Palaeomeander of the Rudava River (SW Slovakia) – an insight into the evolution of landscape and vegetation

IF 0.5 Q3 GEOGRAPHY
P. Pišút, Juraj Procházka, E. Uherčíková, I. Matečný, Adam Rusinko, T. Čejka
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引用次数: 0

Abstract

Palaeomeander of the Rudava River (SW Slovakia) – an insight into the evolution of landscape and vegetation This study is focused on a cut - off palaeomeander of the Rudava River (SW Slovakia). Along its middle reach, Rudava passes through the extensive plain of Quaternary eolian sands covered with Scots Pine woodland. Specific landforms – semi - circled cut - bluffs (wagrams) are commonly found on either side of the river valley. They have been triggered by a meandering river in contact with both lower terraces and sand dune pseudoterrace and postgenously shaped by mass wasting. The left - bank palaeomeander and cut - bluff at river kilometre 13.2 is one of the most completely evolved and, until today, the best - preserved landforms of this kind. A palaeoecological study of the palaeomeander infill (two cores) combined with a digital elevation model, AMS radiocarbon dating, cartographic data analysis and a survey of present - day vegetation suggest the river meander was most probably cut - off in the 18th Cen- tury. Due to the flow hydrological regime, meandering dynamics at this reach is relatively slow. Numerous springs and seepage along the south edge of the river valley play an important role in the initiation and evolution of cut - bluffs. Also, at the site under study, such spring draining into the Rudava River has significantly contributed to the present - day variability of local soils, wood and marsh habitats. According to plant macrofossil records and ecogroups - based vegetative macrozones a riparian land- scape in the time of meander abandonment and earlier was much more open and with a markedly human impact. Probably upon the pastureʼs decline, the Holocene flood- plainʼs adjacent reach was completely reforested until the mid - 19th Century. Current hardwood alluvial woodland (of the association Ficario vernae - Ulmetum campestris ) originated in 1916 mainly from natural and perhaps artificial regeneration.
鲁达瓦河(斯洛伐克西南部)的古测量仪-对景观和植被演变的洞察
古鲁达瓦河(斯洛伐克西南部)断裂带——景观与植被演化的新视角。沿着它的中游,鲁达瓦穿过覆盖着苏格兰松林的广阔的第四纪风成沙平原。特定的地形-半圆形的切崖(wagrams)通常在河谷的两侧发现。它们是由一条曲流河流与低阶地和沙丘假阶地相接触而引发的,并在形成后由大量的浪费形成。河长13.2公里处的左岸古堤岸和切崖是这类地貌中演化最完整、保存最完好的地貌之一。对古河段填充物(两个岩心)进行的古生态学研究,结合数字高程模型、AMS放射性碳测年、制图数据分析和对现代植被的调查,表明这条河的曲流最有可能在18世纪被切断。由于水流水文状况的影响,该河段的曲流动力相对缓慢。河谷南缘大量的泉水和渗流对切崖的形成和演化起着重要作用。此外,在研究的地点,这种流入鲁达瓦河的春季排水对当地土壤、木材和沼泽栖息地目前的变化有重大影响。根据植物大化石记录和基于生态群的植被大带,曲流废弃时期及更早时期的河岸景观更为开阔,人类活动影响显著。可能是由于牧场的衰落,直到19世纪中期,全新世洪泛平原的邻近地区才完全重新造林。目前的阔叶林冲积林地(隶属于森林协会-榆木协会)起源于1916年,主要是由自然和人工再生形成的。
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来源期刊
CiteScore
1.30
自引率
22.20%
发文量
14
期刊介绍: The journal publishes original and timely scientific articles that advance knowledge in all the fields of geography and significant contributions from the related disciplines. Papers devoted to geographical research of Slovakia and to theoretical and methodological questions of geography are especially welcome. In addition, the journal includes also short research notes, review articles, comments on published papers and reviews of selected publications. Papers are written in the Slovak language with English summary or in English and occasionally in some other world languages.
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