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Assemblages of molluscs from Sulisławice (Małopolska Upland, southern Poland) and their significance for interpretation of depositional conditions of calcareous tufas in small water bodies

Alexandrowicz W. P.

Annales Societatis Geologorum Poloniae

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2012

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Vol. 82, No. 2

161–-176

EN

Small water bodies, occurring behind barriers across valleys, create very advantageous conditions for the sedimentation of calcareous tufas. These sediments usually contain rich and diversified malacocoenoses. The composition and structure of these associations are closely linked to environmental changes during the accumulation of the sediments. At the Sulisławice locality, the remnants of two barriers, composed of hard, calcareous tufa, were found. Behind them, sequences of granular, calcareous tufas were preserved, forming terraces, elevated up to 3 m above the level of the present stream bed. The age of the sediments was obtained from radiocarbon dating and is referable to the Atlantic Phase. The rich malacofauna, occurring in these tufas, permitted the recognition of four types of faunistic association, in a sequence that corresponds to phases in the development of the water bodies. Three of them are characterised by the dominance of aquatic species and permit the reconstruction of specific features of the body of water. In the fourth association, terrestrial species predominate. A detailed, malacological analysis was the basis for a model of the evolution of the water bodies, occurring behind the barriers. The model is more widely applicable to the sediments of similar origin, frequently found in upland regions of Poland and other parts of Europe.

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Molluscan assemblages of Late Glacial and Holocene calcareous tufas in southern Poland

Alexandrowicz W.P.

Folia Quaternaria

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2004

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nr 75

309-309

EN

The calcareous tufas and travertines of the Weichselian Late Glacial and Holocene age host very abundant and diversified molluscan assemblages. Most of the 80 studies localities are located in southern Poland, namely in the Carpathians and in the zone of Mid-Polish Uplands. Malocological analysis has enabled for distinguishing several types of molluscan assemblages and detailed description of their stratigraphic sequences. The malacological sequences reflect environmental changes during the last 12,000 years caused by both natural factors (mainly climatic oscillations) and anthropopressure. Moreover, these results allow one to characterize the differences and similarities among geographical regions, and to select phases during which increased migration took place. The possibility of malacostratigraphic subdivision of the Late Glacial and Holocene is particulary important for Quaternary stratigraphy, Malacological data, which are the basis for interpretation, have been supplemented by the results of palynological, isotopic, and archaelogical studies, as well as by the results of radiocarbon datings

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Wpływ martwicy wapiennej na obszarze wsi Mszana Górna na warunki pozyskiwania wody

Satora S.

Inżynieria Rolnicza

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2002

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R. 6, nr 3

177--187

PL

W artykule przedstawiono wyniki badań związanych z odkryciem nowego stanowiska występowania wśród utworów fliszowych martwicy wapiennej na obszarze okna tektonicznego Mszany i terenie wsi Mszana Górna. Martwica ta znajduje się przy wypływach trzech źródeł skalnych, szczelinowych, zstępujących i wstępujących oznaczonych nr 1, 2 i 6. Zlewne pokrywy martwicy występują w miejscach wypływów wody ze źródeł na powierzchnię terenu oraz wzdłuż rynnowatych zagłębień w powierzchni terenu utworzonych przez odpływające ze źródeł wody. Przeprowadzone w okresie 9.01.1979-31.12.1981 r., stacjonarne badania wydajności źródła nr 1 wykazały zmienność jego wydajności 0,5-4,44 m3·h-1 i samowypływie na rzędnej 494,32 m n.p.m., natomiast źródła nr 2 - 0,19-10,65 m3·h-1 przy samowypływie na rzędnej 499,43 m n.p.m. Źródło nr 6 jest ujęte i obudowane. Prowadzone wieloletnie obserwacje badanego źródliska wskazują na to, że wstrzymany jest obecnie w tym rejonie rozwój martwicy. W opracowaniu przedstawiono również skład mineralny oraz przypuszczalne procesy zachodzące przy tworzeniu się martwicy. Procesy te związane są ze wzbogaconymi w CO2 wodami wgłębnymi, które ługują tutaj z podłoża fliszu węglan wapnia i migrując uskokami ku górze wytrącają go w miejscach wypływów źródeł w postaci martwicy.

EN

In the article were presented research results connected with a discovery of a calcareus tufas new occurrence position among flysh formations at the tectonics window of Mszana and Mszana Górna village area. The tufas is located near three rocky springs outflow, crevice, descending and ascending, signed as nr 1, 2 i 6. A tufas cast caver are situated at water outflow from spring on a ground surface and along guttered hollows on a surface of area that were formed by flown away waters from spring. Stationary research of spring nr 1 procutiveness, that were carried out between 9.01.1979 and 31.12.1981, showed variability of its productiveness from 0,5 to 4,44 m3·h-1 and with selfdischarge on a datum 494,32 m a.s.l., however spring nr 2 - 0,19-10,65 m3·h-1 and with selfdischarge on a datum 499,43 m a.s.l. The spring nr 6 is tapping and cased. A long-term obseravtion of tested spring showed, that a development of tufas is hołd in this area. In this study were also presented minerał composition and presumable processes that occured during a tufas formation. Those processes are connected with CO2-rich groundwaters, that leached in this area from a flysh ground calcium carbonate and during migration to a surface precipitate this compound as a tufas.