Specifying the External Impact on Fluvial Lowland Evolution
The Last Glacial Tisza (Tisa) Catchment in Hungary and Serbia
Bibliographic Data
| ID | 15801841 |
|---|---|
| Authors | J Vandenberghe (0000-0001-9910-1319, Vrije Universiteit Amsterdam, corresponding author), C Kasse (0000-0002-1466-1016, Vrije Universiteit Amsterdam), Dragan Popov (University of Novi Sad), Slobodan B Marković (0000-0002-4977-634X, University of Novi Sad), Dimitri Vandenberghe (0000-0002-2047-7039, Ghent University), Sjoerd Bohncke (Department of Earth Sciences, Vrije Universiteit, 1081HV Amsterdam, The Netherlands), S J P Bohncke (Vrije Universiteit Amsterdam), Gyula Gábris (Eötvös Loránd University) |
| Year | 2018 |
| Volume | 1 |
| Issue | 2 |
| Pages | 14-14 |
| Publication date | 2018-08-16 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Quaternary (JOURNAL) |
| Journal identifiers | ISSN: 2571-550X • E-ISSN: 2571-550X |
| Publisher | Multidisciplinary Digital Publishing Institute (PUBLISHER • CH) |
| DOI | 10.3390/quat1020014 |
| OpenAlex | W2809711917 |
| Language | EN |
| Citations received | 9 |
| References cited | 64 |
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 geomorphological–sedimentological 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
Climate change · Drainage basin · Erosion · Fluvial · Geography · Geomorphology · Glacial period · Holocene · Last Glacial Maximum · Physical geography · Pleistocene · Structural basin · Tectonics · Geological formations and processes · Geology and Paleoclimatology Research · Marine and environmental studies · Geology · Oceanography · Paleontology
Geomorphological evolution of the Petrovaradin Fortress Palaeolithic site (Novi Sad, Serbia)
Evaluating Holocene natural hazards in the French Massif Central from a regional lake sediment approach
European small mammal faunas during Dnieper (Saale) glaciation and transition to the Mikulino (Eem) interglacial
A new deer species (Cervidae, Mammalia) from the upper Siwaliks (Pakistan)
The evolution of meandering and anabranching rivers in postglacial and loess landscapes of Europe
Evolution of the European regional large mammals assemblages in the end of the Middle Pleistocene – The first half of the Late Pleistocene (MIS 6–MIS 4)
The last 40,000 years of a floodplain area (Tisza, Hungary) comparative case study of 14C and OSL methods
Sediment provenance and fluvial reorganization during the pleistocene-holocene transition in the Southern Pannonian Basin (Central to Southeastern Europe)
Anthropogenic drivers for exceptionally large meander formation during the Late Holocene
Interaction of fluvial and eolian sedimentation processes, and response to climate change since the last glacial in a semiarid environment along the Yellow River
Tectonic and climatic controls on Quaternary fluvial processes and river terrace formation in a Mediterranean setting, the Göksu River, southern Turkey
Comparison of laser grain size analysis with pipette and sieve analysis
Danube loess stratigraphy — Towards a pan-European loess stratigraphic model
The single aliquot regenerative dose protocol
Distinguishing quartz and feldspar in single grain luminescence measurements
The Full-Glacial Forests of Central and Southeastern Europe
Developments in radiation, stimulation and observation facilities in luminescence measurements
Dose-rate conversion factors
Late Pleistocene loess‐palaeosol sequences in the Vojvodina region, north Serbia
Dose-rate conversion factors
Cosmic ray contributions to dose rates for luminescence and ESR dating
Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol
Fluvial response to climate change during and after the Last Glacial Maximum in Central Anatolia, Turkey
A typology of Pleistocene cold-based rivers
Uplift-driven valley incision and climate-controlled river terrace development in the Thames Valley, UK
Preservation patterns of Late Cenozoic fluvial deposits and their implications
River terraces as a response to climatic forcing
Quatermalacological analyses for modeling of the Upper Weichselian palaeoenvironmental changes in the Carpathian Basin
Atmospheric circulation patterns in central and eastern Europe during the Weichselian Pleniglacial inferred from loess grain-size records
The relation between climate and river processes, landforms and deposits during the Quaternary
Investigating the penultimate and last glacial cycles of the Süttő loess section (Hungary) using luminescence dating, high-resolution grain size, and magnetic susceptibility data
A general model of paraglacial landscape response
Thermoluminescence Dating
Thermoluminescent Age Evaluation and Assessment of Error Limits
The Assessment of Error Limits in Thermoluminescent Dating
| Unique citing works | 9 |
|---|---|
| Citations per year | 1,5 |
| Citation span | 2020 - 2026 (7) |
| Citation velocity | current |
| Highly cited | No |
| Citation types | Neutral: 8 |