangre de Cristo (SDC) mountain ranges.MethodsDendroecological techniques were used to reconstruct tree establishment dates that were compared with 20th-century climate data using correlation and regime shift analyses. Spatial patterns of tree establishment were analysed by Ripley's K and used to determine local-scale interactions capable of ameliorating broad-scale climate inputs through positive feedback.ResultsSignificant correlations (P < 0.01) between tree establishment and climate were confined to the FR, where a positive correlation was found with summer (June-August) and cool season (November-April) temperature range (T-max - T-min). These trees were almost exclusively situated in a random spatial pattern. Similar patterns exist in the BH, yet their establishment was contingent on the availability of local shelter in the lee of boulders. Trees in the MB and SDC were primarily clustered in space and had no significant correlations with climate. Considerable lag times exist between regime shift changes in climate towards more favourable growing conditions and corresponding shifts in tree establishment in all mountain ranges except the FR, where synchronous shifts occurred in the early 1950s.Main conclusionsThese results suggest that the influence of broad-scale climate on upper tree line dynamics is contingent on the local-scale spatial patterns of tree establishment and related influences of positive feedback. This research has important implications for understanding how vegetation communities will respond to global climate change.
机译:目的是二十世纪的气候,树木树立的空间格局和正反馈影响上林线生态交错带。在这里,我研究了这些因素如何相互作用,以更全面地了解非生物性和局部规模的场地条件如何调节上林线生态交错带内的树木建立。位置美国的纬度梯度(约35-45度)落基山脉。研究地点(n = 22)位于比格霍恩(BH),梅迪辛鲍(MB),前线山脉(FR)和桑格里克里斯多(SDC)山脉。方法采用树状生态学技术重建树木的建立日期,与使用相关和政权转移分析的20世纪气候数据。通过Ripley的K分析树的空间分布格局,并通过积极的反馈来确定能够改善大规模气候输入的局部尺度相互作用。结果树的建立与气候之间的显着相关性(P <0.01)限于FR,其中与夏季(6月至8月)和凉爽季节(11月至4月)温度范围(T-max-T-min)呈正相关。这些树木几乎完全排在随机的空间格局中。 BH中也存在类似的模式,但它们的建立取决于在巨石背风处是否有当地庇护所。 MB和SDC中的树木主要聚集在空间中,与气候没有显着相关性。在气候变化向更有利的生长条件转变的过程中,以及除FR以外的所有山区,树木的建立都发生了相应的变化之间存在相当长的滞后时间,而FR在1950年代初发生了同步变化。主要结论这些结果表明,大规模气候的影响上层树线的动态取决于树的建立的局部尺度空间格局以及正反馈的相关影响。这项研究对于理解植被群落将如何应对全球气候变化具有重要意义。

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