Late Paleo-Indian Activity At The Lubbock Lake Site

Abstract

Excavations at Lubbock Lake (41 LU1), Southern High Plains of Texas, revealed the presence of a complex, late Paleo-Indian feature containing a camping area and bison (Bison antiquus) kill/butchering locale. The feature is found within a cienega or marsh deposit and dates from 8300 to 8600 years. At least two camping episodes are indicated, separated by the kill/butchering event. Camp debris consists of a projectile point midsection, unifacial and bifacial tools, and flakes. Faunal debris includes remains of butchered pronghorn antelope, rabbits, ducks, grouse, and turtles. The kill/butchering locale contains remains of four bison and three fetuses, a bone expediency tool, a reworked projectile point base, unifacial butchering tools, and flakes. Projectile points, other lithic tools, and age of the feature indicate a Firstview occupation. From faunal and geologic data, site environs are reconstructed as a marshlands rimmed by a narrow border of wet meadows grading into a mixed grass prairie. Although several late Paleo-Indian kill/butchering locales are known on the Southern High Plains, this feature is the first late Paleo-Indian camp.     

A Plainview Kill/Butchering Locale On The Llano Est Acado-The Lubbock Lake Site

Abstract

The Lubbock Lake site is a multi-component, stratified locality on the Llano Estacada (Southern High Plains). Part of a Plainview (Paleo-Indian) period bison kill/butchering locale is being excavated. Cultural designation is based on recovered projectile points, stratigraphic position, and radiocarbon dates. Tool assemblage consists of lithic and bone expediency tool kits. Geological, faunal, and paleoenvironmental settings create an interpretative framework for the cultural event. Only part of the Plainview lifeway system is reflected at the site. The locale represents a different level of social organization than seen at other Plainview period bison kill sites. Preliminary statements include a few differences and similarities between excavated Plainview sites.     

the Risley Bison Kill:West-Central Montana

Abstract

The Risley Bison Jump, a large kill site approximately 50 miles west of Great Falls, Montana, was test excavated in 1974. The badly vandalized site was scheduled to be destroyed by land subdivision.Even though the site was badly disturbed, our excavations show that the site was a well-used bison jump with at least four usages evident. Processing and butchering areas were located along the margins of the kill middens. Side-notched projectilepoints recovered from the site suggest that it dates from the latter part of the Late Prehistoric Period.     

The Gore Pit Site: An Archaic Occupation in Southwestern Oklahoma and a Review Of the Archaic Stage in the Southern Plains

Abstract

The Gore Pit site (34CM131), which is within the city limits of Lawton, Comanche County, Oklahoma, has been revealing evidence of Archaic occupation through excavation and surface collection since 1963. The site is contained in the bottom of a large borrow pit which was sera ped to a depth of 15 to 20 feet by he Highway Department.The pit is on the active flood plain of East Cache Creek and borders the creek a few feet to the east. The artifacts recovered by surface collection include projectile points, scrapers, scraper planes, Clear Fork gouges, andgrinding stones and basins. Three burned rock middens were excavated, one of which yielded radiocarbon dates, 6030 + 300 B.P. (Bastian 1964) and 6145+ 130 B.P. (GX1558). In the spring of 1968, a partially preserved, semiflexed human burial was discovered in the pit. There were no associated artifacts. A radiocarbon date obtained from the apatite fraction of the bone resulted in a determination of 7100+350 B.P. (GX2009). The earliest Archaic on the Southern Plains is presently dated around 6000 B.P. However, there is a paucity of dated and documented sites for the preceding 2000 years. Archaic subsistence patterns occur at least 2000 years earlier in areas to the west and east. The origin and age of the earliest Archaic in the Southern Plains remains undetermined. The Archaic must ultimately be identified on the basis of subsistence patterns and not on the basis of projectile point styles.     

The Glenrock Buffalo Jump, 48C0304: Late Prehistoric Period Buffalo Procurement and Butchering

Abstract

The Glenrock Buffalo Jump, 48C0304 is part of a Late Prehistoric period buffalo procurement complex in central Wyoming along the south side of the North Platte River. Operation of the jump required controlled movements of buffalo herds for as far as one to three miles before they were finally stampeded over a bluff 40 feet high. The effective width of the bluff was small and as a result the herd had to be under control during the final stampede as well as the initial drive.

Good bone preservation in much of the site allowed recovery of large samples for analysis and in addition large numbers of simple but functional tools were found in context. Marks that reflected a number of butchering operations appeared repeatedly suggesting stylized methods, and from this a model of Late Prehistoric butchering is postulated which needs further testing in other mass butchering contexts.     

A Preliminary Report on Two Sites at Piney Creek,Wyoming 48J03Ll and 48J031

Abstract

During the summer of 1964, the University of Wyoming and the Wyoming Archaeological Society conducted exploratory excavations in two sites near Buffalo, Wyoming. Site 48J03ll consists of a number of stone circles and is apparently a camp site and site 48J0312 is a bison kill and butchering site. Artifact assemblages suggest an affiliation with late prehistoric and early historic sites in the Yellowstone River drainage.     

Variability of the sediment phosphate composition of a temporary pond (Doñana National Park,SW Spain)

This study reports on the spatial and temporal variability of the phosphate composition in the sediment of a temporary pond over a period of 3 years using the EDTA-method for P-fractionation. Sediment samples were collected at three different sites (open-water, littoral and flood plain) to compare the effect of the length of the wet/dry phase on the sediment phosphate composition, with special emphasis on the potential bioavailability of the P-fractions.Fine sediments (<0.1 mm) were rich in organic matter (9–25%) and contained high mean concentrations of Tot-P (182–655 mg kg^–1 d.w.), especially in the flood plain sediment. The sediment P composition was dominated by P-organic fractions at all sites (64–94%). The average C/N ratios were 8.8, 6.0 and 5.9 for sediments of the flood plain, littoral and open-water sites, respectively. The flood plain sediment was significantly poorer in iron-bound P (FeOOHP), but richer in the P-organic fractions extracted by EDTA than the sediment of the open-water site (P<0.01). The percentage of organic matter increased significantly in the sediment of the open-water site at the end of each dry season (P<0.05), while it decreased in the sediment of the flood plain site (P<0.01). In all sediments, the fraction of Fe(OOH)P decreased at the end of each dry season and some of these changes were significant (P<0.05). The decrease in the fraction of Fe(OOH)P was not related to changes in the sediment redox potential. Although the flood plain site was dry longer than the open-water site during the study period, the differences between the sediment composition of both sites were probably due to the effect of plant growth on the dry sediments of the flood plain site rather than to a direct effect of desiccation.     

Non-Bison Remains from the Vore Bison Jump,Crook County,Wyoming

Abstract

The Vore. Bison Jump is a multi-component Late-Preh1stonc B1son kill site in the Black Hills of Crook County, Wyoming. Examination of the non Bison revealed a large number of carnivores, mainly wolves. Analysis of these wolf remains showed a need for more careful identification of canid remains from archaeological sites in light of incipient domestication of wolves at this site.     

Chasseurs épigravettiens dans le territoire de l’ours des cavernes : le cas du Covolo Fortificato di Trene (Vicenza,Italie)

The Covolo Fortificato di Trene site is located on the eastern slope of the Berici hills, Vicenza, in the middle of the great Po-venetian plain in Northern Italy, at a height of 360 m.a.s.l. The cavity was the object of systematic excavations made by the University of Ferrara in 1956, which yielded a 1.14 m-thick deposit, subdivided into seven stratigraphic units. The lithic industry, associated with macromammals remains, bird bones and charcoal, ascribe the anthropic frequentation of the archeological layers to the early Epigravettian. This is confirmed by two dates obtained on bone (17.640 ± 140 AMS ¹⁴C B.P. and 18.630 ± 150 AMS ¹⁴C B.P.). This work presents a taxonomic revision and zooarchaeological analysis of already published faunal remains, whose spectrum shows a clear dominance of Ursus spelaeus over the other determined taxa. During human frequentation, the site was in a predominantly forest environment under cold-temperate climate conditions with wetland areas on the underlying plain, as shown by the presence of elk, deer, wild boar and fish vertebrae. The taphonomic analysis has shown anthropic traces on the remains of elk and cave-bear, which used the cave as den during wintering. The study focused on Ursidae remains, affected by butchering marks due to fur extraction, mostly from young individuals. Moreover, a limited comparison (Berici hills) with contemporary sites (Paina cave, Buso Doppio cave), associates cave-bear presence with shouldered points.     

Evidence from the Lake Champlain Valley for a later onset of the Champlain Sea and implications for late glacial meltwater routing to the North Atlantic

Ocean circulation models indicate that freshwater runoff from the North American continent during the last deglaciation may have had an effect on North Atlantic Ocean circulation, and thereby have altered regional climate. One such example is a flood from Lake Agassiz, which has been proposed by previous workers to have caused the onset of the Younger Dryas at around 12,850 calibrated years B.P. by entering the North Atlantic through the Gulf of St. Lawrence. We present two radiocarbon ages from terrestrial organic sources in the Champlain Valley that we associate with the pre-Champlain Sea proglacial lake phases; a musk-ox bone with an AMS age of 11,362 ± 115 ¹⁴C years B.P. (13,438-13,020 calibrated years B.P.), and a wood fragment with an AMS age of 10,901 ± 76 ¹⁴C years B.P. (12,995-12,793 calibrated years B.P.). These ages together with a glacial lacustrine varve estimate suggest that the initiation of the Champlain Sea may not have occurred until after the onset of the Younger Dryas. If the Lake Agassiz flood event occurred before the opening of the Champlain Sea then the floodwaters would have been diverted down the Champlain and Hudson valleys to the North Atlantic. Another possibility is that the Agassiz flood may have been contemporaneous with the opening of the Gulf of St. Lawrence. It is also possible that there may have been a large enough flood produced by meltwater originating in the Champlain Valley and St. Lawrence Lowlands at the inception of the Champlain Sea to have affected ocean circulation without the influence of Lake Agassiz.     

桦甸仙人洞遗址出土的动物化石与孢粉

桦甸仙人洞旧石器遗址的上、下文化层出土了大量动物化石, 本文通过动物化石的分布状况、出土状态分析, 复原了上、下文化层沉积时期古人类的狩猎和处置猎物的行为, 总体来看, 远古人类生计方式以狩猎为主, 晚期古人类比早期对猎物资源开发得更彻底。另外, 从洞穴内大量碎骨片和石制品来看, 该洞穴可能为临时的营地或者屠宰场。通过对动物群组成、年代和孢粉分析的综合研究, 认为该遗址所处环境经历了剧烈的变化, 总体处于寒冷干燥的气候环境中, 植被以草原为主, 伴有少量森林。这一研究为探讨中国东北地区晚更新世人类的生存行为和演化特征提供了重要的研究材料和数据。     

The Strohacker Site: A Review of Pre-Archaic Manifestations in Texas

Abstract

Investigations at the Strohacker site in central Texas produced a number of late Paleo-Indian and pre-Archaic artifacts. These are described and the site is compared to several other Texas sites from which similar artifacts were recovered in recent years. On the basis of present evidence, it is proposed that the latter part of the Paleo-Indian period ended in parts of Texas around 6000 B.C. and was followed by a transitional preArchaic phase which extended throughout the Altithermal. This phase was succeeded by a developed Archaic tradition about 3500 B.C.     

On The Significance of Additional Radiocarbon Dates from Bonfire Shelter,Texas

Abstract

Two hitherto unreported dates from charcoal samples associated with remains attributed to a Paleo-Indian bison kill at this site are provided. These dates further substantiate a minimal antiquity of ca. 10,000 years for the deposit and, by inference, give evidence of the use of a “bison jump” technique of hunting at this early time period. Definitional problems, differing views on the antiquity, basic comparability of cited examples, and temporal continuity of this mode of mass killing are briefly discussed. Some suggestions are made as to the cultural implications made probable by acceptance of an early date for this practice.     

Plant Remains From Phillips Spring,A Multi Component Site In The Western Ozark Highland Of Missouri

Abstract

Phillips Spring (23Hi216) is a multicomponent archaeological site associated with an active artesian spring on a terrace of the Pomme de Terre river in western Missouri. Preservation of both carbonized and uncarbonized plant remains is excellent and remains of plants representing 32 taxa, including 24 potential food plant, occur atthe site as well as eight taxa of wood charcoal. In addition, there are remains of squash (Cucurbita pepo) and bottle gourd (Lagenaria siceraria) dating 4260 B.P., 40008.), 1999 B.P., and squash dating 2293 B.P. When combined with data from a Woodland storage pit at nearby Boney Spring (squash dated at 1920 B.P.) and Blackwell Cave (bottle gourd at 730 B.P.), it appears that these cultigens were being grown in the western Missouri Ozarks for much of the last 4000 years. Phillips Spring is a multicomponent (Late Archaic and Middle Woodland) site situatedon a terrace of the Pomme de Terre River in Hickory County, Missouri. Discovered in 1973, the site was subsequently excavated during four field seasons: 1974, 1976, 1977 and 1978. The 1974 excavations defined four cultural horizons including three Late Archaic and a Woodland component (Chomko 1976) and produced numerous well preservedplant remains. The presence of squash (Cucurbita pepo) in the earliest component, later associated with a date of3927 B. P., prompted additional testing of the site in 1976 and full scale excavation in 1977 and 1978 (Kay 1978, Robinson 1978). Results of the 1974 excavations have been previously discussed (Chomko 1978, Chomko and Crawford 1978) and the present paper discusses the plant remains from the 1976 and more extensive 1977 excavations. While the 1978 material, presently awaiting analysis, will undoubtedly increase both our knowledge of activity patterns at the site and our sample size of specific types of features and biotic remains, it will probably not add substantially to the extensive list of plant taxa which have been recovered from the spring.     

宁夏鸽子山遗址第10地点出土动物骨骼的埋藏学初步观察

宁夏鸽子山遗址第10地点(QG10)位于青铜峡市西北约20km的贺兰山南麓。2014-2017年,中国科学院古脊椎动物与古人类研究所与宁夏文物考古研究所联合组队对该遗址进行了发掘,出土大量动物化石、近万件石制品以及装饰品、骨制品、结构性火塘等。本项研究基于遗址第4层出土动物化石的埋藏学初步观察认为:晚更新世末期的古人类是遗址中动物骨骼的富集者和改造者;QG10的狩猎-采集人群采取狩猎而非主动食腐的方式获取了遗址附近的大中型食草类动物,并将其完整搬运至遗址内进行后续的肢解、食肉与敲骨取髓等营养性处理过程。相对于上述动物种类而言,遗址内的小型动物则是在其营养物质之外,古人类还利用了它们的骨骼材料以制作器型规整的骨角类工具。     

Fat Residue and Use-Wear Found on Acheulian Biface and Scraper Associated with Butchered Elephant Remains at the Site of Revadim,Israel

The archaeological record indicates that elephants must have played a significant role in early human diet and culture during Palaeolithic times in the Old World. However, the nature of interactions between early humans and elephants is still under discussion. Elephant remains are found in Palaeolithic sites, both open-air and cave sites, in Europe, Asia, the Levant, and Africa. In some cases elephant and mammoth remains indicate evidence for butchering and marrow extraction performed by humans. Revadim Quarry (Israel) is a Late Acheulian site where elephant remains were found in association with characteristic Lower Palaeolithic flint tools. In this paper we present results regarding the use of Palaeolithic tools in processing animal carcasses and rare identification of fat residue preserved on Lower Palaeolithic tools. Our results shed new light on the use of Palaeolithic stone tools and provide, for the first time, direct evidence (residue) of animal exploitation through the use of an Acheulian biface and a scraper. The association of an elephant rib bearing cut marks with these tools may reinforce the view suggesting the use of Palaeolithic stone tools in the consumption of large game.     

王府井东方广场遗址骨制品研究

王府井东方广场遗址不仅出土了丰富的石制品,而且也含有较为丰富的骨制品。骨制品可分为骨核、人工骨块、骨片、骨屑和骨器五大类;骨片约占骨制品总数一半;骨器包括刮削器、尖头器、雕刻器和骨铲四类。观察发现：79件骨制品和骨骼可以拼合成33组,45件上有古人类砍砸、切割或刻划的痕迹。丰富的骨制品进一步反映了王府井古人类文化的进步性;同华北地区类似制品比较,它们之间存在着密切的渊源关系。遗物分布特征表明,东方广场遗址是一处古人类的临时居住地。出土的石器、骨器遗物以及大量的动物骨骼化石表明,王府井古人类不仅能够制作石器与骨器用来宰杀与支解猎物,而且具有用火、控火进行烹饪的能力。     

Early Prehistoric Killing of Bighorn Sheep in the Southeastern Canadian Rockies

Abstract

The remains of three bighorn sheep were excavated from early Holocene pond deposits in the Crowsnest Pass, Alberta. The sheep show evidence of patterned disarticulation and butchery. The types of bones recovered suggest the presence of some form of communal hunting and meat sharing. Although sheep were present in the Rockies throughout the Holocene, their remains are scarce from Early Prehistoric sites in Canada. It is suggested that the sheep kill dates to 8500 B.P., based upon a radiocarbon date and a projectile point from the same pond deposit.     

Perry Ranch:A Plainview Bison Kill On the Southern Plains

Abstract

Salvage excavations at the Perry Ranch site in southwestern Oklahoma uncovered the association of Plainview projectile points with an extinct subspecies of bison. A radiocarbon date of 7030 ± 190 B.P. has been obtained from bison bone at the site. However, stratigraphic disturbances limit inferences about the cultural activities at the site.