Mingying Quan, Wei Zhong, Xiaojun Wang, Bingxiang Wang, Tianhang Li
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引用次数: 0
Abstract
Understanding the responses of vegetation composition to climate, fire regimes and human disturbance is crucial to provide valuable insights to protect current and future ecosystems. However, relevant studies were poorly performed on the heavily forested montane areas in subtropic East Asia. In this study, we present pollen and charcoal records from a 95-cm long peat core in the subalpine Daping swamp in the western Nanling Mountains in subtropic China, to discuss the possible interactions among vegetation, fire, climatic change, and human activities in the late-Holocene. Our results suggest that the vegetation in the study area was composed of deciduous–evergreen mixed forests with few fire events during 3140–630 cal yr BP, and its changes were mainly controlled by climate with rare human impacts reflected by low concentrations of charcoals, low proportions of Poaceae pollen, and high AP/NAP ratios. After 630 cal yr BP, pollen data indicate an obvious shift from dense forests to more open landscape. The sharp increase of charcoal concentrations, the extremely low AP/NAP and increased Poaceae percentages suggest that this vegetation shift is not only impacted by the dry climate conditions, but also by the intensified deforestation due to enhanced human activities such as the slash-and-burn cultivation, etc. This study reveals a vital transitional timing from the natural to the superimposed anthropogenic forcing of vegetation composition and fire regimes at ~630 cal yr BP. Regional comparison of charcoal records indicates that the onset timing of intensified human disturbance in the inland montane areas is much later than that in the coastal areas in subtropic China. We infer the obstacle impacts of the montane terrain and the different responses of the dissemination of agriculture and enhanced population migration have played a crucial role in this asynchronous spreading pattern.
了解植被组成对气候、火情和人类干扰的反应,对于保护当前和未来的生态系统提供有价值的见解至关重要。然而,对东亚亚热带森林茂密的山地地区的相关研究却很少。在本研究中,我们提供了中国亚热带南岭西部亚高山大坪沼泽中一个95厘米长的泥炭芯的花粉和木炭记录,以讨论植被、火灾、气候变化和人类活动在全新世晚期的可能相互作用。我们的研究结果表明,研究区域的植被由落叶-常绿混合林组成,在3140–630年期间很少发生火灾 cal-yr-BP,其变化主要受气候控制,低浓度的木炭、低比例的禾本科花粉和高AP/NAP比率反映了罕见的人类影响。630之后 cal yr BP,花粉数据表明,从茂密的森林到更开阔的景观有了明显的转变。木炭浓度的急剧增加、极低的AP/NAP和禾本科植物百分比的增加表明,这种植被变化不仅受到干旱气候条件的影响,还受到人类活动(如刀耕火种)加强导致的森林砍伐加剧的影响。这项研究揭示了植被组成和火情从自然到人为叠加的重要过渡时间,约为630 cal yr BP。木炭记录的区域比较表明,中国亚热带内陆山区人类干扰加剧的发生时间远晚于沿海地区。我们推断,山地地形的障碍影响以及农业传播和人口迁移增强的不同反应在这种异步传播模式中发挥了至关重要的作用。
期刊介绍:
The Holocene is a high impact, peer-reviewed journal dedicated to fundamental scientific research at the interface between the long Quaternary record and the natural and human-induced environmental processes operating at the Earth''s surface today. The Holocene emphasizes environmental change over the last ca 11 700 years.