Cal Ky BP Research Articles

Cultural Dynamics in the Levantine Upper Paleolithic, ca. 40–33 ky BP: Insights Based on Recent Advances in the Study of the Levantine Aurignacian, the Arkov-Divshon, and the Atlitian

The chrono-cultural sequence of the Levantine Upper Paleolithic went through several major revisions during approximately a century of focused research, each revision contributing to shedding light on the mosaic of cultural entities and the complex social and cultural dynamics composing the Levantine Upper Paleolithic. The current state of research suggests the co-inhabitance of two cultural groups: the Early Ahmarian and the Levantine Aurignacian. Two other cultural entities, the Arkov-Divshon and the Atlitian, are regarded as younger manifestations and were tentatively suggested to relate to the Levantine Aurignacian. This paper presents a research synthesis of two case studies: Manot Cave, located in western Galilee, Israel, and Nahal Rahaf 2 Rockshelter in the Judean Desert. The application of high-resolution excavation methods, alongside detailed documentation of the stratigraphy and site-formation processes and wide-scale radiocarbon-based absolute dating, marked these sites as ideal for chrono-cultural study through the analyses of flint industries. The results indicate a clear distinction between the Levantine Aurignacian and the Arkov-Divshon/Atlitian industries and a chronological overlap between the Arkov-Divshon, Levantine Aurignacian, and possibly with the Early Ahmarian. Subsequently, we suggest another revision of the currently accepted chrono-cultural model: not two, but at least three cultural entities co-inhabited the Levant at ca. 40–30 ky cal BP. This study further suggests an evolvement of the Atlitian flint industries from the Arkov-Divshon and stresses the foreign cultural features of the Levantine Aurignacian. These results were used to construct an updated model of migration and possible interaction patterns.

Revisiting macromammal exploitation in the Spanish Cantabrian region during the lower Magdalenian (ca. 20-17 ky cal BP)

Understanding the ways in which human groups use the environment for their survival is one of the main fields of study in Prehistory. Subsistence strategies, understood as the set of techniques, processes and activities through which human groups organise the tasks related to their survival, are a fundamental element for understanding the economic and sociocultural processes derived from these practices in the past. In this sense, archaeozoological and taphonomic studies are the main tool to reconstruct the ways in which our ancestors acquired, processed, consumed, and managed meat resources for their survival. In this research we examine the ways in which hunter-gatherer groups in the Spanish Cantabrian region exploited ungulates through a palaeoecological and palaeoeconomic analysis of a total of 32 archaeological levels at 19 sites dated between 20 and 17 ky cal BP. To this end, through research on faunal resources in this region, we will address the ways in which prey was acquired and transported, the age ranges, the seasonality of the captures and the nutritional energy contribution to the diet of the human groups, taking into account the cost of acquiring them, thus generating an updated view of subsistence strategies in the Cantabrian region.

Development and physical characteristics of the Irish shelf-edge Macnas Mounds, Porcupine Seabight, NE Atlantic

Modern cold-water corals (CWCs) occur in a wide range of water depths, with Desmophyllum pertusum being one of the most common species. Pleistocene, Holocene, and modern coral mound formation by living CWC reefs have previously been described in the Porcupine Seabight from water depths greater than 700 m in the vicinity of the transitional zone between the Eastern North Atlantic Water and Mediterranean Outflow Water. Here we document occurrence of fossil corals retrieved from two cores at 370 m depth in the Macnas Mounds, a relatively shallow occurrence for mounds on the Irish shelf-edge. Both cores feature D. pertusum restricted to the upper two metres, immediately overlying an erosive surface and a coeval major down-core change in grain size from sand to mud. Radiocarbon dating of coral specimens indicates the CWC mounds initiated 7.82 Cal ky BP. Our study unequivocally documents the existence of Holocene shelf-edge coral mounds in the eastern Porcupine Seabight and highlights the possibility of other occurrences of CWCs in similar settings elsewhere in the northeast Atlantic. Given that no living CWCs were encountered in the study area, we suggest that the area previously experienced more favourable conditions for CWC mound initiation and development along the shelf-edge margin, possibly due to differing conditions in the European Slope Current which flows northward along the continental slope from south of the Porcupine Bank to the Faroe-Shetland Channel.Graphical

Sequence stratigraphy and evolution of the southern Central Vietnam Shelf during Late Pleistocene-Holocene

The central Vietnam continental shelf is located on the western margin of the East Vietnam Sea (South China Sea). This study provides new findings regarding the Late Pleistocene-Holocene evolution of the southern central Vietnam shelf off Binh Dinh province using high-resolution seismic profiles and sediment cores. The study found that the Late Pleistocene-Holocene sequence stratigraphic model of the study area can be divided into three systems tracts: the regressive systems tract (RST), the transgressive systems tract (TST), and the highstand systems tract (HST). The RST is the oldest and thickest of the three systems tracts and is characterized by forced regressive and lowstand deposits. These deposits likely formed between the Marine Isotope Stages (MIS) 5e highstand and the Last Glacial Maximum (LGM) termination. The RST is well-preserved at water depths deeper than 60 m and has a maximum thickness of about 40 m. The TST is the middle systems tract and was likely deposited during a postglacial transgressive period, from the LGM lowstand termination to around 8 cal ky BP. The TST is thickest in shallow water depths in the southern part of the study area and within incised-valley systems. The HST is the youngest of the three systems tracts and is dominated by thick mud clinoforms that prograde onto the shelf following mid-Holocene sea-level highstand until the present day. The HST was primarily deposited in shallow water depths of 0–50 m and decreases in thickness towards the outer shelf, ending at a water depth of around 80 m.The study also found that Late Pleistocene-Holocene relative sea-level change is the main factor controlling the overall stratigraphic organization of units on the study area. The presence of the beach-ridge structure at a water depth of approximately 140 m below the modern sea level in the southernmost part of the study area suggests that the region experienced a sea-level lowstand in the past. This lowstand was likely a result of subsidence due to a high sedimentation rate. This discovery is consistent with earlier studies conducted on the central Vietnam shelf. There are similarities in the deposition of Late Pleistocene-Holocene deposits between Binh Dinh and other shelves worldwide, indicating that there may be consistent controlling factors that govern the geological history of these regions. However, the thickness and distribution of deposits in the study area may be different due to local factors that interacted to shape the area differently than others.

Surf and turf. Animal resources in the human diet in Cantabrian Spain during the Mesolithic (11.5 – 7.5 Ky cal. BP)

The beginning of the Holocene involved a series of climatic and environmental changes that affected the ways of life of the last hunter-gatherers. In the case of the Spanish Cantabrian region, these changes transformed the material culture and the way human groups interacted with the environment and, therefore, the subsistence strategies of the end of the Upper Pleistocene. In terms of the use of faunal resources, this period was characterised by an increase in the exploitation of coastal resources, mainly molluscs, but also crustaceans and echinoderms, which make up the so-called “shell middens”, while at the same time the percentage of macromammals was reduced and animals considered to have a “low energy range” were introduced into the diet. In this paper we assess the role played by each of these animal resources in the subsistence of Mesolithic human groups, determining their nutritional contribution and establishing a prey ranking based on the caloric intake of each resource. For this purpose, we collected archaeofaunal data from 14 sites from recent archaeological excavations with levels dated between ca. 11.5 and 7.5 ky cal BP in which the consumption of vertebrates and invertebrates is documented. At each of these sites we analysed diversity, homogeneity and species richness using Simpson's and Shannon's indexes, as well as the effective numbers of species for terrestrial and coastal resources, assessing the relationship between the two. With the palaeoecological and palaeoeconomic data from these archaeological sites (most of them located in caves), we estimate the weight that the different animal resources consumed by the last hunter-gatherer communities of the Cantabrian region had in their diet.

Climatic control on the Holocene hydrology of a playa-lake system in the western Mediterranean

Evaporitic lakes such as playa-lakes are characteristic of many arid regions and are unique environments with respect to fauna and flora, while being very vulnerable to climate and environmental fluctuations and threatened by the current global change scenario. Water balance oscillations in these systems can trigger the precipitation or dissolution of different evaporitic minerals, negatively impacting local biodiversity and economic activities. Here, we study the sedimentary record of a small saline pond from a playa-lake complex in southwestern Iberia in order to reconstruct the paleohydrological evolution of this area and assess potential anthropogenic disturbances. The different proxies studied in the ∼11.9 ky old sedimentary record of the Laguna de la Ballestera suggest that the greatest lake extension and the highest water levels occurred during the Early Holocene, pointing to the wettest period of the record. Climate transitioned towards more arid conditions during the Middle Holocene, and even more dramatically during the Late Holocene. In this last stage the wetland surface and the water level largely diminished and gypsum precipitation gradually increased pointing towards a negative precipitation/evapotranspiration balance and lowest water levels. Summer desiccation likely occurred under this scenario, especially after ∼1.0–0.9 cal ky BP coeval with the Medieval Climate Anomaly, when gypsum content started to rise abruptly. However, this significant gypsum precipitation was only associated with a massive drop in the siliciclastic content and scarce carbonates (dolomite and calcite) during the last ∼400 years. This evidence suggests a shift from a (semi) permanent to a temporal/seasonal hydrological regime. The environmental evolution of this wetland responded to the general climatic evolution of the western Mediterranean during the Holocene, being mostly controlled by changes in insolation. Our data also show that the environmental response of the studied wetland to natural climate variations was only significantly disturbed by human activities since the 20th century, especially in the second half of the century, deduced by abrupt fluctuations in the siliciclastic, gypsum and organic content in the sediments, as well as by the enhanced sedimentary accumulation rates, probably as a response to changes in the hydroperiod of the lake and in the catchment land use.

Climatic and hydrological variability as a driver of the Lake Gościąż biota during the Younger Dryas

The Younger Dryas (YD) is a roughly 1,100-year cold period marking the end of the last glaciation. Climate modelling for northern Europe indicates high summer temperatures and strong continentality. In eastern Europe, the scale of temperature variation and its influence on ecosystems is weakly recognised. Here, we present a multi-proxy reconstruction of YD conditions from Lake Gościąż (central Poland). The decadal-resolution analysis of its annually varved sediments indicates an initial decrease in Chironomidae-inferred mean July air temperature followed by steady warming. The pollen-inferred winter-to-summer temperature amplitude and annual precipitation is highest at the Allerød/YD transition and the early YD (ca. 12.7–12.4 ky cal BP) and YD/Holocene (11.7–11.4 ka cal BP) transition. Temperature and precipitation were the main reasons for lake level fluctuations as reflected in the planktonic/littoral Cladocera ratio. The lake’s diatom-inferred total phosphorus decreased with increasing summer temperature from about mid YD. Windy conditions in the early YD until ∼12.3 ka cal BP caused water mixing and a short-lived/temporary increase in nutrient availability for phytoplankton. The Chironomidae-inferred summer temperature and pollen inferred summer temperature, winter temperature and annual precipitation herein are one of only a few in eastern Europe conducted with such high resolution.

Chronostratigraphy of Jerzmanowician. New data from Koziarnia Cave, Poland

Lincombian-Ranisian-Jerzmanowician (LRJ) industries are extremely scarce in Central Europe. Therefore, each LRJ site is of great importance. One of them is Koziarnia Cave in Poland situated eastwards relative to other LRJ sites. Our investigations of this cave provided new chronostratigraphic data for the LRJ industries. A detail debitage analysis recognised the ventral thinning chips and enabled identification of the LRJ assemblage-containing stratum. Besides the LRJ assemblage, strata with traces of Late Middle Palaeolithic and Early Gravettian occupation were found at the site. The radiocarbon dates of Koziarnia samples show that the archaeological settlement represents one of the oldest Gravettian stays north to the Carpathians. Moreover, these dates demonstrate that humans and cave bears had alternately occupied the cave. Additionally, the radiocarbon dates indicate relatively young chronology of the Jerzmanowician occupation in Koziarnia Cave (ca. 39-36 ky calBP). The results suggest the long chronology of the LRJ technocomplex, exceeding the Campanian Ignimbrite event.

Collaboration, not competition: A geoarchaeological approach to the social context of the earliest pottery

The invention of pottery by Palaeolithic hunter-gatherer groups is often associated with the development or introduction of new social practices. While some studies connect pottery, especially in glacial environments, to broadening of hunter-gatherer subsistence strategies, in Eastern Asia a number of studies suggests that the earliest pottery is connected to the appearance of hierarchy through self-aggrandizement and feasting in trans-egalitarian societies. In this paper, we assess this hypothesis using the early pottery site of Yuchanyan (China) as a case study. Geoarchaeological studies at Yuchanyan have confirmed the hunter-gatherer context of the pottery (18.3 cal ky BP) and also reconstructed the site’s stratigraphy and human occupation of the cave. Here we reconstruct the pyrotechnology and cooking practices at Yuchanyan with the goal of better understanding labor commitments. We argue that humans used several techniques to increase cooking efficiency to make bone soup and render grease. This multifaceted activity would have required large-scale efforts and collaboration, and consequently, we argue that the end product could not have been monopolized by a single individual. If feasting did in fact take place, it was probably yet another activity inducing group cohesion.

Combining Bayesian age models and genetics to investigate population dynamics and extinction of the last mammoths in northern Siberia

To understand the causes and implications of an extinction event, detailed information is necessary. However, this can be challenging when working with poorly resolved paleontological data sets. One approach to increase the data resolution is by combining different methods. In this study, we used both radiocarbon and genetic data to reconstruct the population history and extinction dynamics of the woolly mammoth in northern Siberia. We generated 88 new radiocarbon dates and combined these with previously published dates from 626 specimens to construct Bayesian age models. These models show that mammoths disappeared on the eastern Siberian mainland before the onset of the Younger Dryas (12.9–11.7 ky cal BP). Mammoths did however persist in the northernmost parts of central and western Siberia until the early Holocene. Further genetic results of 131 high quality mitogenomes, including 22 new mitogenomes generated in this study, support the hypothesis that mammoths from, or closely related to, a central and/or west- Siberian population recolonized Wrangel Island over the now submerged northern Siberian plains. As mammoths became trapped on the island due to rising sea levels, they lived another ca. 6000 years on Wrangel Island before eventually going extinct ca. 4000 years ago.

Exploring late Paleolithic and Mesolithic diet in the Eastern Alpine region of Italy through multiple proxies.

ObjectivesThe analysis of prehistoric human dietary habits is key for understanding the effects of paleoenvironmental changes on the evolution of cultural and social human behaviors. In this study, we compare results from zooarchaeological, stable isotope and dental calculus analyses as well as lower second molar macrowear patterns to gain a broader understanding of the diet of three individuals who lived between the end of the Late Pleistocene and the Early Holocene (ca., 17–8 ky cal BP) in the Eastern Alpine region of Italy.Materials and methodsWe analyze individuals buried at the sites of Riparo Tagliente (Verona), Riparo Villabruna, and Mondeval de Sora (Belluno). The three burials provide a unique dataset for diachronically exploring the influence of climatic changes on human subsistence strategies.ResultsIsotopic results indicate that all individuals likely relied on both terrestrial and freshwater animal proteins. Even though dental calculus analysis was, in part, hindered by the amount of mineral deposit available on the teeth, tooth macrowear study suggests that the dietary habits of the individuals included plant foods. Moreover, differences in macrowear patterns of lower second molars have been documented between Neanderthals and modern humans in the present sample, due to a prevalence of Buccal wear among the former as opposed to higher values of Lingual wear in modern human teeth.DiscussionIsotopic analyses have emphasized the contribution of animal proteins in the diet of the three foragers from the Eastern Alpine region. The possible intake of carbohydrate‐rich plant foods, suggested by the retrieval of plant remains in dental calculus, is supported by the signal of macrowear analysis. Moreover, the latter method indicates that the distribution of macrowear in lower second molars (M2s) allows us to discriminate between Neanderthals and modern humans within the present reference sample. Overall, our results show these three prehistoric hunter‐gatherers were well adapted to the environment in which they lived exploiting many natural resources.

Investigating the exploitation pattern of a newly established species, the case of the Late-Glacial roe deer (Capreolus capreolus) at La Fru (Savoie, France)

The Late-Glacial period offers a key window into the expansion of temperate species from southern refugia towards northern areas and the impact of faunal change on hunting strategies. In the Jura and in the Alps, the arrival of red deer and the withdrawal of reindeer are coeval with the warming of the GI-1e. Very little is known about roe deer, however. A high-resolution study of the rich archaeofauna from the Early Azilian occupation at the Northern Alpine site of La Fru provides data on the habitat and exploitation of roe deer. Roe deer populations were already established in the region in the early Bolling (~GI-1e), as is shown by the earliest radiocarbon date of roe deer bones (14.7–14.3 ky cal BP, 1σ). This is the earliest post-Last Glacial Maximum evidence of this species in northern France. The specimens from the site show the highest δ15N values among the deer species present in the areas. This is probably linked to the roe deer’s selective foraging of highly nutritious vegetation already available in the open habitat at that time. Our zooarchaeological study shows that roe deer was a key resource at La Fru and was intensively hunted between May and September. The mortality profile indicates a “deliberate” targeting of inexperienced subadults and weaker older animals. These new data provide further evidence that there was both a reorganization of the animal environment and a reorientation of hunting on red deer and roe deer associated with the Early Azilian culture during the Bolling chronozone.

Holocene evolution and Anthropocene destruction of the Krishna Delta on the east coast of India: Delta lobe shifts, human impacts, and sea-level history

The Holocene evolution of the Krishna Delta was inferred using landform characteristics and 11 sediment cores with 59 Accelerator Mass Spectrometry 14C dates. The landform assemblages in a 5880 km2 area of the Krishna Delta indicate an upper (landward) river-built fluvial plain and a lower (seaward) marine-built beach-ridge plain. Holocene sediment unconformably overlying a Pleistocene basement consists of 11 sedimentary facies, mainly shallowing-upward and deltaic succession. Sea level indicators such as the basal mangrove peat layers above the Pleistocene basement and the foreshore sediments indicate that the sea level rose from −9 m to −3 m during 8.3–6.3 cal ky BP, and stabilised at the present level around 5 cal ky BP. The 3539 km2 area of the Krishna Delta beach-ridge plain developed in five major stages during the last 6 cal ky, with distinct lateral and seaward migration of delta lobes (depocentre shifts). Delta progradation accelerated in the last 500 years, forming an out-building lobate delta. However, predominant erosion along the sediment-starved coast during the past five decades, due to impoundment of riverine inputs at the burgeoning upstream dams, has pushed the Krishna Delta into a persistent destruction phase.

Source to sink reconstruction of a Holocene Fjord‐infill: Depositional patterns, suspended sediment yields, wind‐induced circulation patterns and trapping efficiency for Lake Strynevatnet, inner Nordfjord, Norway

AbstractThis paper reconstructs the sedimentation volumes and patterns, suspended sediment yields, wind‐induced circulation patterns and sediment trapping efficiency of Lake Strynevatnet, western Norway as an integrated source to sink system. The lake became deglaciated ca 11 ky cal bp, with glacio‐isostatic uplift isolating the basin from the nearby fjord (Nordfjord) ca 9.2 ky cal bp. Based on geophysical data collected in 2010, the upper 15–20 m of Holocene sediment accumulation in the lake was mapped. A sediment body in the centre of the lake indicates a depositional mechanism dominated by suspension sedimentation. The source of this sediment is associated with the adjacent glaciated catchments westward of the lake. Three seismic units were identified based on seismic facies generating an evolutionary model utilizing three depositional units (U1, U2 and U3), in which unit U2 represents the Storegga tsunami event. Unit U3 is further divided into three subunits; U3a, U3b and U3c based on their spatial continuity and subtle downlapping and onlapping relationships. The degree to which wind conditions could have affected the lake depositional patterns were studied utilizing an open‐source coupled hydrodynamic and sediment transport model. The results show that fluvial discharge alone is incapable of generating a circulation pattern in the lake currents. Suspended sediment concentrations in the lake are highest for strong winds. Modelled sediment accumulation on the lake floor shows that mild or absent winds lead to a proximal to distal sediment thickness trend, while strong winds result in uniform sediment thickness. Based on this it is argued that the thickness trends of seismic subunits U3a‐c are related to a variable palaeowind climate. As such, seismic data of lake infills, in combination with numerical modelling, may provide valuable palaeoclimatic information on wind patterns.

The earliest double dog deposit in the Palaeolithic record: The case of the Azilian level of Grotte‐abri du Moulin (Troubat, France)

AbstractIt is now largely accepted that the wolf was the first animal to be domesticated during Pleistocene time. Although the exact timing of this event is still the subject of considerable debate, it is generally agreed upon that dogs lived side‐by‐side with humans for at least the last 15,000 years. Recent discoveries from the “Grotte‐abri du Moulin” (Troubat, France) provide crucial new information as to our understanding of the relationships between humans and dogs during prehistory. The site produced a deep stratigraphic sequence demonstrating that the cave was occupied from the Middle Magdalenian (ca. 17.5 ky cal BP) to the Sauveterrian period (ca. 9.5 ky cal BP). Faunal remains from layer 6, attributed to the Azilian culture, included a small Canis. The biometric study of these remains is fully consistent with their attribution to the dog (Canis familiaris). A total of 147 dog remains were isolated and represent a minimum of two individuals. These remains were recovered from a restricted space, and several skeletal elements remained in anatomical connection or in loose connection. The most labile elements were only slightly dispersed, and there is no evidence of human or carnivore modification on these bones. Direct radiocarbon dates obtained from a complete tibia demonstrate the dog remains to be contemporaneous with the Azilian occupation of the cave. The Grotte‐abri du Moulin evidence represents, therefore, the earliest known occurrence of an intentional double dog deposit and evidence for a particularly close relationship between Azilian groups and their dogs.

Lithic production in the centre and south of the Iberian Mediterranean region (Spain) throughout the Pleistocene–Holocene transition (14.5–10.5 ky cal BP)

For the first time we compare lithic production systems from the three archaeological phases identified in the Iberian Mediterranean region between 14.5 and 10.5 ky cal BP: final Magdalenian, microlaminar Epipalaeolithic and sauveterroid Epipalaeolithic. These phases coincided with rapid palaeoenvironmental changes, whose effects on a peripheral region of southern Europe require a regional analysis. The basic blanks used in all three phases were blades and bladelets and there is considerable typological homogeneity.The results obtained in the study of the three phases identified at Coves de Santa Maira provide new grounds for discussion about lithic production systems during the Pleistocene–Holocene transition. Through this study it has been possible to establish the local and regional origin of the raw materials. At the same time, it has been observed that the standardisation typical of the classic Magdalenian decreased and there was an increase in more flexible and opportunistic chaînes opératoires, in addition to the absence of some stone points that are characteristic of more northern facies and cultures. The results have made it possible to contextualise the known data for the central–southern region of the Iberian Peninsula, allowing us to draw up a regional model of lithic production systems and assess the continuity or break between the three phases, as well as providing new possibilities to investigate the relationship with other facies and regional groups.

Holocene environmental changes in northern Poland recorded in alkaline spring-fed fen deposits – A multi-proxy approach

Spring-fed fen deposits (peat-tufa sequences) from northern Poland were investigated for Holocene environmental reconstruction (climate and hydrology) using multi-proxy analysis (lithofacies, molluscs, pollen, plant macrofossils, geochemistry, and stable oxygen- and carbon-isotopes). The main aims of these studies were: (1) comparison of several similar sites with the same type of groundwater supply and sedimentation on a widespread space scale, (2) detailed reconstruction of their long-term development, assessing their sensitivity to climate change, (3) verification of the synchronicity of the record of different proxies in distant sites in the context of Holocene climate changes in relation to specific well-known global and/or regional climate events (so-called Bond events), and (4) discussion on permafrost degradation as a driver of spring-fed fens development.Based on our palaeogeographical data, we have distinguished an asynchronicity of the beginning of the development of spring-fed fens in the eastern and western parts of the studied region that is associated with different times of ascending groundwater supply unblocking after complete permafrost degradation. Therein, asynchronicity of permafrost degradation was brought about by multiple climatic, geological and structural conditions. Our results also indicate significant differences in the trends of succession (ecological and lithological) caused by the geographical location of the studied sites. Asynchronicity of the occurrence of wet and dry phases, as well as significant differences in their duration were noted. This depended upon the influence of oceanic (western part) or continental climates (eastern part). Warm and humid oceanic climate promoted the domination and longer duration of wet phases (especially in the Eo- and early Mesoholocene), while the harsh continental climate promoted the more frequent occurrence of dry phases, with short episodes of increased humidity. From the middle Mesoholocene, this marked regional diversification becomes less pronounced. Results also allowed for the recognition of several palaeoclimatic events on a regional scale. Four main cold episodes (Bond events 8–5): during LG/H transition (11.5 ky cal BP), Eo- (∼10.25 ky cal BP, ∼9.4 ky cal BP) and at the beginning of the Mesoholocene (∼8.2 ky cal BP) are well-documented by multiple proxies at all study sites. Other cold episodes (Bond events 4–0) are slightly less documented and are not clear for interpretation. The results of our study demonstrate the importance of spring-fed fen deposits for detailed palaeoenvironmental reconstruction on a regional scale.

Improving North Atlantic Marine Core Chronologies Using 230Th Normalization.

Producing independent and accurate chronologies for marine sediments is a prerequisite to understand the sequence of millennial‐scale events and reveal potential temporal offsets between marine and continental records, or between different marine records, possibly from different regions. The last 40 ky is a generally well‐constrained period since radiocarbon (14C) can be used as an absolute dating tool. However, in the northern North Atlantic, calendar ages cannot be directly derived from 14C ages, due to temporal and spatial variations of surface reservoir ages. Alternatively, chronologies can be derived by aligning Greenland ice‐core time series with marine surface records. Yet this approach suffers from the lack of clearly defined climatic events between 14.7 and 23.3 cal ky BP (hereafter ka), a crucial period encompassing Heinrich Stadial 1 and the onset of the last deglaciation. In this study, (i) we assess the benefits of 230Th normalization to refine the sedimentation history between surface temperature alignment tie points and (ii) revisit the chronologies of three North Atlantic marine records. Our study supports the contention that the marked increase in the Greenland Ca2+ record at 17.48 ka ± 0.21 ky (1σ) occurred within dating uncertainty of sea surface temperature cooling in the North Atlantic at the onset of Heinrich Stadial 1. This sharp feature might be useful for future chronostratigraphic alignments to remedy the lack of chronological constraint between 14.7 and 23.3 ka for North Atlantic marine records that are subject to large changes in 14C surface reservoir age.

REEs and Sr-Nd isotope variations in a 20 ky-sediment core from the middle Okinawa Trough, East China Sea: An in-depth provenance analysis of siliciclastic components

We analyzed rare earth elements (REEs) and SrNd isotope compositions of siliciclastic components in a sediment core from the middle Okinawa Trough (OT), to elucidate spatiotemporal variations in the sediment provenance, and their underlying mechanisms for the last 20 ky. Our results show that the trough deposits were characterized by different proportions of Changjiang- and Taiwan-derived (especially, the western rivers) sediments over time, from which we infer dramatic changes in sea-level, intensity of the Kuroshio Current (KC) inflow, and the East Asian monsoon since the last glacial maximum (LGM). In contrast to previous studies, the sea-level lowstand proximity of the paleo-Changjiang to the middle OT, and the contemporaneous enhancement of the East Asian winter monsoon (EAWM) may have played pivotal roles in supplying terrigenous inputs and forming middle OT deposits during the last glacial period, whereas the paleo-Huanghe was of lesser importance. After the early Holocene (especially the late Holocene cold period between ~4.8 and ~2.7 cal ky BP), a remarkable shift in the combined records of REEs and Nd isotopes reveals a causal link between variations in the Taiwan source and the KC inflow, coupled with climate changes in the East China Sea (ECS). This study suggests that SrNd isotope compositions and REEs are useful proxies for understanding the links between river development and paleoenvironmental/paleoclimatic changes in East Asian marginal regions.

Pleistocene landslides and mammoth bone deposits: The case of Dolní Věstonice II, Czech Republic

AbstractThe formation of extensive mammoth bone deposits is a characteristic feature of the large Upper Paleolithic settlements of the Moravian Gravettian (approximately 30 ky cal BP). Some of these were preferentially deposited in moist locations, possibly for reasons of hygiene and conservation. Here, we present a case of a mammoth bone deposit located in a side gully below the Dolní Věstonice II settlement, where an earlier a Pleistocene landslide temporarily created a shallow water basin. The environmental record is provided by analyses of pollen and mollusks. The structure of the osteological and archaeological assemblages suggests the use of this location as a place for storage, garbage disposal, and related activities. We suggest that the mammoth remains were transported to such places by humans either directly from nearby kill sites, or, after first selection, from the nearby settlement. We also discuss possible facilities for such transport.