Aldona Mueller-Bieniek

The environmental and cultural contexts of the late Iron Age and medieval settlement in the Mazurian Lake District, NE Poland: combined palaeobotanical and archaeological data

Pollen analysis of sediments from three lakes and analysis of plant macroremains including charcoal from archaeological sites in the Mazurian Lake District provide new data for the reconstruction of vegetation changes related to human activity between the 1st and 13th century ad. At that time settlements of the Bogaczewo culture (from the turn of the 1st century ad to the first part of the 5th century ad), the Olsztyn Group (second part of the 5th century ad to the 7th or beginning of the 8th century ad), and the Prussian Galinditae tribes (8th/9th–13th century ad) developed. The most intensive woodland clearing occurred between the 1st and 6th/7th century ad. Presence of Cerealia-type, Secale cereale and Cannabis-type pollen, as well as macroremains of Hordeum vulgare, S. cereale, Triticum spelta, T. cf. monococcum, T. cf. dicoccum, Avena sp. and Panicum miliaceum documented local agriculture. High Betula representation synchronous with microcharcoal occurrence suggests shifting agriculture. After forest regeneration between c. ad 650 and 1100, the area was strongly deforested due to the early medieval occupation by Prussian tribes. The archaeobotanical examination of samples taken in a cemetery and a large settlement of the Roman Iron Age revealed strong differences in the taxonomic composition of the fossil plant remains. An absolute dominance of birch charcoal in the samples from the cemetery indicates its selective use for funeral pyre construction. There is a difference between cereals found in both contexts: numerous grains of Triticum have been found in the cemetery, while in the settlement crops were represented mostly by Secale and Hordeum. Grass tubers, belonging probably to Phleum pratense, are among the particularly interesting plant remains found in the cemetery.

Cultivated plants in medieval Kraków (Poland), with special reference to amaranth (Amaranthus lividus L. cf. var lividus) and ruderal communities

Abstract This paper summarises archaeobotanical studies of plant macroremains derived from medieval town deposits of Kraków, focusing on cultivated plants. Correspondence analysis was used in interpreting the botanical data and their archaeological context. Changes in cultivated plant composition were connected mainly with the chartering of the town under Magdeburg law in 1257, and are discussed in terms of their temporal relation to the chartering of Kraków and possible changes in the food preferences and wealth of the residents. Millet and wheat remains are rarer in specimens from after the establishment of the town; this seems connected mainly with the relocation of the mills outside the city walls. The number of cultivated plants generally increased in the late medieval samples, but hop and mallow were more frequent in the tribal period than later. Problems in the definition of cultivated plants are discussed. The probable escape of cultivated amaranth (Amaranthus lividus L. var. lividus) from gardens to ruderal communities is indicated in the samples. A comparison of archaeobotanical data from written sources shows the incompleteness of both types of source, including the clear underrepresentation of some cultivated plants in the archaeological deposits of the town (especially peas, Pisum sativum), a deficiency which should be considered in other archaeobotanical and palaeodietary studies.

Plant macroremains from an early Neolithic site in eastern Kuyavia, central Poland

Abstract The study examined plant remains from the Smólsk 2/10 site, situated on the border of two different landscapes and preserving traces of Neolithic occupation from several cultures: Early Linear Pottery culture (LBK, ca 5300-5200 cal. BC to ca 5000 cal. BC). Stroke Band Pottery culture (SBP, ca 4700-4400 cal. BC), the Brześć Kujawski group of Lengyel culture (BKG, ca 4500-4000/3900 cal. BC), Funnel Beaker culture (TRB, ca 3950-3380 BC), and also some features of the Lusatian culture (Hallstatt C, ca 970-790 cal. BC). Mostly hulled wheat remains (Triticum monococcum, T. dicoccum) were found in the LBK, SBP, and BKG cultures; they were completely absent in younger cultures (TRB, Lusatian), where barley remains appeared. Among other plants the most numerous were remains of small-grain grasses (mostly cf. Hierochloë type), feather grass (Stipa sp.), wild buckwheat (Fallopia convolvulus), and goosefoot (Chenopodium album type), but the plant remains are relatively scarce. The archaeobotanical data obtained from the site supplement data from neighbouring Osłonki to the west and Wolica Nowa to the north-west. The differences between those microregions are reflected mostly in the earlier appearance of feather grass (Stipa sp.) in the Smólsk area as well as the higher quantity of crop chaff remains in the Osłonki area, but their random occurrence, along with the fragmentariness of the archaeological data, must be taken into account. However, intentional introduction of feather grass by the first Neolithic settlers in eastern Kuyavia cannot be excluded. The relatively high proportion of small-grain grasses, usually interpreted as traces of fodder, together with the scarcity of crop remains at the Wolica Nowa site, suggests that the site was connected more with animal husbandry than with agriculture. On the other hand, the small-grain grasses at Smólsk are represented mainly by a large number of non-weedy grass (cf. Hierochloë type) grains from the crop sample, which cannot be explained in a simple way. A comparison of the anthracological data from the Osłonki and Smólsk microregions reveals differences in woodland management and differences between the local environments. Pine wood was more accessible at Smólsk than at Osłonki, due to local landscape characteristics.

Plant materials used as temper in the oldest Neolithic pottery from south-eastern Poland

Plant materials were frequently used as a temper as an important part of the process of making pottery. However, identification of the presence of tempering material and its taxonomic composition are still uncommon practices. This paper presents the results of a study of plant remains observed in pottery dated to the oldest Neolithic from south-eastern Poland, as a tool for detecting or confirming changes in the method of making the pottery. In previous studies, plant material was noticed sporadically in coarse ware and its identification was based on macroscopic plant morphology. On the other hand, remains of plants were not usually observed in the other finer ware types since their surfaces were frequently smoothed and decorated, while their sections were very thin. Therefore, in the present study, these groups of pottery have been studied in detail. A preliminary observation of surfaces and fresh sections of selected potsherds has shown that plant temper was neither evident nor abundant in them. However, with microscopy, small fragments of plant tissues and their imprints have been seen inside the clay. Their identification was not possible on the basis of plant morphology, but was carried out with the help of plant anatomy, especially by observing the microscopic features of plant epidermis. Previous archaeobotanical studies from the area indicated that the plants used as temper in coarse ware mostly included remnants of cereal chaff. Consequently, this paper will test this hypothesis in the case of the finer Neolithic ceramics.

Benefits and weaknesses of radiocarbon dating of plant material as reflected by Neolithic archaeological sites from Poland, Slovakia and Hungary

Abstract Radiocarbon dating of the plant material is important for chronology of archaeological sites. Therefore, a selection of suitable plant samples is an important task. The contribution emphasizes the necessity of taxonomical identification prior to radiocarbon dating as a crucial element of such selection. The benefits and weaknesses of dating of taxonomically undetermined and identified samples will be analysed based on several case studies referring to Neolithic sites from Hungary, Slovakia and Poland. These examples better illustrate the significance of the taxonomical identification since plant materials of the Neolithic age include only a limited number of cultivated species (e.g. hulled wheats) and typically do not contain remains of late arrived plants (e.g. Carpinus betulus and Fagus sylvatica). For more accurate dating results cereal grains, fruits and seeds, which reflect a single vegetative season, are preferred. Among charred wood, fragments of twigs, branches and external rings should mainly be taken into account, while those of trunks belonging to long-lived trees should be avoided. Besides the absolute chronology of archaeological features and artefacts, radiocarbon dating of identified plant remains might significantly contribute to the history of local vegetation and food production systems.

An insight into Bronze Age subsistence strategy in forested Carpathian foothills, based on plant macro-remains

Lipnik site 5, from which a storage pit dated to the Middle Bronze Age (ca. 1400–1100) was studied, gave more than 70 plant taxa in the extraordinarily well-preserved charred assemblage. In the paper, a detailed description of selected plants is presented followed by environmental interpretation. Acorns (Quercus) dominated in volume and proso millet (Panicum miliaceum) in the number of specimens. The first large find of that late incomer north of the Carpathian Mountains is presented here. The pit users also used hulled wheat (einkorn, emmer, and spelt); barley; and probably peas. In the pit, a large number of grassland plants were noted accompanied by a very few remains of aquatic (Elatine) and forest herbaceous plants (Astrantia major). Weeds and ruderal plants were also present. The composition of plant remains is very unusual for this type of archeological feature, suggesting a mixed type of food strategy for its users, dominated by plant gathering and animal husbandry. The site is located in a newly settled ecotone zone, on the margin of fertile loess areas and mountain foothills.