Variety in cereal cultivation in the Late Bronze and Early Iron Ages in relation to environmental conditions

The objective of this paper is to assess the relationship between the cereals cultivated in the Late Bronze and Early Iron Ages (ca. 1250–400 BC) within the area of the present-day Czech Republic, and their environmental settings. The various charred caryopses of cereal species represented in the archaeobotanical assemblages from 35 archaeological sites differ, especially in the proportion of wheat and barley. The cereal assemblages were compared regarding site altitude, weather conditions, soils and soil productivity. The most important environmental variable influencing the choice of a particular crop seemed to be altitude which is correlated with other variables such as the length of growing season, mean annual temperature, soil quality etc. Although the ecological requirements of cereals cultivated in the Late Bronze and Early Iron Ages are not known, they presumably thrived under similar conditions to present-day species/varieties, and the strategy of past crop husbandry was based on similar principles as today, e.g. flexible adaptation to local environmental conditions, in an effort to achieve optimal yields and reduce the danger of crop failure.     

Urban regeneration in Poland’s non-core regions

ABSTRACT

After many years of efforts aimed at reaching a cohesive and inclusive socio-economic development, Poland keeps witnessing some significant disparities in the distribution of wealth. Moreover, these disparities intensified in the course of the post-socialist transition and they have not been diminished by the regional policy of the EU. In this light, urban regeneration appears as an important, emerging sphere of public intervention intended to support the less developed regions. The objective of this study is twofold: first, to characterize the place of urban regeneration in the Polish strategic planning system, and second, to carry out an in-depth analysis of planning strategies and practices of urban regeneration at the regional level and conclude with recommendations for planning. The latter is achieved by examining the Polish experience with urban regeneration practices in the 1999–2015 period using Wielkopolska region as a case study. In order to reach this objective: (a) all strategic documents related to urban regeneration have been collected and analysed, (b) a survey has been conducted in 100 cities and towns of the region and finally (c) 50 interviews have been carried out with various stakeholders involved in the urban regeneration process. The article concludes with recommendations for planning and further urban regeneration projects aiming to alleviate the development disparities between core and non-core regions.     

Chemical analysis of white porcelains from the Ding Kiln site, Hebei Province, China

The Ding kilns were some of the most famous early kilns of medieval China, producing huge quantities of white and cream-white porcelains of outstanding technical and aesthetic quality. Since 1949 they have been excavated three times, in 1965, in 1987, and in 2009 respectively. In this latest study 69 white porcelain sherds from assured contexts and from the 2009 excavations were analyzed using laser ablation techniques (ICP-AES). The samples date from Five Dynasties, Northern Song and Jin Dynasties respectively (early 10^th to early 13^th C CE). The results show that Ding wares of different times show different characteristics that can be demonstrated through chemical composition. During the early phase of production the Ding ware bodies consisted largely of high firing kaolinitic clays with predominantly calcareous materials as fluxes. After the early Northern Song Dynasty, some calcareous material was replaced by a more potassic material. The compositions of the glazes show a parallel evolution to the bodies. However, because the glazes are very low in titania it seems unlikely that the main clay ingredients of the bodies could have been used in the glaze recipes. For much of the kiln site’s history the glazes appear to have been made mainly from the same siliceous flux-rich materials that had been blended with the main body-clays used to make the Ding ware porcelains, plus some extra calcareous material. The P₂O₅ contents of the glazes suggest that wood ash may have been one source of CaO in the glaze recipes.     

Contesting Conquests: Nineteenth-Century German and Polish Historiography of the Expansion of the Holy Roman Empire and the Polish-Lithuanian Union

The problem of conquests and territorial expansion, including their interpretation, evaluation, and legitimisation, has been crucial for European national historiographies. Consequently, attempts by the Holy Roman emperors, particularly of the Saxon and Hohenstaufen dynasties, to control Italy and Burgundy were hotly debated among nineteenth-century German historians, while Poland's union with Lithuania, and the annexation of the vast territories of the east which followed, was a central topic for Polish historians of the time. Modern historians of historiography in both countries have carefully analysed these narratives, emphasising their ideological and political contexts, such as their involvement in the Grossdeutsch versus Kleindeutsch controversy and the controversy between the so-called Cracow and Warsaw historical schools. In this paper I propose a comparative analysis of these two discourses which dealt with analogical issues and, as I demonstrate, developed with a parallel dynamic. Such an analysis, I argue, allows an escape from the paradigm of national exceptionalism, and the discovery of what was typical or, perhaps, constitutive of the discourse on territorial expansion of the time, instead of focusing on the uniqueness of the national context. This analysis embraces the conceptualisation, argumentation, and rhetoric of those nineteenth-century German and Polish historians discussing the expansion of the medieval Holy Empire and early-modern Poland. Moreover, it locates their interpretations within an international context of a broader Western historiographical tradition, involving issues of domination, cultural transfer, and colonialism. Finally, it examines the parallel mechanism of searching for, advocating, and perpetuating the idea of uniqueness of national history.     

New Late Permian rugose corals from Pahang,peninsular Malaysia

Aye Ko Aung, Ng Tham Fatt, Kyaw Kyaw Nyein & Myo Htut Zin, 2013. New Late Permian rugose corals from Pahang, peninsular Malaysia. Alcheringa 37, 422–434. ISSN 0311-5518.

Late Permian rugose corals are described from a limestone unit of the Gua Musang Formation at Selborne Estate, Padang Tengku area, Pahang, peninsular Malaysia. These include one genus, Iranophyllum, which is reported for the first time from Malaysia, with two new species Iranophyllum aequabilis and I. pahangense belonging to Waagenophyllidae. A Late Permian age is confirmed by a Paleofusulina–Colaniella–Reichelina foraminiferal fauna co-preserved with the corals.

Aye Ko Aung [akaung.mm@gmail.com], Ng Tham Fatt [thamfatt@gmail.com], Kyaw Kyaw Nyein [konyein@gmail.com], Department of Geology, University of Malaya, 50603, Kuala Lumpur, Malaysia and Myo Htut Zin [myohtutgreat@googlemail.com], Lab. Services, Pte. Co. Ltd., Singapore. Received 16.10.2012; revised 5.1.2013; accepted 17.1.2012.     

The analysis of two historic fired artificial stonewares: Coade stone (18th–19th centuries) and a recent discovery from Oxnead Hall,Norfolk (16th–17th centuries)

Coade stone has played a significant role in architectural and ornamental design since its inception in the early 18th century. It is well known that earlier, experimental, architectural stoneware products existed, but few of these have been studied in detail scientifically, and only one major analytical study of Coade stone has appeared in the literature. This paper presents a new spectroscopic analysis of Coade stone along with that of a newly discovered sample from Oxnead Hall in Norfolk where it known that Sir Clement Paston experimented with artificial stone in the late 16th century. The results demonstrate that it is possible to differentiate between the two variants on the basis of both the raw materials used and the different phases formed in their production processes.     

Complex Pathways Towards Emergent Pastoral Settlements: New Research on the Bronze Age Xindian Culture of Northwest China

Journal of World Prehistory - The Xindian culture of northwest China has been seen as a prototypical example of a transition toward pastoralism, resulting in part from environmental changes that...     

Record of the meso- and neoholocene palaeoenvironmental changes in the Jesionowa landslide peat bog (Beskid Sądecki MTS. Polish Outer Carpathians)

The paper presents an analysis of depositional sequences of landslide peat bog situated in the depressions developed within the landslide landforms Jesionowa in the Beskid Sądecki Mts. (Outer Carpathians). The peat bog, with depositional sequence 2.80 m long, started to form at the beginning of the Atlantic Phase ca. 6390–5910 cal BC. Palynological and lithological analyses as well as several (14) radiocarbon age determinations of different horizons in the sediments enabled the reconstruction of palaeoenvironmental changes during the Meso-and Neoholocene. The increase in climate humidity at the beginning of the Subboreal and Subatlantic Phases was observed as delivery of minerogenic material to the peat bog basin and formation of a mineral horizon and an illuvial level within the peat. The particularly intensive delivery of allochthonous material to the peat bog took place at the beginning of the Subboreal Phase and was the result of both significant humid climate and increased human impact (colonization of the Funnel Beaker Culture) in the landslide area. Similar influence of younger colonisations of landslide area (Przeworsk Culture and, later, Valachian colonisation) was also recorded within the deposits of peat bog (illuvial and mineral horizons) in the early Subatlantic Phase. Rejuvenation of the landslide zone and formation of the younger landslide were connected with the increase in climate humidity at the beginning of the Subboreal Phase. The peat bog deposits situated within this younger landslide, which are ca. 1.8 m thick, are significantly contaminated with mineral material.     

Revolutionary responses to the Myanmar coup

While Myanmar's recent military coup has devastated many people in the country, particularly those from the Bamar majority, who had been enjoying a decade of quasi-democracy, it has also produced a massive uprising against the military's seizure of power that appears to constitute a revolution. This is because amidst protests, general strikes, and guerrilla warfare, this majority has also been grappling with the failures of the last 10 years: through conversations facilitated by social media platforms, some are not only demanding changes to their democratic leadership's authoritarian chauvinism but are acknowledging the structural inequalities and exclusions built into Myanmar society.     

The Environment and Subsistence of the Early Neolithic Settlement Area at Těšetice-Kyjovice,Czech Republic

This paper presents a reconstruction of environmental conditions and subsistence strategies in the Early Neolithic (6th Millenium BC) settlement area at Tě?etice-Kyjovice (Czech Republic). Our detailed reconstruction of the environment contributes to the unravelling of the genesis and spread of steppes and the formation of secondary anthropogenic forest-free areas in the Holocene in eastern-Central Europe. Mollusc shells, charcoals and plant macroremains were used as on-site evidence of a settlement environment. A relatively warm and dry anthropogenic forest-free area is reconstructed for the immediate vicinity of the Early Neolithic settlement. Communities of mixed deciduous forests are recorded in the surroundings of the settlement. Plant macroremains reflect the characteristic Neolithic range of cultivated plants (e.g. Triticum monococcum, Triticum dicoccon, Lens culinaris and Pisum sativum). Papaver somniferum seeds were also found, possibly constituting the oldest evidence of its presence and cultivation in the territory of the Czech Republic.