Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey

IF 0.2 Q4 ANTHROPOLOGY
D. Król, J. Niebieszczański
{"title":"Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey","authors":"D. Król, J. Niebieszczański","doi":"10.24916/iansa.2019.2.2","DOIUrl":null,"url":null,"abstract":"In recent years, numerous sites of the Eneolithic Funnel Beaker culture (FBC) have been identified in the Rzeszów Foothills (south-eastern Poland). Among them, a large settlement in Skołoszów 16 seems to be particularly significant due to its internal characteristics. In order to determine its extent, spatial arrangement and chronology, an interdisciplinary investigation (including excavations and a noninvasive geophysical survey) was carried out in 2017–2018. As a consequence of two seasons of field work campaigns, we have recognized numerous morphologically diverse features (mainly pits) and the settlement (cultural) layer. Excavations documented the intense usage of the settlement’s space which encouraged carrying out a geophysical survey over the wider area of the site. The magnetic anomaly distribution reflects many presumable anthropogenic features. Several particular concentrations of features visible on the magnetometry image seem to be related with the FBC, thus delimiting the spatial extent of the site. Based on the geophysical picture, it was possible to estimate that the site measured at least 65×40 m, while the excavations conducted revealed that the settlement was comprised of numerous pits and one settlement layer. IANSA 2019 ● X/2 ● 121–128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey 122 2. Location of settlement The settlement in Skołoszów 16 is located in the northeastern region of the Rzeszów Foothills (Figure 1) on a loess zone in the south-eastern part of the Sandomierz Basin (Kondracki, 1988). It is situated on a slightly flattened small hill, on the right bank of the valley of the Łęg Rokietnicki River, about 380 m away from its present-day riverbed and Figure 1. Distribution of the FBC in the Rzeszów Foothills. a – Skołoszów 16 settlement; b – others sites in the studied area; c – others sites in the neighbouring areas. 0 5 km Figure 2. Skołoszów 16, Subcarpathian voivodeship. A 3D model of the settlement location. Red spot – settlement; blue spots – non-outflowing ponds. IANSA 2019 ● X/2 ● 121–128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey 123 approx. 13 m above its bottom. In its nearest surroundings, there are also two non-outflowing ponds (Figure 2). This topographic-hydrological configuration of the environment is typical of this part of the Rzeszów Foothills. These conditions favoured the development of the FBC settlement network in south-eastern Poland (cf. Kruk, 1973; 1980; Kruk et al., 1996). Within a radius of 5 km from the site, up to 30 functionally diverse FBC sites, including one cemetery with two non-megalithic long barrows, have been registered (Król et al., 2014; Król, 2017; 2018, Cwaliński et al., 2018). 3. Previous excavations An archaeological excavation at the new FBC site in Skołoszów 16 was carried out during two fieldwork seasons in 2017 and 2018. The first season aimed to check whether the settlement identified during the surface survey mission could be prospective for excavation and to examine its state of preservation. To this end, preliminary excavations were realized and provided a number of valuable items of information, which are presented below. As a consequence of the excavation of two small trenches with a total surface of 32 m2, we have recognized 8 diverse features and a settlement layer of 0.4 m thickness (Figure 3). In the context of these features, as well as the cultural layer we have identified numerous FBC sherd and flint assemblages (cf. Król, 2018). The presence of relatively well-preserved anthropogenic relics and particularly distinct clustered features (Figure 3) has confirmed the scientific importance of this site and justified the second season of the excavation. This excavation carried out in an area of ca. 100 m2 resulted in the identification of another 17 diverse features, especially in the western sector (Figure 3). As in the case of the preliminary excavations in 2017, numerous artefacts relating to FBC were identified. Sherds that imitate Figure 3. Skołoszów 16, Subcarpathian voivodeship. The distribution of excavated FBC features: a – trapezoidal pits; b – tubular pits, c – rectangular pits, d – plausible hearth; e – unknown pits; f – postholes; g – area excavated in 2017; h – area excavated in 2018. 0 10 cm IANSA 2019 ● X/2 ● 121–128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey 124 the Tripolye culture (hereinafter TC) technology have also been found. These and the typical FBC finds are subject of a separate study. The excavation revealed a total of 25 morphologically and functionally diverse anthropogenic features, among which the most numerous group might be categorized as storage and/or rubbish pits – features 1–14 and 19–23 (Table 1). In fact, all these pits were conspicuous as being oval in plan and they differed more in size from 0.94 m to 2.87 m in diameter (Table 1). More crucial differences were visible in the case of their cross-section and type of backfill. During excavations in Skołoszów 16, we distinguished mainly trapezoidal and tubularshaped pits (Figure 3; Table 1). The first of these were slightly deeper and stratified, while the second had usually a uniform backfill (Table 1). Most of these pits were clustered very densely below the cultural layer and some of them overlapped each other (e.g. features 5 → 12). However, the deepest and multistratified trapezoidal pit 19, as well as pit 20 containing peculiar burnt layers, were situated quite independently of this cluster (Figure 3). Another category within the scope of the examined space were the poorly preserved postholes and the one feature which can be carefully interpreted as a hearth located to the south of pits 11 and 14 (Figure 3). Presumably, all these lattermentioned features might be seen as the remains of a dwelling and its interior. The spatial arrangement of the features recognized seems interesting and may suggest some preferences as to the functioning and development of the settlement. The occurrence of the cluster of trapezoidal and tubular-shaped pits probably do not indicate the short-term inhabitation of this site, and its more complex structure may be confirmed by the intersections of older pits by younger ones (Figure 3). These stratigraphic relationships demonstrate that some pits were not contemporaneous. However, it is intractable to determine their detailed temporal relationships due to the mainly unspecific sherds and lack of a large set of AMS radiocarbon dating. Thus far, only two absolute indicators have been obtained from the context of pits 5 (which disturbed the pit 13) and 6 (Figure 4). Both of these dates Poz-100857 4765±35 and Poz-100856 4680±35 suggest that the settlement was inhabited within a period of ca. 3650–3350 BC (cf. Król, 2018). Only a small section of the settlement was examined and it would be difficult to expect much in the way of general Table 1. Skołoszów 16. Basic specification of features. Feature no. Feature type Cross-section Top size (m) Depth (m) Backfill 1 pit tubular 1.22×1.14 0.32 uniform 2 pit tubular 1.42×1.12 0.30 uniform 3 pit rectangular 1.88×1.30 0.35 uniform 4 pit trapezoidal unknown* 0.42 uniform 5 pit trapezoidal 2.08×1.05 0.68 stratified 6 pit tubular 1.47×1.45 0.42 uniform 7 pit tubular 1.58×1.21 0.40 uniform 8 pit trapezoidal unknown* 0.50 uniform 9 pit tubular 2.06×1.95 0.48 uniform 9A pit tubular unknown* 0.42 uniform 10 pit trapezoidal 1.45×1.26 0.41 uniform 11 pit tubular 1.75×1.59 0.64 uniform 12 pit trapezoidal 2.87×2.26 0.76 stratified 13 pit trapezoidal 1.19×1.35 0.35 uniform 14 pit tubular 2.36×2.07 0.65 uniform 15 posthole irregural 0.48×0.46 0.25 uniform 16 posthole irregular 0.46×0.42 0.22 uniform 17 unknown unknown 0.88×0.64 0.15 uniform 18 hearth basin 1.20×0.81 0.12 uniform 19 pit trapezoidal 1.03×0.95 1.05 stratified 20 pit tubular 3.23×?* 0.75 stratified 21 pit tubular 2.43×?* 0.72 uniform 22 pit trapezoidal 0.94×?* 0.80 stratified 23 pit rectangular 1.52×?* 0.40 uniform 24 posthole irregular 0.36×0.34 0.12 uniform * – not fully explored features IANSA 2019 ● X/2 ● 121–128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey 125 conclusions regarding the spatial arrangement, range and detailed dynamics of its inhabitation based on these limited data. Despite the results of the excavations, it is open to question whether the examined cluster of pits were part of a much larger concentration of features and if there were other clusters within the settlement. This seems justified given the current research experience from the loess area of the eastern part of the Rzeszów Foothills. Such different pit groups have been identified, for instance, in Pawłosiów 52 (Rybicka et al., 2014) and Mirocin 27 (Sznajdrowska, 2016). Undoubtedly, in order to realistically estimate the space of the settlement in Skołoszów 16, large-scale excavations should be carried out. However, preceding these future investigations, we have decided to conduct a geophysical survey in order to locate the most suitable areas for excavations as well as to provide a spatial view of the distribution of archaeological features. 4. Geophysical survey The main aim of the non-invasive research was to investigate the Skołoszów 16 area in order to estimate the po","PeriodicalId":38054,"journal":{"name":"Interdisciplinaria Archaeologica","volume":"60 1","pages":"121-128"},"PeriodicalIF":0.2000,"publicationDate":"2019-12-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Interdisciplinaria Archaeologica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.24916/iansa.2019.2.2","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: 1

Abstract

In recent years, numerous sites of the Eneolithic Funnel Beaker culture (FBC) have been identified in the Rzeszów Foothills (south-eastern Poland). Among them, a large settlement in Skołoszów 16 seems to be particularly significant due to its internal characteristics. In order to determine its extent, spatial arrangement and chronology, an interdisciplinary investigation (including excavations and a noninvasive geophysical survey) was carried out in 2017–2018. As a consequence of two seasons of field work campaigns, we have recognized numerous morphologically diverse features (mainly pits) and the settlement (cultural) layer. Excavations documented the intense usage of the settlement’s space which encouraged carrying out a geophysical survey over the wider area of the site. The magnetic anomaly distribution reflects many presumable anthropogenic features. Several particular concentrations of features visible on the magnetometry image seem to be related with the FBC, thus delimiting the spatial extent of the site. Based on the geophysical picture, it was possible to estimate that the site measured at least 65×40 m, while the excavations conducted revealed that the settlement was comprised of numerous pits and one settlement layer. IANSA 2019 ● X/2 ● 121–128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey 122 2. Location of settlement The settlement in Skołoszów 16 is located in the northeastern region of the Rzeszów Foothills (Figure 1) on a loess zone in the south-eastern part of the Sandomierz Basin (Kondracki, 1988). It is situated on a slightly flattened small hill, on the right bank of the valley of the Łęg Rokietnicki River, about 380 m away from its present-day riverbed and Figure 1. Distribution of the FBC in the Rzeszów Foothills. a – Skołoszów 16 settlement; b – others sites in the studied area; c – others sites in the neighbouring areas. 0 5 km Figure 2. Skołoszów 16, Subcarpathian voivodeship. A 3D model of the settlement location. Red spot – settlement; blue spots – non-outflowing ponds. IANSA 2019 ● X/2 ● 121–128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey 123 approx. 13 m above its bottom. In its nearest surroundings, there are also two non-outflowing ponds (Figure 2). This topographic-hydrological configuration of the environment is typical of this part of the Rzeszów Foothills. These conditions favoured the development of the FBC settlement network in south-eastern Poland (cf. Kruk, 1973; 1980; Kruk et al., 1996). Within a radius of 5 km from the site, up to 30 functionally diverse FBC sites, including one cemetery with two non-megalithic long barrows, have been registered (Król et al., 2014; Król, 2017; 2018, Cwaliński et al., 2018). 3. Previous excavations An archaeological excavation at the new FBC site in Skołoszów 16 was carried out during two fieldwork seasons in 2017 and 2018. The first season aimed to check whether the settlement identified during the surface survey mission could be prospective for excavation and to examine its state of preservation. To this end, preliminary excavations were realized and provided a number of valuable items of information, which are presented below. As a consequence of the excavation of two small trenches with a total surface of 32 m2, we have recognized 8 diverse features and a settlement layer of 0.4 m thickness (Figure 3). In the context of these features, as well as the cultural layer we have identified numerous FBC sherd and flint assemblages (cf. Król, 2018). The presence of relatively well-preserved anthropogenic relics and particularly distinct clustered features (Figure 3) has confirmed the scientific importance of this site and justified the second season of the excavation. This excavation carried out in an area of ca. 100 m2 resulted in the identification of another 17 diverse features, especially in the western sector (Figure 3). As in the case of the preliminary excavations in 2017, numerous artefacts relating to FBC were identified. Sherds that imitate Figure 3. Skołoszów 16, Subcarpathian voivodeship. The distribution of excavated FBC features: a – trapezoidal pits; b – tubular pits, c – rectangular pits, d – plausible hearth; e – unknown pits; f – postholes; g – area excavated in 2017; h – area excavated in 2018. 0 10 cm IANSA 2019 ● X/2 ● 121–128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey 124 the Tripolye culture (hereinafter TC) technology have also been found. These and the typical FBC finds are subject of a separate study. The excavation revealed a total of 25 morphologically and functionally diverse anthropogenic features, among which the most numerous group might be categorized as storage and/or rubbish pits – features 1–14 and 19–23 (Table 1). In fact, all these pits were conspicuous as being oval in plan and they differed more in size from 0.94 m to 2.87 m in diameter (Table 1). More crucial differences were visible in the case of their cross-section and type of backfill. During excavations in Skołoszów 16, we distinguished mainly trapezoidal and tubularshaped pits (Figure 3; Table 1). The first of these were slightly deeper and stratified, while the second had usually a uniform backfill (Table 1). Most of these pits were clustered very densely below the cultural layer and some of them overlapped each other (e.g. features 5 → 12). However, the deepest and multistratified trapezoidal pit 19, as well as pit 20 containing peculiar burnt layers, were situated quite independently of this cluster (Figure 3). Another category within the scope of the examined space were the poorly preserved postholes and the one feature which can be carefully interpreted as a hearth located to the south of pits 11 and 14 (Figure 3). Presumably, all these lattermentioned features might be seen as the remains of a dwelling and its interior. The spatial arrangement of the features recognized seems interesting and may suggest some preferences as to the functioning and development of the settlement. The occurrence of the cluster of trapezoidal and tubular-shaped pits probably do not indicate the short-term inhabitation of this site, and its more complex structure may be confirmed by the intersections of older pits by younger ones (Figure 3). These stratigraphic relationships demonstrate that some pits were not contemporaneous. However, it is intractable to determine their detailed temporal relationships due to the mainly unspecific sherds and lack of a large set of AMS radiocarbon dating. Thus far, only two absolute indicators have been obtained from the context of pits 5 (which disturbed the pit 13) and 6 (Figure 4). Both of these dates Poz-100857 4765±35 and Poz-100856 4680±35 suggest that the settlement was inhabited within a period of ca. 3650–3350 BC (cf. Król, 2018). Only a small section of the settlement was examined and it would be difficult to expect much in the way of general Table 1. Skołoszów 16. Basic specification of features. Feature no. Feature type Cross-section Top size (m) Depth (m) Backfill 1 pit tubular 1.22×1.14 0.32 uniform 2 pit tubular 1.42×1.12 0.30 uniform 3 pit rectangular 1.88×1.30 0.35 uniform 4 pit trapezoidal unknown* 0.42 uniform 5 pit trapezoidal 2.08×1.05 0.68 stratified 6 pit tubular 1.47×1.45 0.42 uniform 7 pit tubular 1.58×1.21 0.40 uniform 8 pit trapezoidal unknown* 0.50 uniform 9 pit tubular 2.06×1.95 0.48 uniform 9A pit tubular unknown* 0.42 uniform 10 pit trapezoidal 1.45×1.26 0.41 uniform 11 pit tubular 1.75×1.59 0.64 uniform 12 pit trapezoidal 2.87×2.26 0.76 stratified 13 pit trapezoidal 1.19×1.35 0.35 uniform 14 pit tubular 2.36×2.07 0.65 uniform 15 posthole irregural 0.48×0.46 0.25 uniform 16 posthole irregular 0.46×0.42 0.22 uniform 17 unknown unknown 0.88×0.64 0.15 uniform 18 hearth basin 1.20×0.81 0.12 uniform 19 pit trapezoidal 1.03×0.95 1.05 stratified 20 pit tubular 3.23×?* 0.75 stratified 21 pit tubular 2.43×?* 0.72 uniform 22 pit trapezoidal 0.94×?* 0.80 stratified 23 pit rectangular 1.52×?* 0.40 uniform 24 posthole irregular 0.36×0.34 0.12 uniform * – not fully explored features IANSA 2019 ● X/2 ● 121–128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 – A Spatial Arrangement of the Eneolithic Settlement of the Funnel Beaker Culture in the Rzeszów Foothills (South-Eastern Poland) in the Light of Previous Excavations and Geophysical Survey 125 conclusions regarding the spatial arrangement, range and detailed dynamics of its inhabitation based on these limited data. Despite the results of the excavations, it is open to question whether the examined cluster of pits were part of a much larger concentration of features and if there were other clusters within the settlement. This seems justified given the current research experience from the loess area of the eastern part of the Rzeszów Foothills. Such different pit groups have been identified, for instance, in Pawłosiów 52 (Rybicka et al., 2014) and Mirocin 27 (Sznajdrowska, 2016). Undoubtedly, in order to realistically estimate the space of the settlement in Skołoszów 16, large-scale excavations should be carried out. However, preceding these future investigations, we have decided to conduct a geophysical survey in order to locate the most suitable areas for excavations as well as to provide a spatial view of the distribution of archaeological features. 4. Geophysical survey The main aim of the non-invasive research was to investigate the Skołoszów 16 area in order to estimate the po
Skołoszów 16 -根据先前的挖掘和地球物理调查,Rzeszów山麓(波兰东南部)漏斗烧杯文化的新石器时代聚落的空间安排
近年来,在Rzeszów丘陵地带(波兰东南部)发现了许多新石器时代漏斗烧杯文化(FBC)的遗址。其中,Skołoszów 16中的一个大型定居点,由于其内部特征,显得尤为重要。为了确定其范围、空间排列和年代,2017-2018年开展了跨学科调查(包括挖掘和非侵入性地球物理调查)。经过两季的实地工作,我们发现了许多形态各异的特征(主要是坑)和聚落(文化)层。挖掘记录了定居点空间的密集使用,这鼓励了在更广泛的地区进行地球物理调查。磁异常分布反映了许多可能的人为特征。在磁力计图像上可见的几个特别集中的特征似乎与FBC有关,从而划定了该地点的空间范围。根据地球物理图像,可以估计该遗址的长度至少为65×40 m,而进行的挖掘显示,该定居点由许多凹坑和一个沉降层组成。IANSA 2019●X/2●121-128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 -根据先前的挖掘和地球物理调查,Rzeszów山麓(波兰东南部)漏斗烧杯文化的新石器时代聚落的空间安排122。Skołoszów 16中的居民点位于位于桑多梅日盆地东南部黄土带Rzeszów Foothills(图1)的东北部(Kondracki, 1988)。它坐落在一个稍微平坦的小山上,在Łęg Rokietnicki河山谷的右岸,距离现在的河床和图1约380米。FBC在Rzeszów山麓地区的分布。a - Skołoszów 16结算;B -研究区内的其他地点;C -邻近地区的其他地点。图2。Skołoszów Subcarpathian vovodesship。沉降位置的三维模型。红斑-沉降;蓝点-没有流出的池塘。IANSA 2019●X/2●121-128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 -根据先前的挖掘和地球物理调查,Rzeszów山脚(波兰东南部)漏斗烧杯文化的新石器时代聚落的空间安排。高出底部13米。在它最近的周围,还有两个不外流的池塘(图2)。这种地形水文环境是Rzeszów丘陵地区这部分的典型特征。这些条件有利于FBC定居网络在波兰东南部的发展(cf. Kruk, 1973;1980;Kruk et al., 1996)。在距离遗址5公里的半径内,登记了多达30个功能多样的FBC遗址,包括一个带有两个非巨石长墓的墓地(Król et al., 2014;Krol, 2017;2018, Cwaliński et al., 2018)。3.在2017年和2018年的两个实地调查季节中,对Skołoszów 16的新FBC遗址进行了考古发掘。第一季的目的是检查在地面调查任务中发现的定居点是否有可能进行挖掘,并检查其保存状况。为此目的,进行了初步挖掘,并提供了一些有价值的资料,现列于下。由于挖掘了两个总面积为32平方米的小沟渠,我们识别出了8个不同的特征和0.4米厚的沉降层(图3)。在这些特征的背景下,以及文化层,我们已经确定了许多FBC碎片和燧石组合(参见Król, 2018)。保存相对较好的人类遗迹和特别明显的群集特征(图3)的存在证实了该遗址的科学重要性,并证明了第二季挖掘的合理性。这次挖掘在大约100平方米的区域内进行,发现了另外17个不同的特征,特别是在西部地区(图3)。与2017年的初步挖掘一样,发现了许多与FBC有关的人工制品。类似图3的碎片。Skołoszów Subcarpathian vovodesship。开挖FBC分布特征:a -梯形坑;B -管状凹坑,c -矩形凹坑,d -似是而非的凹坑;E——未知坑;F - postholes;G——2017年挖掘面积;H -区域于2018年挖掘。 0 10 cm IANSA 2019●X/2●121-128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 -根据先前的挖掘和地球物理调查,Rzeszów丘陵地区(波兰东南部)漏斗烧杯文化的新石器时代聚落的空间排列124 Tripolye文化(以下称TC)技术也被发现。这些和典型的FBC发现是另一项研究的主题。挖掘共发现了25个形态和功能各异的人为特征,其中数量最多的一类可能被归为储存和/或垃圾坑-特征1 - 14和19-23(表1)。事实上,所有这些坑都是椭圆形的,它们的直径从0.94米到2.87米不等(表1)。在断面和回填类型的情况下,更重要的差异是可见的。在Skołoszów 16的挖掘过程中,我们主要区分了梯形和管状坑(图3;表1)。第一个坑略深且分层,而第二个坑通常有均匀的回填(表1)。这些坑大多数非常密集地聚集在文化层下方,其中一些相互重叠(例如特征5→12)。然而,最深的和multistratified梯形坑19日以及坑20包含特殊的燃烧层,位于完全独立于这个集群(图3)。另一个类别范围内的检查空间是保存差柱坑和一个特性,可以仔细解读为炉位于南坑11和14(图3)。据推测,所有这些lattermentioned特性可能被视为住宅及其内部的残骸。所识别的特征的空间安排似乎很有趣,可能暗示了一些关于聚落功能和发展的偏好。梯形和管状坑群的出现可能并不表明该遗址曾有过短期的居住,其更复杂的结构可以通过较老的坑与较年轻的坑的相交来证实(图3)。这些地层关系表明,一些坑不是同时期的。然而,由于主要是不特定的碎片和缺乏大量的AMS放射性碳定年,很难确定它们的详细时间关系。到目前为止,仅从坑5(干扰了坑13)和6(图4)的背景下获得了两个绝对指标。这两个日期Poz-100857 4765±35和Poz-100856 4680±35都表明该定居点在大约公元前3650-3350年期间有人居住(cf. Król, 2018)。只研究了一小部分定居点,很难期望得到一般表1所示的情况。Skołoszow 16。功能的基本规格。功能没有。特征类型断面顶尺寸(m)深度(m)回填1坑管1.22×1.14 0.32均匀2坑管1.42×1.12 0.30均匀3坑矩形1.88×1.30 0.35均匀4坑梯形未知* 0.42均匀5坑梯形2.08×1.05 0.68分层6坑管1.47×1.45 0.42均匀7坑管1.58×1.21 0.40均匀8坑梯形未知* 0.50均匀9坑管2.06×1.95 0.48均匀9A坑管未知* 0.42均匀10坑梯形1.45×1.26 0.41均匀11坑管式1.75×1.59 - 0.64统一12坑梯形2.87×2.26 - 0.76分层13 14坑坑梯形1.19×1.35 - 0.35统一管2.36×2.07 - 0.65统一15柱坑irregural 0.48×0.46 - 0.25统一16洞不规则0.46×0.42 - 0.22统一17未知的未知0.88×0.64 - 0.15统一18炉盆地1.20×0.81 - 0.12统一19坑梯形管3.23×1.03×0.95 - 1.05分层20坑吗?* 0.75层状21坑管2.43×?* 0.72均匀22坑梯形0.94×?* 0.80分层23坑矩形1.52×?* 0.40均匀24后孔不均匀0.36×0.34 0.12均匀* -未完全探索的特征IANSA 2019●X/2●121-128 Dariusz Król, Jakub Niebieszczański: Skołoszów 16 -根据先前的挖掘和地球物理调查,Rzeszów山脚(波兰东南部)漏斗烧杯文化的新石器时代定居点的空间安排125关于其居住的空间安排,范围和详细动态的结论基于这些有限的数据。尽管发掘工作取得了成果,但这些被检查的坑群是否是更大的特征集中的一部分,以及在定居点内是否还有其他集群,这一点还有待商榷。从目前Rzeszów山麓东部黄土地区的研究经验来看,这似乎是合理的。例如,在Pawłosiów 52 (Rybicka等人,2014)和Mirocin 27 (Sznajdrowska, 2016)中已经发现了这些不同的坑群。毫无疑问,为了真实地估计Skołoszów 16中定居点的空间,应该进行大规模的挖掘。 然而,在这些未来的调查之前,我们决定进行一次地球物理调查,以确定最适合挖掘的区域,并提供考古特征分布的空间视图。4. 非侵入性研究的主要目的是调查Skołoszów 16区域,以估计po
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来源期刊
Interdisciplinaria Archaeologica
Interdisciplinaria Archaeologica Arts and Humanities-Archeology (arts and humanities)
CiteScore
1.00
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0.00%
发文量
15
审稿时长
24 weeks
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