Justices and Injustices: the Order of St John,the Holy See,and the Appeals Tribunal in Rome

In the early seventeenth century it became customary for knights of Malta who committed crimes to appeal to the tribunal of the Apostolic Chamber (Audentia Camera) in Rome. The Grand Masters of the Order of St John in Malta blamed this practice on the advent of the Apostolic Visitor and Roman Inquisitor in 1574 and saw its activities as a direct infringement of their authority over members of the Order and their subjects in Malta. Therefore on occasions successive Grand Masters found ways to “protest” with the Holy See claiming that the activities of the Apostolic Chamber were a threat to their rule, but the Grand Masters could not go beyond protesting because the Order of St John was above all a Catholic religious institution and the Pope in Rome was its ultimate head.     

“Ill‐natured comparisons”: Racism and relativism in European representations of ni‐Vanuata from Cook's second voyage

Landes’ anthropological theorizing, highlighting the connections between race, gender, sexuality and class, expressed an Eastern European Jewish female praxis well-established by the late 1920s and early ‘30s when Landes began her research career. Landes’ changing Jewish identification through her life resulted from gendered aging and the reformulation of Jewish racialization processes in the U.S. Her late life reflections are evidence of what Susan Watkins calls ‘gendered late-style’ as well as Jewish conceptions of time as anti-linear and counter-normative. I investigate how her Jewish socialist Yiddish-speaking family background inflected her interpersonal and professional networks and her writings on anti-racist, class and gender-based themes.

Abbreviations: RLP: Ruth Landes Papers; NAA: National Anthropological Archives; SI: Smithsonian Institution; RBP: Ruth Benedict Papers; ASC: Archives and Special Collections Library; VCL: Vassar College Libraries     

Stable isotope dietary analysis of prehistoric populations from the Minusinsk Basin,Southern Siberia,Russia: a new chronological framework for the introduction of millet to the eastern Eurasian steppe

We report the results of stable carbon and nitrogen isotope analysis of 354 human and faunal samples from five archaeological cultures of the Minusinsk Basin, Southern Siberia – Afanasyevo, Okunevo, Andronovo, Karasuk and Tagar (ca. 2700–1 BC) – a key location in Eurasia due to its position on a northern corridor linking China and central Eurasia. The results indicate that the diet of Eneolithic to Middle Bronze Age (Afanasyevo to Andronovo) populations was primarily C₃-based, with C₄ plants only becoming an important component of the diet in the Late Bronze Age Karasuk and Early Iron Age Tagar cultures. Freshwater fish seems to have been an important constituent of the diets in all groups. The findings constitute the earliest concrete evidence for the substantial use of millet in the eastern Eurasian steppe. We propose that it was probably introduced from Northwestern China during the Karasuk culture at the start of the Late Bronze Age, ca. 1500 BC. We conclude with a discussion of the implications for the nature of pastoralist economies on the steppes.     

The China Maps of Jean-Baptiste Bourguignon d’Anville: Origins and Supporting Networks

Abstract

By 1735, Jean-Baptiste Bourguignon d’Anville had produced forty-one maps of the Qing Empire, or China, a process significantly more complex than scholars have hitherto appreciated. A close study of d’Anville’s maps and their originals has revealed their relationship with the different versions of a Chinese atlas, the first of which was completed early in 1718, the outcome of nearly a decade of collaborative surveying between officials of the Qing Empire and European missionaries. The precise origins of some of the maps are identified for the first time, and the network behind the remarkable intercontinental exchange of cartographical material that allowed d’Anville to produce his China maps is also discussed, thereby illustrating the central role of the French Jesuits, as well as the connection with St Petersburg.     

Late Mississippian (Early Carboniferous) brachiopods from the western Daba Mountains,central China

Qiao L. & Shen S.Z., September 2012. Late Mississippian (Early Carboniferous) brachiopods from the western Daba Mountains, central China. Alcheringa 36, 287–309. ISSN 0311–5518.

Fifteen brachiopod species in 12 genera are described for the first time from four intervals in the middle and upper parts of the Zhanpo Formation at the Huoyanxi section near Zhenba in the western Daba Mountains, southern Shaanxi, central China. The Zhenba brachiopod fauna is dominated by diverse and abundant species of Productida, together with some species of Athyridida, Orthida, Orthotetida and Spiriferida. It ranges from late Viséan to Serpukhovian in age based on the presence of Gigantoproductus species in association with diagnostic foraminifera and conodonts. This fauna generally shows palaeobiogeographical links with the palaeoequatorial realm, including Western Europe, the Moscow Basin, the Ural Mountains, Japan, eastern Tibet and South and North China. Its closest palaeobiogeographical affinity is with South China assemblages rather than those of North and Northwest China, therefore, indicating that the Zhenba area was palaeogeographically close to the South China Block and relatively far from the blocks in Northwest China (e.g., the Qilian Mountains and Qaidam Basin, Kunlun Mountains, Tarim Basin and Tianshan Mountains) during the late Viséan–Serpukhovian.     

Early Carboniferous brachiopod faunas from the Baoshan block,west Yunnan,southwest China

38 brachiopod species in 27 genera and subgenera are described from the Yudong Formation in the Shidian-Baoshan area, west Yunnan, southwest China. New taxa include two new subgenera: Unispirifer (Septimispirifer) and Brachythyrina (Longathyrina), and seven new species: Eomarginifera yunnanensis, Marginatia cylindrica, Unispirifer (Unispirifer) xiangshanensis, Unispirifer (Septimispirifer) wafangjieensis, Brachythyrina (Brachythyrina) transversa, Brachythyrina (Longathyrina) baoshanensis, and Girtyella wafangjieensis. Based on the described material and constraints from associated coral and conodont faunas, the age of the brachiopod fauna from the Yudon Formation is considered late Tournaisian (Early Carboniferous), with a possibility extending into earlyViséan.     

Ordovician series and stages in Chinese stratigraphy: steps toward a global usage

The first Chinese Ordovician series was erected by Lee & Chao (1924). Since then, many regional Ordovician series and stage names have been established and mostly published in Chinese. The present study is a review of these regional units with a discussion of their definitions and correlation to the international standard. Among them, the Ichang series, Neichiashan series, Chientangkiang series, Yushanian stage and Dawanian Stage are most important; all regarded as regional stage divisions in China. The Lower, Middle and Upper Ordovician Series with their new definitions (Webby 1998) are now accepted in China. The global stage names, which have been approved (Tremadocian and Darriwilian), and “Caradocian” and “Ashgillian”, which are potentially to be part of the global standard, should be formally used in China. The Darriwilian Stage is defined in a global stratotype section near Huangnitang, Changshan, SE China. Only two regional stage names, the Yushanian and Dawanian, still remain since the international correlation of these two units has not yet been resolved. The main type Ordovician successions of China are identified, revised and regional correlations briefly outlined.     

Possible fossil impression in sandstone from the late Palaeoproterozoic-early Mesoproterozoic Semri Group (lower Vindhyan Supergroup), central India

The Lower–Middle Ordovician Zitai Formation of the South China palaeoplate consists of a succession of purple red, nodular argillaceous limestones. Palaeogeographically, it is distributed along the southeastern margin of the Yangtze Platform, and is of late Floian to Dapingian age, correlative with the Dawan Formation of the Middle and Lower Yangtze Platform. In Shitai County, Anhui Province, East China, the Zitai Formation is rich in conodonts, enabling the recognition of four biozones based on first appearance data. Detailed palaeontological and biostratigraphical study of these conodonts reveals that the Ordovician conodont radiation in the Lower Yangtze Platform attained its first diversity peak low in the Oepikodus evae Biozone. This diversification is generally consistent with macroevolutionary trends of brachiopods of South China and graptolites of the Upper Yangtze Platform, but was earlier than that of trilobites and acritarchs of the same palaeoplate. Correlation with the sea-level curve for South China suggests that conodont diversity change during the Ordovician radiation was mainly controlled by regional sea-level fluctuations.     

Middle Devonian gastropods from Xiangzhou and Wuxuan,Guangxi, South China

Eighteen taxa of Middle Devonian (Givetian) gastropods, including two new genera and five new species, are présent in the Tungkangling and Yingtang Formations, Wuxuan and Xiangxhou counties, Guangxi Province, China. Pingtianispira tuberculata gen. et sp. nov., Wuxuanella nodusa gen. et sp. nov. and Wuxuanella luifengshanensis sp. nov., Crenulazone wuxuanensis sp. nov. and Murchisonia luifengshanensis sp. nov. are erected from this distinct fauna. The fauna is dominated by nodose and unusual murchisonioids and has strong European and other Old World realm affinities.     

Significance of Claraia from the Late Permian of South Guizhou,China

Recently collectée material of two Claraia taxa, Claraia zhiyunica Yang et al, 2001 and Claraia sp. nov. from the Late Permian of South China, are described. Late Permian Claraia species are compared with those from the Early Triassic, and the survival of Claraia across the mass extinction period across the Permian- Triassic boundary (PTB) is discussed.