scholarly journals A 3000-Year Culture Sequence from Palau, Western Micronesia

2005 ◽  
Vol 44 (2) ◽  
pp. 349-380 ◽  
Author(s):  
Geoffrey R. (Geoffrey Richard) Clark
Keyword(s):  
1970 ◽  
Vol 50 (1) ◽  
pp. 67-85 ◽  
Author(s):  
Barry Cunliffe

SummaryExcavations at Portchester Castle have produced evidence of occupation throughout the Saxon period. After the cessation of standard Roman wares and local hand-made types early in the fifth century two Grubenhäuser were built. The contemporary assemblage, assignable to the mid fifth century, included (?) imported carinated bowls and local hand-made grass-tempered wares made in the Roman tradition. Late in the fifth or early in the sixth century stamped Saxon urns appear and probably continue, alongside the grass-tempered tradition, into the seventh century. An association of a grass-tempered pot with an imported glass vessel of eighth-century date shows that the local tradition persisted, but by the middle of the eighth century hand-made jars in gritty fabrics, like those from Hamwih, appear in a substantial rubbish deposit which belongs to the initial occupation of the hall complex. By the tenth century a new style of wheel-thrown pottery, called here Portchester ware, is dominant. It is mass produced and distributed largely from the Isle of Wight to central Hampshire and from the Sussex border to the River Mean. Contemporary forms include imported wares, green-glazed pitchers, pots from the Chichester region, and an assemblage made in a wheel-made continuation of the local gritty-fabric tradition. Portchester ware had gone out of use by 1100 at the latest.


1973 ◽  
Vol 38 (1) ◽  
pp. 101-111 ◽  
Author(s):  
W. Raymond Wood

AbstractThe Old Fort (23SA104), an earthwork enclosure and mound complex on a high ridge near the Missouri River in central Missouri, has long been considered a Middle Woodland or Hopewell construction. Excavations in 1970 cross-trenched prehistoric ditches and embankments on the north end of the enclosure. A well-developed soil profile containing predominantly Middle Woodland pottery was exposed, into which aboriginal ditches had been cut. Oneota pottery lay on the floors of these ditches, embedded in a thin laminated horizon of alluvium. Oneota and Middle Woodland pottery are mixed in ditch fills. Field data, although limited, thus support the identification of the enclosure as Oneota, aboriginally constructed on a Middle Woodland habitation site.


1936 ◽  
Vol 16 (3) ◽  
pp. 260-264 ◽  
Author(s):  
J. P. T. Burchell

Archaeologists in France have for many years recognized hand-axes of St. Acheul facies in association with flake-implements of Levallois type, which are contemporary with the mid-Pleistocene deposits of the Somme valley. Their place in the culture-sequence is after the cold period that produced the main Coombe-rock of South-East England, and the Little Eastern or Upper Chalky Boulder-clay of East Anglia. The Coombe-rock referred to overwhelmed the Levallois II factory-site at Baker's Hole, Northfleet, Kent.In England, however, it has taken much longer to trace these mid-Pleistocene hand-axes in contemporary beds. The first was found by the late F. G. Spurrell on the classic ‘floor’ at the base of the Crayford Brickearth, though it was not until quite recently that the correct age of the Crayford series was determined. This specimen is now in the British Museum (Natural History), but is not figured in the present note.


1934 ◽  
Vol 7 (3) ◽  
pp. 366-372 ◽  
Author(s):  
J. P. T. Burchell

In 1931 I described two newly-discovered stone age industries of post-glacial age situated in north-east Ireland which had been made by myself and worked in conjunction with my friend C. Blake Whelan: the one from the Lower Estuarine Clay on Islandmagee, and the other from what is probably a fluviatile gravel intercalated between the Upper and Lower Estuarine Clays in the raised-beach formation at Cushendun.The former of these cultures has its counterpart in the blade industry beneath alluvium in the Orwell Estuary at Ipswich, Suffolk; whilst the latter finds its parallel in the raised-beach at Campbeltown in Argyllshire, Scotland. Adopting the familiar culture-sequence of Central Europe I had previously designated these two groups as phases of the Magdalenian period, but, in order to avoid confusion between the time-periods and the nomenclature of continental cultures, I have decided to base my chronology of the north Irish industries upon the natural changes of climate revealed by a study of the deposits in which they were found. The industries to be described below were contemporary with the Mesolithic Forest Cultures distinguished by Childe and Clark over the plain of northern Europe.


2018 ◽  
Vol 44 ◽  
pp. 306-325 ◽  
Author(s):  
Malcolm C. Lillie ◽  
Chelsea E. Budd ◽  
Inna D. Potekhina ◽  
Douglas Price ◽  
Mykhailo Sokhatsky ◽  
...  

This paper presents an analysis of human and animal remains from Verteba cave, near Bilche Zolote, western Ukraine. This study was prompted by a paucity of direct dates on this material and the need to contextualise these remains in relation both to the transition from hunting and gathering to farming in Ukraine, and their specific place within the Cucuteni-Trypillia culture sequence. The new absolute dating places the remains studied here in Trypillia stages BII/CI at c. 3900–3500 cal BC, with one individual now redated to the Early Scythian period. As such, these finds are even more exceptional than previously assumed, being some of the earliest discovered for this culture. The isotope analyses indicate that these individuals are local to the region, with the dietary stable isotopes indicating a C3 terrestrial diet for the Trypillia-period humans analysed. The Scythian period individual has δ13C ratios indicative of either c. 50% marine, or alternatively C4 plant inputs into the diet, despite δ18O and 87Sr/86Sr ratios that are comparable to the other individuals studied.


1992 ◽  
Vol 12 (9) ◽  
pp. 4123-4131 ◽  
Author(s):  
S M Smolik ◽  
R E Rose ◽  
R H Goodman

In this report, we describe the isolation and initial characterization of a Drosophila protein, dCREB-A, that can bind the somatostatin cyclic AMP (cAMP)-responsive element and is capable of activating transcription in cell culture. Sequence analysis demonstrates that this protein is a member of the leucine zipper family of transcription factors. dCREB-A is unusual in that it contains six hydrophobic residue iterations in the zipper domain rather than the four or five commonly found in this group of proteins. The DNA-binding domain is more closely related to mammalian CREB than to the AP-1 factors in both sequence homology and specificity of cAMP-responsive element binding. In embryos, dCREB-A is expressed in the developing salivary gland. A more complex pattern of expression is detected in the adult; transcripts are found in the brain and optic lobe cell bodies, salivary gland, and midgut epithelial cells of the cardia. In females, dCREB-A is expressed in the ovarian columnar follicle cells, and in males, dCREB-A RNA is seen in the seminal vesicle, ejaculatory duct, and ejaculatory bulb. These results suggest that the dCREB-A transcription factor may be involved in fertility and neurological functions.


1952 ◽  
Vol 17 (4) ◽  
pp. 348-351 ◽  
Author(s):  
Joel L. Shiner

The river Basin Surveys' program, particularly in the Columbia River Basin, has had a peculiar role in American archaeology. Generally speaking, archaeological research programs should be oriented toward a specific problem such as the study of a certain culture sequence or an inquiry into a particular time horizon. In contrast River Basin Surveys' problem has been to examine in detail almost every phase of every culture that is represented over a vast area. True, the field of research has been limited to those portions of river basins that are scheduled to be inundated upon the completion of a number of dams, but because of the aridity of the Columbia Basin a vast majority of the aboriginal population was concentrated along the major streams. Thus the reservoirs planned for those streams will flood a large portion of the cultural material existing in the region.


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