<abstract xml:lang="en" xmlns="http://www.w3.org/1999/xhtml"><p>Sediments exposed in a construction excavation form a sequence: alluvial deposits > black soil > made ground. Peat-like deposits, organic muds and occasionally sand occur between the soil and the made ground. High aeolization of alluvial sediments allows relating their age to the Late Vistulian. The sediments were eroded and in the washout at first organic muds were deposited and subsequently sands. The lowest layer, radiocarbon-dated at 4510±60 uncal. years BP (Gd-12724), can be probably linked to climate moistening at the transition between the Holocene Atlantic and the Subboreal period. Pollen grains found in muds, black soil and peat-like deposits reflect the changes of local plant cover from dominated by pine woodlands (at the transition between the Atlantic and the Subboreal period) to strongly deforested with single trees, meadows, small crop fields and gardens in the Medieval period. Palynological results describing the character of vegetation might have been influenced also by direct human activity on site, e.g. by storage of wood and branches (then used as construction material or fuel), crops, fodder or waste. Microartefacts found in soil suggest metal processing in the vicinity during the Bronze Age. In the made ground, which has been accumulating since the 14th century, quartz, clay minerals and micas were identified together with fragments of bricks, concrete, ceramics, bones, slag, charcoal, organic matter, limestone fragments and metals. Horizons enriched in slag fragments are also high in metals: Fe, Mn and Pb, which reveal a twofold increase in metal processing activity.</p></abstract>

Sediments exposed in a construction excavation form a sequence: alluvial deposits > black soil > made ground. Peat-like deposits, organic muds and occasionally sand occur between the soil and the made ground. High aeolization of alluvial sediments allows relating their age to the Late Vistulian. The sediments were eroded and in the washout at first organic muds were deposited and subsequently sands. The lowest layer, radiocarbon-dated at 4510±60 uncal. years BP (Gd-12724), can be probably linked to climate moistening at the transition between the Holocene Atlantic and the Subboreal period. Pollen grains found in muds, black soil and peat-like deposits reflect the changes of local plant cover from dominated by pine woodlands (at the transition between the Atlantic and the Subboreal period) to strongly deforested with single trees, meadows, small crop fields and gardens in the Medieval period. Palynological results describing the character of vegetation might have been influenced also by direct human activity on site, e.g. by storage of wood and branches (then used as construction material or fuel), crops, fodder or waste. Microartefacts found in soil suggest metal processing in the vicinity during the Bronze Age. In the made ground, which has been accumulating since the 14th century, quartz, clay minerals and micas were identified together with fragments of bricks, concrete, ceramics, bones, slag, charcoal, organic matter, limestone fragments and metals. Horizons enriched in slag fragments are also high in metals: Fe, Mn and Pb, which reveal a twofold increase in metal processing activity.

Changes of Natural Environment in Kraków Downtown - Its Chronology and Directions. Case Geoarchaeological Studies of Krupnicza Street Site

Faculty of Geology, Geophysics and Environmental Protection, Stanisław Staszic AGH University of Science and Technology, Aleja Mickiewicza 30, PL-31-590 Kraków, Poland

Władysław Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, PL-31-512 Kraków, Poland

Institute of Physics, The Silesian University of Technology, Krzywoustego 2, PL-44-100 Gliwice, Poland

Institute of Botany, Jagiellonian University, Lubicz 46, PL-31-512 Kraków, Poland

Institute of Physico-Geographical Sciences, Warsaw University, Krakowskie Przedmieście 30, PL-00-950 Warszawa, Poland

Sienkiewicza 14/8, PL-30-033 Kraków, Poland

Geochronometria

Sediments exposed in a construction excavation form a sequence: alluvial deposits > black soil > made ground. Peat-like deposits, organic muds and occasionally...

Changes of Natural Environment in Kraków Downtown - Its Chronology and Directions. Case Geoarchaeological Studies of Krupnicza Street Site

Publicado en línea: 01 oct 2008

Páginas: 7 - 19

DOI: https://doi.org/10.2478/v10003-008-0013-x

Palabras clave
Wisła River valley, river deposits, made ground, pollen analysis, chemical and mineralogical analysis, radiocarbon dating, environmental changes

This content is open access.

Changes of Natural Environment in Kraków Downtown - Its Chronology and Directions. Case Geoarchaeological Studies of Krupnicza Street Site

Publicado en línea: 01 oct 2008

Páginas: 7 - 19

DOI: https://doi.org/10.2478/v10003-008-0013-x

Palabras claveWisła River valley, river deposits, made ground, pollen analysis, chemical and mineralogical analysis, radiocarbon dating, environmental changes

This content is open access.

Palabras clave
Wisła River valley, river deposits, made ground, pollen analysis, chemical and mineralogical analysis, radiocarbon dating, environmental changes