Specifying the external impact on fluvial lowland evolution: the last glacial Tis(z)a catchment in Hungary and Serbia.

Jef Vandenberghe; C. Kasse; D. Popov; Slobodan Markovic; Dimitri Vandenberghe; S.  Bohncke; G. Gabris

doi:10.3390/quat1020014

Specifying the external impact on fluvial lowland evolution: the last glacial Tis(z)a catchment in Hungary and Serbia.

Jef Vandenberghe, C. Kasse, D. Popov, Slobodan Markovic, Dimitri Vandenberghe, S. Bohncke, G. Gabris

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

External impact on the development of fluvial systems is generally exerted by changes in sea level, climate and tectonic movements. In this study, it is shown that a regional to local differentiation of fluvial response may be caused by semi-direct effects of climate change and tectonic movement; for example, vegetation cover, frozen soil, snow cover and longitudinal gradient. Such
semi-direct effects may be responsible for specific fluvial activity resulting in specific drainage patterns, sedimentation series and erosion–accumulation rates. These conclusions are exemplified by the study of the fluvial archives of the Tis(z)a catchment in the Pannonian Basin in Hungary and Serbia from the middle of the last glacial to the Pleistocene–Holocene transition. Previous investigations in that catchment are supplemented here by new geomorphologicalsedimentological data and OSL-dating. Specific characteristics of this catchment in comparison with other regions are the preponderance of meandering systems during the last glacial and the presence of very large
meanders in given time intervals.

Original language	English
Article number	14
Pages (from-to)	1-23
Number of pages	23
Journal	Quaternary
Volume	1
Issue number	2
DOIs	https://doi.org/10.3390/quat1020014
Publication status	Published - 16 Aug 2018

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Special Issue: Special External Effects on Fluvial System Evolution

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title = "Specifying the external impact on fluvial lowland evolution: the last glacial Tis(z)a catchment in Hungary and Serbia.",

abstract = "External impact on the development of fluvial systems is generally exerted by changes in sea level, climate and tectonic movements. In this study, it is shown that a regional to local differentiation of fluvial response may be caused by semi-direct effects of climate change and tectonic movement; for example, vegetation cover, frozen soil, snow cover and longitudinal gradient. Suchsemi-direct effects may be responsible for specific fluvial activity resulting in specific drainage patterns, sedimentation series and erosion–accumulation rates. These conclusions are exemplified by the study of the fluvial archives of the Tis(z)a catchment in the Pannonian Basin in Hungary and Serbia from the middle of the last glacial to the Pleistocene–Holocene transition. Previous investigations in that catchment are supplemented here by new geomorphologicalsedimentological data and OSL-dating. Specific characteristics of this catchment in comparison with other regions are the preponderance of meandering systems during the last glacial and the presence of very largemeanders in given time intervals.",

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AU - Markovic, Slobodan

AU - Vandenberghe, Dimitri

AU - Bohncke, S.

AU - Gabris, G.

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Specifying the external impact on fluvial lowland evolution: the last glacial Tis(z)a catchment in Hungary and Serbia.

Abstract

Bibliographical note

UN SDGs

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