THE BEGINNING OF THE EARLY DYNASTIC PERIOD AT UR

Iraq ◽  
2014 ◽  
Vol 76 ◽  
pp. 1-17 ◽  
Author(s):  
Giacomo Benati

This article presents a reconsideration of the architecture, stratigraphy and finds from Building Level H, excavated in Trial Pit F at Ur. Analysis of Woolley's original excavation records, kept at the British Museum, provides the basis for a contextual reconstruction. A new complete study of published and unpublished materials now housed at the British Museum and at the Penn Museum of Philadelphia is offered here. Distribution of in situ artefacts is examined here in order to provide insights on the function of the excavated loci. Finally, pottery and glyptic assemblages, considered from a regional perspective, are used to define the chronological horizon of Level H.

Author(s):  
G. T. Prior

In connection with the investigation of ægirine-anorthoclase rocks from Abyssinia, belonging to the grorudite-tingusite series, an examination was made of specimens of the so-called green phonolite from Elfdalen, which in the British Museum collection accompanied the more ordinary brown and red porphyry from that locality. In the descriptions of the well-known porphyry quarries of Elfdalen, mention is made of this green variety as occurring only in boulders. Törnebohm was the first to record the occurrence of these rocks in situ, and to describe their characters, They were found in the form of dykes in the neighbourhood of Heden, near Särna, Dalarne, Sweden, and were interesting as containing cancrinite in clear, well-defined porphyritic crystals as undoubtedly a primary constituent.


Radiocarbon ◽  
1991 ◽  
Vol 33 (1) ◽  
pp. 51-68 ◽  
Author(s):  
Janet Ambers ◽  
Keith Matthews ◽  
Sheridan Bowman

The following list consists of dates, obtained by liquid scintillation counting of benzene, for archaeologic samples mostly measured between June 1987 and October 1989.Charcoal and grain samples were pretreated with 1M HCl followed by washing in water and, where considered necessary, with dilute alkali for the removal of humic acids. Wood samples were treated either in the same way, or, where large enough, were reduced to cellulose by the action of chlorine dioxide produced in situ. All antler and bone samples were treated with cold dilute acid. The term ‘collagen’ is used throughout to mean the acid insoluble organic fraction produced by this treatment. Peat samples were treated with dilute acid and alkali to separate the humin and humic acid fractions, which were dated individually.


Radiocarbon ◽  
1994 ◽  
Vol 36 (1) ◽  
pp. 95-111 ◽  
Author(s):  
Janet Ambers ◽  
Sheridan Bowman

The following list consists of dates for archaeological samples measured mostly between October 1989 and November 1990. Charcoal and grain samples were pretreated with 1M HC1 followed by washing in water and, in the majority of cases, with dilute alkali for the removal of humic acids. Wood samples were treated in the same way, or, if large enough, reduced to cellulose with chlorine dioxide produced in situ. Antler and bone samples were treated with cold dilute acid. We use the term “collagen” to mean the acid-insoluble organic fraction produced by this treatment rather than the true biochemical definition.


1970 ◽  
Vol 37 (292) ◽  
pp. 880-887 ◽  
Author(s):  
G. J. H. McCall ◽  
P. M. Jeffery

SummaryThe fall of a shower of meteorites numbering several hundred fragments at Wiluna, Western Australia, on the night of 2 September 1967, has been investigated. Although the dispersion ellipse had been largely obscured by removal of fragments before a party of scientists were able to make a field investigation, it has, nevertheless, been possible to make a reasonable estimate of the shower distribution pattern. In spite of this removal of fragments, a number of pieces of meteorite were still found in situ. The bulk of the total recovery is in the collections of the Western Australian Museum, and the physical characteristics of these masses and their petrography is described. In all, some 490 individual fusion-crust coated stones and a large number of broken stony fragments are known to have been recovered. The meteorite is an olivine bronzite chondrite remarkably rich in discrete nodules of nickel iron, up to an inch across, commonly aggregated with troilite. A full chemical analysis of this fresh meteoritic material has been supplied by the British Museum (Natural History).


2006 ◽  
Vol 7 ◽  
pp. 307-311
Author(s):  
M. G. Sotillo ◽  
M. L. Martín ◽  
F. Valero ◽  
M. Y. Luna

Abstract. Generation of a Mediterranean long-term (1958-2001) homogeneous high resolution environmental database constituted the main objective whitin the HIPOCAS Project. The high number of parameters included in this database allows a complete characterization of Mediterranean storms. In this paper, the HIPOCAS precipitation reliability over the Iberian Peninsula and the Balearic Islands is evaluated against long-term in-situ observations from Iberia. In order to provide a more complete study, comparisons of the HIPOCAS field with NCEP/NCAR and ERA global reanalysis show the important improvement in the characterisation of the observed precipitation introduced by the HIPOCAS hindcast.


2021 ◽  
Vol 12 ◽  
Author(s):  
Ana Castaño ◽  
Alexander Prosenkov ◽  
Diego Baragaño ◽  
Nerea Otaegui ◽  
Herminio Sastre ◽  
...  

Nanoscale Zero-Valent Iron (nZVI) is a cost-effective nanomaterial that is widely used to remove a broad range of metal(loid)s and organic contaminants from soil and groundwater. In some cases, this material alters the taxonomic and functional composition of the bacterial communities present in these matrices; however, there is no conclusive data that can be generalized to all scenarios. Here we studied the effect of nZVI application in situ on groundwater from the site of an abandoned fertilizer factory in Asturias, Spain, mainly polluted with arsenic (As). The geochemical characteristics of the water correspond to a microaerophilic and oligotrophic environment. Physico-chemical and microbiological (cultured and total bacterial diversity) parameters were monitored before and after nZVI application over six months. nZVI treatment led to a marked increase in Fe(II) concentration and a notable fall in the oxidation-reduction potential during the first month of treatment. A substantial decrease in the concentration of As during the first days of treatment was observed, although strong fluctuations were subsequently detected in most of the wells throughout the six-month experiment. The possible toxic effects of nZVI on groundwater bacteria could not be clearly determined from direct observation of those bacteria after staining with viability dyes. The number of cultured bacteria increased during the first two weeks of the treatment, although this was followed by a continuous decrease for the following two weeks, reaching levels moderately below the initial number at the end of sampling, and by changes in their taxonomic composition. Most bacteria were tolerant to high As(V) concentrations and showed the presence of diverse As resistance genes. A more complete study of the structure and diversity of the bacterial community in the groundwater using automated ribosomal intergenic spacer analysis (ARISA) and sequencing of the 16S rRNA amplicons by Illumina confirmed significant alterations in its composition, with a reduction in richness and diversity (the latter evidenced by Illumina data) after treatment with nZVI. The anaerobic conditions stimulated by treatment favored the development of sulfate-reducing bacteria, thereby opening up the possibility to achieve more efficient removal of As.


The Geologist ◽  
1860 ◽  
Vol 3 (9) ◽  
pp. 328-328 ◽  
Author(s):  
S. P. Woodward
Keyword(s):  

Opercula of Ammonites are common in many localities, especially in banks and sections of the Kimmeridge Clay; but they usually occur in broken fragments, and very rarely with their valves paired, unless sheltered within the last whirl of the shell to which they belonged. Even when thus protected the valves are generally displaced, as might be expected if we consider how slight is their union along the suture, and how great were the chances of being shifted by the contraction of the animal after death, by the pressure of external mud.The British Museum contains several examples of Ammonites Jason, A. Brightii, A. fluctuosus, A. lingulatus, and other species with their opercula more or less shifted; and Mr. Charles Moore, of Bath, has several small shells of Ammonites planorbis from the Lower Lias, with the opercula remaining in their true position; the smallest individual is only one quarter of an inch in diameter.


PMLA ◽  
1932 ◽  
Vol 47 (3) ◽  
pp. 759-765
Author(s):  
Chas. W. Cooper

The recent inclusion of the triple-portrait of John Lacy in Shakespeare Improved prompts the question: How certain is it that the picture shows a character from a Restoration “improvement” of Shakespeare? The identification of one of the figures as Sauny the Scot in the Restoration adaptation of The Taming of the Shrew must rest upon more than The Catalogue of Engraved Portraits in the British Museum and Wheatley's annotation of Evelyn. It must, as will be shortly apparent, rest upon a complete study of the history of the portrait and of the actor's rôles.


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