Honghao Niu , Yuanhao Sun , Jiangyong Wang , Laurent Marquer , Jet Vessies , Dorothy Sack , Frank M. Chambers , Dongmei Jie
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Human impacts on ecosystems in the study area gradually intensified after 4 ka when societies entered the Bronze Age. In addition, we used a novel methodological approach on three pollen datasets for reconstructing the land cover and plant compositional changes of the three different studied landscapes (steppe, forest, and steppe-forest ecotone) in Northeast China. Results show that total land cover changes in forests were relatively low (i.e. stable) over the studied time period owing to their comparatively higher plant diversity whereas significant fluctuations occurred in the steppe and the steppe-forest ecotone. By comparing these results with regional climate records, climate change was found to dominate plant changes during two periods--before ca. 6 ka and after ca. 0.8 ka. In addition, during ca. 6–4 ka BP, even though climate still played the most significant role in vegetation changes, anthropogenic impacts on plant changes were revealed for the steppe-forest ecotone. During 4–2.3 ka BP, the anthropogenic impacts on plants gradually increased and became the dominant driving force, especially for the forest and steppe-forest ecotone during ca. 2.3–0.8 ka BP. These varied impacts of human activity and climate change on vegetation among the study areas can be related to </span>human migration trends and human subsistence patterns.</span></p></div>","PeriodicalId":50254,"journal":{"name":"Journal of Archaeological Science","volume":null,"pages":null},"PeriodicalIF":2.6000,"publicationDate":"2024-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Drivers of land cover and plant compositional changes in Northeast China since the mid-Holocene: Climate versus human activities\",\"authors\":\"Honghao Niu , Yuanhao Sun , Jiangyong Wang , Laurent Marquer , Jet Vessies , Dorothy Sack , Frank M. 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During 4–2.3 ka BP, the anthropogenic impacts on plants gradually increased and became the dominant driving force, especially for the forest and steppe-forest ecotone during ca. 2.3–0.8 ka BP. 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引用次数: 0
摘要
全新世中期以后,人类活动逐渐开始对土地植被和植物成分的变化产生显著影响。评估人类与气候对区域生态系统的影响程度和时空变化正成为当前全球变化研究的一个重点领域。本研究利用从 5473 个考古遗址中收集的 478 条 AMS 14C 测定记录,帮助评估中国东北地区史前人口规模的变化,这表明自全新世中期以来当地人类活动的性质发生了变化。研究结果表明,在约 7-4 ka 间期,史前人类活动的影响相对较小。除了两次小的波动之外,史前人类的影响在约 7-4 ka 期间一直处于相对较低的水平。4 ka以后,当社会进入青铜时代时,人类对研究地区生态系统的影响逐渐加剧。此外,我们还采用了一种新颖的方法,利用三个花粉数据集重建了中国东北地区三种不同研究景观(草原、森林和草原-森林生态带)的土地覆盖和植物组成变化。结果表明,由于森林的植物多样性相对较高,因此在所研究的时间段内,森林的总土地覆被变化相对较小(即稳定),而草原和草原-森林生态带则出现了显著的波动。通过将这些结果与区域气候记录进行比较,发现气候变化在两个时期主导了植物的变化--约 6 ka 之前和约 6 ka 之后。6 ka 和 ca.0.8 ka.此外,在约 6-4 ka BP 期间,尽管气候在植被变化中仍起着最重要的作用,但在草原-森林生态带,人为因素对植物变化的影响已经显现。在 4-2.3 ka BP 期间,人为活动对植物的影响逐渐增加,并成为主要的驱动力,尤其是在约 2.3-0.8 ka BP 期间对森林和草原-森林生态带的影响。人类活动和气候变化对研究地区植被的不同影响可能与人类迁徙趋势和人类生存模式有关。
Drivers of land cover and plant compositional changes in Northeast China since the mid-Holocene: Climate versus human activities
After the mid-Holocene, human activities gradually began having a notable impact on land cover and plant compositional changes. Evaluating the extent and spatiotemporal variations of the human versus climate impacts on regional ecosystems is becoming an area of focus of current global change research. The present study uses 478 AMS 14C dating records collected from 5473 archaeological sites to help evaluate variations in prehistoric population size in Northeast China, which suggest changes in the nature of human activities there since the mid-Holocene. Results indicate that prehistoric human impacts remained at a relatively low level during the ca. 7–4 ka interval except for two minor fluctuations. Human impacts on ecosystems in the study area gradually intensified after 4 ka when societies entered the Bronze Age. In addition, we used a novel methodological approach on three pollen datasets for reconstructing the land cover and plant compositional changes of the three different studied landscapes (steppe, forest, and steppe-forest ecotone) in Northeast China. Results show that total land cover changes in forests were relatively low (i.e. stable) over the studied time period owing to their comparatively higher plant diversity whereas significant fluctuations occurred in the steppe and the steppe-forest ecotone. By comparing these results with regional climate records, climate change was found to dominate plant changes during two periods--before ca. 6 ka and after ca. 0.8 ka. In addition, during ca. 6–4 ka BP, even though climate still played the most significant role in vegetation changes, anthropogenic impacts on plant changes were revealed for the steppe-forest ecotone. During 4–2.3 ka BP, the anthropogenic impacts on plants gradually increased and became the dominant driving force, especially for the forest and steppe-forest ecotone during ca. 2.3–0.8 ka BP. These varied impacts of human activity and climate change on vegetation among the study areas can be related to human migration trends and human subsistence patterns.
期刊介绍:
The Journal of Archaeological Science is aimed at archaeologists and scientists with particular interests in advancing the development and application of scientific techniques and methodologies to all areas of archaeology. This established monthly journal publishes focus articles, original research papers and major review articles, of wide archaeological significance. The journal provides an international forum for archaeologists and scientists from widely different scientific backgrounds who share a common interest in developing and applying scientific methods to inform major debates through improving the quality and reliability of scientific information derived from archaeological research.