Laura Höhn, Maria Leunda, Erika Gobet, Willy Tinner, Christoph Schwörer
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引用次数: 5
Abstract
Predicting the effects of ongoing climate warming on vegetation requires a long-term perspective of past ecosystem dynamics. We therefore analysed the sedimentary record from the mire Gola di Lago (985 m a.s.l.) in southern Switzerland, to better understand the vegetation response to past rapid climate change. We present a high-resolution pollen and plant macrofossil study from the Lateglacial to the Early Holocene (13 400–10 400 cal. a BP), a climatic transition that represents a close analogue to current global warming. The vegetation responses during this time match previously analysed palaeoecological sites south of the Alps. At the end of the Bølling-Allerød interstadial, the site was surrounded by open larch forest. The beginning of the Younger Dryas was characterized by the local presence and rapid expansion of Pinus cembra, whereas the second part was dominated by Pinus sylvestris, Betula and Larix decidua. These vegetation dynamics agree well with independent climate data indicating a cold and dry start and a subsequent shift to slightly warmer climate. The following rapid temperature increase at the beginning of the Holocene resulted in an increase in forest density and the establishment of novel temperate vegetation assemblages, without major changes in species diversity. Noteworthy, during the Younger Dryas–Early Holocene transition, long-lived cold-adapted tree line species such as P. cembra and L. decidua persisted over several centuries, while open boreal forests dominated by P. sylvestris and Betula expanded, indicating high resilience to climatic changes. The results of Gola di Lago suggest that climate warming led to a significant change in vegetation communities through species range shifts. Our study also indicates that some species may potentially be able to locally persist under current global warming, forming novel vegetation assemblages with newly establishing species.
预测持续的气候变暖对植被的影响需要对过去的生态系统动态有一个长期的看法。因此,我们分析了瑞士南部Gola di Lago泥沼(985 m a.s.l)的沉积记录,以更好地了解植被对过去快速气候变化的响应。本文介绍了从冰川期到全新世早期(13400 - 10400 cal)的高分辨率花粉和植物大化石研究。这是一种气候转变,与当前的全球变暖非常相似。在这段时间里,植被的反应与先前分析的阿尔卑斯山以南的古生态遗址相吻合。在Bølling-Allerød公路的尽头,场地被开阔的落叶松森林包围。新仙女木期初期以松在当地的存在和迅速扩张为特征,而新仙女木期则以松、桦木和落叶松为主。这些植被动态与独立的气候数据很好地吻合,这些数据表明,开始时气候寒冷干燥,随后气候转向略微温暖。随后在全新世开始的快速升温导致森林密度增加和新的温带植被组合的建立,物种多样性没有发生重大变化。值得注意的是,在新仙女木-全新世早期的过渡时期,长寿命的冷适应林系物种,如cembra和L. decidua持续了几个世纪,而以P. sylvestris和Betula为主的北方开阔森林则扩大了,表明对气候变化具有较高的适应能力。Gola di Lago的结果表明,气候变暖通过物种范围的变化导致了植被群落的显著变化。我们的研究还表明,在当前的全球变暖背景下,一些物种可能能够在局部持续存在,并与新建立的物种形成新的植被组合。
期刊介绍:
Boreas has been published since 1972. Articles of wide international interest from all branches of Quaternary research are published. Biological as well as non-biological aspects of the Quaternary environment, in both glaciated and non-glaciated areas, are dealt with: Climate, shore displacement, glacial features, landforms, sediments, organisms and their habitat, and stratigraphical and chronological relationships.
Anticipated international interest, at least within a continent or a considerable part of it, is a main criterion for the acceptance of papers. Besides articles, short items like discussion contributions and book reviews are published.