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Geoarchaeological studies of humic soil horizons and anthropogenic infillings at the multicultural archaeological excavation Site 28 in Rozbórz near Przeworsk, Southern Poland
This publication is protected by copyright. Access to its digital version is possible on computer terminals in the institution that shares it.
This publication is protected by copyright. Access to its digital version is possible on computer terminals in the institution that shares it.

Title: Geoarchaeological studies of humic soil horizons and anthropogenic infillings at the multicultural archaeological excavation Site 28 in Rozbórz near Przeworsk, Southern Poland

Creator:

Budek, Anna ; Gębica, Piotr ORCID ; Okoński, Jerzy

Date issued/created:

2013

Resource type:

Text

Subtitle:

Archaeologia Polona Vol. 49 (2011-2013)

Publisher:

Institute of Archaeology and Ethnology Polish Academy of Sciences

Place of publishing:

Warszawa

Description:

ill. ; 24 cm

Type of object:

Journal/Article

Abstract:

This paper presents the results of geoarchaeological investigations at Site 28 in Rozbórz. The study area is about 5 km east of Przeworsk, at the foot of the Kańczuga Upland (Rzeszów Foreland). The loess slopes of the uplands descend to the floor of the Forecarpathian Trough with the site being at a height of 185–183 m a.s.l. During the fieldwork four profiles in laminated delluvial sediments and buried humic soil horizons were studied in the north and east part of the site. The archaeological features, identified as storage pits with artefacts dated to the Neolithic Funnel Beaker culture, were buried by delluvial deposits and humic soil horizons. In the southwest part of the excavation the pits occur in sandy alluvial deposits on the Vistulian terrace. An extensive and flat depression filled with organic material and drained by a ditch system occurs in the western part of the area. Micromorphological studies and archaeological dating show that an increase in intensity of pedogenesis took place during the brake in human settlement. A Fluvisol developed in the alluvial deposits and then the rising of ground water table in the valley bottom caused hydromorphic soils to form. Finally after stabilization of environmental conditions Cambisol are developed. The beginning of swamping in this area started in the Subboreal wetter phase at about 2900–2500 cal. BC. The swampy soil was covered by delluvial sediments in the Early Medieval period c. 750–1050 cal. AD

References:

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Bullock, P., Fedoroff, N., Jongerius, A., Stoops, G. and Tursina, T. 1985. Handbook for Soil Thin Section Description, 1–152. Wolverhampton
Czopek, S. and Pelisiak, A. 2011. Archeologia i autostrada. Badania Fundacji Rzeszowskiego Ośrodka Archeologicznego w latach 2005–2011. Autostradą w przeszłość. Muzeum Okręgowe w Rzeszowie, 5–23. Rzeszów
Gębica, P. 2004. Przebieg akumulacji rzecznej w górnym Vistulianie w Kotlinie Sandomierskiej. Prace Geograficzne Instytutu Geografii i Przestrzennego Zagospodarowania PAN 193: 1–229
Gębica, P. 2011. Stratigraphy of alluvial fills and phases of the Holocene floods in the lower Wisłok river valley, SE Poland. Geographia Polonica 84, Special Issue Part I: 39–60
Kalicki, T. 1991. The evolution of the Vistula river valley between Cracow and Niepołomice in Late Vistulian and Holocene Times. In L. Starkel (ed.), Evolution of the Vistula river valley during the last 15000 years, part IV, Geographical Studies, Special Issue 6: 11–37
Kemp R., 1998. Role of micromorphology in paleopedological research. Quaternary International 51/52: 133–141
Konecka-Betley K. 1996. Zastosowanie metody mikromorfologicznej do badań gleb kopalnych. Materiały z konferencji „Metody badań paleopedologicznych i wykorzystanie gleb kopalnych w paleopedologii” Łódź, 26–28 czerwca 1996, 65–66. Łódź
Nowak, M., Kozłowski, K.J., Kaczanowska, M., Vizdal, M., Kalicki, T., Moskal-del Hoyo, M., Budek, A., Litvinyuk, G., Lityńska-Zając, M., Sobierska, E. and Wyszomirski, P. 2010. Early Neolithic in the upper Tisza basin: New data from Moravany, Eastern Slovakia. Eurasian Prehistory 7 (1): 159–219
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Starkel L. 2001. Historia doliny Wisły od ostatniego zlodowacenia do dziś. Monografie Instytutu Geografii i Przestrzennego Zagospodarowania PAN 2: 1–259
Starkel L., Czopek S., Madeja J., Budek A. and Harmata K., 2002. Ewolucja środowiska a osadnictwo pre¬historyczne na przedpolu brzegu Karpat w rejonie Sędziszowa i Rzeszowa. Materiały i Sprawozdania Rzeszowskiego Ośrodka Archeologicznego XXIII: 5–28
Starkel, L., Kalicki, T., Krąpiec, M., Soja, R., Gębica, P. and Czyżowska, E. 1996. Hydrological changes of valley floor in the upper Vistula Basin during Late Vistulian and Holocene. In L. Starkel (ed.), Evolution of the Vistula river valley during the last 15 000 years VI, Geographical Studies, Special Issue 9: 1–128
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Relation:

Archaeologia Polona

Volume:

49

Start page:

121

End page:

133

Detailed Resource Type:

Article

Format:

application/pdf

Resource Identifier:

oai:rcin.org.pl:61751 ; 0066-5924

Source:

IAiE PAN, call no. P 357 ; IAiE PAN, call no. P 358 ; IAiE PAN, call no. P 356 ; click here to follow the link

Language:

eng

Rights:

Rights Reserved - Restricted Access

Terms of use:

Copyright-protected material. Access only on terminals at the Institute of Archaeology and Ethnology of the Polish Academy of Sciences, may be used within the limits of statutory user freedoms.

Digitizing institution:

Institute of Archaeology and Ethnology of the Polish Academy of Sciences

Original in:

Library of the Institute of Archaeology and Ethnology of the Polish Academy of Sciences

Access:

Closed

Object collections:

Last modified:

Apr 7, 2023

In our library since:

Feb 27, 2017

Number of object content downloads / hits:

23

All available object's versions:

https://www.rcin.org.pl/iae/publication/77029

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