Palaeohydrology of the Seim River basin, Mid-Russian Upland, based on palaeochannel morphology and palynological data

Borisova, Olga; Sidorchuk, Aleksey; Панин, А. В.

doi:10.1016/j.catena.2005.07.010

Cited by 62 publications

(64 citation statements)

References 6 publications

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“…An increase in fluvial activity during the YD has been widely reported from Polish and European valleys (e.g. Huisink 2000; Andres et al 2001;Starkel 2002Starkel , 2011Borisova et al 2006;Gao et al 2007;Starkel et al 2007Starkel et al , 2015Pawłowski et al 2015b;Petera-Zganiacz et al 2015). The floodwaters may significantly decrease the water temperature in the oxbow lake, as at the Ldzań site.…”

Section: Reliability Of the Cladoceran-based Temperature Reconstructionmentioning

confidence: 80%

The usefulness of subfossil Cladocera remains in Younger Dryas climatic reconstructions in central Poland

Pawłowski

2017

Acta Geologica Polonica

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ABSTRACT:Pawłowski, D. 2017. The usefulness of subfossil Cladocera remains in Younger Dryas climatic reconstructions in central Poland. Acta Geologica Polonica, 67 (4), 567-584. Warszawa.Cladoceran-based paleotemperature estimates for the Younger Dryas for ten sections of paleo-oxbow lakes, valley mires, and lacustrine sediments from central Poland are presented, and their potential usefulness to climatostratigraphy is described. Most of the changes observed in the cladoceran assemblages are responses to climate changes. The cladoceran-based temperature reconstructions reflect cold conditions during the Younger Dryas (YD) and allow a division of this period into two phases: an older colder phase, between 12,800 and 12,000 cal yrs BP, and a younger, warmer phase, between ca. 12,000 and 11,500 cal yrs BP. The geomorphological features of the study sites and local environmental forces are also taken into consideration. The cladoceran-inferred summer temperature estimates from all of the study sites correspond closely with the available climate reconstruction for the YD in central Europe.

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Section: Reliability Of the Cladoceran-based Temperature Reconstructionmentioning

confidence: 80%

The usefulness of subfossil Cladocera remains in Younger Dryas climatic reconstructions in central Poland

Pawłowski

2017

Acta Geologica Polonica

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“…Both in Poland (Gębica, 2013) and in the European part of Russia (Borisova et al, 2006;Sidorchuk et al, 2012) dated to this time were small palaeochannels whose sizes and consequently river channel-forming discharges were similar to that of present-day rivers. On the other hand, continuation of high runoff from the Late Glacial into the first half of the Holocene has been found in some parts of North America: large river meanders were dated to 12-9.5 ka cal BP in the Great Lakes region (Arbogast et al, 2008) and to 15-5 ka cal BP in the Southeastern USA (Leigh, 2006).…”

Section: Discussion and Final Remarksmentioning

confidence: 77%

“…It brings up the question of chronology of the high river runoff epoch in Central and Eastern Europe. In the central part of the East European Plain large meandering palaeochannels (macromeanders) were dated between 18 and 13 ka cal BP (Borisova et al, 2006;Sidorchuk et al, 2009 (Szumanski, 1983(Szumanski, , 1986Vandenberghe et al, 1994;Gębica et al, 2009) and Hungary (Kasse et al, 2010), about 15.5 ka cal BP (12.8 ka 14 C BP) in the Lower Danube region (Howard et al, 2004). In southern Poland some rivers did not change their pattern from braiding to large meanders during the Late Glacial and kept braiding to the beginning of the Holocene (Starkel et al, 1996;Gębica, 2011), other rivers transformed from meandering back to braiding in the Younger Dryas (Starkel and Gębica, 1995), but in all cases the Late Glacial phase of increased fluvial had declined almost exactly at the Younger Dryas / Holocene transition (Gębica, 2013).…”

Section: Discussion and Final Remarksmentioning

confidence: 99%

“…Fluvial history of the Dnieper River and its tributaries has been studied in Byelorussia Sańko, 1992, 1998;Kalicki 1995Kalicki , 2006Kalicki et al, 2008), in the Dnieper's left tributary catchments (Panin et al, 2001;Borisova et al, 2006). Nevertheless, a systematic chronology of fluvial events in the Dnieper River system has not been proposed yet.…”

Section: Introductionmentioning

confidence: 99%

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Absolute chronology of fluvial events in the Upper Dnieper River system and its palaeogeographic implications

et al. 2014

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A set of 121 radiocarbon and OSL dates has been compiled from the Upper Dnieper River and tributary valleys, Western European Russia. Each date was attributed according to geomorphic/sedimentological events and classes of fluvial activity. Summed probability density functions for each class were used to establish phases of increasing and reducing fluvial activity. The oldest detected reduction of fluvial activity was probably due to glacial damming at LGM. Within the Holocene three palaeohydrological epochs of millennial-scale were found: (1) high activity at 12,000-8,000 cal BP marked by large river palaeochannels; (2) low activity at 8,000-3,000 cal BP marked by formation of zonal-type soils on -floodplains; short episodes of high floods occurred between 6,500-4,400 cal BP; (3) contrasting hydrological oscillations since 3,000 cal BP with periods of high floods between 3,000-2,300 (2,000) and 900-100 cal BP separated by long interval of low floods 2,300 (2,000)-900 cal BP when floodplains were not inundated -zonal-type soils were developing and permanent settlements existed on floodplains. In the last millennium, four centennialscale intervals were found: high flooding intervals are mid-11-mid-15 th century and mid-17-mid-20 th century. Intervals of flood activity similar to the present-day were: mid-15-mid-17 th century and since mid-19 th century till present. In the context of palaeohydrological changes, discussed are selected palaeogeographic issues such as: position of the glacial boundary at LGM, role of changing amounts of river runoff in the Black Sea level changes, floodplain occupation by Early Medieval population.

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“…Large palaeochannels are known from many regions of Central and Eastern Europe (Szumanski, 1983(Szumanski, , 1986Vandenberghe et al, 1994;Howard et al, 2004;Borisova et al, 2006;Gębica et al, 2009;Sidorchuk et al, 2009;Kasse et al, 2010). In most cases they have a meandering pattern and a Lateglacial age.…”

Section: -Introductionmentioning

confidence: 99%

Fluvial response to proglacial effects and climate in the upper Dnieper valley (Western Russia) during the late Weichselian and the Holocene

Panin¹,

Adamiec²,

Филиппов³

2015

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Palaeohydrology of the Seim River basin, Mid-Russian Upland, based on palaeochannel morphology and palynological data

Cited by 62 publications

References 6 publications

The usefulness of subfossil Cladocera remains in Younger Dryas climatic reconstructions in central Poland

The usefulness of subfossil Cladocera remains in Younger Dryas climatic reconstructions in central Poland

Absolute chronology of fluvial events in the Upper Dnieper River system and its palaeogeographic implications

Fluvial response to proglacial effects and climate in the upper Dnieper valley (Western Russia) during the late Weichselian and the Holocene

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