The Thule region in north Greenland formerly supported a population of musk-oxen (Ovibos moschatus). Radiocarbon dating of bones of this mammal collected on the terrain surface and from archaeological sites has yielded late Holocene ages, indicating that the species was a late immigrant to this part of Greenland. The species may have arrived at a time when the area was uninhabited, and it had at least a thousand years to spread south, before the Late Dorset people arrived. The heavy glaciation of Melville Bugt in the late Holocene was probably the main reason that the musk-ox did not disperse south to west Greenland. The population of musk-ox in the region may have peaked during the Medieval Warm Period, and the species survived during the occupation of the region by the Late Dorset people. The size of the population may have declined during the beginning of the Little Ice Age, and musk-ox was probably exterminated from the region shortly after the arrival of the mobile Thule people.

This article assesses the current state of UK-Argentine relations with reference to the South Atlantic and Antarctic region. Three major themes are pursued: the current state of UK-Argentine relations, with the contested Falklands/Malvinas looming large in the assessment, alongside fisheries management around South Georgia; the mapping of Argentine Antarctic territory in the context of extended continental shelf delimitation; and finally, the recent UK White Paper on Overseas Territories is noted insofar as it marks the most recent public assessment of how the coalition government is attempting to manage the most southerly portions of the British Overseas Territories portfolio. The article concludes with a warning that there is a danger that worsening UK-Argentine relations might begin to have more profound implications for the Antarctic Treaty System as resource, sovereignty and territorial issues acquire more piquancy.

Fifty dogs were ordered from Greenland for use on Douglas Mawson's Australasian Antarctic Expedition (1911–1914). Twenty-one more were later donated to the expedition by Roald Amundsen, when he reached Hobart after his successful attainment of the South Pole. Numerous pups were born during the expedition. This note gives the details of the individual dogs during the expedition, including their names (and why they were so named), descriptions (when known), and fates.

Climate and environmental change places a variety of different pressures on remote, indigenous Arctic communities. The sea ice is the platform on which the Inugguit culture of northwest Greenland is based and thus it is inevitable that its retreat will have implications for the indigenous notion of place and for the manner in which the Inugguit articulate their sense of belonging with respect to the natural environment. With the demise of story-telling, the traditional vehicle for knowledge transmission, and the squeeze on hunting by consumer society and the Greenland Self Rule imposed quota system, it is apparent that some younger people are now engaging with more western ontologies of place. The relationship between man and nature is for some beginning to be expressed in terms of detachment and not extension. Whilst the way the Inugguit relate to their immediate natural environment might be in flux, other social practices of belonging such as naming and visiting are unchanged and still characterise these communities. In northwest Greenland, the need to ‘belong’ remains the social imperative that it has always been and the mechanisms used to reinforce this remain intact.

A small number of educational programmes for university students include field experience in Antarctica. These programmes contain a range of educational objectives, approaches and academic assessment related to the field component and the intended on-site learning for students. However, it is possible that the on-site experiences of students in these programmes have an influence on later decisions and behaviour beyond the course itself in the years following participation. This paper investigates the possibility of such influence for students who participated in ship-based tourism field trips to the Antarctic Peninsula and adjacent locations (South Georgia, the Falkland Islands, and South Shetland Islands) and explores whether students link their participation to particular post-course outcomes. It examines how participants report being affected by a trip to the Antarctic Peninsula, particularly in terms of later decisions regarding learning, professional lives, and environmental behaviour. Influences noted by respondents include effects on choices made in relation to academic pursuits and career paths, as well as development of their environmental values through increased awareness of tourism impacts, Antarctic region sustainability issues, and global issues such as climate change.

In writing and interviews Roland Huntford has stated that at the end of his life Captain Robert Falcon Scott ‘probably’ had no reason to wish to survive, and that he ‘persuaded’ Dr Edward A. Wilson and Lieutenant Henry Bowers to remain in the tent with him when they could have gone forward. This commentary demonstrates that Huntford's interpretation of events shows a serious misunderstanding of the primary sources and historical context; that Wilson and Bowers could not have survived had they gone forward, a fact which Huntford himself understands; and that Scott had extremely strong motivation to wish to return home.

This article presents a model for the analysis of the domestic-international nexus of Arctic politics. It offers a preliminary attempt at mapping the domestic politics of Arctic boundary disputes in Canada. It explores the potential impact of domestic politics on such disputes by identifying the interests of domestic stakeholders in the Canadian Arctic. The paper views maritime boundary negotiations as a ‘two-level game’ in which negotiations occur internationally and domestically. The paper argues that the domestic level negotiation is contingent on how the issues are ‘framed’ between policymakers and their constituents. The paper identifies ways that domestic actors can reduce the number of acceptable outcomes in a two-level game, thereby impeding cooperation.

In thirteen (mostly soil) mixed samples, collected from nine localities on the Antarctic continent and some of the neighbouring islands, 788 specimens and 32 eggs of tardigrades were found. In total, five species were identified: Acutuncus antarcticus, Echiniscus jenningsi, Diphascon (D.) victoriae, Hypsibius dujardini and Ramajendas dastychi sp. nov. A. antarcticus was the most abundant (nearly 90% of all specimens) and was the prevailing taxon found in the majority of locations. R. dastychi sp. nov. is the fourth species described in the exclusively Antarctic/sub-Antarctic genus. The new species differs from all other congeners by the presence of four gibbosities on the caudo-dorsal cuticle (configuration II:2–2) and also by some morphometric characters. In this paper we also briefly discuss the taxonomy and zoogeography of the genus Ramajendas.

This article describes the human biological data that was collected from the participants of the Antarctic expeditions of the ‘heroic age’ (1897–1922). Routine body weights, waist circumference, spirometry and grip strength measurements were performed on a number of the expeditions for monitoring health and at least four expeditions measured the haemoglobin level and demonstrated that anaemia did not occur. The only true research was done by Dr A.L. McLean of the Australasian Antarctic Expedition, who measured hair and nail growth and investigated immunity. By modern standards, the data collected is of little value but McLean's work laid the groundwork for modern research into the effects of Antarctic residence on the human organism.

The loss of the expedition ship SY Endurance, and the subsequent dispersal of staff and crew, resulted in very little scientific information emerging from the Imperial Trans-Antarctic Expedition 1914–1917. Among surviving records were the charts and diaries maintained by the ship's master, F.A. Worsley. During the voyage in January 1915 along the ice cliffs of the Weddell Sea coast, Worsley recorded the ship's daily progress, soundings and trawling and dredging activities, and also daily encounters with seals, whales and seabirds, On 12 January he noted a group of fledgling emperor penguin chicks (Aptenodytes forsteri) on an ice foot, clearly a remnant of what was then only the third-known breeding colony of the species. Shackleton's first published account of the expedition mentioned the chicks only in a brief note (one that was omitted from later editions), and no further report covering Worsley's observations appeared in scientific literature. In consequence the discovery of the breeding colony and records of emperor penguin distribution along the Weddell Sea coast have since been overlooked by avian biologists, regrettably including the present author. This paper discusses the identity of the colony, Worsley's observations that foreshadowed the later discovery of more breeding concentrations along the coast, and a possible reason why colonies occur at points of particular glaciological disturbance.

The aim of this study was to determine the differences in cellulolytic activity of soils around the coastal lowlands of the southwestern part of Wedel Jarlsberg Land (west Spitsbergen). Two positions (Calypso and Skilvika) representing typical soil types in this area were chosen for investigation. Within the area of Calypso, arctic brown soils formed from loamy sands with a significant addition of coarser gravel and pebble fractions occur. The Skilvika position represents the arctic gley soils of a loamy texture, with significant content of silt, associated with the occurrence of cell grounds created under the strong influence of cryogenic processes. Cellulolytic activity of the soils was determined by a gravimetric method involving estimation of a weight loss of cellulosic material buried in the surface soil horizons. The investigation showed significant differences in the cellulose decomposition rate between the two research locations. The cellulolytic activity of arctic brown soils –0,412–0,656 g*g−1*year−1 during the vegetation season (Olson's k = 0,231–0,563), was twice higher than the activity in the case of Skilvika gley soils –0,185–0,310g*g−1*year−1 during vegetation season (k = 0,089–0,131). This should be attributed, among other factors, to the grain size distribution, thereby determining more favourable water-air conditions of soils within the area of Calypso.

This commentary reviews Maruyama's article ‘Japan's post-war Ainu policy: why the Japanese Government has not recognised Ainu indigenous rights?’ (Maruyama 2013a), published in this journal. Maruyama criticises the government for its reluctance to enact a new Ainu law to guarantee indigenous rights, even after Japan's ratification of the United Nations Declaration on the Rights of Indigenous Peoples (UNDRIP). However, in actuality, the government is searching for the foundation of new Ainu policies in the existing legal frameworks and trying to guarantee some elements of indigenous rights. Japan's case suggests the possibility of realising indigenous rights without the enactment of a specific law.

In order to explore further Japan's Ainu policy, this reply firstly outlines the differences in opinions that between Dr. Nakamura and myself, and secondly addresses some of the main points of my paper published in this journal. Dr. Nakamura takes into consideration domestic circumstances instead of international human rights law, while I emphasise that Japan's international obligations lies in its adherence to international human rights law and that domestic law must conform to international obligations for the Ainu. My paper chronologically summarises Japan's post-war Ainu policy and investigates who and what has influenced this policy and the law.

None of the logbooks or officers’ journals of the 1819–1821 Russian Antarctic expedition, commanded by Junior Captain Faddei Faddeyevich Bellingshausen, have yet been found. The discovery of Peter I Island was recorded in two reports from the commander, on Sheet 13 of a 15-sheet track chart of the expedition which he prepared during the voyage home (Belov 1963: 32), in his subsequent book (Bellinsgauzen 1831), and in narratives penned by four other eye-witnesses.

Prolonged chasing of an adult reindeer (Rangifer tarandus) by a polar bear (Ursus maritimus) was observed both on land and in the sea, in Magdalenefjorden, northwest Spitsbergen. Polar bears were also observed catching black guillemot (Cepphus grylle) in the sea in northwest Spitsbergen and feeding on chicks in the arctic tern (Sterna paradisea) colony in Hornsund, southwest Spitsbergen. While feeding on seabird species is unsurprising, the prolonged chasing of adult reindeer is unusual for polar bear hunting behaviour. The few documented cases of polar bear hunting reindeer consist of either surprising and killing resting/sleeping prey or stalking and a short rapid chase of the reindeer. Our observations describe new feeding habits of polar bears that may be in response to decreasing seal availability due to shrinking sea-ice cover in the Arctic.

The Antarctican Society, based in the United States, has produced a medallion (Fig. 1) in recognition of the centennial of the discovery of the South Pole by Roald Amundsen and Captain Robert Falcon Scott, in 1911 and 1912, respectively. This item is representative of both expeditions.

The occurrence of two basal sections of southern beech trees (Nothofagus sp.) embedded in raised cobble beaches and exposed by receding icefields at widely separated locations on islands off the western coast of the Antarctic Peninsula is reported. These are the most southerly records of naturally occurring driftwood. Both are of Fuegian or southern Patagonian origin but whether they arrived at their destinations directly from the north or by circumnavigating the Southern Ocean eastwards is uncertain. While their stranding probably occurred several centuries ago this can only be speculated.

The accompanying table gives a pragmatic indication of current national interests in polar research and other activities through association of states with four international agreements. Two of these are inter-governmental treaties and the two committees are non-governmental scientific organisations. One of each pertains to the Arctic and the others to the Antarctic. Each agreement has two classes of association, which are indicated in the table.

After learning in the first week of September 1909 that the North Pole had been claimed, the career and prospects of the Norwegian explorer Roald Amundsen hung in the balance. Scheduled to lead an exploration of the north polar basin, Amundsen suddenly found himself without adequate funding or a clear objective. His self-described ‘coup’ to turn southwards and reach for the South Pole was perhaps the most dramatic and best-kept secret in the history of polar exploration. Amundsen shared his decision only with a very select few, including his brother and manager, Leon Amundsen, a scene dramatised in the 1985 television mini-series The last place on earth. The location used in the film is identified at the unusual grave markers of the Ingier family outside Oppegård kirke in Oppegård, Norway, about five km from the site of Amundsen's home on Bunnefjorden, a branch of Oslofjord.