Archaeological Sequence Research Articles

Early hunters and herders of northern Ethiopia: The fauna from Danei Kawlos

It is generally agreed that Ethiopia is one of the world’s primary centers of prehistoric plant domestication. It is also known that domestic fauna (cattle and domestic caprines) were brought in from outside. Unfortunately, very few Holocene archaeological sequences have been excavated in the Horn. Even fewer sites have yielded domestic fauna dating to > 3000 years ago. The excavations at the site Danei Kawlos in northern Ethiopia provide new Holocene archaeological sequences for Northern Ethiopia and document the presence of cattle, sheep and goat with a direct date of 3358 ± 47 BP on a Bos molar. We discuss here the zooarchaeological data from the site.

A late Pleistocene to Holocene archaeological record from East Kalimantan, Borneo

Recent archaeological excavations at Liang Jon, a limestone rockshelter in the East Kalimantan province of Indonesian Borneo, have revealed a cultural sequence covering the period from around 16,700 calibrated radiocarbon years before present (16.7 kyr cal BP) until the late Holocene—a time of dynamic environmental, social, and economic change throughout Island Southeast Asia. There are few published archaeological sequences from this period of human history from Borneo, a geographically strategic region in the wider early human settlement of the region, highlighting the importance of our initial finds and dating work at Liang Jon. We describe our excavation and present chronostratigraphic and initial summary data to outline the significance this cultural sequence has in reconciling archaeological evidence and dated rock art records from early human cultural behaviour at the easternmost margin of the Late Pleistocene continental landmass of Sunda. Summary data, including stone artefacts, marine shell beads, faunal remains, and a pre-Austronesian burial, contributes to our understanding of regional trends associated with widespread cultural and technological change during the Pleistocene to Holocene transition, when the present-day island of Borneo was formed.

Technical and conceptual behaviours of bone and antler exploitation of last hunter-gatherers in Northern Iberia. The osseous industry from the Magdalenian layers of Ekain cave (Basque Country, Spain)

The site of Ekain Cave presents a large archaeological sequence encompassing all the Upper Palaeolithic periods. Here we present results of a technological analysis conducted on the bone and antler industry from the Magdalenian (Lower, Middle and Upper) levels. The industry reflects the pattern seen at other Magdalenian sites in north Spain and the Pyrenees, such as the choice of bone for domestic activities (awls, needles and polishers) whereas antler was employed mainly for hunting and/or fishing weapons (projectile points and barbed points). The succession of cold and amelioration phases recorded during the Magdalenian has its effect on the fauna present and on the availability of raw material, in particular, cervid antler.The present study identifies for the first time the use of debitage by fracturation in northern Iberia. A hypothesis that may explain the incentives behind the adoption of such a procedure in Ekain is proposed. These results are put in the context of the operational sequences for the osseous industry in the north of Iberia during the last Upper Palaeolithic. Indeed, our study reinforces the hypothesis that a high degree of exchange of technical and conceptual behaviours between the North and the South of the Pyrenees and the Iberian Mediterranean area as already suggested by works on lithic technology and cave and mobile art.

THE DISTRIBUTION OF AGE DISPARITIES IN CONIFER CHARCOAL FROM ARCHAEOLOGICAL STRUCTURES AND APPLICATIONS FOR TREE-RING-RADIOCARBON DATING

ABSTRACTAge disparities between charcoal samples and their context are a well-known problem in archaeological chronometry, and even small offsets could affect the accuracy of high-precision wiggle-matched dates. In many cases of taphonomic or anthropogenic loss of the outermost rings, sapwood-based methods for estimating cutting dates are not always applicable, especially with charcoal. In these instances, wiggle-matchedterminus post quem(TPQ) dates are often reconciled with subjective or ad hoc approaches. This study examines the distribution of age disparities caused by ring loss and other factors in a large dendroarchaeological dataset. Probability density functions describing the random distribution of age disparities are then fit to the empirical distributions. These functions are tested on an actual wiggle-matched non-cutting date from the literature to evaluate accuracy in a single case. Simulations are then presented to demonstrate how an age offset function can be applied in OxCal outlier models to yield accurate dating in archaeological sequences with short intervals between dated episodes, even if all samples are non-cutting dates.

Zeng state cemetery at Zaoshulin during the Spring and Autumn period, Suizhou, Hubei

Abstract The Zaoshulin cemetery includes five large tombs with an entry ramp leading to a central chamber on one side, 19 medium tombs, and 62 small tombs. According to the inscriptions on the bronze vessels, the layout of the tombs, and the grave assemblages, this cemetery was the burial place for the high-ranking noblemen of the Zeng state. Three hierarchies of tombs from large to small in size correspond to the social ranks of marquises, high-ranking noblemen, and low-ranking noblemen. Amongst these tombs, the occupants of five large burials in three groups are identified as Lord Qiu of Zeng and his wife Yu, Marquis Bao of Zeng and his wife Mi Jia, and Marquis De of Zeng. The Zaoshulin cemetery, along with the sites and cemeteries at Yejiashan, Wenfengta, Guojiamiao, Sujialong, presents a clear and complete archaeological sequence of the culture of Zeng. It also establishes a reference point for Bronze Age archaeological culture in South China.

Aboriginal serrated and perforated shell artefacts from the Murray River, South Australia

ABSTRACTThis article describes three freshwater mussel shell artefacts recently documented for the Murray River in South Australia. These finds more than double the known examples of such artefacts from this region. Two of the modified shells are perforated, with the other serrated. The finely serrated item is a rare artefact and we have not located any similar published examples in Australia, although international correlates exist. The function/s and cultural significance of the objects are also considered in this paper. Hypotheses for the perforated finds include ornamentation, tool stringing and fibre scraping. Ornamentation, idle tinkering and food utensil use are considered as possible intended functions for the serrated artefact. Given the age range of the objects reported here (c. 6181–517 cal BP), together with other finds in the Murray Darling Basin, we tentatively suggest that shells have been a material resource used continually in this region for a range of purposes. However, as argued by other researchers, we concur that there has probably been infrequent identification and reporting of such shell artefacts. This is considered particularly likely given that our finds were recovered from relatively small scale excavation/coring and surface sampling efforts. As such, this paper attempts to raise awareness of this form of material culture in archaeological sequences.

ABU SALABIKH – ABSOLUTE RADIOCARBON CHRONOLOGY

This article presents a new absolute chronology for the archaeological site of Abu Salabikh, Southern Iraq, during the 4th and 3rd millennia BC. The main goals of this study were to synchronise the sequences of the West and Main Mounds, corroborating the dating schemes based on archaeological and textual finds, and assigning an absolute date to the transition between Uruk and Early Dynastic (ED) periods. Previously published dates and newly produced 14C measurements were used in tandem with Bayesian statistical models to arrive at more precise time estimates. Some inconsistencies in the results point to possible disturbance of the archaeological sequence in the context of tannur kilns and highlight the need for careful sample collection and selection methodology. The results suggest a hiatus in settlement between the Uruk and ED periods c. 3000 BC, and confirm the date of c. 2650-2500 BC for the Early Dynastic ED IIIa Fara-style texts.

URBAN DEVELOPMENTS IN PERSEPOLIS DURING THE REIGN OF ACHAEMENID KINGS

The point of this examination is to understand the metropolitan advancements that happened in the city of Persepolis during the Achaemenids' time and the role of rulers in transforming it through various timeframes. The targets of the exploration are revealing insight into the main metropolitan changes that occurred in the city of Persepolis, and zeroing in on the progressions that made the city of Persepolis such an incredible city that the Achaemenid rulers did their most extreme to create and succeed, other than focusing on the explanations for its significance to the Achaemenids. Concerning the logical hole corresponding to past examinations, since numerous analysts managed the city of Persepolis as an authentic city and some of them managed the archeological part of it, what recognizes the current exploration is the recorded and archeological sequence for the city of Persepolis through the most noticeable changes that happened in the hour of the Achaemenid rulers. With respect to the examination, the exploration followed the recorded and elucidating parts of this city and mixed them by featuring the main metropolitan viewpoints in the city of Persepolis. The results assigned the main attributes of our exploration and the most noticeable techniques that were utilized in the improvement of the city of Persepolis, and how the Achaemenid lords had the option to foster it and make it a city similar to the antiquated archeological urban areas.

A Late Pleistocene high-resolution paleoclimate reconstruction: insights from the archaeobotanical assemblage and the carbon isotope analysis of wild almond (Amygdalus sp.) from Raqefet Cave, Mount Carmel, Israel

Raqefet Cave is located in southeast Mount Carmel, Israel. It contains a long archaeological sequence with two major occupations: in the early Upper Paleolithic (Levantine Aurignacian culture, ca. 36,000–35,000 cal. BP) and the Late Epipaleolithic (Natufian culture, ca. 14,000–12,000 cal. BP). Abundant charred remains were found in the cave's deposits consisting of various species. Drawing on Δ13C values of dated Amygdalus sp. (almond) charcoal specimens, we sought to reconstruct Late Pleistocene precipitation patterns from a high-resolution archaeological record. The results produced the longest, single-site, plant-based paleoclimatic sequence in the southern Levant, and they generally correspond to other paleoclimatic proxies generated for the region. They indicate that the plant taxa and reconstructed precipitation levels were all in the range of modern eastMediterranean climate but with some notable fluctuations. Specifically, we highlight the rainfall differences between the dryer Levantine Aurignacian and the wetter Natufian cultures.

Tracing the geomagnetic field intensity variations in Upper Mesopotamia during the Pottery Neolithic to improve ceramic-based chronologies

The transdimensional Bayesian method AH-RJMCMC applied to archeomagnetic intensity data available in the Balkans and the Near East allows us to estimate the variations in intensity of the geomagnetic field in Upper Mesopotamia during the 7th and 6th millennia BCE (Late Neolithic), with adequate treatment of the dating and intensity uncertainties. The results for the 6th millennium BCE appear particularly interesting because there is enough data to trace rapid geomagnetic field intensity variations, with two century-scale peaks around 5800 BCE and 5550 BCE, associated with rates of changes (>0.2 μT/year) higher than the maximum rate observed in the current geomagnetic field. We show that these variations could help decipher the correlations between different archeological sequences or periodizations established from scattered sites in Upper Mesopotamia. So far documented only from the Balkan data, the intensity peak occurring around 5800 BCE may provide accurate chronological constraints for the Early Halaf phase. New insights are also obtained for the Halaf-Ubaid Transitional phase (end of the 6th millennium BCE), which remains poorly defined from an archeological point of view. The AH-RJMCMC results imply that either the archeointensity data currently available from Upper Mesopotamia document only the beginning of this phase, or that this phase occurred between ~5400 and ~5200 BCE, shorter than often considered. Such preliminary archeological inferences will progress and broaden with the addition of new archeointensity data.

Multi-method approach using small vertebrate assemblages to reconstruct the Marine Isotope Stage 6 climate and environment of the Lazaret cave sequence (Maritime Alps, Nice, France)

Marine Isotope Stage 6 (MIS 6; ca. 185–135 ka) is the penultimate glacial stage and constitutes the end of the Middle Pleistocene. This glacial period is typified by generally cold and dry conditions in the western Mediterranean region. Despite the relatively large number of pollen and speleothem studies of MIS 6 in this region, the number of MIS 6 archaeological sites is low. Lazaret cave, situated at 26 m a.s.l. in the city of Nice in southern France, contains an archaeological sequence (layers CII inf. to CIII) dated to MIS 6. We present a multi-method approach using the small-vertebrate assemblages (mainly rodents and herpetofauna) from the entire sequence to characterize the climate and the environment of the site. The Mutual Ecogeographic Range, the Bioclimatic Model andthe Quantified Ecology methods, as well as the Taxonomic Habitat Index, Climatograms and the Simpson Diversity Index were used to reconstruct the palaeoenvironmental and palaeoclimatic conditions. The results suggest a generally cold climate with a relatively humid environment and a landscape dominated by deciduous temperate forests. The findings are consistent with the general trends reported from other proxies (large mammals, birds and marine gastropods) studied at Lazaret cave, other MIS 6 sites in the Mediterranean region with small vertebrate studies and the general trends shown by marine cores, terrestrial pollen sequences and speleothems from western Europe. Given the scarcity of data for MIS 6 archaeological sites, Lazaret cave constitutes an important site for our knowledge of the climate and the environment of this period.

Late Pleistocene environmental dynamics and human occupation in Southwestern Europe

This paper focuses on palaeoenvironmental conditions and climate variability during the Upper Late Pleistocene (c. 28,000–11,700 cal BP) in SW Europe (Iberian Peninsula) and their influence on human settlement patterns. All the palaeoenvironmental and archaeological sequences available for this period are analysed, together with a new palaeoenvironmental study related to a key deposit: Verdeospesoa mire (northern Iberian Peninsula). The multiproxy analysis (pollen, spores, non-pollen palynomorphs, magnetic susceptibility, organic content and macrocharcoal) of this sequence, with the support of six Accelerator Mass Spectrometry (AMS) radiocarbon dates, shows the climatic variability of that period, with some dry/cold and humid/temperate episodes. While in vast regions of central and northern Europe very few archaeological sites of this age are known, in the Iberian Peninsula no occupation gaps have been detected in all this period, supporting the idea of SW Europe as a glacial refugium for human groups during the worst periods of the Upper Late Pleistocene.

The newly discovered bronze age site of Koken: Merging micro-regions with major study zones in the high steppes of Kazakhstan

Bronze Age eastern Kazakhstan sat at the intersection of two distinct cultural interaction spheres: the Eurasian Steppe and the Inner Asian Mountain Corridor. Despite its importance, the region has not been extensively researched by archaeologists. Recent fieldwork in the Kokentau Mountains in eastern Kazakhstan has uncovered a multi-period archaeological sequence, presenting an opportunity to document this crucial area in detail. We present preliminary data obtained from initial settlement and cemetery excavations at the site of Koken that contribute to ongoing research about economy and interaction in the Eurasian Bronze Age. The site's long occupational history, supported by radiocarbon dates, reveals shifting cultural patterns stretching from the Mesolithic to the historical period. Current and future research in the Kokentau Mountains can clarify the timing and local trajectories of Bronze Age economic and cultural transitions through the integration of evidence from ritual, craft production, and habitation contexts at a resolution rare for this region and time period.

The charcoal assemblage from Nesher Ramla, Israel: A contribution to the paleo-environmental dataset from Marine Isotope Stage (MIS) 5 in the Levant

This paper presents the results of the wood charcoal analyses from the Middle Paleolithic open-air site at Nesher Ramla, on the central coastal plain of Israel. The study focuses on the interpretation of the charcoals left by fires used by Middle Paleolithic hominins during early Marine Isotope Stage (MIS) 5. Moreover, this study sheds light on the arboreal taxa present in the vegetation and environmental conditions in the southern Levant during the Middle Paleolithic. A small quantity of identifiable charcoals was retrieved from the 8-m-thick archaeological sequence of the site (Units II to VI). The largest charcoal assemblage was recovered from part of the sequence dated to MIS 5e. The results show the presence of deciduous Quercus sp. and Prunus. The presence of these taxa, together with other proxies from the multidisciplinary studies at Nesher Ramla, indicate an arboreal setting with relatively humid and mild climatic conditions in MIS 5e. Our results further suggest that wood was used as fuel at Nesher Ramla. Given the scarcity of Middle Paleolithic sites in the Levant that have yielded charcoal, this new data from Nesher Ramla constitutes an important contribution to the study of past environments and the exploitation of plant resources by human groups.

A chrono-cultural reassessment of levels III-V from El Cuco rock-shelter: a new sequence for the late Middle Palaeolithic – early Upper Palaeolithic boundary in the Cantabrian region (northern Iberia)

The Iberian Peninsula is one of the key areas for studying the last populations of Neanderthals and the arrival in Europe of the first anatomically modern humans. In the Cantabrian region, this process can be traced in just a few sites with levels dating to the final stages of the Middle Palaeolithic and the earliest phases of the Upper Palaeolithic. One of these singular enclaves is El Cuco rock-shelter, where the sequence was initially dated by 14C only to the early Upper Palaeolithic sensu lato. However, new studies and datings now place this archaeological sequence in the late Mousterian and the Aurignacian. In this article we present a chrono-cultural reassessment of the upper levels of El Cuco (III-V), including a study of the large mammals. Levels Vc and Vb (>43.5-40.5 ky uncal BP) date from the late Mousterian, whereas levels Va, IV and III (c. 36.5-30 ky uncal BP) cover an interval extending at least from the Early Aurignacian to the Evolved Aurignacian. Particularly noteworthy is the discovery in level Va of a set of decorative beads made from marine shells in a context of possible symbolic behaviour.

THE BEGINNING OF THE IRON AGE AT ARSLANTEPE: A14C PERSPECTIVE

ABSTRACTThe Iron Age chronology at Arslantepe is the result of the interpretation of Luwian hieroglyphic inscriptions and archaeological data coming from the site and its surrounding region. A new round of investigations of the Iron Age levels has been conducted at the site over the last 10 years. Preliminary results allowed the combination of the archaeological sequence with the historical events that extended from the collapse of the Late Bronze Age empires to the formation and development of the new Iron Age kingdoms. The integration into this picture of a new set of radiocarbon (14C) dates is aimed at establishing a more solid local chronology. High precision14C dating by accelerator mass spectrometry (AMS) and its correlation with archaeobotanical analysis and stratigraphic data are presented here with the purpose of improving our knowledge of the site’s history and to build a reliable absolute chronology of the Iron Age. The results show that the earliest level of the sequence dates to ca. the mid-13th century BC, implying that the site started developing a new set of relationships with the Levant already before the breakdown of the Hittite empire, entailing important historical implications for the Syro-Anatolian region at the end of the 2nd millennium BC.

Inferring human activities from the Late Pleistocene to Holocene in Topogaro 2, Central Sulawesi through use-wear analysis

Recent excavations in Topogaro 2 Cave, Central Sulawesi produced an archaeological sequence beginning c. 29 ka. The site is located along the eastern coast of Sulawesi, a key location for prehistoric movements from mainland Southeast Asia to Sahul through Wallacea during the Late Pleistocene. In this paper, we test our hypothesis that prehistoric activities associated with hunter-gatherers can be identified through the study of microscopic traces on stone tools and their functions. We report on the use-wear analysis on lithic tools from the Late Pleistocene and Early Holocene. Our results indicate that a variety of activities were conducted at the site throughout its occupation. While most of the artefacts with use-wear traces were unmodified flakes typical for this region, a number of retouched tools provided indication of specialised functions and certain traits of modern behaviour such as the possible use of hafted projectile implements. Plant processing, an activity associated with the development of tool assemblages from Island Southeast Asia supporting the ‘Bamboo Hypothesis’, was also identified. The results contribute to our understanding of technology and behaviour in the Late Pleistocene in Wallacea, an important geographical region to discuss island adaptation and human migrations.

Using archaeological data and sediment parameters to review the formation of the Gravettian layers at Krems‐Wachtberg

ABSTRACTThe Gravettian site Krems‐Wachtberg in northeast Austria produced a wealth of archaeological and sedimentary data. Precondition for a detailed study of the formation processes is co‐occurrence of find layers with in situ and redeposited material. We use archaeological data and sediment parameters to review and refine a formation model that was based solely on field observations. The archaeological perspective relies upon the rich chipped stone assemblage where each artefact is attributed with 3D position, orientation, stratigraphy, typo‐technological description, and raw material determination. This enabled systematic refitting and 3D analyses of the results. High‐resolution sampling of the sediment sequence which was conducted in six columns at different locations of the excavated area provided comparable results for grain size, colour and carbonate content. The study illustrates the complementary benefits of field observations, archaeological data and sediment parameters. While detailed loess stratigraphy creates the frame for understanding palaeoenvironmental processes, archaeological data enhances visibility of local post‐occupational sedimentary processes. This allows the archaeological sequence to be placed into a cycle of gradual de‐ and restabilisation of the palaeosurface. Burial of the ~31k cal abp occupation layer occurred by solifluction, slope wash and aeolian deposition between two stable phases marked by tundra gley soils.

Cova de les Malladetes (Valencia, Spain): New Insights About the Early Upper Palaeolithic in the Mediterranean Basin of the Iberian Peninsula

New excavations carried out at Cova de les Malladetes confirm and improve previous information on the archaeological sequence of this site. A total of 29 new dates allow to specify the chronology of the Aurignacian (levels XIVA–XII) and Gravettian (levels XI–VII). Furthermore, concerning the results obtained during the 1970 excavation, three new levels were identified: level XIVB, which represents a short temporal human occupation hiatus, and levels XV and XVI with some hearths and anthropic evidence, although the lithic material does not permit a cultural attribution. This paper presents data obtained from the analysis of archaeobotanical, micro- and macrofaunal assemblages and lithic and osseous industry. Results are relevant concerning the palaeoclimatic and palaeoenvironmental characterisation of the Early Upper Palaeolithic, as well as for assessing the human occupation patterns during the Gravettian and Aurignacian. Moreover, we evaluate the chronological implications of the basal levels (XIVB, XV and XVI), drawing attention to the absence of an important temporal gap between this phase and the start of the Early Upper Palaeolithic at the site. Finally, our new data extend the information provided by other sites in the Spanish Mediterranean region, allowing a more defined characterisation of the Early Upper Palaeolithic, especially regarding the Evolved Aurignacian chronology and its techno-typological structure, with the presence of Roc-de-Combe subtype Dufour bladelets.

The Ceramic Assemblage of Tse Dura (Indyer Mbakuv) Rockshelter in Benue State, Central Nigeria

We analyzed the ceramic assemblage from a re-excavated section of Tse Dura rockshelter (KA4RS1) in central Nigeria’s Ushongo area to understand the archaeological sequence of human occupation and cultural changes. The analysis, focusing on motifs, forms, and petrography, identifies three phases of human occupation. The petrographic results, in particular, revealed three main fabric groups—TD-AC1, TD-AC2, and TD-AC3—all of which contain inclusions that are indicative of clay sources local to the Tse Dura rockshelter region. The first two groups, TD-AC1 and TD-AC2, contain similar inclusions; however, the third group, TD-AC3, exhibited slight variability. The variations in fabrics and inclusions are most probably related to the potters’ choice of different techniques and unique raw materials for specific vessels.