Excavations of an Early Neolithic Site at Tăşnad, Romania

The town of Tăşnad, in north-west Romania, is situated at the western end of the Tăşnad Hills which rise to a height of up to 230m above sea-level; the site ‘Sere’ is situated south-west of the town near a thermal spa on the banks of the Cehal river, a tributary of the Ier. The Cehal valley opens towards the Ier and Someş plains which form the north-easternmost part of the Great Hungarian Plain, a marshy area until the large-scale drainage-works of the 19th and 20th centuries. Even today, the Cehal valley is quite swampy, especially at the confluence with the Ier. The Austrian military maps demonstrate large-scale forest-clearance during the last three centuries; at the end of the 18th century, the site itself was still forested. Several prehistoric sites from different periods are located on the first and second terraces of the Cehal, at altitudes of around 140m.

. The posterior part of a steatopygian figurine was also found. There are numerous bones of cattle, pig, ovicaprids and wild boar, as well as aurochs' horn-cores and red deer antlers.
Several houses were found in the course of the excavations -three of which were marked by post-holes (Fig. 3). Feature 100/2009, measuring 8.5x6m, had posts along the walls, with a central row of three to support the roof. On its southern side, three post-holes seem to have belonged to an annex. The other two post-built houses were of similar size (9x10m and 7.5x7m) and construction. Another house was partly dug into the soil. It was oval in shape, with the roof supported by seven posts; an oven had been dug into its subterranean wall. Inside, enormous quantities of pottery, burnt bone and ash were discovered, with numerous loom-weights indicating its use as a weaving hut. As flax is best worked when slightly wet, semi-subterranean houses were used for this purpose up into the Middle Ages. A second semi-subterranean house could only be partly excavated. Large oval and irregular pits with post-holes, traditionally interpreted as pit-houses, were also found -one of which contained further loom-weights.
Four single graves of the Criş culture have been excavated at Tăşnad. Three of them were located in proper grave-pits, but the other was buried in a feature that was probably a refuse pit or a pit-house. All the skeletons lay in a contracted position on their left sides. One grave contained two obsidian blades; the other burials had no grave goods at all.
There are also later features at Tăşnad Sere, dating to the Middle Neolithic Pişcolt culture, the Late Copper Age Coţofeni culture and the Przeworsk culture of the Roman period. Excavation reports from Tăşnad have been published as short reports in the Chronicle of Archaeological Research of Romania (www. cimec.ro), but a detailed publication of the discoveries remains a task for the future.
Based on the pottery style, the site of Tăşnad Sere can be attributed to phases IIIB and IVA of the Criş culture, according to the chronological system of Gh. Lazarovici (1984). The Criş culture, known as Starčevo in Serbia, Bosnia and Macedonia, and as Körös in Hungary (Fig. 1), is the oldest Neolithic culture of the Balkans and the Pannonian Basin, dating to 6300-5200 BC (Schubert, 1999). It is characterised by organic tempered pottery, decorated with painted and incised patterns. Both tell settlements and open settlements are known, with the houses normally consisting of small, one-room, rectangular structures, built of wattle and daub, containing a hearth (Lazarovici and Lazarovici, 2006;2011). Emmer, einkorn and millet were cultivated, as well as lentils, field peas, opium poppy and flax, but wild plants also formed an important part of the diet (Gyulai, 2010). Animal-bone assemblages are normally dominated by ovicaprids, followed by cattle and pig, as well as numerous wild mammal species. Birds, fishes (Kovács et al., 2010: 248f.) and molluscs (Gulyás et al., 2007) were also exploited.
In north-west Romania, the Neolithization process (understood as the appearance of pottery and ground stone tools) took place later than in the neighbouring areas of central Transylvania, the Banat and the Tisa valley, during the period Criş IIIB-IVA. The Criş communities may have arrived in Tăşnad from central Transylvania, reaching the Sălaj area, then following the Barcău and Ier valleys, and maybe the Crasna valley. Settlements of Criş type are known from Sălacea, Tarcea, Voievozi, Văşad, Pişcolt, Berea and Urziceni. The material uncovered at Tăşnad is also similar to contemporary sites in both north-western Romania (Homorodu de Sus, Homorodu de Mijloc, Zăuan, Suplacu de Barcău/Porţ and Călineşti Oaş) and northeastern Hungary (Méhtelek and Nagyecsed), towards the west. Thus, Németi (1999) has claimed that the first agricultural settlers of the middle Tisa valley arrived from the south, following the river.
Pottery forms found at Tăşnad include characteristic biconic vessels with a rounded, slightly everted rim, biconic bowls, biconic jars with a short neck, and vessels with a hollow pedestal. The majority of the pottery from Tăşnad is tempered with sand, grog, silt and chaff, which is characteristic for the evolved phases of the Criş culture. Because of the use of silty clay and organic temper, the pottery is very soft and has a 'soapy' surface, a phenomenon that starts in the later phases of the Criş culture (IIIB-IVA). This dating is supported by sherds with incisions below the rim, as such incised ornament is typical for the IIIB-IVA phases of the culture. There are also polished ornaments, barbotine decoration and fingernail imprints.

UCL Institute of Archaeology excavations
In summer 2011, Ulrike Sommer visited the site and decided that the existence of a thick, well-preserved, occupation layer made Tăşnad Sere ideal for research on deposition processes and the activity structure of a Criş settlement. In addition, the large-scale rescue excavations by the Satu Mare County Museum would enable a small, detailed, research excavation to be placed in the wider context of the overall settlement-site. Early Neolithic settlements in both southeast and central Europe normally contain numerous pits and, in flat settlements, these can often be the only surviving structures. Since the 1970s, finds in the long pits along the sides of Linearbandkeramik (LBK) houses have been used to date these houses which are normally only represented by postholes, as the original Neolithic surface has been eroded. Complex chronologies of settlement development (Stehli, 1994), and of the development of individual settlements (Lüning, 2005), have thus been developed. In southeast Europe, on the other hand, it has often been thought that irregular pits could have served as dwellings (pit-houses or sunken houses), especially in the early phases of settlements. Finds in these pits have thus been seen as in situ refuse which could be used for dating their use as houses. However, in 1988, Harald Stäuble conducted a detailed study of the distribution of the finds in the long pits of Friedberg-Bruchenbrücken (Germany), a settlement of the earliest LBK and, for the first time, raised doubts concerning the contemporaneity of LBK houses and the long-pit finds (Stäuble, 1997). Several LBK occupation horizons are known, e.g. Olszanica (Milisauskas, 1976), but none of them has so far been excavated in sufficient detail to evaluate the relationship between houses, occupation layers and finds in pits.
In south-east Europe, where occupation layers are more common than in central Europe, occupation layers have often been treated as 'unstratified' and thus of little value for establishing chronologies and investigating the use of space in Neolithic settlements. During the excavations of Ecsegfalva 23, in County Békés (Hungary), detailed recording of finds took place and clear indications of settlement-like concentrations of daub were located, but no distinct structures could be identified (Whittle and Zalai-Gaál, 2007).
In Tăşnad, the coexistence of a thick occupation layer, deep pits and house remains provides ideal conditions for the examination of the relationship between these features in order to answer the difficult questions of how finds get into pits and how they relate to adjacent houses.
The archaeological remains in the area of Tăşnad Spa were not only threatened by building activities for the burgeoning thermal bath, but also by erosion along the Cehal acerbated by the activities of cows which daily climb the increasingly unstable banks of the river on their way to graze in the Cehal valley (Fig. 4). In 2012, the Satu Mare County Museum started rescue excavations on the right bank of the Cehal channel, conducted in cooperation with the UCL Institute of Archaeology, under the direction of Cristian Virag, Ulrike Sommer and Ciprian Astaloş.
After a magnetometry survey, a 10x10m trench was dug to assess both the depth of the occupation layer and the preservation and distribution of Neolithic finds. Six testpits helped to delimit the extent of the settlement and to elucidate the alluvial history of the Cehal river. Evidence of a former riverbed was discovered, and early Iron Age (Gáva) remains, c.1m deep, have allowed us to date the formation of hillwash in the Cehal valley.
The occupation layer is being excavated in a system of quadrants and spits to provide a close spatial control on the location of finds and botanical remains (Fig. 5). Every find >1cm is recorded three-dimensionally, together with information on its orientation and dip. Thus, it will be possible to reconstruct how the finds were deposited and their subsequent depositional history (cf. Sommer, 1991). Often, several sherds of the same vessel are found close together (Fig.  5), separated by empty space from the next find-concentrations. This is likely to indicate distinct dumping events, perhaps on the site of an abandoned house. The layer below is generally much poorer in finds.
The finds consist mainly of pottery, but daub, hearth remains, ground stone, animal bones and lithics have also been uncovered. Both local raw materials, such as jasper and limnic quartzite, and imported siliceous rocks were used: Hungarian/Slovakian obsidian, blond Balkan flint from north-eastern Bulgaria, and Prut flint from Moldavia or the Ukraine. These indicate the far-flung connections of the early farmers at Tăşnad. Most of the obsidian pieces are rather small and often cortical. Debitage, as well as formal tools, has been recovered, whereas the blond Balkan flint is only represented by regular blades and blade fragments. In contrast, large obsidian cores were discovered at Căuaş and Urziceni (Németi, 1999: 19); this may point to the existence of specialized settlements or internal trade. By systematic bucket-flotation, we have recovered plenty of charcoal, but so far very few seeds. Fishbones and the remains of other aquatic resources are similarly missing, running counter to expectation given the riverine environment. This can only be further explored once deeper levels of the site and the contents of pits have been excavated and analysed. Animal bones also remain rare, but have been common in the rescue excavations on the site. They have not yet been analysed; the article of El Susi (2011) is based on a limited selection of finds that is probably not representative.
Already, the excavations are offering tantalising glimpses of daily life in the early Neolithic, but only the detailed mapping of all the different find-categories and their distribution, as well as refitting-studies, will allow us to understand how a Criş settlement actually functioned through time.