T-W-DIamond,a Stone Ring Site in Northern Colorado

Abstract

The T-W-Diamond Site, 4LR200, is a large teepee ring village on the? edge of the High Plains in northern Colorado. Seventeen out of the 47 remaining stone ring areas were excavated or tested by the Colorado State University Archae-ological Field School in 1971. Artifacts, fire hearths and midden materials were scarce but indicated the domestic nature of the structures. Stone and ceramic artifacts indicate cultural affiliations with the Late Prehistoric period as reported at Birdshead Cave, and the Piney Creek sites in Wyoming; and at the Agate Bluff Rock Shelters, and the Dipper Gap site in northern Colorado. Carbon-14 dates of A. D. 1020±230 years and A.D. 1170±220 years support the time of the occupation. A third date of A.D. 400±340 seems improbably early. It is hypothesized that the village was occupied seasonally for a short time by a small group of people, perhaps of Shoshonean affiliation, exploiting a mixedbase subsistence economy.     

A Late Prehistoric Bundle Burial From Southern Wyomingc

Abstract

A Late Prehistoric bundle burial from the Stone Fence Site in south-central Wyoming produced partial skeletal remains of a middle-aged male of Shoshonean biological affinities.A total of 19 bone beads were found in the grave. Both osteological and cultural interpretations were possible from the previously undisturbed grave and its contents.     

An example of de‐Tai‐isation? Longue durée ethnic change in a mountainous area of southern China

Inspired by Grant Evans’ work Tai‐ization: Ethnic Change in Northern Indo‐China, this article explores aspects of historical ethnic change in the Yunkai and Yunwu Mountain Ranges, a small upland region intersected by the boundary of Guangdong and Guangxi provinces in southern China over the period 600–1700 C.E. The discussion begins with some of the early linguistic evidence for populations of Tai speakers in the region and what is known of their political and cultural systems, then moves on to consider how Chinese military conquests of the eighth century coupled with the migration of Sinitic and Mien peoples from the eleventh century onwards altered the ethnic composition and political landscape of the region. This is followed by an examination of different exonyms used in Chinese texts for populations of southern China from the fifteenth century onwards and how these might have related to linguistic groupings and identities on the ground, demonstrating that historical usage of Chinese exonyms now connected with Tai or Mien speakers is not always a reliable indicator of a corresponding presence of historical Tai or Mien‐speaking populations. Further research drawing on a number of disciplines is required on a localised level in order to determine when Tai and Mien languages were abandoned in the region and how the inhabitants of the area shifted from the status of named Others to ordinary Chinese subjects.     

The role of human disturbance in Late Holocene vegetation changes on Kullaberg, southern Sweden

A pollen record from a small peatland located on Kullaberg in northwestern Sk?ne, southern Sweden, revealed that grazing pressure might have been the major disturbance agent controlling the vegetation, at least from ca. 1500 B. C. until the latter part of the nineteenth century. The pollen data also indicate a step-by-step increase in grazing pressure, expressed as a marked increase in non-arboreal pollen representation at ca. 1500 B. C., A. D. 650 and A. D. 1650. The increase at A. D. 650 probably indicates a more regular and intensive use of the area, resulting in a forest structure that was much more open than earlier, together with an expansion of Fagus, which rapidly replaced Quercus as the local forest dominant. At about this time the first patches of heath vegetation originated, but they probably only covered a small part of Kullaberg. Larger areas with an intensively grazed Calluna heath, as shown by eighteenth century maps, probably evolved around ca. A. D. 1650, when much of Kullaberg seems to have been deliberately deforested. Received February 20, 2001 / Accepted September 12, 2001     

Lunulichnus Tuberosus Ichnogen. and Ichnosp. Nov. from the Early Eocene Wasatch Formation,Fossil Butte National Monument,Wyoming: An Arthropod-Constructed Trace Fossil Associated with Alluvial Firmgrounds

A new trace fossil, Lunulichnus tuberosus, is described from fluvial deposits of the Wasatch Formation (early Eocene) at Fossil Butte National Monument, southwestern Wyoming, USA. L. tuberosus are straight, vertical to obliquely oriented, unlined cylindrical burrows with pronounced crescent-shaped wall sculptings. In situ examples of these trace fossils are most commonly preserved as sand-filled casts emanating from the erosional bases of fluvial channel sandstone bodies into underlying floodplain mudstone/siltstone beds. L. tuberosus is interpreted as the dwelling trace of a stream-dwelling decapod crustacean. Excellent preservation of fine detail, particularly their diagnostic crescent-shaped wall sculptings, support the hypothesis that L. tuberosus were excavated in firm substrata subjacent to fluvial erosional surfaces. As such, they are interpreted as constituents of alluvial Glossifungites trace fossil assemblages.     

The Turk Burial Site, 48WA301

Abstract

This fissure burial in the southern mountains contained four adults and one child. Its age is estimated to be between 100 and 300 years, and the anthropometric evidence is consistent with a Shoshonean affiliation. Though considerably disturbed prior to investigation, the site yielded important information about the burial mode and artifacts of a fairly recent people.     

Sources of Steatite and Methods of Prehistoric Procurement and use in Wyoming

Abstract

Carved steatite vessels are common to the mountCJins and intermontane basins of northwestern Wyoming and immediately adjacent areas of Idaho and Montana. Steatite occurs in Precambrian rock throughout several mountain ranges of Wyoming. Surface material was used and much was quarried from buried deposits. Finished vessels are flatbottomed and occur in a variety of sizes and shapes.     

New notharctine primate fossils from the early Eocene of New Mexico and southern Wyoming and the phylogeny of Notharctinae

Previously undescribed notharctine primate fossils are reported from the early Eocene San Jose Formation, San Juan Basin, New Mexico, and the early Eocene Wasatch Formation, southern Wyoming. These collections include the most complete specimens yet discovered of the poorly known species Copelemur tutus and Copelemur praetutus; the first upper dentitions of Cantius angulatus and Cantius frugivorus from the type area of these taxa; and fossils attributable to two new notharctine species, Copelemur australotutus and Smilodectes gingerichi. These new fossils reveal that current ideas concerning notharctine phylogeny are incorrect. Two major, monophyletic clades are apparent within the subfamily: the tribe Copelemurini, consisting of the genera Copelemur and Smilodectes, and the tribe Notharctini, comprising the genera Cantius, Pelycodus, and Notharctus. Analysis of the paleobiogeographic distribution of the Copelemurini indicates that this clade was limited to more southerly regions of western North America during early Eocene time. Northward migration of more tropical habitats during the late Wasatchian and early Bridgerian in western North America, associated with an overall climatic warming trend through the early and middle Eocene, appears to have allowed several mammalian taxa, including Smilodectes, to extend their ranges northward during this time interval. Such taxa thus possess diachronous distributions and have been partly responsible for the long-standing confusion regarding the biostratigraphic correlation of early Eocene faunas from New Mexico with those from Wyoming. Based on several taxa which are also known from the Wasatchian of Wyoming, the age of the San Jose Formation appears to be middle Wasatchian.     

Platycleis vittata (Orthoptera: Tettigoniidae) in the northwestern part of its range is close to extinction: is this the result of landscape changes?

The northwestern distributions of several steppe species of Orthoptera extend to the southeastern part of the Czech Republic (Pannonia) and occupy more or less isolated fragments of optimal habitats. Their distributional limits are not conditioned by macroclimate in most cases but reflect landscape development (physical structure, plant community type and microclimate) and the insects’ dispersal abilities. These species prefer permanent grassland, and assessment of land use records indicates that the area occupied by permanent grassland has been greatly reduced by agriculture over the last two centuries. The area occupied by permanent grasslands in Pannonia was highest in the nineteenth century, declined until the second half of the twentieth century, and slightly increased at the beginning of the twenty first century. These changes in the area of permanent grassland generally reflect economic and political processes; in particular, consolidation of land plots and expropriation of private property brought an end to grazing. The distribution of a model Orthoptera specialist, Platycleis vittata, on steppe habitats was surveyed at 48 potentially suitable locations from 2004 to 2010. The survey determined that the area with suitable habitat is currently very limited at all 48 locations. Occurrence was confirmed in just two locations that are 3 km apart. The research suggests that Platycleis vittata in the Czech Republic is on the brink of extinction because of extreme fragmentation of suitable biotopes and degradation of optimal habitats.     

Changes in fish condition and mercury vary by region,not Bythotrephes invasion: a result of climate change?

We compared changes in body condition (relative weight) and mercury concentrations ([Hg]) in two species of coregonid fish (lake herring Coregonus artedi, lake whitefish C. clupeaformis) among discrete populations in Ontario between 1967 and 2006. Temporal comparisons among populations were made to determine whether 1) the establishment of Bythotrephes longimanus had affected coregonid populations, or 2) if changes in body condition or [Hg] were related to regional differences in the degree of climate change during the time period investigated. Climate data from northwestern, northeastern and southern Ontario showed a general warming trend in all regions over the period of study. However, greater temporal changes in climate were observed in the northwest where growing degree days >5°C (GDD) increased and precipitation declined over the study period compared with relatively little change in southern or northeastern Ontario. Correspondingly, northwestern Ontario coregonid populations demonstrated significantly greater declines in body condition relative to those from northeastern or southern Ontario. Declines in [Hg] of both species were also greater among northwestern populations compared with those from northeastern or southern Ontario but only significantly so for lake herring. These declines were independent of the invasion of non‐native Bythotrephes, and declines in [Hg] were opposite predictions based on the hypothesis that Bythotrephes invasion lengthened aquatic food chains. Based on our findings and further evidence from the literature, we propose that warming regional climates are capable of contributing to declines in both condition and [Hg] of fishes. Because fish condition affects both reproductive success and overwinter survival, observed condition declines of the magnitude reported here could have profound implications for the structure of future aquatic ecosystems in a warming climate.     

Two Mummies From The Pitchfork Rock Shelter In Northwestern Wyoming

Abstract

A protohistoric rock shelter burial from the Pitchfork Site in northwestern Wyoming produced two partially mummified skeletons of young adult male American Indians. Preserved clothing, buffalorobes, trade goods and additional cultural items were present. Equally well preserved is the twisted and braided scalp hair of one mummy, andother bodily tissues sufficiently preserved to reveal forms of cultural modification and ornamentation. Osteological analysis of the specimens reveals patterns of physical characteristics typical of Late Prehistoric and protohistoric populations of the northwestern Plains.     

Notes on Omaha Ethnohistory, 1763-18201

Abstract

When first known to Whites, the Omaha were east and north of the Missouri River; they are not reported west of that stream until the late 18th century. At that time they occupied parts of what is now northeastern Nebraska, with their major villages and hunting territory in that area. Trade influences, direct and indirect, probably first reached them in 1700. Contact with the Spanish and later French was principally economic, but there were accompanying major changes in political organization, especially in the authority of chiefs, even before the time of Lewis and Clark.     

Geographic variation in reproductive success of the parasitoid Asobara tabida in larvae of several Drosophila species

Abstract.

• 1 Asobara tabida is a parasitoid of Drosophila larvae in fermenting substrates. Because it is a widespread species, it may encounter different biotic and abiotic circumstances in various parts of its range.
• 2 The species composition of the host population varies over the parasitoid's range: D.obscura-group species (especially D.subobscura) are the main hosts for northwestern and central European parasitoids; D.melanogaster is the main host for southern European parasitoids.
• 3 D.melanogaster larvae can defend themselves against A.tabida by encapsulating the parasitoid egg, and survival in D.melanogaster is always lower than in D.subobscura.
• 4 Parasitoids from southern European populations are much better able to survive in D.melanogaster than their northwestern and central European conspecifics; parasitoids from different populations are equally well able to survive in D.subobscura.
• 5 The lower survival in D.melanogaster may be partly compensated for by the larger size of parasitoids emerging from this host species compared to parasitoids emerging from D.subobscura.
• 6 Within population groups, larger A.tabida females have more eggs in their ovarioles. Additionally, southern European females have more eggs and less fat than northern and western/central European females. The relationship between size and longevity is ambiguous.
• 7 It is concluded that parasitoids from different populations are adapted to region-specific circumstances.

     

High Country Adaptations

Abstract

A general model of high country adaptations by hunters and gatherers is proposed. It is derived from a consi eration of the specific nature of high country resources and the social structure that seems to exploit them most efficiently. The general model is then illustrated by two test cases, one from northwestern Wyoming and one from southwestern Asia. The paper concludes with a comparative perspective. and discusses the problem of why Native Amen cans 1n the central Rockies failed to domesticate wild sheep while hunters and gatherers in southwestern Asia did.     

Microconchid encrusters colonizing land plants: the earliest North American record from the Early Devonian of Wyoming,USA

Caruso, JA. & Tomescu, AM.F. 2012: Microconchid encrusters colonizing land plants: the earliest North American record from the Early Devonian of Wyoming, USA. Lethaia, Vol. 45, pp. 490–494. Plant fossils in the Early Devonian Beartooth Butte Formation (Wyoming, USA) are colonized by microconchid encrusters which are found on several plant taxa, at two fossil localities in the formation, and whose tube coil diameters range from 230 to 1170 μm. Colonization is densest on broad Drepanophycus devonicus stems where microconchid individuals encompassing broad size ranges co‐occur in close vicinity. This indicates exposure to microconchid colonization and, therefore, submergence of the plant material for relatively extended periods of time prior to burial. For in situ preserved Drepanophycus, this suggests that the plants grew partially submerged and their submerged parts were colonized by microconchids while still alive. In turn, this indicates that by the Early Devonian microconchids were colonizing freshwater environments. The Beartooth Butte Formation provides the first record of plant colonization by microconchids in North America and, along with only one other Early Devonian record from Germany, the oldest evidence for microconchids colonizing plant substrates. □Devonian, encrusters, microconchid, vascular plants, Wyoming.     

First record of the freshwater snail Pseudosuccinea columella (Gastropoda: Lymnaeidae) in southern Pampas (Argentina) and assessment of future spread

ABSTRACT

The freshwater snail Pseudosuccinea columella was recorded for the first time in Argentina more than 60 years ago. Since then its distribution in the wild has been restricted to the northeastern provinces. Here we record the presence of P. columella in southern Pampas for the first time, extending its distribution more than 500?km southwards. The climatic suitability of this and other areas of South America for its establishment and spread was analysed using habitat modelling software. Hitherto its spread within and between watercourses in southern Pampas has been very limited, probably through a combination of low climatic suitability, recent introduction and low connectivity of the drainage basins. The suitability of other areas where it has been recently recorded indicates a moderate risk of further spread in central and northwestern Argentina and in coastal areas of the Pacific rim of South America (southern Perú and northern Chile). The recent spread of P. columella in the wild in Argentina may be the result of an increase in the trade in aquarium plants or of the evolution of a new lineage with different ecological capabilities.     

A Shoshonean Origin for the Plains Shield Bearing Warrior Motif

Abstract

The shield bearing warrior is a distinctive motif characteristic of the rock art of the Northwestern Plains. It also occurs commonly in the eastern Great Basin as an element of Fremont rock art. Detailed similarities between Plains and Great Basin shield figures suggest cultural relationships between the two areas. This has led some authors to propose that the motif originated in the Northwestern Plains and diffused to the Great Basin. Others argue that the motif spread from the Great Basin to the Plains. Relative dates recently obtained for shield figures at Northwestern Plains sites support the latter hypothesis. A Shoshonean origin for the Northwestern Plains shield figures is suggested by the dates, and the coincidence between the distribution of the motif, the distribution of diagnostic Shoshonean artifacts. and the ethnohistorically known range of the Plains Shoshone. It is suggested that the Shoshone borrowed the motif from the Fremont Culture during a period of interaction between the two groups.

The shield bearing warrior, a distinctive motif that depicts a pedestrian warrior whose body is represented by a large circular shield (Fig. 1), is frequently encountered in the rock art of the western United States. It is especially common at sites on the Northwestern Plains and in the eastern Great Basin (Fig. 2).     

Jemezius,a new omomyid primate from the early Eocene of northwestern New Mexico

Recently collected omomyid primate fossils from the early Eocene Regina Member, San Jose Formation, San Juan Basin, New Mexico, add significant new information to our knowledge of the family in the southern part of the Rocky Mountain region during Wasatchian time. A total of seven specimens represent at least two omomyid species on the basis of size alone, but only the larger of these species, here described as Jemezius szalayi, gen. et sp. nov., is currently known from sufficient material to permit an adequate taxonomic assignment. Jemezius possesses several traits in common with Uintanius that clearly reflect a close phylogenetic relationship between these genera, but lacks the specialized premolar hypertrophy characteristic of that genus. The presence of uintaniinin omomyids in New Mexico during the middle Wasatchian, well before their first appearance in Wyoming during Bridgerian time, supports the hypothesis that several of the exotic mammals that first appear in Wyoming near the Wasatchian-Bridgerian boundary may be immigrant taxa from the south.     

Seasonal variation in the diet of Redshank Tringa totanus in the Odiel Marshes,southwest Spain: a comparison of faecal and pellet analysis

Capsule Redshank diet from southern Europe during migration shows spatial and seasonal variations.

Aims To assess seasonal variation in Redshank diet at a major passage site, and to compare data derived from analysing pellets or faeces.

Methods At the Odiel Marshes in 2001, pellets from spring migration (39), autumn migration (121) and midwinter (15) were analysed, together with faecal samples from autumn (84).

Results The abundance of different invertebrate groups in pellets varied between seasons. In spring, Chironomus salinarius pupae and larvae dominated by volume, followed by Ephydridae larvae and the beetle Paracymus aenus. Polychaetes and molluscs dominated in autumn, and isopods in midwinter. In autumn, chironomid larvae, Mesembryanthemum nodiflorum seeds and Artemia cysts were relatively more abundant in faeces, whereas polychaetes, isopods, molluscs and cestode cysticercoids were more abundant in pellets. Harder and/or larger items were thus relatively more abundant in pellets than faeces. Pellet analysis gave more emphasis to mudflat prey, and faeces to saltpan prey.

Conclusion Pellet and faecal analysis give different results for wader diet, and it is useful to combine the two methods. However, they show significant correlations both in diet range and rank abundance of prey items. Redshank diet shows much seasonal and spatial variation in southern Europe.     

The Fremont Culture: Its Derivation and Ultimate Fate

Abstract

Aikens (1966) has proposed that Fremont-Promontory culture originated on the Northwestern Plains and representsan Athabascan migration into the Utah area at circa A. D. 500, their descendents, he suggests, were later forced back onto the Plains by the 12th century expansion of Shoshoneans from the Great Basin. He also proposes that FremontPromontory culture was ancestral to Dismal River culture. In this paper an alternative hypothesis is proposed, i.e., that Fremont and then Promontory cultures were sequential developments from an indigenous Utaztecan or proto-Utaztecan base and that there is no direct cultural relationship between theUtah cultures and the Dismal River aspect.