J. Beneš, G. Naumov, Tereza Majerovičová, Kristýna Budilová, J. Bumerl, V. Komárková, Jaromír Kovárník, Michaela Vychronova, L. Juřičková
{"title":"An Archaeobotanical Onsite Approach to the Neolithic Settlements in Southern Regions of the Balkans: The Case of Vrbjanska Čuka, a Tell Site in Pelagonia, Republic of Macedonia","authors":"J. Beneš, G. Naumov, Tereza Majerovičová, Kristýna Budilová, J. Bumerl, V. Komárková, Jaromír Kovárník, Michaela Vychronova, L. Juřičková","doi":"10.24916/IANSA.2018.2.1","DOIUrl":null,"url":null,"abstract":"This paper is focused on the Neolithic tell-site of Vrbjanska Čuka in Pelagonia, Republic of Macedonia, where the authors have been performing archaeobotanical research since 2016. Results of the analyses of botanical macroremains and microremains (starch, phytoliths) and faunal microremains collected in season 2016 are presented in the broader context of the Neolithic in the Balkans in order to estimate the bioarchaeological potential of this site. The first and final parts of the paper outline the bioarchaeological studies connected with Neolithic settlements in the southern regions of the Balkans. A substantial proliferation of environmental studies has been recorded in the last decade concerning the archaeobotanical and archaeozoological evidence. Here, most attention is paid to archaeobotanical studies which consider Neolithic settlements and their bioarchaeological context. IANSA 2018 ● IX/2 ● 121–145 Jaromír Beneš, Goce Naumov, Tereza Majerovičová, Kristýna Budilová, Jiří Bumerl, Veronika Komárková, Jaromír Kovárník, Michaela Vychronová, Lucie Juřičková: An Archaeobotanical Onsite Approach to the Neolithic Settlements in Southern Regions of the Balkans: The Case of Vrbjanska Čuka, a Tell Site in Pelagonia, Republic of Macedonia 122 pp. 47–51). This concept substantially favoured those studies dealing with material culture rather than ones addressing environmental and biological issues. Furthermore, the lack of local specialists led to a predominance of artefactual and architectural studies. Bioarchaeological research was concentrated towards large systematic excavations made by international expeditions. This is clearly the case with the older research history of the site of Amzabegovo (Gimbutas, 1974; 1976), Sitagroi (Renfrew et al., 1986; Näslund, 2009), Argissa (Reingruber, 2005), Nea Nikomedeia (Pyke, Yiouni, 1996; van Zeist, Bottema, 1971), Karanovo (Hiller, Nikolov, 1988) and Dikili Tash (Treuil, 1992) being the best examples. The activities of bioarchaeologists have been oriented towards the thematic pioneer research of Neolithic palaeoeconomy. In this regard, R. Dennell studied the archaeobotanical assemblages of such Neolithic sites as Chavdar and Kazanlak in Bulgaria. Dennell established an alternative approach which suggested that the economic value of a Neolithic plant resource can be ascertained by considering its context within the crop-processing activities of a site or area (Dennell, 1972; 1974; 1976). The research of Dennell has opened up new avenues in onsite archaeological interpretations, certainly in comparison to the older common approach of recording the presence/absence of economic plant species in archaeobotanical assemblages. R. Dennell also worked with the archaeozoologist G. Kovačev and attempted to provide a complete onsite bioarchaeological picture of the plants and animals. Likewise, P. Halstead has contributed much to the research area of archaeozoology. He has published a series of papers focused on archaeozoological data of the Neolithic and Bronze Age (Halstead, 1981; 1989). In so doing he has attempted to ascertain the potential of archaeozoological material in helping to identify the part of large-scale pastoral specialization versus small-scale stock husbandry as a component of mixed farming. His concept has opened up such phenomena as the large-scale exchange of animals for meat and the identification of “producer sites” and “consumer sites”, as well as the issues of milking, dairying and similar phenomena (Halstead, 1996). In the southern regions of the Balkans in the 1980s and 1990s, local specialists were also active, such as E. Chakalova and Z. Popova in Bulgaria (see Kreuz et al., 2017). A substantial shift has been recorded in the last decade towards the adoption of a multi-proxy approach: a new trend in the bioarchaeological research of Neolithic sites. In contrast to the best monothematic studies of the 1970s and 1980s, the multi-proxy approach is based on the synergy of two or more analytical methods. The combination of particular methods has been steeply increasing in number up until today (Marinova, Thiebault, 2008; Karkanas et al., 2011; Pappa et al., 2013; Garnier, Valamoti, 2016; Marinova, Ntinou, 2017; Kreuz, Marinova, 2017; Ivanova et al., 2018; Whitford, 2018). In the last 10–15 years, the “critical mass” of specialists and awareness of the necessity to apply multiproxy approaches has increased. Such synthesis should indeed become “state of the art” in the future (Allen et al., 2017; Ethier et al., 2017; Marinova et al., 2016; Krauß et al., 2017; 2018). Transdisciplinary studies constitute presentday research and the near future for prehistoric onsite archaeology. Archaeobotanical research is still rare for archaeological excavation in this study region of the Balkans. It is due to the lack of specialists and the technical difficulty of sampling in archaeological field research – and the time-consuming work involved in the post-excavational phase. On the other hand, archaeobotany can contribute to resolving palaeoeconomical questions and trace the forms of human behaviour on a specific prehistoric site in great detail. 1.2 Natural setting of the southern Balkans and its Neolithic sites Geographically, the southern Balkans region is very variable: its surface is predominantly mountainous. The climate of the coastal regions differs from that inland, it being more continental. Most of the southern Balkans is dominated by a Mediterranean climate, particularly for the area of Thessaly and Greek Macedonia. Towards the north the climate passes to a sub-Mediterranean environment with lower average annual temperatures in the valleys of the rivers Vardar, Haliacmon, Lower Struma and Maritsa (Trifunovski, 1998; Ivanova et al., 2018). Altitude is an important influence on temperature and humidity. Due to the melting of the mountain snow cover and other sufficient sources of water, the Balkan region is rich in lakes, rivers and wetlands (Griffiths et al., 2004). The southern part of the region is today covered by evergreen sclerophyll vegetation, constrained by warm, dry summers and rainy winters (Prach et al., 2009). The southernmost areas of mainland Greece and Greek Macedonia are covered by Mediterranean vegetation characterized by evergreen hardwood forest (with a diverse species composition) combined with alluvial forest (Bohn et al., 2000/2003). In north-facing river valleys, including the area of Pelagonia, these Mediterranean habitats are alternated with sub-Mediterranean oak forests (dominated by Quercus ilex, Q. coccifera, Q. trojana, Q. macedonica) with hornbeam (Carpinus betulus) and ash (Fraxinus ornus). Higher altitudes include Sub-mediterranean Mountain forests dominated by beech and pine trees (Walter, 1985; Marinova, Ntinou, 2017). An important tree species in the study area is Cornus mas: used in the Neolithic period for the construction of fences and wattle-and-daub structures, while its fruits were also collected (Marinova et al., 2013). Palaeoecological research already offers much rich and well-structured data for the reconstruction of the Holocene vegetation – and the natural conditions of the Neolithic period in particular. The archaeobotanical data provides comprehensive knowledge about plant macroremains, pollen or charcoal, as well as many other aspects of palaeoecology (Marinova et al., 2012; Cvetkoska et al., 2014; Thienemann et al., 2016; Lespez et al., 2016; Marinova, Ntinou, 2017). Neolithic settlements were concentrated near water and natural raw material sources. In southeast Europe, there are two types of Neolithic settlement (Figure 1). The IANSA 2018 ● IX/2 ● 121–145 Jaromír Beneš, Goce Naumov, Tereza Majerovičová, Kristýna Budilová, Jiří Bumerl, Veronika Komárková, Jaromír Kovárník, Michaela Vychronová, Lucie Juřičková: An Archaeobotanical Onsite Approach to the Neolithic Settlements in Southern Regions of the Balkans: The Case of Vrbjanska Čuka, a Tell Site in Pelagonia, Republic of Macedonia 123 first type is a horizontal settlement (in other words – flat, extended) with a single layer of settlement (Tolevski, 2009; Nikolov et al., 2015; Pappa et al., 2004; Vuković et al., 2016). The second type is the tell settlement site, which constitutes several settled horizons, due to which the stratigraphy of the settlement is often high – sometimes up to several metres (Rosenstock, 2006; Nikolov, 2007; Darcque et al., 2007; Naumov, 2016). Settlements are usually open; however, fortified sites have been registered as well (Kotsakis, 1999; Raczky, 2015). The considerable stratigraphy of tells demonstrates how deep was the attachment between the inhabitants of a tell and its settled area. However, some tells constitute only two settled horizons and the height of the entire tell is not particularly significant; these tells could therefore be a kind of transitional form between the flat site and the tell-type settlement (Kreuz, Marinova, 2017). The Neolithic tell settlements are initially established in the region of Thessaly and further dispersed along the tributaries Figure 1. Location of Neolithic settlements in the southern Balkans. Settlements are divided by type. Explanatory notes: Legend explanations: S – unspecified type of settlement, C – cave, FS – flat settlement, FS-F – flat settlement with fortification, T – tell, T-F – tell with fortification, T-FS-F – Tell with surrounding flat settlement and fortification. Source: EnviroBalkan database (LAPE USB České Budějovice). Data and visualisation: T. Majerovičová, J. Bumerl. 1 – Pavlovac, 2 – Piperkov Chiflik, 3 – Bersin, 4 – Nevestino, 5 – Vaksevo, 6 – Priboy, 7 – Negovantsi, 8 – Pernik, 9 – Galabnik, 10 – Kremenik, 11 – Kraynitsi, 12 – Kamenik, 13 – Mursalevo, 14 – Drenkovo, 15 – Balgarchevo, 16 – Dobrinishte, 17 – Brezhani, 18 – Ilindentsi, 19 – Kovachevo, 20 – Kremikovtsi, 21 – Slatina, 22 – Slatina Gradini, 23 – Eleshnitsa, 24 – Chavdar, 25 – Ginova mogila, 26 – Rakitovo, 2","PeriodicalId":38054,"journal":{"name":"Interdisciplinaria Archaeologica","volume":null,"pages":null},"PeriodicalIF":0.2000,"publicationDate":"2018-12-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Interdisciplinaria Archaeologica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.24916/IANSA.2018.2.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"ANTHROPOLOGY","Score":null,"Total":0}
引用次数: 2
摘要
本文的重点是马其顿共和国Pelagonia的Vrbjanska Čuka新石器时代的遗址,作者自2016年以来一直在那里进行考古植物研究。2016年季节收集的植物大遗骸、微遗骸(淀粉、植物岩)和动物微遗骸的分析结果在巴尔干地区新石器时代的更广泛背景下进行了展示,以估计该遗址的生物考古潜力。论文的第一部分和最后一部分概述了与巴尔干半岛南部地区新石器时代定居点有关的生物考古研究。在过去的十年里,关于考古植物学和考古动物学证据的环境研究大量增加。在这里,最关注的是考虑新石器时代定居点及其生物考古背景的考古植物学研究。IANSA 2018●IX/2●121-145 Jaromír benehev, Goce Naumov, Tereza majerovi<s:1> ov<e:1>, Kristýna budilov<e:1>, Jiří Bumerl, Veronika Komárková, Jaromír Kovárník, Michaela vychronov<e:1>, Lucie Juřičková:巴尔干南部地区新石器时代定居点的考古现场方法:Vrbjanska的案例Čuka,马其顿共和国Pelagonia的Tell遗址122 pp. 47-51)。这一概念在很大程度上有利于处理物质文化问题的研究,而不是处理环境和生物问题的研究。此外,当地专家的缺乏导致人工制品和建筑研究占主导地位。生物考古研究主要集中在由国际探险队进行的大型系统发掘上。Amzabegovo遗址较早的研究历史(Gimbutas, 1974;1976), Sitagroi (Renfrew et al., 1986;Näslund, 2009), Argissa (Reingruber, 2005), Nea Nikomedeia (Pyke, Yiouni, 1996;van Zeist, Bottema, 1971), Karanovo (Hiller, Nikolov, 1988)和Dikili Tash (Treuil, 1992)是最好的例子。生物考古学家的活动一直以新石器时代古经济的专题先驱研究为导向。在这方面,R. Dennell研究了保加利亚查达尔(Chavdar)和卡赞莱克(Kazanlak)等新石器时代遗址的考古植物组合。Dennell建立了另一种方法,该方法表明,新石器时代植物资源的经济价值可以通过考虑其在一个地点或地区的作物加工活动中的背景来确定(Dennell, 1972;1974;1976)。Dennell的研究开辟了现场考古解释的新途径,当然与记录考古植物组合中经济植物物种的存在/缺失的旧方法相比。R. Dennell还与考古学家G. kova<e:1>合作,试图提供一幅完整的现场动植物生物考古图片。同样,P.霍尔斯特德对考古学的研究领域也作出了很大贡献。他发表了一系列关于新石器时代和青铜时代考古数据的论文(Halstead, 1981;1989)。在这样做的过程中,他试图确定考古材料的潜力,以帮助确定大规模畜牧专业化与小规模畜牧业作为混合农业组成部分的一部分。他的概念开辟了诸如大规模动物交换肉类和“生产者地点”和“消费者地点”的识别等现象,以及挤奶,乳制品和类似现象的问题(Halstead, 1996)。在20世纪80年代和90年代的巴尔干南部地区,当地专家也很活跃,如保加利亚的E. Chakalova和Z. Popova(见Kreuz et al., 2017)。在过去的十年中,对采用多代理方法的重大转变已被记录:新石器时代遗址生物考古研究的新趋势。与1970年代和1980年代最好的单主题研究相反,多代理方法是基于两种或两种以上分析方法的协同作用。直到今天,特殊方法的组合数量一直在急剧增加(Marinova, Thiebault, 2008;Karkanas et al., 2011;Pappa et al., 2013;Garnier, Valamoti, 2016;马里诺娃,恩蒂诺,2017;克鲁兹,马里诺娃,2017;Ivanova et al., 2018;美国华福,2018)。在过去的10-15年里,专家的“临界质量”和对应用多代理方法的必要性的认识有所增加。这种合成在未来确实应该成为“最先进的”(Allen et al., 2017;Ethier et al., 2017;Marinova et al., 2016;Krauß et al., 2017;2018)。跨学科研究构成了史前现场考古的当前研究和不久的将来。在巴尔干地区的考古发掘中,考古植物学研究仍然很少见。 本文的重点是马其顿共和国Pelagonia的Vrbjanska Čuka新石器时代的遗址,作者自2016年以来一直在那里进行考古植物研究。2016年季节收集的植物大遗骸、微遗骸(淀粉、植物岩)和动物微遗骸的分析结果在巴尔干地区新石器时代的更广泛背景下进行了展示,以估计该遗址的生物考古潜力。论文的第一部分和最后一部分概述了与巴尔干半岛南部地区新石器时代定居点有关的生物考古研究。在过去的十年里,关于考古植物学和考古动物学证据的环境研究大量增加。在这里,最关注的是考虑新石器时代定居点及其生物考古背景的考古植物学研究。IANSA 2018●IX/2●121-145 Jaromír benehev, Goce Naumov, Tereza majerovi<s:1> ov<e:1>, Kristýna budilov<e:1>, Jiří Bumerl, Veronika Komárková, Jaromír Kovárník, Michaela vychronov<e:1>, Lucie Juřičková:巴尔干南部地区新石器时代定居点的考古现场方法:Vrbjanska的案例Čuka,马其顿共和国Pelagonia的Tell遗址122 pp. 47-51)。这一概念在很大程度上有利于处理物质文化问题的研究,而不是处理环境和生物问题的研究。此外,当地专家的缺乏导致人工制品和建筑研究占主导地位。生物考古研究主要集中在由国际探险队进行的大型系统发掘上。Amzabegovo遗址较早的研究历史(Gimbutas, 1974;1976), Sitagroi (Renfrew et al., 1986;Näslund, 2009), Argissa (Reingruber, 2005), Nea Nikomedeia (Pyke, Yiouni, 1996;van Zeist, Bottema, 1971), Karanovo (Hiller, Nikolov, 1988)和Dikili Tash (Treuil, 1992)是最好的例子。生物考古学家的活动一直以新石器时代古经济的专题先驱研究为导向。在这方面,R. Dennell研究了保加利亚查达尔(Chavdar)和卡赞莱克(Kazanlak)等新石器时代遗址的考古植物组合。Dennell建立了另一种方法,该方法表明,新石器时代植物资源的经济价值可以通过考虑其在一个地点或地区的作物加工活动中的背景来确定(Dennell, 1972;1974;1976)。Dennell的研究开辟了现场考古解释的新途径,当然与记录考古植物组合中经济植物物种的存在/缺失的旧方法相比。R. Dennell还与考古学家G. kova<e:1>合作,试图提供一幅完整的现场动植物生物考古图片。同样,P.霍尔斯特德对考古学的研究领域也作出了很大贡献。他发表了一系列关于新石器时代和青铜时代考古数据的论文(Halstead, 1981;1989)。在这样做的过程中,他试图确定考古材料的潜力,以帮助确定大规模畜牧专业化与小规模畜牧业作为混合农业组成部分的一部分。他的概念开辟了诸如大规模动物交换肉类和“生产者地点”和“消费者地点”的识别等现象,以及挤奶,乳制品和类似现象的问题(Halstead, 1996)。在20世纪80年代和90年代的巴尔干南部地区,当地专家也很活跃,如保加利亚的E. Chakalova和Z. Popova(见Kreuz et al., 2017)。在过去的十年中,对采用多代理方法的重大转变已被记录:新石器时代遗址生物考古研究的新趋势。与1970年代和1980年代最好的单主题研究相反,多代理方法是基于两种或两种以上分析方法的协同作用。直到今天,特殊方法的组合数量一直在急剧增加(Marinova, Thiebault, 2008;Karkanas et al., 2011;Pappa et al., 2013;Garnier, Valamoti, 2016;马里诺娃,恩蒂诺,2017;克鲁兹,马里诺娃,2017;Ivanova et al., 2018;美国华福,2018)。在过去的10-15年里,专家的“临界质量”和对应用多代理方法的必要性的认识有所增加。这种合成在未来确实应该成为“最先进的”(Allen et al., 2017;Ethier et al., 2017;Marinova et al., 2016;Krauß et al., 2017;2018)。跨学科研究构成了史前现场考古的当前研究和不久的将来。在巴尔干地区的考古发掘中,考古植物学研究仍然很少见。 这是由于缺乏专家和考古实地研究取样的技术困难- -以及发掘后阶段所涉及的耗时工作。另一方面,考古植物学可以帮助解决古经济问题,并非常详细地追踪特定史前遗址上人类行为的形式。1.2巴尔干半岛南部的自然环境及其新石器时代遗址在地理上,巴尔干半岛南部地区变化很大:其表面主要是山地。沿海地区的气候与内陆地区不同,更具有大陆性。巴尔干半岛南部大部分地区属于地中海气候,特别是色萨利和希腊马其顿地区。向北,气候转变为亚地中海环境,瓦尔达尔河、哈利亚克蒙河、下斯特鲁玛河和马里察河流域的年平均气温较低(特里富诺夫斯基,1998;Ivanova et al., 2018)。海拔高度对温度和湿度有重要影响。由于高山积雪的融化和其他充足的水源,巴尔干地区湖泊、河流和湿地丰富(Griffiths et al., 2004)。如今,该地区的南部被常绿硬叶植被覆盖,受到夏季温暖干燥和冬季多雨的限制(Prach等人,2009)。希腊大陆和希腊马其顿的最南端地区覆盖着地中海植被,其特征是常绿阔叶林(物种组成多样化)和冲积林(Bohn et al., 2000/2003)。在朝北的河谷地区,包括Pelagonia地区,这些地中海栖息地与亚地中海栎林(以栓皮栎、圆木栎、trojana栎和马其顿栎为主)和角木(Carpinus betulus)和白蜡(Fraxinus ornus)交替存在。高海拔地区包括以山毛榉和松树为主的亚地中海山林(Walter, 1985;Marinova, Ntinou, 2017)。研究区域的一种重要树种是山茱萸(Cornus mas),它在新石器时代用于建造围栏和木条和涂抹结构,同时也收集了它的果实(Marinova et al., 2013)。古生态学研究已经为重建全新世植被——特别是新石器时代的自然条件——提供了许多丰富和结构良好的数据。考古植物学数据提供了关于植物大遗骸、花粉或木炭以及古生态学的许多其他方面的全面知识(Marinova et al., 2012;Cvetkoska et al., 2014;Thienemann et al., 2016;Lespez et al., 2016;Marinova, Ntinou, 2017)。新石器时代的定居点集中在水源和天然原料来源附近。在东南欧,有两种类型的新石器时代定居点(图1)。IANSA 2018●IX/2●121-145 Jaromír Beneš v, Goce Naumov, Tereza majerovi<s:1> ov<e:1>, Kristýna budilov<e:1>, Jiří Bumerl, Veronika Komárková, Jaromír Kovárník, Michaela vychronov<e:1>, Lucie Juřičková:巴尔干南部地区新石器时代定居点的考古现场方法:第一种类型是水平聚落(换句话说,是平坦的、延伸的),具有单层聚落(Tolevski, 2009;Nikolov et al., 2015;Pappa et al., 2004;vukoviki et al., 2016)。第二种类型是tell沉降点,它由几个沉降层组成,因此沉降层的地层通常很高——有时高达几米(Rosenstock, 2006;Nikolov, 2007;Darcque et al., 2007;Naumov, 2016)。定居点通常是开放的;然而,防御工事遗址也已登记(Kotsakis, 1999;Raczky, 2015)。大量的泰尔地层学研究表明泰尔的居民与其定居地区之间的联系有多深。然而,有些层只构成两个固定的视界,整个层的高度并不特别重要;因此,这些tell可能是平面场地和tell型聚落之间的一种过渡形式(Kreuz, Marinova, 2017)。新石器时代的定居点最初建立在色萨利地区,并沿着支流进一步分散(图1)。巴尔干半岛南部新石器时代定居点的位置。聚落按类型划分。注释:图例说明:S-未指定类型的聚落,C -洞穴,FS-平聚落,FS- f -平聚落带工事,T- tell, T- f - tell带工事,T-FS- f - tell与周围平聚落和工事。来源:EnviroBalkan数据库(LAPE USB České bud<e:1> jovice)。数据和可视化:T. majerovi<e:1> ov<e:1>, J. Bumerl。
An Archaeobotanical Onsite Approach to the Neolithic Settlements in Southern Regions of the Balkans: The Case of Vrbjanska Čuka, a Tell Site in Pelagonia, Republic of Macedonia
This paper is focused on the Neolithic tell-site of Vrbjanska Čuka in Pelagonia, Republic of Macedonia, where the authors have been performing archaeobotanical research since 2016. Results of the analyses of botanical macroremains and microremains (starch, phytoliths) and faunal microremains collected in season 2016 are presented in the broader context of the Neolithic in the Balkans in order to estimate the bioarchaeological potential of this site. The first and final parts of the paper outline the bioarchaeological studies connected with Neolithic settlements in the southern regions of the Balkans. A substantial proliferation of environmental studies has been recorded in the last decade concerning the archaeobotanical and archaeozoological evidence. Here, most attention is paid to archaeobotanical studies which consider Neolithic settlements and their bioarchaeological context. IANSA 2018 ● IX/2 ● 121–145 Jaromír Beneš, Goce Naumov, Tereza Majerovičová, Kristýna Budilová, Jiří Bumerl, Veronika Komárková, Jaromír Kovárník, Michaela Vychronová, Lucie Juřičková: An Archaeobotanical Onsite Approach to the Neolithic Settlements in Southern Regions of the Balkans: The Case of Vrbjanska Čuka, a Tell Site in Pelagonia, Republic of Macedonia 122 pp. 47–51). This concept substantially favoured those studies dealing with material culture rather than ones addressing environmental and biological issues. Furthermore, the lack of local specialists led to a predominance of artefactual and architectural studies. Bioarchaeological research was concentrated towards large systematic excavations made by international expeditions. This is clearly the case with the older research history of the site of Amzabegovo (Gimbutas, 1974; 1976), Sitagroi (Renfrew et al., 1986; Näslund, 2009), Argissa (Reingruber, 2005), Nea Nikomedeia (Pyke, Yiouni, 1996; van Zeist, Bottema, 1971), Karanovo (Hiller, Nikolov, 1988) and Dikili Tash (Treuil, 1992) being the best examples. The activities of bioarchaeologists have been oriented towards the thematic pioneer research of Neolithic palaeoeconomy. In this regard, R. Dennell studied the archaeobotanical assemblages of such Neolithic sites as Chavdar and Kazanlak in Bulgaria. Dennell established an alternative approach which suggested that the economic value of a Neolithic plant resource can be ascertained by considering its context within the crop-processing activities of a site or area (Dennell, 1972; 1974; 1976). The research of Dennell has opened up new avenues in onsite archaeological interpretations, certainly in comparison to the older common approach of recording the presence/absence of economic plant species in archaeobotanical assemblages. R. Dennell also worked with the archaeozoologist G. Kovačev and attempted to provide a complete onsite bioarchaeological picture of the plants and animals. Likewise, P. Halstead has contributed much to the research area of archaeozoology. He has published a series of papers focused on archaeozoological data of the Neolithic and Bronze Age (Halstead, 1981; 1989). In so doing he has attempted to ascertain the potential of archaeozoological material in helping to identify the part of large-scale pastoral specialization versus small-scale stock husbandry as a component of mixed farming. His concept has opened up such phenomena as the large-scale exchange of animals for meat and the identification of “producer sites” and “consumer sites”, as well as the issues of milking, dairying and similar phenomena (Halstead, 1996). In the southern regions of the Balkans in the 1980s and 1990s, local specialists were also active, such as E. Chakalova and Z. Popova in Bulgaria (see Kreuz et al., 2017). A substantial shift has been recorded in the last decade towards the adoption of a multi-proxy approach: a new trend in the bioarchaeological research of Neolithic sites. In contrast to the best monothematic studies of the 1970s and 1980s, the multi-proxy approach is based on the synergy of two or more analytical methods. The combination of particular methods has been steeply increasing in number up until today (Marinova, Thiebault, 2008; Karkanas et al., 2011; Pappa et al., 2013; Garnier, Valamoti, 2016; Marinova, Ntinou, 2017; Kreuz, Marinova, 2017; Ivanova et al., 2018; Whitford, 2018). In the last 10–15 years, the “critical mass” of specialists and awareness of the necessity to apply multiproxy approaches has increased. Such synthesis should indeed become “state of the art” in the future (Allen et al., 2017; Ethier et al., 2017; Marinova et al., 2016; Krauß et al., 2017; 2018). Transdisciplinary studies constitute presentday research and the near future for prehistoric onsite archaeology. Archaeobotanical research is still rare for archaeological excavation in this study region of the Balkans. It is due to the lack of specialists and the technical difficulty of sampling in archaeological field research – and the time-consuming work involved in the post-excavational phase. On the other hand, archaeobotany can contribute to resolving palaeoeconomical questions and trace the forms of human behaviour on a specific prehistoric site in great detail. 1.2 Natural setting of the southern Balkans and its Neolithic sites Geographically, the southern Balkans region is very variable: its surface is predominantly mountainous. The climate of the coastal regions differs from that inland, it being more continental. Most of the southern Balkans is dominated by a Mediterranean climate, particularly for the area of Thessaly and Greek Macedonia. Towards the north the climate passes to a sub-Mediterranean environment with lower average annual temperatures in the valleys of the rivers Vardar, Haliacmon, Lower Struma and Maritsa (Trifunovski, 1998; Ivanova et al., 2018). Altitude is an important influence on temperature and humidity. Due to the melting of the mountain snow cover and other sufficient sources of water, the Balkan region is rich in lakes, rivers and wetlands (Griffiths et al., 2004). The southern part of the region is today covered by evergreen sclerophyll vegetation, constrained by warm, dry summers and rainy winters (Prach et al., 2009). The southernmost areas of mainland Greece and Greek Macedonia are covered by Mediterranean vegetation characterized by evergreen hardwood forest (with a diverse species composition) combined with alluvial forest (Bohn et al., 2000/2003). In north-facing river valleys, including the area of Pelagonia, these Mediterranean habitats are alternated with sub-Mediterranean oak forests (dominated by Quercus ilex, Q. coccifera, Q. trojana, Q. macedonica) with hornbeam (Carpinus betulus) and ash (Fraxinus ornus). Higher altitudes include Sub-mediterranean Mountain forests dominated by beech and pine trees (Walter, 1985; Marinova, Ntinou, 2017). An important tree species in the study area is Cornus mas: used in the Neolithic period for the construction of fences and wattle-and-daub structures, while its fruits were also collected (Marinova et al., 2013). Palaeoecological research already offers much rich and well-structured data for the reconstruction of the Holocene vegetation – and the natural conditions of the Neolithic period in particular. The archaeobotanical data provides comprehensive knowledge about plant macroremains, pollen or charcoal, as well as many other aspects of palaeoecology (Marinova et al., 2012; Cvetkoska et al., 2014; Thienemann et al., 2016; Lespez et al., 2016; Marinova, Ntinou, 2017). Neolithic settlements were concentrated near water and natural raw material sources. In southeast Europe, there are two types of Neolithic settlement (Figure 1). The IANSA 2018 ● IX/2 ● 121–145 Jaromír Beneš, Goce Naumov, Tereza Majerovičová, Kristýna Budilová, Jiří Bumerl, Veronika Komárková, Jaromír Kovárník, Michaela Vychronová, Lucie Juřičková: An Archaeobotanical Onsite Approach to the Neolithic Settlements in Southern Regions of the Balkans: The Case of Vrbjanska Čuka, a Tell Site in Pelagonia, Republic of Macedonia 123 first type is a horizontal settlement (in other words – flat, extended) with a single layer of settlement (Tolevski, 2009; Nikolov et al., 2015; Pappa et al., 2004; Vuković et al., 2016). The second type is the tell settlement site, which constitutes several settled horizons, due to which the stratigraphy of the settlement is often high – sometimes up to several metres (Rosenstock, 2006; Nikolov, 2007; Darcque et al., 2007; Naumov, 2016). Settlements are usually open; however, fortified sites have been registered as well (Kotsakis, 1999; Raczky, 2015). The considerable stratigraphy of tells demonstrates how deep was the attachment between the inhabitants of a tell and its settled area. However, some tells constitute only two settled horizons and the height of the entire tell is not particularly significant; these tells could therefore be a kind of transitional form between the flat site and the tell-type settlement (Kreuz, Marinova, 2017). The Neolithic tell settlements are initially established in the region of Thessaly and further dispersed along the tributaries Figure 1. Location of Neolithic settlements in the southern Balkans. Settlements are divided by type. Explanatory notes: Legend explanations: S – unspecified type of settlement, C – cave, FS – flat settlement, FS-F – flat settlement with fortification, T – tell, T-F – tell with fortification, T-FS-F – Tell with surrounding flat settlement and fortification. Source: EnviroBalkan database (LAPE USB České Budějovice). Data and visualisation: T. Majerovičová, J. Bumerl. 1 – Pavlovac, 2 – Piperkov Chiflik, 3 – Bersin, 4 – Nevestino, 5 – Vaksevo, 6 – Priboy, 7 – Negovantsi, 8 – Pernik, 9 – Galabnik, 10 – Kremenik, 11 – Kraynitsi, 12 – Kamenik, 13 – Mursalevo, 14 – Drenkovo, 15 – Balgarchevo, 16 – Dobrinishte, 17 – Brezhani, 18 – Ilindentsi, 19 – Kovachevo, 20 – Kremikovtsi, 21 – Slatina, 22 – Slatina Gradini, 23 – Eleshnitsa, 24 – Chavdar, 25 – Ginova mogila, 26 – Rakitovo, 2