AMS 14C Dates Research Articles

Holocene vertical velocity fields in the Calabrian Arc (southern Italy): New insights from uplifted sea-level markers in the Crotone Peninsula

The study of fossil coastlines is one of the most widely used methods to unravel the vertical movements of the Earth's solid surface. All along the coast of the Calabrian Subduction Arc, well preserved Pleistocene marine terrace sequences document a protracted uplift history. Although Pleistocene vertical movements have been extensively explored, the Holocene history is not well understood. Numerous uplifted coastlines of the Holocene period have been studied along the Tyrrhenian side of Calabria, but the Ionian coastal sector is considerably under-studied. Our new data from the coast of the Crotone Peninsula fill this crucial data-gap. AMS 14C dating of seventeen sea level markers, elevated above the current mean sea level, show ages between 2300 and 7000 Cal. Yr BP. The elevation of the markers was corrected for the paleo sea level using the most updated GIA models ICE-6G (VM5a) and ICE-7G (VM7). We found that a coastline dated to 7 ka shows uplift rates of 0.8 mm/yr, consistent with late Pleistocene uplift rates (≈0.8 mm/yr). In contrast, a 2.3 ka coastline was uplifted by only 1 m, resulting in lower uplift rates of ≈0.5 mm/yr. However, there are clues that the abandonment of this younger coastline may have occurred with a rapid uplift pulse. Reconstructing the past vertical movements of the Crotone Peninsula reveals an unsteady uplift history. At some times fast uplift rates are required, while for other periods, lasting as long as 3–4 kyr, the uplift rate is slower or zero. An uplift history consisting of periods of accelerated uplift, or even coseismic pulses, would also explain the difference in uplift rates between short term (<5 ka) and long term (>5 ka) markers through a metric we have defined as uplift rate sensitivity. Understanding the details of this uplift history has social relevance. The co-seismic uplift hypothesis requires further investigation but if confirmed would likely affect the seismic and tsunami hazard of the Crotone Peninsula. Similarly, the unsteady uplift rate would cause a risk given the current rapid rate of global sea level rise. Periods of sustained vertical stability would increase the risk of flooding even in areas characterized by long-term uplift and thus considered safe.

Garnys: An underwater riverine site with delayed Neolithisation in the southeastern Baltic

This paper presents the first results of both dryland and underwater investigations at the multi-period Garnys riverine site situated on the Žeimena River in eastern Lithuania. There, during 2017–2020 a professional diver and amateur archaeologist collected hundreds of Mesolithic-Neolithic archaeological finds made of wood, bone, antler, stone, and ceramic from the riverbed and on its bank. Moreover, in eroded places of the riverbed, the wooden remains of several fish weirs were observed. In 2021 professional archaeologists continued the research, including field investigations followed by various laboratory analyses. These included AMS 14C dating of 16 various ecofacts, artefacts and wooden constructions, wood and animal taxa determinations, and the results of traceological analysis of the flint and osseous artefacts. Our research demonstrates that the site was intensively used for hunting, gathering and fishing during the Mesolithic and subsequent Subneolithic and Neolithic. Intriguingly, there was no evidence for agriculture, while the numerous Neolithic ceramics largely follow the Subneolithic traditions. The Garnys site is therefore unique and a clear example for delayed Neolithisation in a forested and lacustrine area in the eastern Baltic region. During the Metal Ages, the site had been used exclusively for stationary fishing.

First AMS radiocarbon dating of Río Chico style paintings (southernmost Patagonia, Argentina): Older than expected

This paper presents the first AMS 14C dating of the Río Chico Style from southernmost Patagonia (52°S). These paintings are characterised by the dominance of geometric linear motifs and a low frequency of figurative ones. According to a few indirect radiocarbon dating of stratified pigments and the chronology of nearby sites, the Río Chico Style has traditionally been dated to ca. 2000 BP, although an earlier chronology (ca. 8000 BP) has also been proposed according to Fell Cave (Magallanes, Chile) stratigraphy. Here we present the first AMS 14C dating for this style from three rock paintings at Romario Barría Rockshelter (Pali Aike volcanic field, Santa Cruz province, Argentina). The main objectives of this work are, first, to discuss the chronology of the Río Chico style from direct and indirect datings, second, evaluate the use of the site according to painting manufacture, and finally, analyse the distribution of Río Chico style at the regional scale and its connections with other lines of evidence, such as lithic assemblages, to discuss the role of rock art in highly mobile southern Patagonia hunter-gatherer societies.

Diet of the fortified settlement communities in Lithuania from 1000 cal. BC to 200 cal. AD

The fortified settlements in Lithuania attest to a long-term phenomenon representing the behaviour of early farmers after the adoption of crop cultivation ca. 1300–1250 cal. BC. Hitherto, the subsistence economy and diet of this population were primarily understood via zooarchaeological and archaeobotanical analyses, however, understudied are the food residues in pottery. In this paper, we present the first results of stable isotope analysis on 209 charred organic residues sampled in pottery from nine sites. The food remains in pottery consisted of δ13C and δ15N values inherent for terrestrial sources with indications of millet consumption during the Late Bronze Age (1100–500 cal. BC). By comparison to the data from earlier periods, a significant dietary change in the local population ca. 1000 cal. BC was distinguished. Furthermore, 34 new AMS 14C dates acquired during this research allowed to better understand the chronology of fortified settlements. Our results provide the earliest evidence for the spread of this type of site in Lithuania and demonstrate the significance of the Daugava River basin during the early stages of this process.

Incised valleys on the Algarve inner shelf, northern Gulf of Cadiz margin: Stratigraphic architecture and controlling factors in a low fluvial supply setting

A network of cross-shelf paleovalleys has been recognized over the paleo-inner shelf off the Gilão-Almargem Estuary, a small fluvial drainage system that presently receives minor sediment supply in the eastern Algarve shelf, northern margin of the Gulf of Cadiz (SW Iberian Peninsula). This study is aimed at determining the driving controls that triggered substantially different paleohydrological conditions and sedimentary dynamics of ancient fluvial systems in this margin. We focus on evidences of secondary controls on valley genesis and evolution, superimposed to primary glacio-eustatic control such as antecedent geology, low fluvial supply and changing hydrodynamic regimes. The architecture and spatial distribution of these paleovalleys were interpreted based on a grid of seismic profiles with different resolutions. Likewise, a sediment core obtained in a distal position of the paleovalley system provided information about sedimentary processes during the most recent stage of valley infilling. The chronostratigraphic framework was constructed based on regional seismic horizons defined in previous studies and complemented with two AMS 14C dates obtained from bivalve shells.The inner shelf paleovalley system is composed of several incised valley features which exhibit a remarkable similar internal architecture. These inner valley features exhibit two major incision phases (from oldest to youngest; IP 2 and IP 1) that are thought to constitute a simple paleovalley system formed during the last glacial cycle. The origins of the incision are considered to be different. The older one is related to fluvial incision during the sea-level fall leading into the Last Glacial Maximum, whereas the recent one is interpreted as the result of tidal scour during the postglacial transgression. Their corresponding infillings are interpreted, respectively, as estuarine bay-fill deposits and estuary-mouth sands. Overlying the paleovalley infilling, a distinctive reflective unit is in agreement with the generation of coastal barriers and related depositional systems.The formation of the paleo-inner-shelf paleovalley system was strongly conditioned by antecedent geology, which strongly limited the generation of wide incised valleys and determined the amount of incision landward of a well-defined break of slope. Its postglacial infilling was mainly estuarine in nature, likely involving the development of a dendritic system, with numerous barriers interrupted by tidal inlets and channels in a mixed estuarine system with low fluvial supply.

Rapid environmental changes in the Lake Qinghai basin during the late Holocene

The Lake Qinghai Basin is sensitive to global and regional climate change because of its unique geographical location. It is the hotspot for paleoclimate research in East Asia. In this study, we reconstructed the environmental evolution of the Lake Qinghai since ∼9 ka by using a high-resolution peat and fluvial-lacustrine record (Laoyinggou profile) obtained at the foot of Nanshan Mountain. Based on 8 AMS14C dates and lithology, loss on ignition (LOI), total organic matter (TOC), X-ray fluorescence (XRF) core-scanning measurements, ratio of total organic carbon to nitrogen (TOC/TN), and sediment particle sorting coefficients, we show that during the Middle Holocene (∼9–4.4 ka BP) this region was primarily dominated by the Asian summer monsoon, with a consistent, warm, and humid environment. By contrast, during the late Holocene (4.4 ka to present), the climatic context in this area fluctuated dramatically at the millennial scales. The low TOC content, lower TOC/TN ration and strong hydroclimatic indicate six rapid climate change events, which occurred at ∼4.0 ka, ∼3.6 ka, ∼3.2 ka, ∼2.8 ka, ∼2.1 ka, and ∼1.4 ka, all of which coincided to cold episodes in the North Atlantic Ocean.

Channel migration in the northeastern margin of the Tibetan Plateau and its implication for fluvial response to the interaction between rapid tectonic activity, climatic fluctuation and human influence

Fluvial response to allogenic and autogenic controls concerns the understanding of landform evolution related to the interaction between tectonic movements, climate, surface process and human activity. Paleo-channels, as part of geomorphic archives, have been widely employed to study this issue during recent decades. Previous work has however concentrated on the mechanisms driving river migration. A new approach, in which multiple elements are considered, is employed here in the examination of paleo-channel formation in the Jiudong Basin, located at the northeastern margin of the Tibetan Plateau and characterized by active tectonic deformation, a dry climate and ancient human activity. Based on geomorphic and sedimentary analysis, eight paleo-channels formed by the Taolai and Hongshuiba rivers (two tributaries of the Beida River catchment) have been identified. AMS14C dating of the overlying lacustrine sediments defined their respective abandonment at ca. 22.2, 20.9, 15.3, 18.8, 13.9, 11.9, 3.5 and 1.1 cal. Ka BP. The migration histories of the two rivers have been reconstructed, and then well correlated with reference to archives of tectonic, climatic and human influence. Our results suggest that these controlling factors seem to be coupled and have a competitive relationship in driving river migration. In the northeastern margin of the Tibetan Plateau, channel migration can therefore be regarded as a result of fluvial response to the interaction between rapid tectonic activity, climatic fluctuation and human influence.

Geochemical Records of the Late Glacial and Holocene Paleoenvironmental Changes from the Lake Kaskadnoe-1 Sediments (East Sayan Mountains, South Siberia)

Long-term and continuous lake sedimentary records offer enormous potential for interpreting paleoenvironmental histories and for understanding how terrestrial environments might respond to current global warming conditions. However, sedimentary records that contain the Late Glacial and Holocene epochs are scarce in deep continental high-mountain regions. A 150 cm sediment core was obtained from Lake Kaskadnoe-1 in the East Sayan Mountains (South Siberia, Russia, 2080 m above sea level), containing a unique record of the last 13,200 calibrated years (cal yr). Chronological control was obtained by AMS 14C dating. Here, we show the first detailed X-ray fluorescence (XRF) geochemical record, with the goal of broadening our knowledge of the paleoenvironmental history of the East Sayan Mountains in the past. The determination of major compounds and trace elements (Sr, Zr) was performed from each centimeter of the Lake Kaskadnoe-1 sediment core. The inorganic geochemistry indicates significant variations in elemental composition between two major lithological units of the sediment core: the Late Glacial dense grey silty clay (150–144 cm), and the upper interval (0–143 cm) mostly consisted of dark biogenic-terrigenous silt, accumulated during the Holocene. The Late Glacial sediments accumulated 13,200–12,800 cal yr BP are characterized by high values of CIA, Mg/Al, K/Al, and Mn/Fe, and are depleted in Si/Al, Fe/Al, and Ca/Al. During the Younger Dryas cold episode, LOI enrichment was probably caused by the presence of less oxic conditions, as seen in lower Mn/Fe values, due to a longer period of lake ice-cover. The Early Holocene (12,000–7500 cal yr BP) is associated with a decreasing trend of mineral matter with fluvial transport to Lake Kaskadnoe-1 (low K/Al, Mg/Al) and stronger chemical weathering in the lake basin. The increase in Ti/Al, K/Al and CIA values over the last 7500 years suggests an increase in the terrigenous input into the lake. Low LOI values can be possibly explained by the presence of less dense vegetation cover in the basin. In summary, our data indicate that the geochemical indices and selected elemental ratios mirror the sedimentation conditions that were triggered by environmental and climate changes during the Late Glacial and Holocene.

A new chronological framework for Chuandong Cave and its implications for the appearance of modern humans in southern China

Chuandong Cave is an important Late Paleolithic site because it documents the early appearance of bone tools in southern China. We used the single-aliquot regenerative-dose protocol for optically stimulated luminescence dating to improve the precision of the chronology for the Chuandong Cave sedimentary sequence. The age of each layer was determined using a Bayesian modeling approach which combined optically stimulated luminescence ages with published AMS 14C dates. The results showed that Layer 10 began accumulating since 56 ± 14 ka and provides the upper age limit for all artifacts from the sequence. Bone awl tools from Layer 8, the earliest grinding bone tools in this site, were recovered within sediments between 40 ± 7 ka and 30 ± 4 ka. Layer 8 also indicates the appearance of modern humans in the Chuandong Cave sequence. Layers 4–2, ranging from 15 ± 3 ka until 11 ± 1 ka and including the Younger Dryas period, contain a few bone awls and an eyed bone needle. The shift from bone awls to eyed bone needles in the Chuandong Cave sequence indicates that modern humans adapted to the changing climate of southern China. We conclude that modern human behavior in bone tools appeared in southern China as early as 40 ± 7 ka, became more sophisticated during the Last Glacial Maximum, and spread more widely across southern China during the Younger Dryas.

New radiocarbon dates and the prehistoric human occupation at the Lake Qinghai Basin, northeast Tibetan Plateau

The Tibetan Plateau is known as the rooftop of the planet. Its hypoxic atmosphere in low oxygen partial pressure, extreme seasonal climate variation, and aridity poses severe challenges as harsh living environments for prehistoric human to occupy in such high-altitude niches. However, the Lake Qinghai is the largest lake on the Tibetan Plateau and the basin has rich water, mineral, and wild food resources, and prehistoric human occupied the Lake Qinghai Basin long before local farming was in practice. In this paper we present results of faunal assemblages associated with variable stone artifacts and pottery shards with bone collagen accelerator mass spectrometry radiocarbon (AMS 14C) dates from 3 new archaeological sites to investigate human occupation history in the southern Lake Qinghai Basin. The AMS 14C dating results reveal that the occupation occurs intermittently from the late Glacial to entire Holocene. Through compilation and synthesis of regional archaeological records, we found that prehistoric humans went through 3 phases of subsistence strategies: 1) hunting large and medium ungulates; 2) hunting medium ungulates; 3) foraging small size mammals with birds and fish diets. At the end, prehistoric humans increasingly adapted to forage and consume caprinaes species (goat), which represents a precursor of domestication or semi-domestication of wild animals in the Lake Qinghai Basin. We further attribute the utilization of caprinaes animal resources to the lower limbs of toe and phalange bones with low nutritious values to advanced social organization that implied prehistoric humans separated hunting activity from protein processing practices. Our investigation of zooarchaeology with reliable bone collagen AMS 14C dates could become a novel approach to study adaptation strategy and social structure changes of prehistorical Tibetan humans.

AMS 14C dating of bioapatite: Advantage and disadvantage

Most methods of bone preparation for 14C dating are designed to extract collagen or individual compounds. The problem becomes acute for poorly preserved bones, since they have no collagen. The bioapatite is stable against microbiological decomposition and dissolution over millennium scales. However, it may be exposed to isotopic exchange with environmental carbonates.We are reviewing our research during the last decades comparing the dating different fractions of bones of different ages and differing preservation degrees. The results have shown that preservation of bioapatite depends on the conditions of the environment in which samples were buried. The wet environment affects bioapatite by enriching it with 14C due to isotopic exchange with environmental carbonates. 14C depletion of bone bioapatite deposited in caves and in limestone is possible. The results for the samples from arid, semi-arid and non-carbonate environments are in a good agreement with dates on other materials.

The timing of the deglaciation in the Atlantic Iberian mountains: Insights from the stratigraphic analysis of a lake sequence in Serra da Estrela (Portugal)

AbstractUnderstanding the environmental response to the last glacial termination in regions located in transitional climate zones such as the Atlantic Iberian mountains is crucial to estimate potential changes in regions affected by current glacial melting. We present an 8.5 m‐long, solid last deglaciation and Holocene chronostratigraphic record including detailed sediment analysis from Lake Peixão, a pro‐glacial lake in the Serra da Estrela (Central Portugal). The age–depth model relies on a Bayesian approach that includes 16 AMS 14C dates and 210Pb–137CS measurements, robustly dating the lake formation at 14.7 ± 0.32 cal. ka BP. This chronological reconstruction shows an average sedimentation rate of ca. 0.07 cm yr−1 (15 yr cm−1), enabling proxy analyses at decadal timescales. The sediment sequence is composed of five lithological units: (U1) coarse and unsorted fluvioglacial lacustrine deposits; (U2) massive fluvioglacial lacustrine deposits (863–790 cm below surface [bsf]; 14.7 ± 0.32–13.8 ± 0.12 cal. ka BP); (U3) water current fluvioglacial lacustrine deposits (790–766 cm bsf; 13.8 ± 0.12–12.9 ± 0.29 cal. ka BP); (U4) laminated/banded lacustrine deposits characterized by terrigenous deposits from ice‐covered lake periods and episodic events of ice and snow melting (766–752 cm bsf; 12.9 ± 0.29–11.7 ± 0.15 cal. ka BP); and (U5) massive muddy lacustrine deposits (752–0 cm bsf; 11.7 ± 0.15 cal. ka BP–present). The occurrence of U2 to U4 deposits defines the transition from glacial cold (U1) to net warm postglacial conditions (U5). These climate transitions are marked by changes in sediments and the presence of very low sedimentation rate periods, possibly related to the Intra‐Allerød Cold Period and the coldest phase of the Younger Dryas. Our results support the previously proposed timing of the retreat of the Serra da Estrela glaciers ca. 13.8 ± 0.12 cal. ka BP. The robust chronology of Lake Peixão highlights the potential of Iberian pro‐glacial lakes for dating deglaciation processes and will lead to unprecedented decadal‐to‐centennial timescale palaeoclimate reconstructions in this region since the last glacial–interglacial transition.

Multidisciplinary Research in Late Bronze Age Kukuliškiai Settlement (Klaipėda District): Methods and Primary Results

The aim of this article is to present the most important results of the archaeological research of the Kukuliškiai settlement (Klaipėda district) in 2017–2020. During 3 seasons of the research, more than 3 hectares of the territory on the Littorina sea terrace were scanned by GPR, 101 geological drills were hammered, and an area of 45m2 was investigated. Fifteen AMS 14C dates were taken from different objects and stratigraphic layers of the settlement. Dating showed that settlement was contemporaneous and occupied around c. 800–400 cal BC. The complexity and scope of the research provides valuable insights into the lifestyle of Late Bronze Age coastal community. The discovery of wooden structures, organic artefacts and ecofacts indicates that the site provides excellent conditions for the survival of organics, of which there are only a dozen in Lithuania. The site and the collected research data, therefore, offer exceptional opportunities for the study of Bronze Age life not only in the coastal Lithuanian, but also in the southeastern Baltic region.

Metal tools of the Petrovka Culture of the Southern Trans-Urals and Middle Tobol: chemical and metallurgical characteristics

In this paper, the chemical composition of tools and ingots of the Petrovka Culture of the Southern Trans-Urals and Middle Tobol region is characterized with identification of main recipes of the alloys using several analytical methods (spectral, X-ray fluorescence, and atomic emission spectrometry analyses carried out in the laboratories of the Institute of Archaeology of the Russian Academy of Sciences and the Institute of Inorganic Chemistry of the Si-berian Branch of the Russian Academy of Sciences). The complexes of the Petrovka Culture of the Sou-thern Trans-Urals have been dated by a set of AMS 14C dates to 19th–18th centuries BCE. Recently introduced in the scientific discourse 27 AMS 14C dates (settlement of Stepnoe and burial grounds of Stepnoe 1, 7 and 25) established an ear-lier interval of the Petrovka series — 2133–1631 BCE and point to the synchroneity of the cultures at the northern periphery of the Sintashta area in the local micro-region of the Southern Trans-Urals. The results of the analytical study of 106 metal tools and 70 ingots of the Petrovka Culture of the Southern Trans-Urals and south of Western Siberia are reported. The statistical processing of the analytical results with plotting correlation diagrams of Sn–As, Sn–Pb, As–Ag, As–Sb, and a frequency distribution histogram for the proportions of Sn allowed casting the metal into 4 metallurgical groups — pure copper and tin, arsenic-tin and arsenic bronzes. The first group subdivided into oxide and sulfidic samples. According to the geochemical peculiarity of the metal from the metal industry centers of Ustie 1, Kulevchi 3 and Shibaevo 1, several sources of oxide-carbonated ores were utilized for copper smelting — malachite and azurite-malachite deposits, while sulfidic chalcocite-covelline ores, and sometimes chalcopyrite-pyrite depositions, were added to the melt as a flux agent. The admixture of sulfides was carried out as an experiment and was not purposeful. Petrovka metallurgists supplied copper to the workshops of the Middle Tobol region — the sites of Ubagan 1, 2, 3 and Kamyshnoe 1, 2. The centers of the Petrovka Culture of the Southern Trans-Urals were domi-nated by the production of pure copper implements, including the metal smelted from the oxidized ore. To a lesser extent, low-alloyed bronze was used — Cu+Sn, Cu+Sn+As and Cu+As, whose feedstock was supplied by the kin-dred tribes of Central and Eastern Kazakhstan in the form of ingots and finished products along the eastern part of the Trans-Eurasian transport corridor of metal trade — over the Turgay trough and further along the extensive river system of the Tobol River and its tributaries. The highest concentration of tools of alloyed bronzes was recorded in the burial grounds of the Middle Tobol, which can be explained from the point of view of the prestige value of such goods and observance of special ceremonial practices.

The domestic dog that lived ∼17,000 years ago in the Lower Magdalenian of Erralla site (Basque Country): A radiometric and genetic analysis

Dogs are known to be the first species domesticated by humans, although the geographic and temporal origin of this process is still under debate in different fields of knowledge. In the present study, we examined a humerus from a canid recovered in the Lower Magdalenian level of the site of Erralla (Zestoa, Gipuzkoa, Basque Country, Spain), combining morphology, radiocarbon dating and genetics. Our results confirm the identification of this specimen as Canis lupus familiaris, discarding miss-identification with a dhole (Cuon alpinus) through genetic analyses of cytochrome b gene and mtDNA haplogroup. The direct AMS 14C dating (17,410–17,096 cal. BP) indicated that the Erralla specimen represents one of the earliest domesticated dogs in Europe, in the Lower Cantabrian Magdalenian period. We discuss our results in the light of the debate of the origin of dogs, conducting a critical review of the datings of sites of Eurasia that have provided remains of Paleolithic and Mesolithic dogs, including the so-called “dog-like wolves”.

The Vaza-Barris River: A late Quaternary decoupled accumulation-erosion model for rivers of the NE Brazil Atlantic passive margin

Limited insight is available regarding the links between the upstream-downstream fluvial response to climate changes and alluvial-coastal base-level factors in the passive Atlantic margin of tropical South America. This work attempts to characterize the last glacial-interglacial fluvial response of a typical semi-arid Brazilian Northeast River that drains Central-East Brazil's highlands. We integrate the full extension of the Vaza-Barris River alluvial plain record with the alluvial-coastal plain subsurface record. We used digital elevation models, satellite imagery, cores drill description, high-resolution seismic data, optical luminescence, and AMS 14C dating of alluvial terraces Five terrace levels, in the upstream provinces, and three terrace levels in the Coastal-alluvial province were identified. In the continental margin adjacent to the Vaza-Barris river-mouth, incised-valleys in the coastal shelf. Morphosedimentary proxies indicate that periods of aggradation and incision alternated during the late Quaternary due to different inland and eustatic dominant factors. We also estimate that the estuary stored a sediment fill of approximately ∼55 m since the late Pleistocene,. Thus, climate change and sea-level variations differentially controlled the fluvial response and the morphology of the adjacent continental margin along the fluvial system. The decoupled accumulation/erosion upstream-downstream patterns can be used as a model to be tested in fluvial systems of the passive margin of the Brazilian Northeast.

Sedimentary records of palaeofloods during the late Holocene along the lower Yellow River, China: A comprehensive study based on multi-proxy

In this paper we propose a new super-comprehensive proxy that integrates the sedimentary rhythm indicators of grain size, black carbon, anthropogenic elements, and pollen for the division of alluvial sedimentary rhythms suitable for use on sediments that have or have not been disturbed by past human activity. The new proxy was applied in the analysis of sedimentary records from two boreholes (identified as JM and SZ) in the Kaifeng area of the lower Yellow River, an area that has received less research attention in terms of flood events and sedimentary records compared to its middle and upper reaches. From this analysis, flood events that occurred in the lower Yellow River since the late Holocene were reconstructed. The results suggest there are 15 and 14 sedimentary rhythms in the cores of JM and SZ, respectively. Based on historical documents, archaeological excavation data from the vicinity of the core sites, and AMS14C dating, we established the chronological framework of sedimentary rhythms in both JM and SZ cores. Using this information, we then reconstructed six Yellow River flood events impacting Kaifeng that occurred after the Warring States period in the years 225 BCE, 1387 CE, 1399 CE, 1461 CE, 1642 CE and 1841 CE. Among the six flood events, except for the flood of 225 BCE which was directly caused by human factors, the rest were caused by natural factors, mainly from prevailing climatic conditions but superimposed by human activities. The research results, therefore, can provide a scientific basis for flood prediction, prevention and risk assessment in the Yellow River Basin under the background of global change, and also provide support for clarifying the relationship between regional climate background and human activities in abnormal flood events.

Технологические и культурные традиции гончарства в среднем неолите Байкало-­Енисейской Сибири

Introduction. The lack of known Middle Neolithic burial complexes in Baikal-Yenisei Siberia makes pottery finds from archaeological sites a key source to explore the cultural and historical situation in the region. According to AMS 14C-dates in the range of ~6,8–6,3 ka cal BP in the territory of Baikal-Yenisei Siberia, two types of ceramics are widespread — Posolsk and Ust-Belaya types. Goals. The study seeks to identify technological and cultural traditions of Middle Neolithic pottery. Materials and methods. The work examines Ust-Belaya and Posolsk type pottery samples from fifteen excavated sites of Baikal-Yenisei Siberia. The paper describes morphological and decorative patterns inherent thereto, provides technical and technological analyses following the methodology of A. Bobrinsky. The molding masses of eighteen Ust-Belaya type vessels and sixteen Posolsk type vessels have been studied with the aid of a binocular microscope. Results. In all cases, ferruginous sandy clay containing quartz sand had served as initial plastic raw material. Molding masses are characterized mainly by an unmixed one-component composition without artificial additives. In two cases, quartz grus has been identified, in another there are traces of organic matter (possibly added intentionally). Vessels of the Posolsk type have closed paraboloid forms with a weak profiling of the upper part and a sharpened bottom. The ornament is localized in the upper part of the vessel and is represented by horizontal ‘receding stick’ rows or drawn lines. The composition below ends with separate shapes, such as triangles or short vertical lines. The rim is decorated with prints of a comb stamp and has a line of round holes which is located over the line made by stick through drawing or receding techniques. The study of molding masses of sixteen Posolsk vessels demonstrates an unmixed one-component composition. In all cases, ferruginous sandy clay had been used as initial plastic raw material. The analysis of the modeling features of Middle Neolithic ceramics makes it possible to formulate hypothetical production programs of theirs. To check the latter, experiments were carried out to model the Ust-Belaya and Posolsk types of vessels. Technical and technological analyses, experiments conducted, and comparisons of models with archaeological vessels reveal technological traditions generally characteristic of Middle Neolithic pottery, such as the method of zonal patchwork modeling in combination with walls knocking out techniques, as well as the use of other vessels as base forms. So, Ust-Belaya vessels could have been completely made on such base forms, while upper parts of Posolsk vessels were profiled after removal from such forms. Knocking out tools for Posolsk ceramics included cord and carved shovels, and for Ust-Belaya type — smooth shovels sometimes wrapped with a woven net. Design patterns of the rim are also different. Conclusions. For the preparatory stage of Middle Neolithic ceramics production, there was a stable tradition of using local sandy clays without additives. The modeling principles common for the two types, along with the absence of flat-bottomed forms, reflect the same level of technological development and similar ideas about the making and functions of vessels, which does not necessarily indicate any ethnocultural closeness of culture bearers. Different traditions of morphology, techniques and decoration indicate that the pottery types belong to different populations. In Posolsk ceramics, there are autochthonous features bringing it closer to the Early Neolithic Khaita pottery. Ceramics of the Ust-Belaya type has no visible origins in the Early Neolithic of the region, which indicates its non-local origin. In addition, the materials of the campsites indicate that the bearers of these traditions had tended to choose different habitats.

Технологические и культурные традиции гончарства в среднем неолите Байкало-­Енисейской Сибири

Introduction. The lack of known Middle Neolithic burial complexes in Baikal-Yenisei Siberia makes pottery finds from archaeological sites a key source to explore the cultural and historical situation in the region. According to AMS 14C-dates in the range of ~6,8–6,3 ka cal BP in the territory of Baikal-Yenisei Siberia, two types of ceramics are widespread — Posolsk and Ust-Belaya types. Goals. The study seeks to identify technological and cultural traditions of Middle Neolithic pottery. Materials and methods. The work examines Ust-Belaya and Posolsk type pottery samples from fifteen excavated sites of Baikal-Yenisei Siberia. The paper describes morphological and decorative patterns inherent thereto, provides technical and technological analyses following the methodology of A. Bobrinsky. The molding masses of eighteen Ust-Belaya type vessels and sixteen Posolsk type vessels have been studied with the aid of a binocular microscope. Results. In all cases, ferruginous sandy clay containing quartz sand had served as initial plastic raw material. Molding masses are characterized mainly by an unmixed one-component composition without artificial additives. In two cases, quartz grus has been identified, in another there are traces of organic matter (possibly added intentionally). Vessels of the Posolsk type have closed paraboloid forms with a weak profiling of the upper part and a sharpened bottom. The ornament is localized in the upper part of the vessel and is represented by horizontal ‘receding stick’ rows or drawn lines. The composition below ends with separate shapes, such as triangles or short vertical lines. The rim is decorated with prints of a comb stamp and has a line of round holes which is located over the line made by stick through drawing or receding techniques. The study of molding masses of sixteen Posolsk vessels demonstrates an unmixed one-component composition. In all cases, ferruginous sandy clay had been used as initial plastic raw material. The analysis of the modeling features of Middle Neolithic ceramics makes it possible to formulate hypothetical production programs of theirs. To check the latter, experiments were carried out to model the Ust-Belaya and Posolsk types of vessels. Technical and technological analyses, experiments conducted, and comparisons of models with archaeological vessels reveal technological traditions generally characteristic of Middle Neolithic pottery, such as the method of zonal patchwork modeling in combination with walls knocking out techniques, as well as the use of other vessels as base forms. So, Ust-Belaya vessels could have been completely made on such base forms, while upper parts of Posolsk vessels were profiled after removal from such forms. Knocking out tools for Posolsk ceramics included cord and carved shovels, and for Ust-Belaya type — smooth shovels sometimes wrapped with a woven net. Design patterns of the rim are also different. Conclusions. For the preparatory stage of Middle Neolithic ceramics production, there was a stable tradition of using local sandy clays without additives. The modeling principles common for the two types, along with the absence of flat-bottomed forms, reflect the same level of technological development and similar ideas about the making and functions of vessels, which does not necessarily indicate any ethnocultural closeness of culture bearers. Different traditions of morphology, techniques and decoration indicate that the pottery types belong to different populations. In Posolsk ceramics, there are autochthonous features bringing it closer to the Early Neolithic Khaita pottery. Ceramics of the Ust-Belaya type has no visible origins in the Early Neolithic of the region, which indicates its non-local origin. In addition, the materials of the campsites indicate that the bearers of these traditions had tended to choose different habitats.

The alteration from agricultural to nomadic regimes resulted in human livelihood transformation in North-Central China during the 12th century: The archaeobotanical evidence.

Human livelihoods provided a crucial economic foundation for social development in ancient times and were influenced by various factors including environmental change, agricultural origin and intensification, as well as long-distance exchange and culinary tradition. The effect of geopolitical change on human subsistence, especially the shifts between agricultural and nomadic regimes, has not been well understood due to the absence of detailed historical records and archaeological evidence. During the 12th century, the control of the Zhengding area in Hebei Province of north-central China changed from the Northern Song (960–1127 CE) to the Jurchen Jin Dynasty (Jin Dynasty; 1115–1234 CE). Recent excavation of the Zhengding Kaiyuan Temple South (ZKS) site in the area provides a rare opportunity to study human livelihood transformation in relation to geopolitical change. In total, 21,588 charred crop caryopses including foxtail millet, wheat, broomcorn millet, hulled barley, and rice, and other carbonized remains including 55.15 g of boiled foxtail millet and 353.5 g of foxtail millet caryopses were identified, and nine AMS 14C dates of crop remains were obtained from the Northern Song and Jin layers at the ZKS site. This revealed that the dominant plant subsistence transformed from wheat to foxtail millet during the change from the Northern Song to the Jin Dynasties in Zhengding area. By comparing with historical documents and paleoclimate records, we propose that this abnormal shift of primary staple food from the relatively high-yield wheat to low-yield foxtail millet was induced by the traditional dietary preference for foxtail millet in the nomadic Jin society. The Jin government levied foxtail millet as taxation and promoted massive immigration from northeastern China to north-central China to consolidate their rule, which resulted in the adoption of foxtail millet as the most important crop in Zhengding area. The advantage for the cultivation of this frost-sensitive crop in north-central China over northeast China was probably enhanced by notable cold events during the 12th century, while the primary influencing factor for the transformation of human livelihoods in north-central China during that period was geopolitics rather than climate change.