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.     

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.     

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.     

Heat treatment of Polish flints

In Poland three types of flint (chocolate, spotted and banded) were intensively mined from the Terminal Palaeolithic to the Early Bronze Age. Although heating of flint to improve its flaking properties was practised across the world from ∼110,000 years ago to the recent, particularly in southwestern Europe, heat treatment of flint in Poland is known from only two sites.     

Gebel Ramlah—a Unique Newborns’ Cemetery of the Neolithic Sahara

Post-Pleistocene climatic improvement in the Northern Hemisphere after ca. 9550 BC allowed human populations to recolonize large parts of North Africa in what is today the Sahara Desert. In the Egyptian Western Desert, the beginnings of human occupation date as early as ca. 9300 BC. Occupation continued until the middle of the third millennium BC when final desertification of the area no longer afforded human occupation. The settlement of the Neolithic cattle and sheep/goat herders developed along with the rhythm of alternating wet and dry climatic oscillations. One of the areas occupied intensively during the early and middle Holocene was Gebel Ramlah. Pastoral populations established their settlements around the shores of a paleo-lake adjacent to a rocky massif, to exploit the local savannah environment. During most of the Neolithic, they buried their dead dispersed outside of their settlements. Only during the Final Neolithic (after ca. 4600 BC) did they place them exclusively in cemeteries. Of six Final Neolithic cemeteries investigated at Gebel Ramlah to date, one is entirely unprecedented, not only in North Africa but also globally at such an early date. For just under 200 years (ca. 4500–4300 BC), it served exclusively for the inhumation of infants who died around (perinate) or shortly after the time of birth (neonate). Thirty-two burial pits contained skeletal remains of 39 individuals, not only infants but also at least two adult females accompanied by perinates/neonates. Older children (>?3 years) were interred at a nearby cemetery that primarily comprised adults.     

Do the Buildings Really Matter? Czech,Polish and Slovak Museums and Centres of Contemporary Art in Adapted Buildings

This paper discusses the connection between museums and centres of contemporary art operating in adapted buildings, on the one hand, and on the other, the history of the place where the buildings are located. I discuss seven discrete case studies, representing a variety of approaches to buildings and the areas in which they operate, in the Czech Republic, Poland and Slovakia. My analysis of each case study covers four main subject areas: (1) discussions connecting the building’s history with its new role; (2) the architectural features and appearance of the building; (3) references3 to the history of the site in the institution’s programme and communication; and (4) efforts to build bonds with local communities. In my conclusions, I argue that the identity of the institution may either be rooted in the history of the place presented and discussed in its programme, or be independent of the history of the building but nonetheless connected to the area in which it is located.