Department of Geosciences, National Taiwan University, Taipei, Taiwan.
Institute for Geosciences, University of Potsdam, Potsdam, Germany.
Sci Total Environ. 2023 Mar 25;866:161300. doi: 10.1016/j.scitotenv.2022.161300. Epub 2022 Dec 31.
Human activities impose significant changes on sedimentation processes and vegetation cover within lake catchments. However, the needed time for an anthropogenically disturbed natural state to be reversed back to its natural state by environmental protection programs is still ambiguous. Here we employ a multi-proxy approach to delineate major environmental disturbances such as logging and forest fires on the catchment in Cueifong Lake, a subtropical subalpine lake in northeastern Taiwan. X-ray Fluorescence (XRF) core scanning, bulk total organic carbon (TOC), bulk total nitrogen (TN), stable carbon isotope (δC) analysis, and macro-charcoal counting were utilized to reconstruct changes in the catchment environment based on a sediment core from Cueifong Lake. The results show that the element content changed distinctly around 1975 CE, which coincided with the onset of profound deforestation in the lake vicinity recorded in historical documents and aerial photos. After the cessation of the logging event, the detrital input increased, accompanied by decreasing C/N ratios and increasing δC values. This suggests that increased terrestrial nutrient input promoted algae growth. After the deforestation phase, our results imply a gradual recovery of elemental composition in the catchment environment. By extrapolating the XRF element records, we suggest that it might take >50 years for the sedimentary regime to reach its pre-logging baseline. In contrast to the depositional system, the C/N and δC shifted significantly - potentially irreversibly - towards an algae-dominant environment instead of recovering to the pre-logging condition. This could be due to both 1) the changes in the different vegetation species used for reforestation and/or 2) anthropogenically introduced fishes in the 1980s. This study proposes the first assessment of the needed recovery time for subtropical Asian subalpine forests after large-scale logging activity and thus provides an apparent reference for policy decisions on natural resource development and environmental protection.
人类活动对湖泊流域的沉积过程和植被覆盖产生了重大影响。然而,通过环境保护计划将人为干扰的自然状态恢复到自然状态所需的时间仍然不清楚。在这里,我们采用多指标方法来划定主要的环境干扰,如在台湾东北部亚热带亚高山湖泊翠峰湖流域的伐木和森林火灾。我们利用 X 射线荧光(XRF)核心扫描、总有机碳(TOC)、总氮(TN)、稳定碳同位素(δC)分析和宏观木炭计数,根据翠峰湖的一个沉积核心来重建流域环境的变化。结果表明,元素含量在大约 1975 年左右发生了明显变化,与历史文献和航空照片记录的附近湖泊大规模森林砍伐的开始时间相吻合。在伐木事件停止后,碎屑输入增加,同时 C/N 比值降低,δC 值增加。这表明增加的陆地养分输入促进了藻类生长。在森林砍伐阶段之后,我们的结果表明流域环境中的元素组成逐渐恢复。通过外推 XRF 元素记录,我们建议沉积体系可能需要超过 50 年才能达到其伐木前的基线。与沉积系统相反,C/N 和 δC 显著变化——可能是不可逆转的——向以藻类为主的环境转变,而不是恢复到伐木前的状态。这可能是由于 1)用于重新造林的不同植被物种的变化和/或 2)20 世纪 80 年代人为引入的鱼类。本研究首次评估了亚热带亚洲亚高山森林在大规模伐木活动后的恢复时间,为自然资源开发和环境保护的政策决策提供了明显的参考。