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Hydrological Changes After the Last Ice Retreat in Northern Poland Using Radiocarbon Dating

Bibliographic Data

ID9244131
AuthorsDanuta J Michczyńska (0000-0001-5348-5791), Danuta Michczyńska, Leszek Starkel (0000-0003-1365-441X), Dorota Nalepka (0000-0002-5624-3488), Anna Pazdur (0000-0002-6078-798X)
Year2013
Volume55
Issue3–4
Publication date2013-01-01
Peer ReviewedYes
Open AccessNo
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.2458/azu_js_rc.55.16343
OpenAlexW4235443792
LanguageEN
Citations received10
References cited27

A simplified model of hydrological changes during the Late Glacial and Holocene is presented for the northern Polish regions that were ice covered during the Last Glacial. This reconstruction is based on a group of 197 radiocarbon dates from about 120 localities reflecting the sequence of alternating lake transgressions and regressions. The earliest transgressions were related to dead-ice melting (sometimes in 2–3 phases), while the later ones started during more humid phases. However, these were usually followed by regressions, which may have been connected with the formation of new drainage systems and with the overgrowing of shallow lakes by peat bogs

Archaeology · Bog · Climatology · Geography · Glacial period · Holocene · Ice core · Peat · Physical geography · Radiocarbon dating · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Historical and Archaeological Studies · Peatlands and Wetlands Ecology · Geology · Paleontology

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Unique citing works10
Citations per year0,83
Citation span2014 - 2023 (10)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 10

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