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意大利亚平宁山脉北部地中海山区森林对气候变化、火灾和人类活动的长期响应

Long-Term Responses of Mediterranean Mountain Forests to Climate Change, Fire and Human Activities in the Northern Apennines (Italy).

作者信息

Morales-Molino César, Steffen Marianne, Samartin Stéphanie, van Leeuwen Jaqueline F N, Hürlimann Daniel, Vescovi Elisa, Tinner Willy

机构信息

Institute of Plant Sciences and Oeschger Centre for Climate Change Research, University of Bern, Altenbergrain 21, CH-3013 Bern, Switzerland.

Swiss Federal Institute for Forest, Snow and Landscape Research WSL, A Ramél 18, CH-6593 Cadenazzo, Switzerland.

出版信息

Ecosystems. 2021;24(6):1361-1377. doi: 10.1007/s10021-020-00587-4. Epub 2020 Dec 2.

Abstract

(beech) dominates the montane forests of the Apennines and builds old-growth high-conservation value stands. However, recent severe drought-induced diebacks raise concern on the future persistence of these forests and of Southern European mesophilous woodlands overall, growing at their dry edge. To explore the history of Apennine beech-dominated forests, we draw on the multiproxy paleoecological record from Lago Verdarolo, which includes a robust vegetation-independent temperature reconstruction. Numerical techniques are used to investigate the drivers of long-term Mediterranean mountain forest dynamics. Specifically, we focus on disentangling the ecological factors that caused the shift from high-diversity mixed forests to beech-dominated stands and on assessing the occurrence of legacy effects on present-day forests. Abrupt climate change largely drove vegetation dynamics during the Late Glacial and Early Holocene. Species-rich mixed (silver fir) forests dominated about 10,500-5500 years ago, under rather dry and warmer-than-today conditions (+ 1-2 °C) and limited fire occurrence. Cooler and moister summers and increasing fire activity caused declines in several fire-sensitive temperate deciduous trees (for example, ) and favored the establishment of fir-beech forests around 5500 years ago. Further enhancement of fire activity and farming around 2000 years ago led to local extinction and forest impoverishment. We conclude that the currently widespread monospecific Apennine beech forests are the result of multi-millennial land-use intensification superimposed on Late Holocene cooling and moistening. Given their higher drought-tolerance compared to beech stands, reviving ancient species-rich mixed fir forests represents a feasible and 'tested' possibility to adapt forests to climate change.

摘要

山毛榉主导着亚平宁山脉的山地森林,并形成了具有高保护价值的原始林。然而,近期由严重干旱引发的树木死亡事件引发了人们对这些森林以及整个生长在其干旱边缘的南欧中生林地未来存续的担忧。为了探究亚平宁山毛榉主导森林的历史,我们利用了韦尔达罗洛湖的多指标古生态记录,其中包括一个可靠的与植被无关的温度重建。数值技术被用于研究地中海山区森林长期动态变化的驱动因素。具体而言,我们专注于厘清导致从高多样性混交林向山毛榉主导林分转变的生态因素,并评估对当今森林的遗留效应的发生情况。在末次冰期晚期和全新世早期,气候突变在很大程度上推动了植被动态变化。大约在10500 - 5500年前,物种丰富的混交林(银冷杉)在相当干燥且比现今温暖(+1 - 2°C)且火灾发生有限的条件下占主导地位。更凉爽湿润的夏季以及火灾活动的增加导致了几种对火敏感的温带落叶树(例如……)数量减少,并在大约5500年前有利于冷杉 - 山毛榉林的形成。大约2000年前火灾活动和农业的进一步增强导致了当地……灭绝和森林贫瘠化。我们得出结论,目前广泛分布的亚平宁单种山毛榉林是在全新世晚期降温与湿润叠加的数千年土地利用集约化的结果。鉴于与山毛榉林相比,它们具有更高的耐旱性,恢复古代物种丰富的混交冷杉林是使森林适应气候变化的一种可行且“经过验证”的可能性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/740e/8550115/d6d2b7b3e144/10021_2020_587_Fig1_HTML.jpg

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