The Russian naval officer Faddej Faddeevich Bellingshausen began life with a slightly different surname, in his case ‘Billingshausen’. It is possible to work out roughly when the Russian surname ‘Bellinsgauzen’ was chosen. Considerations prompting the selection of that particular Russian version can also be suggested.

Despite its numerous valuable contributions to Arctic governance, throughout its history the Arctic Council (AC) has been subject to criticism and reform proposals from academic, non-governmental and practitioner communities alike. In order to inform this ongoing debate, the paper evaluates the proposals that have been presented for the AC thus far. The proposals are grouped into three clusters: legal reforms, organisational reforms and functional reforms. Each of them is examined in terms of its applicability and usefulness to the case of the AC, and specifically its suitability given the prevailing conditions in the Arctic. What the conducted analysis reveals is that the ideas regarding means to enhance the AC’s effectiveness can be largely attributed to the assumptions their proponents make—oftentimes implicitly—about the nature of state actors and international relations more broadly, without attending to the particular conditions of the case study at hand. This is an important inference, given the unrelenting change happening in both Arctic and global socio-environmental settings that calls into question the usefulness of past modes of thinking and forms of international cooperation. Far from offering solutions, their continuous application in particular circumstances might even impede progress in addressing present and future challenges.

We used fossil Chironomidae assemblages and the transfer function approach to reconstruct summer air temperatures over the past 300 years from a High Arctic lake in Hornsund, Svalbard. Our aims were to compare reconstructed summer temperatures with observed (last 100 years) seasonal temperatures, to determine a potential climate warming break point in the temperature series and to assess the significance and rate of the climate warming trend at the study site. The reconstructed temperatures were consistent with a previous proxy record from Svalbard and showed good correlation with the meteorological observations from Bjørnøya and Longyearbyen. From the current palaeoclimate record, we found a significant climate warming threshold in the 1930s, after which the temperatures rapidly increased. We also found that the climate warming trend was strong and statistically significant. Compared with the reconstructed Little Ice Age temperatures in late eighteenth century cooling culmination, the present day summer temperatures are >4°C higher and the temperature increase since the 1930s has been 0.5°C per decade. These results highlight the exceptionally rapid recent warming of southern Svalbard and add invaluable information on the seasonality of High Arctic climate change and Arctic amplification.

This article investigates how in the Soviet Arctic researchers and indigenous communities searched and understood the mammoth before and during the Cold War. Based on a vast number of published and unpublished sources as well as interviews with scholars and reindeer herders, this article demonstrates that the mammoth, as a paleontological find fusing together features of extinct and extant species, plays an in-between role among various environmental epistemologies. The author refers to moments of interactions among these different actors as “environmental encounters”, which comprise and engage with the physical, political, social and cultural environments of the Arctic. These encounters shape the temporal stabilisations of knowledge which enable the mammoth to live its post-extinct life. This article combines approaches from environmental history and anthropology, history of science and indigenous studies showing the social vitality of a “fossil object”.

Although archaeological studies focusing on 19th-century sealing have been performed over the past 30 years, its history and sites have traditionally had low visibility in Antarctic narratives and the Antarctic Treaty System policymaking on heritage. Researchers face the challenge of increasing the visibility of sealers’ history and public awareness of the importance of conserving the oldest sites of Antarctica. In this paper, we propose that identifying patterns of tourism activity in the South Shetland Islands, specifically in their temporal and spatial dimensions, could help protect these sites and engage visitors with the early history of Antarctica. Data collected by the International Association of Antarctica Tour Operators were used to calculate landing point usage trends over time and the frequency of passenger landings from 2003–2004 to 2015–2016. We defined six different visitation patterns with temporal tendencies of passenger landings that varied from increasing, constant, or decreasing trends over time, differing in the magnitude and intensity of visitation. This information was used to assess the situation of particular sites located in the vicinity of tourism landing points. We set priorities for their conservation and management decisions and highlighted their relative potential to engage visitors with the stories of 19th-century sealing in Antarctica.

Professional scientist-geographer Erich von Drygalski led the first German expedition to Antarctica in 1901–1903. The expedition saw itself as purely scientific, which turned out to be at odds with the expectations of Imperial Germany at the time. It was one of the first to use photography extensively and effectively to document and record scientific activities and to shape the public’s image of the work that was being done in this remote and unknown part of the world. Ice was the leitmotif of Drygalski’s life. He had prior experience in the Arctic, and the year spent in Antarctica confirmed his nuanced way of viewing the ice: on the one hand, and foremost, scholarly and objective, while still appreciating its aesthetic qualities; on the other, infused with feelings of human vulnerability. Using discourse analysis, this article examines Drygalski’s published work and photographs he chose to illustrate it, in order to investigate what the ice meant to him. In his writings, it was the scholarly, objective attitude which predominated and this may have contributed to the generally lacklustre reception of his Antarctic achievements. The photographs he chose to illustrate his published work, however, were many and varied, often capturing the awe-inspiring beauty of the ice and contributing to good sales of his narrative of the South Polar Expedition.

Barton Peninsula is an ice-free area located in the southwest corner of King George Island (South Shetland Islands, Antarctica). Following the Last Glacial Maximum, several geomorphological features developed in newly exposed ice-free terrain and their distribution provide insights about past environmental evolution of the area. Three moraine systems are indicative of three main glacial phases within the long-term glacial retreat, which also favoured the development of numerous lakes. Five of these lakes were cored to understand in greater detail the pattern of deglaciation through the study of lacustrine records. Radiocarbon dates from basal lacustrine sediments enabled the reconstruction of the chronology of Holocene glacial retreat. Tephra layers present in lake sediments provided additional independent age constraints on environmental changes based on geochemical and geochronological correlation with Deception Island-derived tephra. Shrinking of the Collins Glacier exposed the southern coastal fringe of Barton Peninsula at 8 cal ky BP. After a period of relative stability during the mid-Holocene, the ice cap started retreating northwards after 3.7 cal ky BP, confining some glaciers within valleys as shown by moraine systems. Lake sediments confirm a period of relative glacial stability during the last 2.4 cal ky BP.