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首页> 外文期刊>Vegetation History and Archaeobotany >Palaeobotanical evidence for agricultural activities in the Eifel region during the Holocene: plant macro-remain and pollen analyses from sediments of three maar lakes in the Quaternary Westeifel Volcanic Field (Germany, Rheinland-Pfalz)
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Palaeobotanical evidence for agricultural activities in the Eifel region during the Holocene: plant macro-remain and pollen analyses from sediments of three maar lakes in the Quaternary Westeifel Volcanic Field (Germany, Rheinland-Pfalz)

机译:全新世时期埃菲尔地区农业活动的古植物证据:第四纪韦斯特伊费尔火山场(德国,莱茵兰-普法尔茨州)三个马尔湖沉积物中的植物宏观残留和花粉分析

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As a part of the ELSA-project (Eifel Laminated Sediment Archive) new pollen and plant macro-remain analyses have been carried out on a series of Holocene lacustrine sediments from three open maar lakes of the Quaternary Westeifel Volcanic Field. In combination with already existing pollen analyses, the archaeological record and written sources, the present study casts new light on settlement activities and henceforth the development of agriculture from the prehistoric to historic times in this region. While there are clues that wood pasturing was practised in the Eifel region from the Michelsberg Culture onwards (c. 4300 cal. b.c.), the Vulkaneifel is a remote area with relatively poor soils and a humid climate and was not constantly settled until the Late Neolithic/Early Bronze Age, when cereal pollen was found regularly in the deposits. Plant macro-remains (chaff), which give us direct evidence for arable agriculture in the surroundings of the maars, were also found in layers belonging to the Early Bronze Age (c. 1900 cal. b.c.). At the same time we can observe the massive spread of Fagus sylvatica (beech) in all pollen diagrams, which was most probably caused by a combination of climatic, anthropogenic and competitive factors. Later impacts of agriculture were an abundance of crop weeds and pollen in the following Middle Bronze Age. Nevertheless human impact remained discontinuous until the Urnfield Culture (1200–800 cal. b.c.). A layer of weeds dating at the end of the Urnfield Culture was found and also flax (Linum usitatissimum) cultivation first becomes apparent. However, the subsequent Iron Age and Roman Period reveal only crop weeds and cereal pollen in slightly higher concentrations, but the abundance of Poaceae pollen at this time is most probably consistent with grazing activities. There follows compelling evidence of the importance of flax cultivation and processing at the maars from the Merovingian Period (5th century a.d.) onwards. A detailed insight into the agriculture of the High Medieval comes from flash flood layers of the 14th century a.d., where remains of Secale cereale (rye) and crop weeds reflect winter-sown cultivation of rye. Cannabis sativa (hemp) was also cultivated and processed during the medieval. Finally we can trace the Prussian reforestation in the 19th century a.d., with an increase in Pinus sylvestris (pine) and Picea abies (fir), by both pollen and plant macro-remains.
机译:作为ELSA项目的一部分(埃菲尔积层沉积物档案),已经对来自第四纪韦斯特伊费尔火山场的三个开放的马尔湖的一系列全新世湖相沉积物进行了新的花粉和植物宏观残留分析。结合已有的花粉分析,考古记录和书面资料,本研究为定居活动以及此地区农业从史前到历史时期的发展提供了新的思路。尽管有线索表明,从米歇尔斯伯格文化(约公元前4300年)开始,埃菲尔地区就开始放牧木草,但凡尔肯奈费尔是一个偏僻的地区,土壤相对贫瘠且气候潮湿,直到新石器时代晚期才稳定定居。 /早期青铜时代,定期在矿床中发现谷物花粉。植物早期遗迹(ch壳),也为青铜时代(约公元前1900年代)的层中发现了直接的证据,为我们提供了在马尔斯周边地区进行耕作农业的直接证据。同时,我们可以在所有花粉图中观察到山毛榉(Bugus sylvatica)(山毛榉)的大量传播,这很可能是气候,人为和竞争因素共同作用的结果。后来的农业影响是在随后的青铜时代,大量的农作物杂草和花粉。然而,直到Urnfield Culture(公元前1200-800 cal)为止,人类的影响一直是不连续的。发现了在Urnfield文化末期的一层杂草,亚麻(Linum usitatissimum)的种植也首先显现出来。但是,随后的铁器时代和罗马时期只发现了较高浓度的农作物杂草和谷类花粉,但是此时禾本科花粉的丰度很可能与放牧活动相一致。以下是有力的证据表明,从梅洛芬吉安时代(公元5世纪)开始,在麻坡中种植和加工亚麻非常重要。对高级中世纪农业的详细了解来自公元14世纪的山洪爆发层,这里的Secale谷类(黑麦)和农作物杂草的残骸反映了冬天播种的黑麦种植。中世纪还种植并加工了大麻(大麻)。最后,我们可以追溯到公元19世纪的普鲁士人的造林活动,其中花粉和植物宏观残留物增加了樟子松(松树)和云杉(冷杉)的生长。

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