Oasis evolution and human activities in the central Tianshan Mountains of the Asian inland arid zone: Provenance and environmental reconstruction

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Catena Pub Date : 2024-09-20 DOI:10.1016/j.catena.2024.108410
Ao Yan , Jiangyong Wang , Xudong Liu , Jie Ma , Zhankui Bai , Dongmei Jie , Jihuai Yu
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Abstract

The Asian inland arid zone (AIAZ), the largest inland arid region in the world, forms the core area of the Silk Road. Despite its significance, we have limited knowledge about the sediment provenance in the oases and their evolutionary processes. Studying the evolution of oases is crucial for understanding the complex interactions among environmental changes, human history, and survival strategies in the AIAZ. This study provides insights into the interactions between oases and human populations and offers references for future oasis evolution, which is essential for ecological conservation and sustainable development. We investigated three key factors in the peat profile of oasis wetlands in the central Tianshan Mountains of the AIAZ: humification degree, TOC and grain size. Our goal was to identify the sediment provenance of the oases, reconstruct the sedimentary environment and evolutionary processes, and explore the relationship between the oases and human activities. Our results indicate that the sediments in the oasis wetlands of the central Tianshan Mountains primarily originate from the Kurban Tonggute Desert, the Gobi Desert in the intermountain basins, the Baiyang River floodplain, and weathered debris from the mountains brought about by glacial snowmelt. The transport of these sedimentary materials is primarily driven by wind and water. Oasis evolution is largely influenced by warm season temperatures and recharge from glacial snowmelt. Oases expand with increased glacial snowmelt recharge and contract when it decreases. The intensity of human activity has been closely related to the evolution of oases, as they provide crucial survival sites and resources for humans in arid zones. However, the ecology of these oases faces significant challenges due to global warming and intensified human activities. This paper proposes a series of measures based on our understanding of oasis evolution and sediment sources to provide a reference for oasis conservation and sustainable development.

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亚洲内陆干旱区天山中部绿洲的演变与人类活动:起源与环境重建
亚洲内陆干旱区(AIAZ)是世界上最大的内陆干旱区,也是丝绸之路的核心区域。尽管其重要性不言而喻,但我们对绿洲的沉积物来源及其演变过程的了解却十分有限。研究绿洲的演化过程对于了解亚非拉地区环境变化、人类历史和生存策略之间复杂的相互作用至关重要。这项研究深入揭示了绿洲与人类之间的互动关系,并为未来绿洲的演化提供了参考,这对生态保护和可持续发展至关重要。我们研究了亚非拉地区天山中部绿洲湿地泥炭剖面的三个关键因素:腐殖化程度、总有机碳和粒度。我们的目标是确定绿洲的沉积物来源,重建沉积环境和演化过程,并探索绿洲与人类活动之间的关系。我们的研究结果表明,天山中部绿洲湿地的沉积物主要来源于库尔班通古特沙漠、山间盆地戈壁滩、白杨河冲积平原以及冰川融雪带来的山体风化碎屑。这些沉积物的迁移主要受风和水的驱动。绿洲的演变主要受到暖季温度和冰川融雪补给的影响。当冰川融雪补给增加时,绿洲就会扩大;当冰川融雪补给减少时,绿洲就会缩小。人类活动的强度与绿洲的演化密切相关,因为绿洲为干旱地区的人类提供了重要的生存场所和资源。然而,由于全球变暖和人类活动加剧,这些绿洲的生态面临着巨大挑战。本文根据我们对绿洲演变和沉积物来源的认识,提出了一系列措施,为绿洲保护和可持续发展提供参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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