Journal articles on the topic 'Colophon'

AbstractThe manuscripts of the Iranian Pahlavi Yasna contain two consecutive colophons, the second of which relates the story of how their common ancestor manuscript, which combines the Avestan text of the Yasna with its Pahlavi version, was created. It is argued that Rōstahm Dād-Ohrmazd produced the first Pahlavi Yasna manuscript by taking the Avestan text from one manuscript and the Pahlavi text of a manuscript by Farrbay Srōšayār. Furthermore, it is argued that Rōstahm Dād-Ohrmazd wrote this manuscript both for himself and for Mahayār Farroxzād, who was from the province of Bīšāpuhr. The manuscript of Rōstahm Dād-Ohrmazd was then copied by Māhwindād Narmāhān, who composed the second colophon. This article also discusses the first colophon as it appears in the Iranian Pahlavi Yasna manuscript T54, which differs from other manuscripts of this group as it includes a passage written by a scribe called Kāyūs. It is argued that T54 was produced by Kāyūs, who added this passage to its first colophon. Furthermore, variant readings of these two colophons in two manuscripts of the Iranian Pahlavi Yasna, which also include Kāyūs's passage, are discussed. Unlike T54, Kāyūs's passage forms a separate colophon in these two manuscripts. It is suggested the two colophons are corrected according to the mindset of their respective scribes.

AbstractBald’s Leechbook, the most famous of the Old English medical collections, derives its name from a colophon in Latin hexameter verse that occurs on the final folio of the collection. Previous scholarly attention to the colophon has been nearly entirely directed at discerning the relationship of two named figures (Bald and Cild) and their role (if any) in the creation of Bald’s Leechbook. Yet given the rarity of verse colophons in Anglo-Saxon manuscripts and the unusual placement of this text at the end of a technical work in Old English, these verses also deserve study for their place within the larger genre of poetic colophons and framing texts from Anglo-Saxon England. This article examines for the first time the form of the colophon and its character as a work of Anglo-Latin verse as well as its relationship with the vernacular prefatory tradition associated with King Alfred.

As a note written directly by the copyist/owner of the manuscript outside the text of the manuscript, the colophon can serve as a source of information about the history of its manuscript. Not only that, colophons can also function as a source of past knowledge outside the manuscript’s tradition. This is as shown by the colophons contained in the Malay manuscripts collection of A.B. Cohen Stuart stored in the National Library of Indonesia. This research on colophon manuscripts was carried out using descriptive methods and philological work steps to analyze data sources in the form of colophons. The results of the analysis, it can be concluded that 38 Malay manuscripts from the collection of Cohen Stuart are estimated to have been collected during his duty as conservator at Bataviaasch Genootschap, Batavia (Jakarta) in 1862-1871. These manuscripts were copied and/or owned by as many as 22 copyists/owners who lived in 16 villages in Jakarta in the period 1863-1869, except for two manuscripts which are estimated to be dated to the 1840s. Most of the manuscripts were copied for commercial purposes, i.e. for rent or sale. In addition, this colophon analysis also reveals some of the history of the city of Jakarta in the 19th century, including the structure of government, the villages in Batavia, as well as the formation of the Betawi ethnicity and the livelihoods of its people.

The aim of the Colophon larval study was to enable researchers to identify the species found in the field; to use larvae as an alternative for adults in molecular studies; to comment on possible phylogenetic information that may contribute to the sub-familial placement of the genus; and to obtain habitat preference data. To achieve this, larvae of four Colophon species were examined and their main diagnostic morphological characters identified. Larvae live in a fairly homogeneous micro-habitat of moist, humus-rich soil in protected places such as under rocky overhangs and amongst the roots and tussocks of Restionaceae. Colophon larvae show small inter-specific differences and larval characters contributed little equivocal information from which phylogenetic support for family placement could be deduced. Apparently, as with many scarabaeoid groups (Trogidae, Scarabaeidae), larval morphology may not have diversified much from the basal ground-plan and it remains for other (adult) phylogenetically significant morphological characters or DNA to provide more clarity on Colophon’s subfamilial placement.

Injunctions to secrecy in the colophons of scholarly cuneiform tablets offer potential insights into the classification and protection of knowledge in Mesopotamia. However, most models of a body of “secret knowledge” defined by the so-called “Geheimwissen colophons” have found it difficult to account for a seemingly disparate corpus of protected texts. This study argues first for an expanded definition of intellectual protection, which leads to a larger corpus of protected texts. Through a case study of Late Babylonian colophons from Uruk, it is suggested that there is a strong correlation between texts related to the professional specialism of the tablet owner, and the occurrence of protective formulae in the colophon. This implies that it is fruitful to consider “secret knowledge” less as an abstracted corpus of esoteric texts and more as a mutable categorisation strongly linked to professional and individual intellectual identity.

In Mandaeism, to copy a manuscript is a meritorious act — a Mandaean copyist (usually a priest) may undertake the task as an exercise to remit his own sins, and those of his family — or he may be hired to perform the task for someone else. Almost all Mandaean manuscripts contain colophons; excluded are talismans and other short magical texts. In the case where the transmission of a Mandaean text spans, say, fifteen or sixteen centuries, a colophon may be very long. Copying the Mandaean Ginza is a major piece of work, for it is the most voluminous of all known Mandaean texts. Mark Lidzbarski's Ginza edition and translation did not include the colophons, the lists of scribes that are attached to the text.

The present volume marks the completion of a large research project by the Geological Survey of Denmark and Greenland (GEUS), focused on the northern part of the Palaeoproterozoic Nagssugtoqidian orogen of central West Greenland, and carried out by a team of Danish and international participants. The project comprised geological mapping as well as structural, geochronological, geochemical and economic geological studies. This volume contains reports on both Archaean and Palaeoproterozoic geology as well as a study of neotectonic brittle structures. The field work was carried out in 2000-2003 in the region between Nordre Strømfjord and Jakobshavn Isfjord (see e.g. van Gool & Piazolo 2006, this volume, fig. 1). The project had two immediate purposes, namely to establish an overview of the mineral resource potential of supracrustal rocks in the region between 66° and 70°15'N, and produce four new geological sheets in the Survey's 1:100 000 map series. The first collection of papers about the Nagssugtoqidian orogen, published by the Geological Survey of Greenland (GGU, now part of GEUS), dates back to 1979 (Korstgård 1979). The investigations in this period were mainly based on field descriptions and structural analysis of coastal areas in the southern and central parts of the orogen, combined with limited petrographical, palaeomagnetic and geochronological studies; the results also comprised the first 1:100 000 geological map from within the Nagssugtoqidian orogen (Olesen 1984). The Proterozoic age of the orogen had been established, but it was believed that most, if not all of the quartzofeldspathic basement gneisses were of Archaean origin. Subsequent work in the Nagssugtoqidian orogen by GGU in the 1980s showed that besides Archaean orthogneisses and supracrustal rocks, the central part of the orogen also comprises the root zone of a Palaeoproterozoic magmatic arc and associated panels of Palaeoproterozoic volcanic and metasedimentary rocks (Kalsbeek et al. 1987). These results were confirmed during further investigations by the Danish Lithosphere Centre (DLC) in 1994-1999, and the plate-tectonic collisional history of the southern and central Nagssugtoqidian orogen was described in detail (van Gool et al. 2002). However, these studies added little to previous knowledge of the northern parts of the orogen in the Kangaatsiaq-Aasiaat-Qasigiannguit region, knowledge that was largely based on coastal reconnaissance by Henderson (1969) at the time when the entire orogen was still believed to consist of Archaean rocks. Another project preceding the present work was carried out by GGU in 1988-1991 immediately north of the Nagssugtoqidian orogen, in the southernmost part of the likewise Palaeoproterozoic Rinkian fold belt (Disko Bugt project, Kalsbeek 1999). It was shown that also the latter region comprises Palaeoproterozoic (meta)sedimentary rocks, and that most of the Archaean basement is strongly overprinted by Palaeoproterozoic structures that were formed during overall W- or NW-directed lateral tectonic transport. Although these structures might be related to similar structures in the Nagssugtoqidian orogen, the relationship between the Nagssugtoqidian orogen and the Rinkian fold belt remained speculative. The only previous economic geological study of regional extent in central West Greenland was an airborne reconnaissance study supplemented by local field work, which was carried out in the early 1960s by Kryolitselskabet Øresund A/S. This work resulted in the discovery of a massive sulphide deposit at Naternaq (Lersletten), which was studied again in some detail in 2001 by the Survey (Østergaard et al. 2002) but not reported on in the present volume. The present volume comprises 12 papers with topics ranging geochronologically from mid-Archaean to Palaeogene, and geographically from the southern Nagssugtoqidian foreland to the central part of the Rinkian fold belt. Many of the papers deal with the northern part of the Nagssugtoqidian orogen and are related to the recent field work in that region, while a few contributions are rooted in DLC- or other projects. The papers have been arranged in approximate chronological order and are grouped in terms of their main subjects. The two first papers, by Hollis et al. and Moyen & Watt, deal with Archaean supra- and infracrustal rocks in the northern Nagssugtoqidian orogen: their origin, ages, and structural and metamorphic evolution. These papers provide insight into the age and origin of the continental crustal orthogneisses and granites that underlie most of the region, and discuss the relationships between the supracrustal and plutonic components, using zircon U-Pb age determinations and major and trace element geochemical characteristics. Also the question of Palaeoproterozoic tectonic overprint is discussed, with the conclusion from both study areas that most of the observed structures are Archaean. The third paper with focus on Archaean geology, by Stendal et al., describes a small gold prospect at Attu likewise in the northern Nagssugtoqidian orogen, and discusses the age of the prospect and its host rocks using Pb-Pb geochronology of magnetite. It is concluded that the host rocks at Attu may be as old as 3162 ± 43 Ma, and that the gold prospect itself is around 2650 Ma in age. The fourth paper, by Mayborn & Lesher, is a thorough review of the Kangâmiut dyke swarm in the southern Nagssugtoqidian orogen and its foreland. It includes new whole-rock and mineral chemical data, and a list of sampling sites and corresponding field data. The emplacement mechanism and depth of the dyke swarm are discussed in detail, and it is concluded that the dykes were emplaced during the initial rifting prior to the Nagssugtoqidian collision and that they are unrelated to subduction processes (contrary to the belief by some previous authors). The next three papers provide geochronological constraints on the ages of supra- and infracrustal rocks and the deformation and metamorphism in the northern Nagssugtoqidian orogen, and on late orogenic uplift in the central Rinkian fold belt. In the first of these papers Thrane & Connelly employ zircon U-Pb age determinations (mainly using the laser ICP-MS method), and for the first time provide unequivocal documentation that the Naternaq supracrustal belt is of Palaeoproterozoic age. Other zircon age data from a synkinematic granite southeast of Kangaatsiaq show that the large fold structures in this region are of Archaean age. The subsequent paper by Stendal et al. presents Pb-Pb ages and isotopic signatures of magnetite in amphibolites; the obtained ages are younger than 1800 Ma and are related to cooling of the orogen. Stepwise leaching Pb-Pb ages of monazite and allanite in pegmatites fall in the range of 1750-1800 Ma, and are interpreted to date the emplacement of these rocks. The third paper in this group, by Sidgren et al., deals with new 40Ar/39Ar ages of around 1790 Ma (hornblende) and 1680 Ma (muscovite) from Archaean and Palaeoproterozoic rocks in the central Rinkian fold belt, which are interpreted as orogenic cooling ages. The hornblende ages are significantly older than such hornblende ages previously obtained from the central and northern Nagssugtoqidian orogen, pointing to different uplift histories in the two regions. This may in turn suggest that the Rinkian continental collision preceded that in the Nagssugtoqidian orogen. Four of the remaining five papers deal with the Nagssugtoqidian structural evolution. In the first of these, van Gool & Piazolo present a new method of structural analysis, where a geographical information system (GIS) is used as a framework for visualisation and analysis of large amounts of structural data. The paper graphically presents an overview of thousands of data points within an area of approximately 160 × 180 km in the central and northern parts of the Nagssugtoqidian orogen. This interesting data set points directly towards the two next papers, where crustal-scale structures in the same region and their origin are discussed: Sørensen et al. address the prominent Nordre Strømfjord shear zone just south of this block, and describes the structural and metasomatic transition into the shear zone by means of aeromagnetic and lithological map patterns and geochemical data. Another paper, by Mazur et al., addresses a prominent break in the structural pattern within the Kangaatsiaq-Aasiaat area, where the southern part acted as a rigid block during the Nagssugtoqidian orogeny and thus preserved its Archaean structure. The fourth paper in this group, by Korstgård et al., combines rock and aeromagnetic data to discuss the relationship between structure, metamorphic facies and total magnetic field intensity anomalies in the southern Nagssugtoqidian orogen. The authors show that static metamorphic boundaries are gradual, whereas boundaries along deformation zones are abrupt. The last paper, by Wilson et al., is a novel remote sensing and field geological analysis of onshore brittle structures related to the complex Ungava fault zone in the Davis Strait, which developed during the Cretaceous-Palaeogene opening of the Labrador Sea - Davis Strait - Baffin Bay seaway. The study area is located in the central Nagssugtoqidian orogen, and the authors carefully establish a distinction between old Nagssugtoqidian and younger structures in the basement rocks and identify five main sets of young lineaments. They conclude that the onshore fault patterns are predominantly of strike-slip nature, and that they reflect the stress fields that governed the opening of the seaway. Acknowledgements The editors are grateful to the 14 external reviewers, each of whom reviewed one or more of the individual papers, for their thorough and constructive work.

The following extract comes from a recently discovered Xanthippic dialogue, which tells the story of Archeanassa's return to her native Colophon. Archeanassa travelled, it appears, as the emissary of Plato, who had instructed her to recover the manuscripts of the poet Antimachus, ostensibly for the library of the Academy, but in all probability to take revenge on the poet by burning his literary remains. (See Phryne's Symposium, 1176a, for an account of the distressing relationship between these three people.) The dialogue exists only in fragments: some concern Archeanassa's adventures on the journey, others describe the city of Colophon, now a Persian administrative centre, its Greek culture extinguished, its temples in ruins, and its streets darkened by high-rise buildings. The inhabitants visit the town either for work, or for the girls who dance in the night-clubs. One such girl is Perictione, grand-daughter of the great Perictione, whose talent as a dancer would have been famous throughout Hellas, had not her son Plato done his utmost to conceal it. How Perictione the younger came to Colophon the dialogue does not tell, although it seems that she lived well and independently, was a leading member of the Greek community, and retained the interest in philosophy which had been awakened at Phryne's symposium.

Abstract This paper unfolds parts of the dynamic, yet mostly hidden, history of MS Sinai Arabic 151 based on its paleographical, codicological, paratextual, and textual features. Combining these aspects opens new horizons of research in the Arabic Bible manuscripts that had previously received attention limited solely to the text. MS Sinai, Ar. 151 is an intact manuscript containing the Pauline Epistles, Acts of the Apostles, and the Catholic Epistles. Its fame derives mainly from its colophon, which dates it to 867 CE, and bestows it with the distinction of belonging to the earliest Arabic Bibles. In observing the various stages through which the manuscript evolved from two separate units of production into the codex preserved today, several aspects of the life of MS Sinai, Ar. 151, such as the copies made from it, its damage and restoration, and the functions it served, become clearer. Furthermore, for different reasons, scholars have cast shadows on its colophon’s authenticity. Our investigation clarifies that there is no reason to suspect the authenticity of the colophon.

Abstract As shown in recent studies, East Syriac colophons were rather standardised, at least in the Ottoman period, and they incorporated into the main colophon body not only prose passages, but also poetic ones. The current article discusses one such passage that occurs in both prose and poetic forms in various manuscripts, namely the topos of ‘the five twins that pulled a yoke from the forest through the white field’. It provides a fascinating example of the trope’s transmission over the centuries, as well as the poetic creativity of East Syriac scribes as manifested in the Ottoman period.

The flightless Cape High-mountain stag beetle genus Colophon (Coleoptera: Lucanidae) is studied. All species are endemic to the Cape Floristic Region of the Western Cape, South Africa. The study aimed to determine the specific and phylogenetic status of the described species of Colophon and to determine the main factors driving their evolution by testing the hypothesis of a lowland origin. This was achieved by analysing the mitochondrial COI, 16S rRNA and nuclear CAD genes, using a maximum likelihood and Bayesian approach. Timing of key biogeographical events in the diversification of Colophon was estimated in BEAST. The combined molecular dataset supports the described species. High genetic divergence was found between the described taxa. The mean estimated divergence of the genus was mid-Cretaceous, with a split into two lineages during the early Paleocene to mid Eocene. Species divergence was shown to have occurred during mid to late Miocene. Most species of Colophon showed an allopatric distribution, although contact zones between geographically adjacent species are likely. Climate seems to be the main driving factor behind Colophon evolution and the hypothesis of a lowland origin appears to be supported.

Abstract According to the colophon to the 1st-century Cave 11 Psalms Scroll, the psalmist David was a composing scribe endowed by the divine spirit. In the light of a pattern of legitimation by the divine spirit for social power well attested in the HB, we can discern how the colophon attributes divine efficacy for social power—hitherto exercised only through persons—to David's psalms as they resound in Israel's calendric communal cultic observances. The 11Q Psalms Scroll colophon provides early evidence for an enduring understanding of Scripture as a socially potent spiritual phenomenon that shapes the life of a religious community.

This Review of Survey activities presents a selection of 22 papers reflecting the wide spectrum of activities of the Geological Survey of Denmark and Greenland, from the microscopic to the plate-tectonic level.The Survey's activities in Denmark are illustrated by 13 articles. Five of them deal with petroleum-related topics and two others with groundwater-related topics. Four others describe raw material activities and environmental change, one paper presents a new Base Quaternary map of Denmark and one paper describes the deep structure below Denmark.Activities in Greenland are covered by five papers. Three of these address mineral and petroleum exploration, one concerns monitoring of the Greenland ice sheet and one focuses on historic investigations of Hans Ø, a small island in Nares Strait between Greenland and Canada.International projects and two new geoscientific methods: The survey also carries out many projects outside Denmark, Greenland and the Faroe Islands. This bulletin includes descriptions of a coastal protection project in Kenya and a multinational project dealing with the implementation of the European Union's Water Framework Directive. Finally, two examples of new developments in instrumental geoscience are presented.

Abstract The final form of the Martyrdom of Polycarp has often been dated to the late fourth century on the basis of an alleged link between the “Pionius” who edited its final colophon and the anonymous author of a clearly apocryphal Life of Polycarp. In this article, I argue that the correlation between these two texts is problematic at best and should be discarded in light of recent scholarship. To replace this outdated construct, I submit that the variant Moscow colophon manuscript tradition, generally considered the latest edition of the text, betrays traces of an earlier polemical milieu that may allow us to redate the colophon to the third or early fourth century.

“Graphic design” was not a proper term until the beginning of the twentieth century. This led to confusion in credits/authorship for book covers, typography, which was exacerbated by the fact that printers, in addition to being in charge of the production process of books, were also making decisions regarding their finishings. Venezuela presents an interesting chapter in the history of publishing in the world given the hybrid character of publishing in the country in which traditional national artists, illustrators, and publicists comprised a mix of European and North American immigrants. The lack of current bibliographic material inspired me, as a researcher, to make a timeline of the political and graphic history of the country through its colophons. Colophons, which appear at the end of books and thus are often ignored, are nonetheless providers of essential information—witnesses of our progress in authorship and as a society.

The purpose of this article is to specify a very important feature of the colophons in the Armenian manuscripts - their exemplary character. The objective of the work is to present the importance of colophon-exemplares in codicology. The work is written applying the historical-comparative and comparative methods. The results of the research show that though colophons are mostly written in colophon-patterns, there are colophon-exemplares of a complete colophon too. There is a typical colophon-exemplar in the Ms. 2335 of Matenadaran (M, Jerusalem, 1476), and there are examples of inscriptions-colophons: a colophon for writing on a fountain and on a cup in the Ms. M 3461 (Tʻokhatʻ, 1662). Comparing the information of the colophons written in the same colophon-exemplar of the manuscripts M 3633, 5664, 6059, 8454, 8578, we clarified the "kinship" connections of those manuscripts. We also found out the place of writing of the Ms. M 8578 (Moks province), as well as who the scribe Sargis was. He is Sargis Hizantsʻi, the brother of the famous miniature painter Martiros Hizantsʻi from Hizan province. In other words, due to collecting and classifying colophons written on the basis of the same colophon-exemplar, it is possible to find out not only various data concerning the circumstances of the origin of those manuscripts, but also to solve various codicological issues.