Would North American Paleoindians have Noticed Younger Dryas Age Climate Changes?

Paleoindian groups occupied North America throughout the Younger Dryas Chronozone. It is often assumed that cooling temperatures during this interval, and the impact these would have had on biotic communities, posed significant adaptive challenges to those groups. That assessment of the nature, severity and abruptness of Younger Dryas changes is largely based on ice core records from the Greenland ice sheet where changes were indeed dramatic. This paper reviews climatic and environmental records from this time period in continental North America. We conclude that, on the Great Plains and in the Rocky Mountains, conditions were in reality less extreme. It therefore follows that conditions during the Younger Dryas interval may not have measurably added to the challenge routinely faced by Paleoindian groups who, during this interval, successfully (and perhaps rapidly) dispersed across the diverse habitats of Late Glacial North America.     

Clovis,Folsom, and Midland components at the Debra L. Friedkin site,Texas: context,chronology, and assemblages

The archaeological transition from Clovis to Folsom and Midland in the North American Great Plains coincides with the end of the Pleistocene and onset of the Younger Dryas. Comparisons exploring the adaptive changes that took place during this period frequently employ regional-scale approaches. The focus on regional-scale analyses largely results from the dearth of sites repeatedly visited by multiple early Paleoindian groups. However, regional-scale comparisons have the potential to overlook smaller-scale differences. The Debra L. Friedkin site, Texas offers an opportunity to study Midland, Folsom, and Clovis technology and site-use at a single site. This paper presents the context and chronology of the Midland, Folsom, and Clovis assemblages and a site-scale analysis of lithics from the Friedkin site. It is argued that point production and late-stage reduction were primary activities, and the use of bifacial cores for flake tools was important throughout these occupation periods. Site use at Friedkin differs from early Paleoindian occupation at the nearby Gault site and expands our understanding of settlement and technological organization in the region.     

Radiocarbon dates as data: quantitative strategies for estimating colonization front speeds and event densities

Archaeological analysis of large-scale prehistoric population history requires us to estimate rates of spatial spread during dispersals, and rates and magnitudes of temporal contraction during crashes. Using OxCal’s MCMC sampling routine, I introduce and demonstrate a simple and easily implemented method of estimating front speeds that takes due account of the uncertainty in the archaeological data (in both dates and distances), and argue that this method is more appropriate than those most often used in front speed estimation at present. I also propose a simple and easily implemented method of estimating event densities as a demographic proxy, as an alternative to summed calibrated probability distributions. I argue that this alternative is a significantly better technique, and show that its use also enables us to identify individual archaeological dates that are exerting particularly strong influence on the results, so that we can efficiently allocate our attention when assessing the possible effects of exogenous sampling uncertainty. To illustrate these methods I re-analyse two published datasets relating to the early Paleoindian colonization of North America. My results with the new technique indicate that even with a very noisy dataset, there was clear evidence in the framework of the INTCAL04 calibration curve for a drastic reduction in archaeological event densities following the Younger Dryas onset, followed by a prolonged period of reduced human activity, and a possible renewed phase of rapid growth after the Younger Dryas termination and onset of the Holocene. However, the revised estimate of the Younger Dryas marine reservoir offset in the INTCAL09 calibration curve for ∼12,550–12,900 cal BP changes the picture significantly, by flattening the peak in Clovis-age events and pushing it forward in time into the early Younger Dryas itself.     

Holocene hyrax dung deposits in the afroalpine belt of the Bale Mountains (Ethiopia) and their palaeoclimatic implication

Abstract

The results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits from rock shelters found in the Afroalpine zone of the Bale Mountains (South-Central Ethiopia). Deposits accumulated from about 15,000 to 1500 (cal) years BP and from 7000 (cal) years BP till nowadays, respectively. Pollen spectra of the initial stages of deposit development (up to 15,000 (cal) years BP) correlate with unfavourable conditions in the Late Glacial Maximum. The African Humid Period (AHP) (15,000–5000 (cal) years BP) is registered in this palaeoecological record as well as the Younger Dryas event (about 12,500 (cal) years BP). Upward shift of Afromontane forest belt and expansion of ericoid communities at high altitudes were characteristic of the Pleistocene/Holocene transition (about 10,000 (cal) years BP). The AHP which continues around 10,000 (cal) years BP after Younger Dryas, was interrupted by a dry episode around 8200 (cal) years BP. Principal aridisation trend during the last 5000 years was observed. Presumably the first traces of human activities in this area can be shown for up about 2500 (cal) years BP.     

The Organization of Late Paleoindian Lithic Procurement Strategies in Western Wisconsin

Abstract

The applicability of employing an organization of technology framework to the analysis of prehistoric lithic procurement strategies is demonstrated here. Analysis reveals that a spatial separation is present in the distribution of lithic raw materials used by Late Paleoindian populations in western Wisconsin. This raises the possibility that lithic raw material functioned as a stylistic indicator of group membership. To evaluate this suggestion microstylistic traits present on a large sample of diagnostic Late Paleoindian projectile points were examined. Significant differences in stylistic traits were observed between sample areas. Furthermore, these differences correspond to spatial differences in raw material use. The correlation between lithic raw material use and microstylistic traits is consistent with the idea that lithic raw material serves as a stylistic marker of group membership, and indicates the presence of some form of social boundary within western Wisconsin during the Late Paleo indian Period.     

Plants and Technology: Current and Future Directions

Abstract

Located within the driftless area of southwestern Wisconsin, the Withington site provides a unique opportunity to examine the adaptive responses of Early Paleoindians exploiting this region. With a lithic assemblage dominated by Hixton Silicified Sandstone from sources over 170km to the north, chipped stone technological attributes and raw material diversity suggest that the occupants of the site were highly mobile, employed a mixed organizational strategy of toolstone transport, and possessed a wide knowledge of the lithic and social landscape. While our recent understanding of the early archaeological record of this region has progressed, a lack of published reports continues to hinder the incorporation of data from this area into larger models of Early Paleoindian subsistence and settlement. As part of an on-going research effort to address this, I present here a report and analysis of lithic material recovered from the site.     

CAROLINA BAYS: TIME CAPSULES OF CULTURE AND CLIMATE CHANGE

Abstract

We synthesize results of extensive archaeological surveys and geoarchaeological investigations of Carolina bays and other depressional wetlands on the U.S. Department of Energy’s Savannah River Site (SRS). The SRS is located along the Savannah River in the upper Coastal Plain of South Carolina. These data are augmented with data from Carolina bays elsewhere within their middle to south Atlantic Coastal Plain range. Carolina bays are shallow, oriented upland ponds that formed during the late Pleistocene under climatic conditions very different from present. Their use by prehistoric populations was most intensive during the Paleoindian and Archaic periods. Subsequent use by Woodland and Mississippian populations tended to be ephemeral. Change through time in the prehistoric use of Carolina bays and other depressional wetlands is linked to regional-scale changes in climate, particularly to the hydrologic regime.     

Terra incognita: terrestrial LiDAR documentation of Mound A at Kolomoki (9ER1)

ABSTRACT

The manifest representation of space and place is essential to good archaeology. Our ability to document and relate these concepts, projected into the past and reflected in the present, has increased tremendously with the expansion and availability of technology. We present recent efforts to further document a well-known place in the cultural landscape: the Kolomoki site in southwestern Georgia, occupied primarily during the Middle and Late Woodland periods. Specifically, we summarize older investigations of Mound A, then present the results of recent terrestrial LiDAR documentation. Our work substantiates the claim that Mound A was the largest Woodland-period mound in Eastern North America in terms of overall volume.     

Spatiotemporal Changes in Landscape Pattern in Response to Afforestation in Northeastern Turkey: A Case Study of Torul

Abstract

Monitoring and understanding of land use/forest cover dynamics as well as the factors affecting the changes in land use/forest cover are necessary for the sustainable management of natural resources. This study analyzes the spatial and temporal changes in land use and forest cover patterns in a typical mountain forest area in the Torul State Forest Enterprise area of Northeastern Turkey. The investigation evaluates the temporal changes of the spatial structure of forest conditions through the spatial analysis of forest-cover type maps from 1984 and 2005 using GIS and FRAGSTATS. The evidence presented here showed that there were drastic changes in the temporal and spatial dynamics of land use/forest cover, and between 1984 and 2005 there was a net increase of 19.9% in total forested area. Productive forest area increased by 3161 ha, although degraded forest area increased 9216 ha. In examining the changes of crown closure and development stages of the forest ecosystem during the study period, the forest stand area with low crown closures increased. The regenerated area increased because of regeneration activities while the other development stages were left to grow to older development stages in the period. These results regarding the crown closure and development stage show that forest quality has increased, and this is partly due to emigration of the rural population in Torul. In terms of spatial configuration, the landscape structure in Torul, the State Forest Enterprise area, changed substantially over the 21-year study period, resulting in fragmentation of the landscape as indicated by large patch numbers and smaller mean patch sizes, owing to heavy timber subtraction, illegal cutting, and uncontrolled stand treatments.     

Rethinking the Dawn of History: The Schedule,Signature, and Agency of European Goods in Protohistoric Illinois

Abstract

Interpretations of the archaeological record of the seventeenth century Illinois Country have been temporally compressed, and the richly stratified archival, ethnographic, and material records from that era have not been applied to the archaeological information at hand. A muddied view of the remarkable changes that occurred within the cultural landscape of Illinois is the result. European goods first appear in the region between 1580 and 1630 and the pottery of the Illinois Indians—the Danner series—is present in each early Illinois sample that includes these imports. A reexamination of the Zimmerman, Palos, and Oak Forest sites suggests that temporal changes in trade good assemblages can be better understood in the context of historically documented trade schedules. Further, it is argued that the Illinois Indians actively positioned themselves in the political and economic landscape of the fur trade many decades prior to the arrival of the French in the Illinois Country, serving as the principal agents of the great changes that are associated with protohistory in Illinois.     

The last glaciation in the Western Mourne Mountains,Northern Ireland

During the late‐Midlandian (25–13 ¹⁴C ka BP), the last Irish Ice Sheet was thicker in the Western Mourne Mountains than previously argued. Geomorphological and sedimento‐logical analysis shows that regional ice from the Irish Ice Sheet spilled over the mountains, reaching a major limit 5 km along Pigeon Rock Valley. These findings differ from the previous view that a local valley glacier occupied the valley during this period. The pattern of deglaciation was reconstructed using glacial and periglacial evidence. A complex topographic environment in the upper reaches of the valley suggests that regional ice stagnated as it wasted away. During the Nahanagan Stadial (Younger Dryas, ca. 11–10 ka ¹⁴C BP) an arcuate ridge was formed on the western flank of the valley. Calculations suggest that the Equilibrium Line Altitude, influenced by topographic conditions favourable for snow accumulation, was approximately between 1736 m and 1386 m lower during the Nahanagan Stadial than at present.     

Reconstruction of the Late Glacial and Early Holocene landscape and human presence in Lubrza,Western Poland,on the basis of multidisciplinary analyses

This paper presents the results of a multidisciplinary study that combines archaeological and palaeoenvironmental research to examine the relationship between environment and human activities in Western Poland during the Late Glacial and Early Holocene. The study area lying within the young moraine landscape produced several Late Palaeolithic and Early Mesolithic sites, varied in terms of size and function. Analyses of pollen, plant macro-remains and molluscs accompanied by geomorphological investigations and supported by series of radiocarbon dates have enabled a detailed reconstruction of environment. It has shown that despite climatic fluctuations during the Allerød and Younger Dryas, the studied area provided favourable conditions for hunter-gatherer occupation. The presence of micro- and macroscopic charcoal, charred particles of herbaceous plants and charred mosses in peat deposits of former water bodies evidence various activities carried out by Federmesser and Swiderian groups, for example setting up camp-fires and deliberate burning of the local marsh vegetation. Usewear analyses of flint implements have revealed further traces of diversified human activities undertaken at examined sites. Most importantly, this article focuses on plant-based craft activities undertaken by hunter-gatherers, about which little has hitherto been known.     

Prehistoric shell beads on the Georgia coast

ABSTRACT

The prehistoric peoples living along the Georgia coast fabricated and used shell beads for millennia. Out of a number of mollusk species inhabiting the region, only a few were selected for the fabrication of beads. The knobbed whelk (Busycon carica) was the most common species used, and it represents the most common whelk found in Atlantic coastal waters. The lightning whelk (Busycon sinistrum), the second most common whelk in the region, was occasionally used in the production of beads. Small numbers of beads were made from marginella and olive shells and, rarely, from bivalve species. Small beads were manufactured from the body whorl of whelks, while larger beads were fabricated from whelk collumella. Shell beads appear in small quantities in Late Archaic period contexts, and then almost disappear during the Woodland period. Beads reappear in quantities at about AD 800 in the Early Mississippian period. More shell beads have been recovered from Mississippian period archaeological contexts along the northern Georgia coast than along the southern coast, reflective of cultural differences between these two geographic areas in the post-Woodland period era.     

Using chaîne opératoire and communities of practice to identify interaction in the Contact and Mission periods in southern Georgia,AD 1540–1715

ABSTRACT

In this article, the pottery production of indigenous groups living inside and outside of colonial spaces in southern Georgia is compared by identifying portions of the chaîne opératoire of pottery production. Diachronic and geographic changes to production demonstrate that groups living in the interior of Georgia were in continual interaction with coastal groups in the mission system. This interaction likely contributed to the emergence of the Altamaha pottery tradition, which spread from southern South Carolina to northern Florida during Spanish colonization of the region. This research shows that Native American groups navigating colonialism drew on a wide network of communities to alter traditions in the face of unprecedented social change.     

Intra-Wetland Land Use in the Kankakee Marsh Region of Northwestern Indiana

Abstract

The physical structure and configuration of the landscape play profound roles in how a culture settles and utilizes a region. The following case study in the former Kankakee marsh region of northwestern Indiana exemplifies how subtle topographic variation can have a significant impact on intra-wetland landscape utilization. In the Kankakee marsh landscape, so-called dune islands provided areas of preferential settlement that were reused throughout the prehistory and early history of the region. In particular, these islands were important locales for resource extraction during the Late Archaic period and resource processing and storage during the Middle and Late Woodland and Upper Mississippian periods.     

Microblade technology and the rise of serial specialists in north-central China

Though present before the Last Glacial Maximum, microblade technology is uncommon in the lithic assemblages of north-central China until the onset of the Younger Dryas (12,900–11,600 calBP). While it is clear that microblades here and elsewhere were connected with mobile adaptations organized around hunting, the attendant assumption that they served primarily in hunting weaponry is not. The archaeological record of north-central China, including excavations at Pigeon Mountain (QG3) and Shuidonggou Locality 12 (SDG 12) in Ningxia Autonomous Region, and Dadiwan in Gansu Providence, and a handful of bone/antler tools slotted for microblade inserts, indicate a more direct linkage to mobility. These data suggest the rise of microblade technology in Younger Dryas north-central China was mainly the result of microblades used as insets in composite knives needed for production of sophisticated cold weather clothing needed for a winter mobile hunting adaptation akin to the residentially mobile pattern Binford termed “serial specialist.” Limited time and opportunities compressed this production into a very narrow seasonal window, putting a premium on highly streamlined routines to which microblade technology was especially well-suited.     

Early Paleoindian Mobility and Watercraft: An Assessment from the Mississippi River Valley

Several researchers have suggested use of watercraft during the Early Paleoindian period 11,500 and 10,800 rcybp (13,400–12,700 cal B.P.), but none have brought empirical data to bear on this possibility. This paper addresses the potential for fluted point-making groups to have made and used boats circa 11,000 rcybp (13,000–12,800 cal B.P.). Fluted point data from a large region of the upper and central Mississippi River valley strongly suggest that the Mississippi River was a barrier to movement and that Early Paleoindians in the midcontinent did not routinely use watercraft.     

明至民国时期方志舆图中韩城县境的景观格局与景观变迁

本文通过对韩城方志的舆图 ,尤其是分野图及县境图的制作与内容的比较分析 ,结合方志的文字内容及其他文献资料对明代至民国时期韩城县境景观格局作了简要的概括 ,并从表现及原因两个方面对韩城县境景观的变迁即西北山区森林的减少与童山的增多作了较为细致的考察。结论是韩城方志舆图比较真实地反映了韩城县境的景观格局和景观变迁的趋势与阶段特征。     

The Technology of the Early Oakhurst Lithic Techno-Complex from Klipdrift Cave,Southern Cape,South Africa

The analysis of the lithics recovered from the layers dating between cal bp 10,700 and cal bp 13,700 at Klipdrift Cave, southern Cape, South Africa, provides new information on the Oakhurst techno-complex. A comparison with contemporary sites such as Matjes River Rock Shelter indicates not only technological similarities, but also unexpected differences. The Klipdrift Cave Oakhurst shares many characteristics typical of this techno-complex from the southern Cape, for example, in the dominance of quartzite, irregular and unstandardised flakes; the occurrence of irregular cores; and typical large side and end scrapers. It differs from most coastal Oakhurst sites however, in the more intensive exploitation of quartz, and the presence of a blade component, especially in the lowermost layers. Palaeoenvironmental data, derived from stable isotope analysis of ostrich eggshell, suggest that it was dry in this region during this time period. This was partially a result of the colder conditions that prevailed during the Younger Dryas. The lithic technological production techniques are stable at Klipdrift Cave during the period that the site was occupied from cal bp 13,700 to cal bp 10,700. Our data suggest that the lithic technology did not change in response to possible climatic variability.     

Clovis Blades at Paleo Crossing (33ME274), Ohio

Abstract

This paper describes the previously undocumented Paleoindian lithic blade assemblage from the Paleo Crossing Site, Ohio (33ME274). Qualitative and quantitative comparisons of the Paleo Crossing blade assemblage to blade assemblages from other Paleoindian sites demonstrates its fragmented and utterly exhausted nature, but support its designation as Clovis. This is significant given that a majority of the Paleo Crossing toolstone outcrops 600 km southwest of the site in southern Indiana and western Kentucky, a prominent locale for Clovis prismatic blade manufacture. We propose that blade reduction was practiced for prolonging the use-life of distally retouched endscrapers, a prominent tool form at Paleo Crossing. Since use-wear and ethnographic evidence often show that endscrapers were used for hide-working, Paleo Crossing may be an appropriate venue to test for the presence of intense caribou hide-working.