Humayma's notched peak: a focus of Nabataean and Roman veneration and civic identity

The most distinctive landscape feature at the southern Jordanian site of Humayma is Jebel Qalkha's highest peak, which is split at the top by a wide notch. The Nabataean town of Hawara (Roman Hauarra/Hauara) was built on the plain immediately east of this peak. This paper draws on the site's foundation myth, petroglyphs, betyls and religious and civic structures to illustrate the significance of this notched peak for the site's ancient populations. The evidence suggests that this distinctive peak served as a focus of veneration and a marker of civic identity for Humayma's Nabataean and Roman inhabitants.     

Biodiversity and palaeoecology of Foulden Maar: an early Miocene Konservat-Lagerstätte deposit in southern New Zealand

Lee, D.E., Kaulfuss, U, Conran, J.G., Bannister, J.M. & Lindqvist, J.K., August 2016. Biodiversity and palaeoecology of Foulden Maar: an early Miocene Konservat-Lagerstätte deposit in southern New Zealand. Alcheringa 40, xxx–xxx. ISSN 0311-5518.

This paper highlights the biodiversity and palaeoecology of the 23 million year old Foulden Maar, the first Konservat-Lagerstätte deposit described from New Zealand and a key site for reconstructing early Miocene Southern Hemisphere terrestrial ecosystems. The 1000-m-diameter, ca 200-m-deep Foulden Maar volcanic crater lake was a closed system with anoxic bottom waters, capturing and preserving in exquisite detail organisms from the lake and adjacent rainforest. The fossils include numerous leaves, flowers with in situ pollen, fruits, seeds, fish and arthropods. Surrounding Foulden Maar was an evergreen, Lauraceae-dominated notophyll vine forest with a diverse understorey, lianes, epiphytes and mistletoes. Diverse pollination and seed dispersal modes are evident. Fish include larval to adult stages of articulated specimens of Galaxias, some with preserved soft tissue and a species of eel resembling Anguilla. The arthropod fauna comprises ca 20 families in the orders Araneae (spiders), Plecoptera (stoneflies), Odonata (dragonflies), Isoptera (termites), Hemiptera (true bugs), Diptera (true flies), Coleoptera (beetles), Trichoptera (caddis flies) and Hymenoptera (wasps, ants and bees), representing faunas typical of soil, leaf litter, forest floor or freshwater habitats. Many fossil taxa have close relatives in the extant New Zealand biota; others are now locally extinct. Coprolites containing quartz sands sourced from outside the lake indicate the presence of volant birds, presumably waterfowl. The Foulden Maar Lagerstätte is crucial for reconstructing Miocene lake and forest ecosystems in New Zealand, particularly the terrestrial arthropod component.

Daphne E. Lee [daphne.lee@otago.ac.nz], Department of Geology, University of Otago, PO Box 56, Dunedin, New Zealand., Uwe Kaulfuss [uwe.kaulfuss@otago.ac.nz] and Jon K. Lindqvist, [jonlind@ihug.co.nz], Department of Geology, University of Otago, PO Box 56, Dunedin, New Zealand; John G. Conran [john.conran@adelaide.edu.au], Australian Centre for Evolutionary Biology & Biodiversity and Sprigg Geobiology Centre, School of Biological Sciences, Benham Bldg DX 650 312, The University of Adelaide, SA 5005, Australia; Jennifer M. Bannister [jennifer.bannister@xtra.co.nz], Department of Botany, University of Otago, PO Box 56, Dunedin, New Zealand.     

‘Not All That Is White Is Lime’—White Substances from Archaeological Burial Contexts: Analyses and Interpretations

Archaeological burial contexts may include a variety of white substances, but few analyses have been published. This study reports on the physico‐chemical characterization of such residues from seven archaeological sites. It is often assumed that white materials from burial contexts are lime. Our findings demonstrate that they can be gypsum, calcite (chalk), aragonite, brushite, degraded metal, natural (gum) resins or synthetic polymer–based products. These may be present as the result of diagenetic processes, funerary practices or modern contamination. This paper provides an analytical approach for the holistic investigation of white materials encountered in burial contexts.     

Middle Cambrian to Lower Ordovician faunas from the Chingiz Mountain Range,central Kazakhstan

Tolmacheva, T.JU., Degtyarev, K.E., Samuelsson, J. & Holmer, L.E., December, 2008. Middle Cambrian to Lower Ordovician faunas from the Chingiz Mountain Range, central Kazakhstan. Alcheringa 32, 443–463. ISSN 0311-5518.

The middle Cambrian to Lower Ordovician back-arc sedimentary succession studied in the Kol'denen River and in the Zerbkyzyl Mountains of the central Chingiz Mountain Range is composed predominantly of siltstones, sandstones and volcaniclastic rocks with rare beds of micritic carbonates, black shales and cherts. Fossil assemblages including conodonts, lingulate brachiopods, arthropods, sponges and probable Tasmanites cysts were recorded both from the carbonate and chert beds showing that richly diverse marine environments existed directly adjacent to the volcanic arcs. The Kol'denen River localities contain a diverse upper Cambrian paraconodont assemblage of the open-sea affinity. The representatives of Rossodus, Cordylodus, Drepanodus and Variabiloconus, having an almost pandemic distribution and characteristic of basinal facies, dominate the Lower Ordovician conodont fauna. The Cambrian–Ordovician boundary transition is characterized by chert production that was more likely caused by a local productivity increase than by general changes in palaeooceanographic and palaeogeographical conditions.     

A ‘SMALL TOWN’ DISCOVERED TWICE: A FORGOTTEN REPORT OF MAJOR H. H. KITCHENER

Abstract

This paper revisits the contribution of the Palestine Exploration Fund (PEF) to the study of the ancient copper mines of Faynan, Jordan. It reveals that it was a PEF expedition that first reported smelting remains in the northern part of the Faynan region, and demonstrates that the reported remains are the Iron Age site of Khirbat al-Jariya.     

Development of Local Financial Systems in Mainland China

Two Beijing-based economic geographers present a comprehensive study of local financial systems in China. The paper analyzes the most recently available (2006) regional data on exogenous (state-owned, foreign-owned, and joint shareholder-owned) and endogenous (city commercial banks and rural credit cooperatives) banks, highlighting the differences between the country's coastal and the lagging rural provinces located in China's central and western macroregions. A key component of the analysis is the geographic distribution of bank branches and assets. Special attention is devoted to Shanghai, the country's traditional financial center, which has attracted the bulk of foreign-owned banks and financial service providers seeking entry into the vast Chinese market. Journal of Economic Literature, Classification Numbers: G21, G28, O18, P34. 9 figures, 3 tables, 54 references.     

The Impact of State-Controlled Banks on the Russian Banking Sector

A senior Russian economist examines the structure, governance, and balance sheets of state-controlled banks in Russia, which accounted for over 55 percent of the total assets in the country's banking system in early 2011. The author offers a credible estimate of the size of the country's state banking sector by including banks that are indirectly owned by public organizations. Contrary to some predictions based on the theoretical literature on economic transition, he explains the relatively high profitability and efficiency of Russian state-controlled banks by pointing to their competitive position in such functions as acquisition and disposal of assets on behalf of the government. Also suggested in the paper is a different way of looking at market concentration in Russia (by consolidating the market shares of core state-controlled banks), which produces a picture of a more concentrated market than officially reported. Lastly, one of the author's interesting conclusions is that China provides a better benchmark than the formerly centrally planned economies of Central and Eastern Europe by which to assess the viability of state ownership of banks in Russia and to evaluate the country's banking sector.     

关于郑州商城小型房基的几点认识

郑州商城房基最早发现于20世纪50年代,主要发现地点位于内城东北角的白家庄、外郭城西部的人民公园和内城北部的紫荆山铸铜作坊遗址内。目前发现的商城房基可以分为地面式、半地穴式和窖穴式三类。房基的形状有长方形、方形、圆形、不规则形等。但最常见的形状是长方形,有的房基在建造过程中或建造之后有举行祭祀礼仪的习俗。此外,本文还对郑州商城小型房基发现较少的原因进行了探讨。     

Geomorphic perspectives on the sterkfontein australopithecine breccias

Breccias in the upper Sterkfontein cave system levels have yielded artifact assemblages as well as Homo and Australopithecus africanus remains. As mapped by the author, this sytem can be subdivided into a northern sector, comprising small, bedding-controlled passageways, and a southern one with large galleries controlled by subvertical fracture zones and partly filled with two generations of external, detrital sediment. A four-stage model describes the development of these deposits. The implications of this study include: (1) The caves formed in one rather than two phases, as a result of structural rather than watertable controls. (2) The lowest strata of both depositional generations, 50–60 m below the hillcrest are probably the oldest. T. C. Partridge's Sterkfontein Formation only includes approximately the upper half of the stratigraphic column recognized here. Deposits underlying those he described are also fossiliferous and probably substantially older than the 2·8+ million year age attributed to the lower units of the Sterkfontein Formation. (3) The Sterkfontein Formation, as defined by Partridge, is a composite stratotype, comprising one surface exposure and another underground, at mid to upper levels in the system. Their stratigraphic relationships are obscure and since the lower boundary of the Formation also is in doubt, erection of a formal stratotype is premature. Deep-lying breccias may ultimately warrant another component, extending the Sterkfontein Formation to the lowest known levels of the cave system.