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Witold Paweł Alexandrowicz

Biographic Data

ID7513225
NAMEWitold Paweł Alexandrowicz
GIVEN NAMESWitold Paweł
FAMILY NAMEAlexandrowicz
SIGNATUREALEXANDROWICZ W P
AFFILIATIONSAGH University of Krakow
VERIFIEDNo
TOTAL WORKS7
TOTAL CITATIONS21
WORKS AS AUTHOR7
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2013
LATEST PUBLICATION YEAR2021
H-INDEX2
  • The use of malacological analysis in studies on anthropogenic transformations in microhabitats

    Open Access•Stefan Witold Alexandrowicz, Witold Paweł Alexandrowicz•ARTICLE•Erdkunde•2021

    The presented study is dedicated to the assessment of the scope and degree of anthropopressure, and the dependence of its intensity on the characteristics and nature of micro-environments. The research was based on the subfossil remains of molluscs. Eleven profiles of Late Holocene sediments in the Dulówka valley near Cracow were subjected to malacological analysis. In the upper part of the valley, there are calcareous tufas containing rich mollu…

  • Late Glacial and Holocene paleoecology and paleoenvironmental changes in the northern Carpathians foreland

    Open Access•J Wilczyński, M T Krajcarz et al.•ARTICLE•The Holocene•2020•Cited by: 2•References: 15

    The study of past environments, their ecology, and detailed changes through time has become an important task of environmental science. Records of paleoenvironment usually vary between regions owing to different influences of local climate, vegetation, relief, and depositional processes. Therefore, studying local sequences thoroughly allows paleoenvironmental and paleoecological reconstructions for particular regions, but it also provides importa…

  • The continuous persistence of open oak forests in the Miechów Upland (Poland) in the second half of the Holocene

    Open Access•Magdalena Moskal-Del Hoyo, Aldona Mueller-Bieniek et al.•ARTICLE•Quaternary International•2017•Cited by: 16•References: 10

  • Multi-proxy evidence of Holocene climate variability in Volhynia Upland (SE Poland) recorded in spring-fed fen deposits from the Komarów site

    Open Access•Radosław Dobrowolski, Krystyna Bałaga et al.•ARTICLE•The Holocene•2016•Cited by: 3•References: 15

    Radiocarbon-dated spring-fed fen deposits from the Komarów site (Volhynia Upland, SE Poland) with its multi-proxy data (macrofossils, molluscs, geochemistry, pollen, stable isotopes of oxygen and carbon) enable us (1) to distinguish four main stages of fen evolution, which reflected a distinct variability of water supply conditions and (2) to reconstruct the Holocene humidity–temperature changes. The beginning of peat–tufa deposition took place i…

  • Malacological sequence of Weichselian (MIS 5-2) loess series from a profile in Grodzisko Dolne (southern Poland) and its palaeogeographic significance

    Witold Paweł Alexandrowicz•ARTICLE•Quaternary International•2014

  • Changes to the environment of intramontane basins in the light of malacological research of calcareous tufa

    Open Access•Witold Paweł Alexandrowicz, Marcin Szymanek et al.•ARTICLE•Quaternary International•2014

  • Malacological sequence from profile of calcareous tufa in Groń (Podhale Basin, southern Poland) as an indicator of the Late Glacial/Holocene boundary

    Open Access•Stefan Witold Alexandrowicz, Witold Paweł Alexandrowicz•ARTICLE•Quaternary International•2013

  • The continuous persistence of open oak forests in the Miechów Upland (Poland) in the second half of the Holocene

    Open Access•Magdalena Moskal-Del Hoyo, Aldona Mueller-Bieniek et al.•ARTICLE•Quaternary International•2017•Cited by: 16•References: 10

  • Multi-proxy evidence of Holocene climate variability in Volhynia Upland (SE Poland) recorded in spring-fed fen deposits from the Komarów site

    Open Access•Radosław Dobrowolski, Krystyna Bałaga et al.•ARTICLE•The Holocene•2016•Cited by: 3•References: 15

    Radiocarbon-dated spring-fed fen deposits from the Komarów site (Volhynia Upland, SE Poland) with its multi-proxy data (macrofossils, molluscs, geochemistry, pollen, stable isotopes of oxygen and carbon) enable us (1) to distinguish four main stages of fen evolution, which reflected a distinct variability of water supply conditions and (2) to reconstruct the Holocene humidity–temperature changes. The beginning of peat–tufa deposition took place i…

  • Late Glacial and Holocene paleoecology and paleoenvironmental changes in the northern Carpathians foreland

    Open Access•J Wilczyński, M T Krajcarz et al.•ARTICLE•The Holocene•2020•Cited by: 2•References: 15

    The study of past environments, their ecology, and detailed changes through time has become an important task of environmental science. Records of paleoenvironment usually vary between regions owing to different influences of local climate, vegetation, relief, and depositional processes. Therefore, studying local sequences thoroughly allows paleoenvironmental and paleoecological reconstructions for particular regions, but it also provides importa…

  • Malacological sequence from profile of calcareous tufa in Groń (Podhale Basin, southern Poland) as an indicator of the Late Glacial/Holocene boundary

    Open Access•Stefan Witold Alexandrowicz, Witold Paweł Alexandrowicz•ARTICLE•Quaternary International•2013

  • Malacological sequence of Weichselian (MIS 5-2) loess series from a profile in Grodzisko Dolne (southern Poland) and its palaeogeographic significance

    Witold Paweł Alexandrowicz•ARTICLE•Quaternary International•2014

  • Changes to the environment of intramontane basins in the light of malacological research of calcareous tufa

    Open Access•Witold Paweł Alexandrowicz, Marcin Szymanek et al.•ARTICLE•Quaternary International•2014

  • Multi-proxy evidence of Holocene climate variability in Volhynia Upland (SE Poland) recorded in spring-fed fen deposits from the Komarów site

    Open Access•Radosław Dobrowolski, Krystyna Bałaga et al.•ARTICLE•The Holocene•2016•Cited by: 3•References: 15

    Radiocarbon-dated spring-fed fen deposits from the Komarów site (Volhynia Upland, SE Poland) with its multi-proxy data (macrofossils, molluscs, geochemistry, pollen, stable isotopes of oxygen and carbon) enable us (1) to distinguish four main stages of fen evolution, which reflected a distinct variability of water supply conditions and (2) to reconstruct the Holocene humidity–temperature changes. The beginning of peat–tufa deposition took place i…

  • The continuous persistence of open oak forests in the Miechów Upland (Poland) in the second half of the Holocene

    Open Access•Magdalena Moskal-Del Hoyo, Aldona Mueller-Bieniek et al.•ARTICLE•Quaternary International•2017•Cited by: 16•References: 10

  • Late Glacial and Holocene paleoecology and paleoenvironmental changes in the northern Carpathians foreland

    Open Access•J Wilczyński, M T Krajcarz et al.•ARTICLE•The Holocene•2020•Cited by: 2•References: 15

    The study of past environments, their ecology, and detailed changes through time has become an important task of environmental science. Records of paleoenvironment usually vary between regions owing to different influences of local climate, vegetation, relief, and depositional processes. Therefore, studying local sequences thoroughly allows paleoenvironmental and paleoecological reconstructions for particular regions, but it also provides importa…

  • The use of malacological analysis in studies on anthropogenic transformations in microhabitats

    Open Access•Stefan Witold Alexandrowicz, Witold Paweł Alexandrowicz•ARTICLE•Erdkunde•2021

    The presented study is dedicated to the assessment of the scope and degree of anthropopressure, and the dependence of its intensity on the characteristics and nature of micro-environments. The research was based on the subfossil remains of molluscs. Eleven profiles of Late Holocene sediments in the Dulówka valley near Cracow were subjected to malacological analysis. In the upper part of the valley, there are calcareous tufas containing rich mollu…

Geology (6 works) · Geology and Paleoclimatology Research (6 works) · Holocene (6 works) · Paleontology (6 works) · Ancient and Medieval Archaeology Studies (4 works) · Ecology (4 works) · Geography (4 works) · Glacial period (4 works) · Marine and environmental studies (4 works) · Physical geography (4 works)

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