Schwörer Christoph, Gobet Erika, van Leeuwen Jacqueline F N, Bögli Sarah, Imboden Rachel, van der Knaap W O, Kotova Nadezhda, Makhortykh Sergej, Tinner Willy
Institute of Plant Sciences, University of Bern, Altenbergrain 21, 3013 Bern, Switzerland.
Oeschger Centre for Climate Change Research, University of Bern, Hochschulstraße 4, 3012 Bern, Switzerland.
Veg Hist Archaeobot. 2022;31(2):155-170. doi: 10.1007/s00334-021-00844-z. Epub 2021 Jun 21.
Observing natural vegetation dynamics over the entire Holocene is difficult in Central Europe, due to pervasive and increasing human disturbance since the Neolithic. One strategy to minimize this limitation is to select a study site in an area that is marginal for agricultural activity. Here, we present a new sediment record from Lake Svityaz in northwestern Ukraine. We have reconstructed regional and local vegetation and fire dynamics since the Late Glacial using pollen, spores, macrofossils and charcoal. Boreal forest composed of and with continental and established in the region around 13,450 cal bp, replacing an open, steppic landscape. The first temperate tree to expand was at 11,800 cal bp, followed by , and ca. 1,000 years later. Fire activity was highest during the Early Holocene, when summer solar insolation reached its maximum. and established at ca. 6,000 cal bp, coinciding with the first indicators of agricultural activity in the region and a transient climatic shift to cooler and moister conditions. Human impact on the vegetation remained initially very low, only increasing during the Bronze Age, at ca. 3,400 cal bp. Large-scale forest openings and the establishment of the present-day cultural landscape occurred only during the past 500 years. The persistence of highly diverse mixed forest under absent or low anthropogenic disturbance until the Early Middle Ages corroborates the role of human impact in the impoverishment of temperate forests elsewhere in Central Europe. The preservation or reestablishment of such diverse forests may mitigate future climate change impacts, specifically by lowering fire risk under warmer and drier conditions.
The online version contains supplementary material available at 10.1007/s00334-021-00844-z.
由于自新石器时代以来人类干扰普遍且不断增加,在中欧观察全新世整个时期的自然植被动态变化颇具难度。一种将此限制降至最低的策略是在农业活动边缘地区选择一个研究地点。在此,我们展示了乌克兰西北部斯维佳兹湖的一份新的沉积物记录。我们利用花粉、孢子、大化石和木炭重建了晚冰期以来的区域和局部植被及火灾动态变化。由[具体树种1]和[具体树种2]组成、伴有大陆性[具体树种3]和[具体树种4]的北方森林于约13450 cal bp在该地区形成,取代了开阔的草原景观。最早扩张的温带树木是[具体树种5],出现在11800 cal bp,约1000年后[具体树种6]、[具体树种7]和[具体树种8]也相继出现。火灾活动在全新世早期最为频繁,当时夏季太阳辐射达到最大值。[具体树种9]和[具体树种10]于约6000 cal bp形成,与该地区农业活动的首批迹象以及向更凉爽湿润气候条件的短暂转变同时出现。人类对植被的影响最初非常小,仅在青铜时代(约3400 cal bp)有所增加。大规模森林砍伐和当今文化景观的形成仅发生在过去500年。在缺乏或人为干扰较低的情况下,高度多样化的混交林一直持续到中世纪早期,这证实了人类影响在中欧其他地区温带森林 impoverishment 中的作用。保护或重新建立这种多样化的森林可能会减轻未来气候变化的影响,特别是在温暖干燥条件下降低火灾风险。
在线版本包含可在10.1007/s00334-021-00844-z获取的补充材料。