Fungal spore record of pastoralism on the NE Qinghai-Tibetan Plateau since the middle Holocene
NE Qinghai 西藏的高原上的田园情趣的真菌的孢子记录自从中间的 Holocene作者机构:Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake ResourcesQinghai Institute of Salt LakesChinese Academy of SciencesXining 810008China Qinghai Provincial Key Laboratory of Geology and Environment of Salt LakesQinghai Institute of Salt LakesChinese Academy of SciencesXining 810008China Qinghai Provincial Key Laboratory of Physical Geography and Environmental ProcessesSchool of Geographic ScienceQinghai Normal UniversityXining 810008China Academy of Plateau Science and SustainabilityQinghai Normal UniversityXining 810008China
出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))
年 卷 期:2021年第64卷第8期
页 面:1318-1331页
核心收录:
学科分类:070905[理学-第四纪地质学] 0709[理学-地质学] 07[理学]
基 金:supported by the National Natural Science Foundation of China(Grant No.41877455) the Science and Technology Innovation Platform Project of Qinghai Province(Grant No.2020-ZJ-T06) the Open Foundation of State Key Laboratory of Paleobiology and Stratigraphy(Nanjing Institute of Geology and Palaeontology,CAS Grant No.183123) the Second Tibetan Plateau Scientific Expedition and Research Program(STEP)(Grant No.2019QZKK0805)
主 题:Coprophilous fungal spores Pastoralism Qinghai Lake basin Holocene Qinghai-Tibetan Plateau
摘 要:Pastoralism is considered a crucial factor in the eventual year-round occupation of high-altitude regions(3000 m asl)of the Qinghai-Tibetan Plateau,and the northeastern Qinghai-Tibetan Plateau(NE-QTP)was an important corridor for early human *** analyzed fossil fungal spore records for the last 8500 years from a high resolution aeolian section at Langgeri(LGR)on the ***-two fungal spore types were identified in the LGR section,including seven coprophilous *** combined analysis of coprophilous fungal spores,Cyperaceae,Artemisia,and Hippophae pollen,and the charcoal50µm fraction to explore the timing and controls of pastoralism on the NE-QTP since the middle *** commenced at LGR shortly before ca.5.5 ka and gradually increased between ca.5.5–3.5 ka,but markedly intensified after ca.2.2 ka,with three periods of growth at ca.2.1–1.9,1.4–1.2,and 0.6–0 ka,and a decline at ca.1.1–0.6 *** timing of changes in pastoral activity on the NE-QTP based on the coprophilous fungal spore record is supported by regional archeology and historical *** and political developments,rather than climate change,played key roles in the long-term fluctuations of regional pastoralism on the NE-QTP in the late Holocene.