Holocene Vegetation History and Environmental Change in the Lǎpuş Mountains, North-West Romania

Holocene Vegetation History and Environmental Change in the Lǎpuş Mountains, North-West Romania
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罗马尼亚西北部 LÇpuÅ 山脉全新世植被历史和环境变化

DOI:
10.1080/01916122.2019.1615567
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发表时间:
2019
期刊:
影响因子:
1.5
通讯作者:
C. Metzner-Nebelsick
C. Metzner-Nebelsick
中科院分区:
地球科学3区
文献类型:
--
作者:
M. Peters;A. Friedmann;Ph. Stojakowitz;C. Metzner-Nebelsick

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花粉分析支持25加速器质谱(AMS)14 C日期从Tjuul Negru泥炭沼泽(1143米)在Ljupuju山脉(东喀尔巴阡山脉,罗马尼亚)被用来重建全新世植被历史的山区。在Tubul Negru的植被记录开始于10,500 cal yr BP,以云杉(云杉)和榆树(榆树)为主的茂密山地森林。Corylus avellana(榛)在10,000 cal yr BP后传播,并在9000和7000 cal yr BP之间达到最大频率,然后下降。此后,云杉在森林中与鹅耳枥(角材)扩展后5700卡yr BP,达到最大代表性4200卡yr BP。山毛榉(山毛榉)蔓延从4800卡yr BP起,在3700卡yr BP左右的短期下降。此后又恢复了大规模的扩张,导致云杉、榛属和榆树的最终衰退。小规模的人类影响的景观(谷物型花粉粒,禾本科,和Plantago lanceolata)后,首次出现6000卡年BP。进一步的人为影响后检测到5000卡年BP,2300卡年BP和第十二世纪AD与定期和增加出现的主要和次要文化指标之间的稍强。在过去的500年里,低地和丘陵地带的大规模森林砍伐以及更多的农业导致了现代文化景观的发展。
Pollen analysis supported by 25 accelerator mass spectrometry (AMS)14C dates from the Tăul Negru peat bog (1143 m) in the Lăpuş Mountains (Eastern Carpathians, Romania) is used to reconstruct the Holocene vegetation history of this mountain region. The vegetation record at Tăul Negru starts atc.10,500 cal yr BP with dense montane forests dominated byPicea abies(spruce) andUlmus(elm).Corylus avellana(hazel) spread after 10,000 cal yr BP and reached maximum frequencies between 9000 and 7000 cal yr BP before decreasing. Thereafter,Piceaprevailed in the forests withCarpinus betulus(hornbeam) expanding after 5700 cal yr BP, attaining maximum representation at 4200 cal yr BP.Fagus sylvatica(beech) spread from 4800 cal yr BP onwards with a short decline around 3700 cal yr BP. Mass expansion resumed afterwards, leading to the ultimate recession ofPicea,CorylusandUlmus.Faguspredominates the forests to the present. Small-scale human influence on the landscape (cereal-type pollen grains, Poaceae, andPlantago lanceolata) first appeared after 6000 cal yr BP. Further anthropogenic impact was detected after 5000 cal yr BP, and was slightly stronger between 2300 cal yr BP and the twelfth century AD with regular and increasing appearances of primary and secondary cultural indicators. Large-scale forest clearing in the lowlands and foothills with more agriculture led to the development of the modern cultural landscape in the last 500 years.
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