Plant remains from an early Neolithic settlement at Moravany (eastern Slovakia) (original) (raw)
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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 materialanditstaxonomic compositionarestilluncommon 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,whiletheirsectionswereverythin.Therefore,in thepresentstudy,these groupsofpotteryhavebeenstudied 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 imprintshavebeenseeninsidetheclay.Theiridentification 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 includedremnantsof cereal chaff. Consequently,this paper will test this hypothesis in the case of the finer Neolithic ceramics
Bánffy, E. ed. The Environmental History of the Prehistoric Sárköz Region in southern Hungary, 187-2019 , 2020
As aptly noted by Kalicz et al. (2007, 20), the current state of archaeobotanical research on the Neolithic in Hungary makes it difficult to draw any final conclusions (Tempir 1964; see also Gyulai 2007; 2010). Therefore, the DFG project “Die Besiedlungsgeschichte der Siedlungskammer um Fajsz (Kom. Bács-Kiskun, Südungarn) in der Ältesten Bandkeramik” (2006 – 2010) as well as the excavations ahead of the construction of the Hungarian M6 motorway (Bánffy et al. 2010; 2014; Osztás et al. 2016, and further contributions in the same volume) provided an excellent opportunity to start systematic archaeobotanical investigations in the Sárköz region for the first time. Of the four excavated sites in the Sárköz region, the samples comprise plant remains dating to the Neolithic and, although to a lesser extent, to the Bronze Age (the latter included here for the sake of completeness only). This study reviews and discusses the fully archived and assessed quantitative data with the ArboDat 2016 archaeobotanical database program.
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 vege-tative 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.
Plant macroremains from an early Neolithic site in eastern Kuyavia, central Poland
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 northwest. 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.
Until recently the recovery of plant remains in Croatia was rare, resulting in few studies addressing the nature of Neolithic crop cultivation. This paper presents new archaeobotanical data from eleven Neolithic settlements in coastal and continental Croatia. Within continental Croatia, three sites dating to the Starčevo culture (early/middle Neolithic; ca. 6000–5300 cal bc) and six to the Sopot culture (late Neolithic; ca. 5300–4000 cal bc) are examined along with two Hvar culture sites (late Neolithic; ca. 4800–4000 cal bc) located along the coast. Different settlement types are included in the study: open air sites, tells and cave sites. From the data collected the most common crops identified were einkorn, emmer, barley, lentil, pea and flax, as well as the fruits Cornus mas (Cornelian cherry) and Physalis alkekengi (Chinese lantern), which were particularly dominant in the Sopot culture settlements. By examining formation processes, sieved crop processing products and by-products were identified at six of the sites, suggesting that cereals were processed on a day-to-day basis at the household level. In contrast, the remains from the late Neolithic coastal cave site of Turska Peć suggest two distinct formation processes. At the eastern side of the cave the plant remains suggest that episodes of dung burning occurred, possibly to clear the cave of excess waste during seasonal habitation of the cave by herders and livestock. Towards the back of the cave, cereal remains and higher charcoal densities may suggest an area used for food preparation or cooking.
The present work attempts to provide an understanding of the issue of Mesolithic archaeobotany, especially in terms of plant use, woodland clearance, and a discussion concerning Mesolithic agriculture. Plant use patterns in hunter-gatherers are also presented and discussed. Special attention is paid to taxa occurring within archaeological context at Mesolithic sites in Europe, particularly in the Czech Republic, along with ethnobotanical evidence for their use.
Radiocarbon, 2023
In the absence of wood, bone, and other organics, one possible candidate for determining the age of a site is the radiocarbon (14C) dating of pottery. In central Europe during the Early Neolithic, pottery was ubiquitous and contained substantial quantities of organic temper. However, attempts at the direct dating of organic inclusions raises a lot of methodological issues, especially when several sources of carbon contribute to the resulting radiocarbon age. Hence an alternative approach to dating of the early pottery is necessary. Here, we present a novel method of bulk separation of organic content from the grass-tempered pottery from Santovka (Slovakia). The procedure is based on the consecutive application of three inorganic acids, dissolving clay, silica content, and low molecular or mobile fractions to separate organic inclusions added to the pottery matrix during the formation of vessels. Radiocarbon dates obtained with this method are coherent and produce the shortest time span compared to other pretreatment methods presented in this study. The paired dates of grass-tempered pots with the 14C age of lipids extracted from the same pots point to a difference of 400-600 14C yr, however they are in line with the site's chronostratigraphic Bayesian model. Grasstempered pottery from Santovka (Slovakia) is dated to the first half of the 6th millennium cal BC, making it the earliest pottery north of the Danube. It seems feasible that ceramic containers from Santovka were produced by hunter-gatherers, and pottery predated the arrival of farming in the Carpathian region by a couple of centuries.
Plant remains from an Early Iron Age well at Hajndl, Slovenia
Collegium antropologicum, 2009
The archaeobotanical samples analysed derive from a well-preserved well dated to the Early Iron Age (Hallstatt) according to pottery found in the sampled layers and on a radiocarbon dating (720-520 cal B.C.) of the wooden construction of the well. Cultivated plants (Panicum miliaceum, Linum usitatissimum, Papaver somniferum and Camelina sativa) were recorded in relatively small numbers whereas primary cereals are lacking. Together with quite a large number of accompanied weeds they suggest agriculture activities, but a mixture of weeds and ruderal plants was probably also growing inside the relatively large settlement complex and could have been included in the assemblages just by chance. The plant species composition indicates local vegetation developed under strong anthropogenic influence and on mainly moist and nitrogen-rich soils. Grassland plants and an almost complete lacking of tree and shrub species characteristic for the climax vegetation (deciduous mesophilous mixed forest...
The first permanent occupation in the micro-region localized around Janowice, in the middle valley of the Dunajec river in the Polish Carpathian Foothills, begun at the turn of the Middle Bronze Age and the Late Bronze Age. Different landscape forms were settled, in which the highest part of the hills or areas located in the proximity of the river were especially chosen for stable settlement. All of them were characterized by the presence of fertile loess and alluvial soils. Macroscopic plant remains found in different occupational phases of six archaeological sites represent cultivated and wild plants. The remains of cultivated plants confirmed that plant resources formed an important part of the past subsistence strategies. It was observed that the same spectrum of cultivated species was utilized during about one millennium of occupation in the forelands, from the beginning of the occupation until the end of the Early Iron Age. Hordeum vulgare, Triticum diccocon, Triticum spelta and Panicum miliaceum were the dominant cereal crops. A consistent choice of varied cereal species, along with pulses, may indicate that both winter and summer crops were cultivated and the works dedicated to crop farming were distributed along various months. This strategy could also provide higher and more reliable yields. In addition, the edaphic requirements of weed remains may confirm that people used rich and moderately moist soils for cereal cultivation. Overall, a relatively early cultivation of spelt wheat and millet should be emphasized in the Carpathian Foothills since the oldest phase can be dated back to ca. 1500e1300 cal. BC. A relatively high abundance and ubiquity of spelt wheat resulted very interesting in the context of other cereal remains found in the Late Bronze Age in Poland. In addition, an Agricultural Predictive Model was prepared for the closest regions of the settlements in order to demonstrate areas with optimal environmental conditions for agricultural practices. Altogether, macroscopic plant remains are related mainly to synanthropic habitats from fields to ruderal ones. Moreover, human activities could be also responsible for the development of steppe-like plant communities, which are inferred after the finding of feather grass (Stipa sp.). The remains of wood preserved as charcoals represent a separate group of plants. They were associated to firewood collections and therefore their analysis may be used for the reconstruction of local woodlands. A major formation is the oak-hornbeam forest. Interestingly, at the end of the Subboreal period, woodlands were dominated by late-arriving species to the Polish territory, such as Carpinus betulus and Fagus sylvatica. Abies alba is also well represented, especially in settlements located on the hills. It seems that forest formations were also subjected to anthropization and the main changes included the presence of more open forests and appearance of unstable stands in different successional stages.