Multi-proxy reconstruction of mire development in the Poręby Wojsławskie ecosystem (Sandomierz Basin, southeastern Poland)

Chodorowski, Jacek; Plak, Andrzej; Pidek, Irena Agnieszka; Dobrowolski, Radosław

doi:10.2478/s13386-013-0109-6

Cited by 2 publications

(2 citation statements)

References 20 publications

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“…a multi-proxy reconstruction provides the best approach (eg. Andrič et al 2009;Chodorowski et al 2013;Dietre et al 2014;Karpińska-Kołaczek et al 2018;Kołaczek et al 2018). the aim of our work is to highlight the potential causes of human and/or climate-induced environmental changes for the area between the Kupa and Una rivers, recognised under toponims Kordun and banovina (fig.…”

Section: Uvodmentioning

confidence: 99%

“…Upotreba različitih indikatora je općenito najbolji pristup (npr. Andrič et al 2009;Chodorowski et al 2013;Dietre et al 2014;Karpińska-Kołaczek et al 2018;) razumijevanju čimbenika koji dovode do promjena u prirodnoj sredini (posredovanih klimom ili ljudskim utjecajem). svrha našega rada je istaknuti potencijalni utjecaj antropogenoga pritiska i/ili klimatskih promjena u okolišu na području između Kupe i Une, geografski znanim kao Kordun i banovina (sl.…”

Section: Uvodunclassified

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Dvije tisuće godina okolišnih promjena na području središnje Hrvatske – vegetacija, požari i hidrologija utjecani klimatskim prilikama i ljudskim pritiskom

Hruševar

Bakrač

Miko

et al. 2020

Pril. Inst. arheol. Zagrebu (Online)

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This paper presents the paleoenvironmental reconstruction of a mire sequence near the village Blatuša, with a focus on changes in vegetation composition, hydrological regime and fire history of the Banovina/Kordun area during the last two millennia. For this purpose, pollen, non-pollen and charcoal analysis were done. By the application of CONISS statistical analysis three different pollen assemblage (sub)zones could have been distinguished: a dominance of alder-beech/oaks from the 2nd to the middle of the 7th century, followed by a prevalence of grasses-beech/oaks till the end of the 13th century. Finally, an assemblage of grasses-hornbeam/oaks populated the area from the 14th to the beginning of the 20th century. The high abundance of peat mosses (Sphagnum) from the 11th to the end of the 14th century must indicate increased precipitation and higher frequencies of rainfall during the Medieval Climate Anomaly. Transition from an ombrotrophic to minerotrophic phase of mire evolution during the Little Ice Age is caused by changing in moisture level, with somewhat wetter period prevailing till the middle of the 17th century followed by drier conditions till the beginning of the 20th century. Although cereal pollen grains first appear from the layers dated to the late 14th century and the proportion of secondary anthropogenic indicators were low during the entire Middle Ages, a large number of charcoal particles suggests stronger anthropogenic activity than indicated by observed changes in vegetation composition. Still, a sharp rise of non-arboreal pollen during the Migration period most likely reflect a general natural succession process on mire surface than persuable proof of Avaric-Slavic impact on vegetation. Direct anthropogenic pressure indicated by weeds and cereal pollen can be tracked from the Late Middle Ages onwards.

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Section: Uvodmentioning

confidence: 99%

Section: Uvodunclassified

Dvije tisuće godina okolišnih promjena na području središnje Hrvatske – vegetacija, požari i hidrologija utjecani klimatskim prilikama i ljudskim pritiskom

Hruševar

Bakrač

Miko

et al. 2020

Pril. Inst. arheol. Zagrebu (Online)

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The early Bronze Age feature from Wilczyce, site 10, Sandomierz district – An interpretation of its functioning in light of multidimensional analysis

Jarosz¹,

Boroń²,

Witkowska³

et al. 2020

Ana Arch Resso

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The aim of this paper is to present the multidimensional characteristics of the feature number 4 at the site in Wilczyce located on the Sandomierz Upland. During exploration of the pit rich flint material, fragments of pottery vessels and animal bones were found and just above the bottom a “deposit” involved a human skull of the young female, two cattle mandibles, a sheep/goat tibia and astragalus, a damaged cattle scapula and radius, and a polishing stone were deposited. The C14 date obtained from the tooth from the cattle jaw was 3790 ± 35 BP. Based on the shape and the size of discovered feature it is possible to classify it as a typical storage pit but presence of “deposit” enable to postulate a ritual character of assemblage that reflect some kind of burial practices of the Mierzanowice culture. Rituals in the form of interring the dead or parts of their bodies can be found also in the Unietice culture so such features may indicate the emergence of a certain supra- -regional and cross-cultural trend in the early Bronze Age.

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Multi-proxy reconstruction of mire development in the Poręby Wojsławskie ecosystem (Sandomierz Basin, southeastern Poland)

Cited by 2 publications

References 20 publications

Dvije tisuće godina okolišnih promjena na području središnje Hrvatske – vegetacija, požari i hidrologija utjecani klimatskim prilikama i ljudskim pritiskom

Dvije tisuće godina okolišnih promjena na području središnje Hrvatske – vegetacija, požari i hidrologija utjecani klimatskim prilikama i ljudskim pritiskom

The early Bronze Age feature from Wilczyce, site 10, Sandomierz district – An interpretation of its functioning in light of multidimensional analysis

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