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This paper explores how significant are the ecological and climatic variables to influence the stable isotopes of guanacos. Lama guanicoe bone collagen carbon and nitrogen stable isotope ratios are assumed as a macro regional average value in west Argentina, mostly as a baseline to model archaeological human diet. If stable isotopes on mammals reflex ecology and climate, we need to know how those variables influence mammals bone stable isotope ratio. This paper analyses the 13C/12C and 15 N/14N ratio on bone collagen on 122 guanacos from Northwest Patagonia during the Holocene. The results confirm significant variation in both isotopes between Monte and Andean-Patagonian specimens. Guanacos from Monte shows higher δ13C and δ15N than those from Andean-Patagonian. Temporal trends indicate variation through Holocene but this variation is not spatially homogeneous. In this paper we suggest that Medieval Climatic Anomaly had stronger effect in Monte desert than in Patagonia desert, generating driest and/or hottest conditions between 1250 and 600 years BP. Those variations need to be considered to reconstruct human diet at least during the second part of the Holocene. [ABSTRACT FROM AUTHOR]

Modern Arctic Indigenous peoples face many interconnected pressures, not the least of which is anthropogenic climate change, which is emerging as one of the most dramatic drivers of social and economic change in recent memory. In this paper, we investigate whether or not insights into premodern strategies for coping with climate change—and especially the "deeper histories" of traditional ways-of-knowing—can play a useful role in future planning, management and mitigation efforts. We do this in two ways. First, we assess this special issue's 17 archaeological case studies, in order to determine whether they are conducted within a framework that is consistent with approaches to resilience in studies of modern Arctic communities. Second, we focus on three climate-driven challenges faced by Canadian Arctic Inuit: safe travel, food security and food safety. For each, we identify specific ways in which studies of past social-ecological systems intersect with modern climate adaptation. We conclude that since archaeological insights highlight the operation of decision-making processes within long-term culture-adaptive trajectories, they can offer unique insights into the much shorter-term processes currently underway. While we highlight many potential directions for productive collaboration, much more work is required in local and regional settings to demonstrate the full potential of archaeology for future-oriented planning and mitigation efforts. [ABSTRACT FROM AUTHOR]

Living in remote places can strain the adaptive capacities of human settlers. It can also protect communities from external social, political and economic forces. In this paper, we present an archaeological population history of the Kuril Islands. This string of small volcanic islands on the margins of the Northwest Pacific was occupied by maritime hunting, fishing and gathering communities from the mid-Holocene to recent centuries. We bring together (1) 380 new and previously published archaeological radiocarbon dates, (2) a new paleodemographic model based on a radiocarbon-timestamped temporal frequency distribution of archaeological deposits, (3) recently published paleoclimate trends, and (4) recently published archaeological proxy evidence for changes in the extent of social networks. We demonstrate that, over the last two millennia, inhabitants of the Kuril Islands underwent dramatic demographic fluctuations. Explanations of these fluctuations are considered in the context of environmental hazards, social networks and the emergence of an East Asian “World System”, elucidating the tension between local and external adaptive strategies to social and ecological uncertainty. Results suggest that population resilience to local climate and environmental variability was achieved by virtue of social networks that maintained non-local support in times of crisis. Conversely, the expansion of the East Asian political economy into neighboring regions of the southern margin of the Kuril Islands perhaps in conjunction with exposure to epidemic diseases appears to have undermined the adaptive strategies, resulting in an increase in the vulnerability of Kuril populations to environmental fluctuations. [ABSTRACT FROM AUTHOR]

Tham Lod (Pang Mapha district, Mae Hong Son Province) is one of the rockshelters in the limestone karst of north-western Thailand. The site was excavated from 2002 to 2006 under the direction of one of us (R.S.) in the context of The Highland Archeological Project. The stratigraphical sequence of the site provided dates ranging from late Pleistocene (35 ka, TL), to late Holocene (3000 BP). Thousands of lithic and faunal remains occur throughout the sequence; ceramics and metal items appear in the upper layer (Holocene). Noteworthy are the few human burials in the late Pleistocene layers. This paper presents the lithic material from area 2, sectors S20W10 and S21W10, unearthed from the stratigraphic layers 3 to 10 (late Pleistocene). Artefacts are mostly made in locally available grey sandstone, which is overwhelming in all the layers. The lithic assemblage includes a large proportion (2/3) of rock fragments brought to the site and artificially (or thermally?) broken. These are mostly small fragments (<100 mm) while the big fragments are rare and even absent in the middle layers. Flakes are well represented in the Pleistocene upper and middle layers. Cores proper (meant to produce flakes) are extremely rare and tools proper (shaped) are less than 10% of the material, half of them being larger than 100 mm. All of them, the large and the small tools are mainly shaped on cobbles and cobble fragments and mostly with unifacial shaping. Typical sumatraliths, the signature of the Hoabinhian technical traditions, are conspicuous in the middle layers 6 to 4; they are associated with partial sumatraliths (not shaped all around), especially in the layers 6. They are much less in the lower layers and seem to be absent in the bottom layer. Conversely, the cobble tools are almost exclusively choppers in the lower layers 10 to 8. The scrapers are the major type among the small tools and they are quite constant in number throughout the stratigraphy. As some of the artefacts are definitely considered as “Hoabinhian”, the detailed technological study of the lithic industry will help in understanding this “techno-cultural” facies and in tracing how the stone artefacts were manufactured, used, maintained and finally discarded by the hunters–gatherers. Analysis of the whole sequence in Tham Lod aims at reconstructing the technical evolution in the context of the late Pleistocene climatic changes in this part of Eurasia. [ABSTRACT FROM AUTHOR]

The transition from Late Palaeolithic to early Mesolithic cultures is strongly associated with the major environmental and climatic changes occurring with the shift from the Younger Dryas to the Holocene in northern Europe. In this paper, we present an interdisciplinary study combining archaeological and palaeoenvironmental research in an attempt to examine the relationship between environment and culture during this transition. Lundby Mose is a former kettle hole lake in southern Denmark where the earliest Danish human traces of the Holocene were excavated. Two types of bone deposits were found, 1) ritual offerings of worked, marrow-split elk bones and antler and 2) settlement waste with multiple species. These date to the early Holocene and are affiliated to the early Maglemose culture. The modelled 14 C ages suggest that the bones were deposited in four phases. A pollen based palaeoenvironmental reconstruction suggests that the ritual offerings were deposited in an environment of limited, underdeveloped forest with unstable soils and areas of open grassland. The settlement waste deposit is associated with a more developed Preboreal forest type. This forest type was not fully established until c. 11,250 cal BP and if substantiated by further evidence, may be one of the reasons why there are no known early Maglemose/Preboreal settlement sites in southern Scandinavia. [ABSTRACT FROM AUTHOR]

Abstract: This paper highlights results of a multidisciplinary and multi-analytical study of Holocene archaeological soils around Cecita Lake (Sila massif, Calabria, southern Italy), which represents a typical upland Mediterranean environment. It is focused on assessment of climatic and environmental changes that took place since late Neolithic to Roman times, trying to discriminate natural from anthropogenic signals. Based on an integration of archaeological, geomorphological, stratigraphic, pedological, volcanological and soil charcoal (pedoanthracological) data, the following paleoclimatic/environmental reconstruction is proposed: a warm and humid, seasonally contrasted climate, with an overall geomorphological stability suited for soil development, characterized the late prehistoric environment (Holocene climatic optimum), dominated by a widespread oak forest. The main pedogenetic processes consisted in organic matter accumulation, clay illuviation, phyllosilicate and short-range order mineral neogenesis from weathering of granite and volcanic ash, sourced from late Pleistocene–Holocene eruptions of the Aeolian Islands. One or more mid-Holocene episodes of climate deterioration towards drier conditions (indicated by a decrease of clay translocation processes and possible irreversible dehydration of poorly-crystalline aluminosilicates into phyllosilicate clay minerals) promoted intense land degradation. This was in turn enhanced by increasing human activities for settlement and resource exploitation (among which deforestation and ploughing for agriculture), which led to a shift of the vegetation cover towards a dominant pine forest between 3 ka BP and the Roman epoch. Humid and possibly cooler climatic conditions during the late Holocene are indicated by the decrease of clay illuviation, coupled with short-range order components prevailing over phyllosilicate clays during Roman soil formation. [Copyright &y& Elsevier]

Abstract: As in many other regions of the world, the Late Pleistocene in China underwent rhythmic changes of climate, which caused some obvious changes in mammalian fauna, natural landscape and human cultural adaptations. This paper is a brief introduction of four representative Late Pleistocene sites in North China, which are dated at periods between Middle and Upper Palaeolithic, and demonstrated common or particular features from geographic and geological aspects, archaeological and environmental characters, and chronological position. A large transformation happened, reflected by culture remains, showing that environmental changes profoundly influenced human behaviour and inspired new forms of culture appearance. This indicates the clear existence of Middle Palaeolithic at least in North China, which became a foreshadowing for the coming Upper Palaeolithic. [Copyright &y& Elsevier]

Abstract: Large quantities of archeology and literature records indicate that during the Shang Dynasty and a part of the Zhou Dynasty of Chinese history, about 2000 BC to 1000 BC, there once were wild elephants living in North China. For a long time, it was believed that all of these elephants belonged to the species Elephas maximus. Many scholars suggested that this phenomenon could show a much higher temperature at that time. However, as the research of Chinese historical climate has already indicated, even in the Megathermal Maximum, most of the parts of North China were still controlled by the climate of the Warm Temperate Zone, not the Subtropic Zone. This paper presents evidence suggesting that the so-called “wild elephants” in North China during that time belonged to Palaeoloxodon sp., not E. maximus. [Copyright &y& Elsevier]

Abstract: Due to its diverse geographic and climatic conditions, the Iberian Peninsula is well suited for studies into the relationship between climate, environment and hunter-gatherer adaptation. With focus on the archaeological record, this paper examines to what extent diachronic variations in site density on the Iberian Peninsula are related to climate variability and cultural change. Studies are based on a comprehensive record of technocomplexes that date from the late Middle Palaeolithic, early Upper Palaeolithic, Gravettian and Solutrean. The record comprises altogether 152 archaeological cave sites and rock shelters. Analysis reveals strong regional differences between Northern and Southern Iberia, both in isochronic and in diachronic perspective. This is expressed by the strongly different patterns of human presence in these regions. In particular, within both regions major cultural changes coincide with the environmental impact of North Atlantic Heinrich Events (HE). From previous studies, it is known that the human population on the Iberian Peninsula (IP) must have suffered strongly under the extremely variable climate conditions during the Late Pleistocene. Based on extensive site-mapping, the hypothesis is that during HE a major disintegration of habitats must have occurred, with various but strongly isolated patchy refugia remaining. Further, during HE, Southern Iberia could not uphold its previous function in providing a reliable refuge for humans. Not only does climatic deterioration during the different HE repeatedly lead to a near-complete breakdown of settlement patterns, but following each HE there is a major reorganization in settlement patterns on the IP. [Copyright &y& Elsevier]

Abstract: This paper analyzes the spatial organization of two layers corresponding to the first half of the Middle Holocene from the Hornillos 2 rockshelter (Susques, Jujuy Province). Some important issues taken into account are the good preservation of the site and the sedimentary deposition processes which coincide with paleoclimate aspects. Correlation of different archaeological lines of evidence allows interpretation of the connection between several activity areas and their occupational intensity. There is a trash heap related to a short occupation period at the beginning of the Middle Holocene and a main zone of intense activity ca. 6200 yrs BP. These facts are in accordance with the archaeological expectations proposed for certain periods of the Middle Holocene. [Copyright &y& Elsevier]

Abstract: Whether or not abrupt Younger Dryas climate change affected regional paleoenvironments and late Pleistocene hunter-gatherer populations is an important topic in the archaeology of the American Southwest. This paper reviews multiple, age-resolved proxy evidence to gauge the magnitude and direction of Younger Dryas Chronozone (YDC) environmental changes in different settings and systems. There is no record of YDC pluvial lake highstands in Arizona or New Mexico, but there are impressive records of vegetation, faunal, stable isotope, and geomorphological change coincident with the YDC. These correlate with important adaptive changes in human hunting and land use, as revealed in the analysis of the spatiotemporal distribution of late Pleistocene hunting technologies. Clovis and Folsom projectile point distributions do not support extant models of paleoenvironmental conditions in these interpretations. Significant cultural changes that coincide with the YDC include the Clovis-to-Folsom transition, the demise of mammoth hunting and the development of a highly successful emphasis on bison, increased regionalization, and the abandonment of the northwestern Chihuahuan and the Sonoran deserts by mobile, big-game hunters. [Copyright &y& Elsevier]

Abstract: Human response to climatic conditions during the turbulent terminal Pleistocene has long concerned archaeologists and paleoecologists alike, especially with regards to the Younger Dryas. In some regions of the Northern Hemisphere the Younger Dryas was not significantly felt; however, in far northern regions affects of climate change are often acute. This paper focuses on the central Alaskan record to explore human–environment interactions during the terminal Pleistocene and tackle questions regarding human response to the Younger Dryas. This region of Beringia preserves a wealth of both paleoecological and archaeological data. Relative to other northern landscapes, proxy data from central Alaska indicate the Younger Dryas signal was somewhat muted but still characterized by return to cooler and/or more arid conditions. This phenomenon likely affected distributions and character of both floral and faunal resources, altering human perception of the surrounding landscape and potentially leading to reorganization of technologies, subsistence behavior, and land-use strategies. [Copyright &y& Elsevier]

We introduce the papers of the QI Special Issue: Climate Change and Archaeology which were presented at the Second Frison Institute Symposium at the 2014 Society for American Archaeology annual meeting. Papers here examine the links between climate and cultural change, calling attention to the difficulty of determining the role played by climate in cultural change. Issues include whether chronological resolution of climate and cultural change is sufficient to determine that the former “caused” the latter. An additional issue is, assuming the chronological correlation is resolved, whether an observed behavioral or technological change can be attributed to climate change, or if the correlation is spurious. [ABSTRACT FROM AUTHOR]