Poznań, a city in central-western Poland, is located in the lowland region but has no less attractive geomorphological and human history. It was here that Poland was born at the end of the tenth century. The city's location is connected with the meridian course of the Warta River valley. In contrast, in the northern part of the city, there is a vast area of the frontal moraines of the Poznań Phase of the Weichselian Glaciation. Against the backdrop of the geomorphological development of the city, the article presents the existing geosites, classified as urban geosites. The present geosites include three lapidaries with Scandinavian postglacial erratics, one of them also with stoneware, a fragment of a frontal push moraine and impact craters. Besides, three locations of proposed geosites with rich geomorphological and/or human history were identified. These are as follows: the peat bog located in the northern part of the city, defence ramparts as exhumed anthropogenic forms, and the Warta River valley. The existing and proposed geosites in Poznań were evaluated in three ways. In general, it should be assumed that the proposed new geosites are higher ranked than the current ones.

Das Grab aus Kruszyn, 2009 in Kujawien entdeckt, rechnet zu einer kleinen Regionalgruppe der Schnurkeramik. Es zeichnet sich durch einen verhältnismäßig guten Erhaltungszustand und untypisch zahlreiche, aus Knochen und Geweih gefertigte Werkzeugbeigaben aus. Die aufgedeckten sterblichen Überreste wurden anthropologisch und isotopisch analysiert (La tombe de Kruszyn, découverte en 2009 dans la région de Cujavie, fait partie d’un petit groupe régional de la culture à céramique cordée. Elle est relativement bien conservée et se distingue par un riche assemblage d’outils, fabriqués en os et en cornes. Des analyses anthropologiques et des investigations isotope (Excavated in 2009, the barrow from Kruszyn (the Kujawy region) is related to a small regional group of the Corded Ware culture. Noteworthy is a fairly good state of its preservation and a remarkably numerous assemblage of tools made of bone and antler. Unearthed human remains were anthropologically studied and examined isotopically (Grób z Kruszyna, odkryty w 2009 r. na Kujawach, należy do niewielkiej regionalnej grupy kultury ceramiki sznurowej. Wyróżnia się on stosunkowo dobrym stanem zachowania oraz nietypowo licznym zbiorem narzędzi wykonanych z kości i poroża. Szczątki ludzkie poddano analizom antropologicznym i izotopowym (

No abstract

No abstract

No abstract

A paleoenvironmental reconstruction of the landscape of Nea Raedestos Toumba in the Anthemous River valley in central Macedonia, Greece is undertaken using multidisciplinary geoarchaeological methods. The archaeological site is a settlement mound (tell or toumba) that dates to the Neolithic period and the Bronze Age. The tell’s location on the alluvial plain prompted a multidisciplinary investigation to reconstruct the influence of landscape changes on prehistoric settlements in the valley with an emphasis on alluvial sequences. An electrical resistivity tomography survey and three cores were drilled to study the sedimentary environments in and around the archaeological site. Sedimentologic and palynological analysis combined with accelerator mass spectrometry radiocarbon dating show that the oldest habitation layers at the site, from the Middle and Late Neolithic, were located next to a small, periodically drying water body surrounded by ruderal vegetation. Diatom analysis suggests that this water body was supplied by saline/brackish groundwater. The water body was open until the Early Bronze Age, when it was filled and buried by floodplain sediments. This flooding phase at Nea Raedestos likely occurred at the same time as an increase in fluvial aggradation in the neighboring Thessaloniki Plain, which is dated to the beginning of the third millennium BC.

The Anthemous Valley Archaeological Project is a cooperation between Greek and Polish scientists aiming towards archaeological recognition of the northern Aegean within the alluvial Anthemous Valley. The methodology of the project consists of the multidisciplinary tools of settlement archaeology and geoarchaeology. The timeframe spans the prehistoric periods from the Neolithic to the Early Iron Age. One of the main research tasks is to reconstruct the evolution of the landscape in close reference to the cultural changes in the region. To date, all sites within the valley have been catalogued and identified through archaeological prospection and some with the use of geophysical survey. The results point to an intensive occupation in the past, especially during the Bronze Age. Geoarchaeological research was conducted in the tell of Nea Raedestos, which has shown major landscape transformations in the Holocene due to river activity. The current work focuses on the mouth of the Anthemous River to reconstruct the progradation processes and formation of the deltaic plain in relation to prehistoric human occupation of this area.

This article discusses two cases of so-called double barrows from the Middle Bronze Age Komar ow culture cemetery in Bukivna, in the Upper Dniester Basin (Ukraine), in order to demonstrate the potential of incorporating geophysical image analysis, excavations and sedimentological studies towards identifying subterranean funerary architecture. The magnetometer prospection of the Bukivna necropolis revealed the presence of a specific dipolar anomaly within the extent of a double barrow. The excavations uncovered burnt wooden-clay constructions related to mortuary houses.The sedimentological samples collected from the features below the mound provided data for the increased ferrous content. Another double barrow located in the Pidhoroddia cemetery was prospected by means of magnetometry, which did not reveal any similar anomaly within the magnetometry plan, thus providing evidence for a possible lack of discussed mortuary structure.