Application of electron microprobe analysis to identify the origin of ancient pottery production from the Castillo de Huarmey,Peru

A vast amount of ceramics (among other grave goods) were recovered from Castillo de Huarmey, a Wari culture (650–1050 ce ) archaeological site on the north coast of Peru. In order to assess ceramic production area(s) and possible trade, political or cultural interactions with other regions, and to complement earlier petrographic analysis, electron microprobe analysis (EMPA) was conducted following a rarely used methodology in archaeology. The chemical composition of individual minerals in ceramics and sediments samples from the Huarmey Valley was obtained, focusing mainly on amphiboles, feldspars and pyroxenes. The results of the analyses clearly indicate that the majority of the ceramic analysed was made of raw material of local origin.     

The Environmental History of the Holocaust

ABSTRACT

The introduction conceptualizes environmental history of the Holocaust as a subdiscipline of Holocaust studies. The authors approach this emerging field of research through the context of environmental humanities with its current interest in the Anthropocene, soil science, forensics, multispecies collectives, and explorations of relations between ecocides and genocides. Proposed approach considers post-Holocaust spaces and landscapes as specific ecosystems and examines relations between its actors (human and non-human) in order to show the Holocaust’s spatial markers and long-terms effects. The article outlines existing literature on the subject, identifies the central research problems and questions, and discusses sources and methods. The authors demonstrate that the environmental history of the Holocaust applies a hybrid methodology that uses methods from various disciplines with the aim of creating new theories and interpretive categories and thus should be considered complementary to existing approaches in Holocaust studies. The authors follow the methodological principles of grounded theory in generating new concepts and seeking multidisciplinary methods for explaining nature’s role in the Holocaust and how Holocaust has changed nature. The authors claim that environmental history of the Holocaust broadens Holocaust studies as a field of research and opens up new questions concerning relations between nature and extermination in order to provide a more holistic perspective for exploring the relationship between culture and nature, genocide and ecocide. The approach proposed here shows Holocaust and post-Holocaust landscapes in terms of ecological/natural heritage, which might influence the way these spaces are commemorated, conserved and preserved, as well as used for tourist purposes.     

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.     

Cereal grinding technology in ancient Mesopotamia: evidence from dental microwear

Dental microwear features in a sample of 10 human teeth from Tell Ashara and Tell Masaikh, two archaeological sites in the Middle Euphrates valley, Syria, were compared for possible evidence of a shift in grinding technology in Mesopotamia—parallel to the well-documented introduction of large rotary querns and watermills in the Graeco-Roman world. Two chronological subsets (Bronze Age, n = 4 and Late Roman/Islamic period, n = 6) differred substantially and features related to a more abrasive diet (broad lines, pits and punctures visible on SE micrographs) were significantly less frequent in the later subsample which may indicate that the shift in cereal grinding technology occured in Mesopotamia before the Late Roman period.     

Personal,Professional and Academic Journeys to WAC 8

Two PhD students due to attend WAC 8 reflect on what brought them to Kyoto and what they hope to gain from the encounter.     

Impact of property rights and ownership on the development of Warsaw’s contemporary city centre

The paper raises the problem of the impact of unregulated property and ownership rights on the development of the city centre. It applies to Warsaw as a post-socialist city that has recorded fast economic growth since the country’s communist regime collapsed in 1989. We follow the course of changes in the city centre of Warsaw, in particular, those pertaining to land use and high-rise buildings for office use as investments that encounter difficulties under the unregulated status of construction sites and lack of clear regulations for private property restitution that was nationalized under socialism. To describe and explain the difficulties, we provide data showing the location of large companies and office buildings, and examples of conflicts as well. Unregulated ownership issues and property rights weigh on Warsaw’s city centre, now vastly dispersing and gravitating westwards, and prevent the district from rational and effective development.     

Progress in the holocene chrono-climatostratigraphy of Polish territory

The Holocene delivers a unique possibility to establish climatic stratigraphic boundaries based on detailed chronostratigraphy reflected in various facies of continental sediments, in their lithological parameters and organic remains. These sediments are dated by the ¹⁴C method in the case of organic remains, by counting annual laminations in lacustrine facies, and by dendrochronological method in the case of fluvial sediments. The existence of well dated profiles enables to reconstruct various climatic parameters like amplitudes of seasonal temperatures, types and frequency of extreme rainfalls and floods and, finally, to distinguish rare rapid changes and most frequent gradual ones. This reconstruction is based on the analogous effects of various types of present-day rainfalls. The current authors present a critical review of existing chronostratigraphic divisions starting from simple millennial division by Mangerud based on Scandinavian palynological stratigraphy of peat-bogs and Starkel’s concept based on fluctuations in rainfall and runoff regime reflected in fluvial and other facies of continental deposits. In the last decades, the calibration of ¹⁴C dates allowed a new approach to be used for the construction of the probability distribution function of these dates in various facies or types of sediments, which formed a background for distinguishing and correlating climatic phases and defining boundaries between them. These approaches have been creating new opportunities for revision of the existing chronostratigraphy. The aim of this paper is to present a revised version of chronostratigraphic division based on climatic fluctuations reflected in various facies of sediments on the territory of Poland and discuss their correlation with other European regions and global climatic changes.     

Problems of TL dating of the Mesopleistocene loess deposits in the Podillya and Pokuttya regions (Ukraine)

In many papers different authors was described problem of systematic underestimation of TL ages for sediments older then 100 ka. We presented the results which probably are not significantly rejuvenated. This is another example of the TL dates made in Lublin laboratory which are likely in agreement with the stratigraphic interpretation. In 2002 Kusiak et al. published the TL ages ranging from 200 to 800 ka for the Zahvizdja loess profile in Ukraine. These first promising results of TL dating of so old deposits encouraged us to undertake further studies. In next years were discovered other Ukrainian loess profiles with the Middle and Lower Pleistocene deposits, among others in the Skala Podils’ka, Mamalyha and Vendychany sites. The thermoluminescence dating made for these profiles in the Lublin laboratory gave the next, after Zahvizdja, series of 15 TL ages ranging from 200 to 700 ka. This way we confirmed the possibility of TL dating of the deposits older than 400 ka BP.     

Service or Benefice? Officeholders in Poland and Sweden of the seventeenth century

Exploring the differential structures of social and political power in early modern Europe, this paper examines the contrasting experiences of Poland and Sweden by focusing on the growth of civil office in each country. Central to the study is an understanding of the books of disciplinary regulation imposed on office holders, and how and why these measures were enforced. As the author illustrates, the two case studies give very different conclusions. In Sweden, as exemplified in the trial of leading members of the Swedish Council in 1680, the holder of civic office was constrained by a ‘corset of bureaucratic routine’. Strict, and widely enforced, rules governed activities such as office hours, dress and rates of remuneration. In contrast, Polish office holders pursued appointments not in the name of civic efficiency but to grasp social and political privilege. At the end of the article Kopczyński discusses some of the factors involved in these differences, laying emphasis on the structures of political and military power in each state.