Population migration with improved productivity caused a heterogeneity pattern of Holocene vegetation succession in typical areas of the lower Yangtze region
Li Xiao, Xiaoyu Zhang, Jinqi Dai, Xueming Li, Ning Zhao, Shihao Liu, Jing Chen, Maotian Li, Yuanhao Sun, Haoyan Wang, Kai Li, Yan Liu, Qianli Sun
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引用次数: 0
Abstract
Climate fluctuations and human activities shaped vegetation dynamics during the Holocene, yet the underlying mechanisms remain elusive. Our investigation utilizes the MAT-REVEALS approach to analyze 17 fossil pollen records spanning the past 8500 years collected at three typical areas of the lower Yangtze: South Zhejiang Mountains (SZJM), Taihu Basin (THB), and Yaojiang Valley (YJV). The reconstructed vegetation in SZJM revealed a high proportion of arboreal content during 8500–2000 cal yr BP, and the vegetation succession generally followed the variation of mean annual temperature and precipitation, indicating the Asian monsoon climate dominated the vegetation change. Of note, the minor decline of the broadleaved forest at 6000–5000 cal yr BP coincided with the drop in winter temperature, indicating its role as a limiting factor for the broadleaved arboreal. A marked increase of herbs (15.6 % to 36.5 %) occurred in the coastal region of YJV at 7500–5000 cal yr BP, which was not registered in SZJM, was coeval with a surging population and the start of extensive and intensive rice farming on the newly formed alluvial plain, indicating this noticeable landscape openness was induced by anthropogenic factors. Conversely, significant anthropogenic modifications of vegetation only emerged after 5000 cal yr BP in the THB, likely linked to large immigrations of population and the establishment of the Liangzhu hierarchical state that consumed abundant arboreal resources for large-scale constructions. Since 3000–2000 cal yr BP, a widespread decline of arboreal proportion took place in all three areas, which was coeval with a sharp decline of winter temperature as well as the introduction of bronze and later iron to this region during the Spring and Autumn to Three Kingdoms period. Notably, the decline in forest cover in the SZJM region was relatively late. However, it accelerated in the recent millennium, matching the timing of new immigrants from northern China during the Tang-Song dynasties. Overall, natural vegetation changes mainly followed the pattern of monsoon rainfall and winter temperature variations. Nevertheless, the heterogeneity pattern of vegetation changes on the coast underscored the pivotal role of the spatial-temporal distribution of population and advancing technology. This study highlights the regional and local impact of climatic and anthropogenic forces on vegetation composition, providing new insights for interpreting the timing and scale of human impact on past land cover and land use changes.
在全新世期间,气候波动和人类活动塑造了植被动态,但潜在的机制仍然难以捉摸。本研究利用mat -揭示方法分析了在浙南、太湖盆地和姚江流域3个长江下游典型地区采集的17份8500年花粉化石记录。8500 ~ 2000 cal yr BP期间,长江三角洲植被的乔木含量占比较高,植被演替总体上服从年平均气温和降水的变化,表明亚洲季风气候主导了植被的变化。值得注意的是,在6000 ~ 5000 cal yr BP,阔叶林的轻微下降与冬季气温的下降相吻合,表明冬季气温对阔叶林的限制作用。7500 ~ 5000 cal yr BP期间,长江流域沿海地区草本植物显著增加(15.6% ~ 36.5%),而长江流域未记录到这一变化,这与人口激增和新形成的冲积平原开始广泛集约种植水稻同时发生,表明这种明显的景观开放是由人为因素引起的。相反,人类对THB地区植被的显著改变仅在5000 cal yr BP之后才出现,这可能与人口的大规模移民和良渚等级国家的建立有关,这些国家消耗了大量的树木资源进行大规模建设。自3000-2000 cal yr BP以来,这三个地区树木比例普遍下降,与冬季气温急剧下降以及春秋三国时期青铜和后来的铁传入该地区同时发生。值得注意的是,SZJM地区森林覆盖下降的时间相对较晚。然而,在最近的千年里,它加速了,与唐宋时期来自中国北方的新移民的时间相匹配。总体而言,自然植被变化主要遵循季风降水和冬季气温变化的格局。然而,沿海植被变化的异质性格局强调了人口时空分布和技术进步的关键作用。该研究强调了气候和人为力量对植被组成的区域和局部影响,为解释人类对过去土地覆盖和土地利用变化的影响时间和规模提供了新的见解。
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
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