The socioecology of fear: A critical geographical consideration of human-wolf-livestock conflict

Animal fear can be an important driver of ecological community structure: predators affect prey not only through predation, but also by inducing changes in behaviour and distribution—a phenomenon evocatively called the “ecology of fear.” The return of wolves to the western United States is a notable instance of such dynamics, yet plays out in a complex socioecological system where efforts to mitigate impacts on livestock rely on manipulating wolves' fear of people. Examining Washington state's efforts to affect wolf behaviour to reduce livestock predation, we argue that this approach to coexistence with wolves is predicated on relations of fear: people, livestock, and wolves can arguably share landscapes with minimal conflict, as long as wolves are adequately afraid. We introduce the “socioecology of fear” as an interdisciplinary framework for examining the interwoven social and ecological processes of human-wildlife conflict management. Beyond frequently voiced ideas about wolves' “innate” fear, we examine how fear is (re)produced through human-wolf interactions and deeply shaped by human social processes. We contribute to the critical physical geography project by integrating critical social analysis with ecological theory, conducted through collaborative interdisciplinary dialogue. Such integrative practice is essential for understanding the complex challenges of managing wildlife in the Anthropocene.     

Rewriting the end of the Early Bronze Age in the United Arab Emirates through the anthropological and artefactual evaluation of two collective Umm an-Nar graves at Hili (eastern region of Abu Dhabi)

The Hili archaeological complex in Al Ain (U.A.E.) is important for its wealth of third-millennium BC Umm an-Nar burial and settlement sites. Two of the most significant burial sites are Tomb N at Hili and Tomb A Hili North. The latter is a classic circular Umm an-Nar monumental grave, while Hili N is a pit-grave, one of only two Umm an-Nar period pit-graves discovered so far in the U.A.E. Both of these tombs contained the remains of hundreds of individuals, in the case of Tomb A Hili North, more than 300, while around 600 people had been deposited in Hili N. Both population groups have been the subject of anthropological and artefactual analyses and a comparison of the findings help to shed light on the chronology of the end of the Umm an-Nar period.     

Family and influence to the south of Normandy in the eleventh century: the lordship of Bellême

The Bellême family were among the most important of the new families to emerge in the unsettled conditions of northern France in the tenth century. They illustrate well the manner in which those families extended their influence at the expense of declining central authorities. The nature of their relations with their overlords, the counts of Maine and the dukes of Normandy, is examined and a new chronology proposed for the complex divisions of estates among the family. It is suggested that family quarrels of the 1040s and 1050s seriously weakened their position and that the lordship was easily dominated by Geoffrey Martel, count of Anjou, the most powerful figure in mid-eleventh century northern France. A reversal is traced in the pro-Angevin sympathies of Bishop No of Sées, the last surviving male member of the family, after the failure of the coalition of Angevins and Capetians against the duke of Normandy in 1054. However, it was not until the estates of the family were eventually reunited in 1071 on the succession of Ivo's niece, Mabel, and her Norman husband, that the lordship came completely under the influence of the ascendant Normandy.     

The geographic origins of Nasca trophy heads using strontium,oxygen, and carbon isotope data

Scholars continue to debate the identity of individuals curated as trophy heads in the Nazca Drainage of southern Peru (c. 1–800 AD). What was the role of trophy heads in Nasca society? Were they victims of warfare or venerated ancestors? Strontium, oxygen, and carbon isotope data from archaeological human tooth enamel from Nasca trophy heads from Aja, Cahuachi, Cantayo, Majoro Chico and Paredones, and from individuals buried in Nasca cemeteries at Cahuachi, Cantayo, and Majoro Chico elucidate the geographic origins and paleodiet of trophy heads in the Nazca Drainage. The ⁸⁷Sr/⁸⁶Sr and δ¹⁸O_c(V-PDB) data from both the trophy heads and the Nazca Drainage burials are all quite variable, and do not support the hypothesis that the Nasca trophy heads were obtained from a geographically-distinct population. Similarly, the δ¹³C_c(V-PDB) data demonstrates that the individuals included in this study consumed similar diets. These data suggest that the Nasca trophy heads likely derive from the local Nasca population. Rather than obtain heads from enemy warriors through geographic expansion or warfare as seen in other parts of the world, this complex social practice existed within the Nasca polity throughout space and time.     

EXEMPLIFYING ACCUMULATION BY DISPOSSESSION: MINING AND INDIGENOUS PEOPLES IN THE PHILIPPINES

Using a case study from the Philippines, this article applies David Harvey's theory of accumulation by dispossession to show how neoliberal policies enable mining corporations to locate, lay claim to, and develop mineral resources in formerly inaccessible areas, which for centuries have provided safe haven for indigenous peoples and their cultures. It explains why these factors are leading to an increase in armed conflict between military forces and guerrilla groups, which recruit their members from displaced indigenous people. The article concludes that the theory of accumulation by dispossession offers an appropriate analytical tool for understanding these processes.     

Flood-Damaged Canals and Human Response,A.D. 1000–1400, Phoenix,Arizona, USA

The scale of prehistoric canal construction in the North American Southwest peaked in a.d. 450–1450, during what has been named the Hohokam Millennium. Explanations for the eventual Hohokam “collapse” remain elusive. Environmental disturbances, such as floods, that were once manageable may have become unmanageable. Recent archaeological excavations of Hohokam canals in Phoenix identified stratigraphic evidence for three destructive floods that date to a.d. 1000–1400 within two large main canals in System 2, Hagenstad and Woodbury’s North. Woodbury’s North Canal was flood-damaged and abandoned sometime after a.d. 1300. Thereafter, no main canals of similar size were constructed to supply villages within System 2 and the area was depopulated. Our investigation provides the first stratigraphic evidence for a destructive flood during the late Classic period in the lower Salt River Valley and is compatible with the hypothesis of diminished resilience to environmental disturbance at the end of the Hohokam Millennium.