Swedish attempts in 1903–04 to rescue Otto Nordenskjöld's expedition to Antarctica are examined in the context of an international competition involving Sweden, Argentina, and France. The Swedish relief expedition, led by Captain Olof Gyldén, is viewed partly as a little-known expedition and partly for its potential as a major national event. The developments and progress of the Swedish and French expeditions are shown alongside those of the Argentine expedition, which ultimately was successful in its attempts to rescue Nordenskjöld. The Swedish relief expedition never produced a significant national collective memory, unlike several other unsuccessful rescue operations. Potential reasons for this are examined, including the role of internal conflicts among individuals both on the expedition and in Sweden, and the failure to make the expedition a national event. The different attempts to make the relief expedition a major nationalist effort included issues concerning choice of vessel, staff, and equipment; media accounts of competing relief expeditions in which Sweden's positive national features were contrasted with those of ‘others;’ and the views on the competition expressed by various participants.

The search for Sir John Franklin (1847–59) coincided with a growing interest in mesmerism and modern spiritualism in Britain. Several clairvoyants, claiming to ‘see’ Franklin's ships and crews in the Arctic, made statements about the status and location of the overdue expedition, and at least three mediums described communications with Franklin’s spirit. Although the Admiralty provided assistance to Dr Haddock, the mesmerist of Emma, the Bolton clairvoyant, they did not take any action on the basis of her statements, probably because the various accounts were contradictory and could not be verified, and because the Admiralty Lords were sceptical of paranormal phenomena. Lady Franklin, on the other hand, visited clairvoyants and altered the plans for her search expeditions under Forsyth and Kennedy on the basis of a revelation. Recently, an American medium has described more than two dozen conversations with the spirits of Sir John and Lady Franklin.

The International Conferences on Contaminants in Freezing Ground are organised under the auspices of an International Steering Committee to promote a better understanding of the unique characteristics and problems posed by contaminants in freezing ground. The first meeting was held in Cambridge in 1997 and was attended by 33 participants from nine countries. Results from the meeting were reported in Polar Record in 1998 (volume 35). The themes covered at the first meeting reflected a broad range of interests, including a synthesis of the Arctic environmental strategy as it stood in 1997; the fundamental physical, chemical, and biological properties of contaminated frozen soils; experimental approaches to determining contaminant movement; and possibilities for in situ bioremediation of petroleum spills.

The requirement for an Antarctic component to the 2001 Australian State of the environment report initiated the development of a state of the environment system designed to remain current, yet minimize the resources required for maintenance. A series of environmental indicators was developed and refined by a group of experts during a period of 18 months. A simple descriptive template and data for each indicator were incorporated into a web-accessible database system called SIMR (System for Indicator Management and Reporting). The system captures indicator data either dynamically from sensors or by web input by indicator custodians. The system also prompts custodians for regular input of evaluations of indicator status. The system (http://www-aadc.aad.gov.au/soe) has been an effective framework for considering all aspects of state of the environment reporting and a practical tool in research and operational aspects of the Australian Antarctic Division.

During the last decade, aboriginal peoples in Russia have sought to improve their legal rights, including their rights to their homelands and the resources of these lands. The Russian government initially responded to an aboriginal lobby by including discrete articles addressing aboriginal rights in a number of its laws, including those on forests, sub-surface resources, and protected areas. More comprehensive laws, specifically addressing aboriginal rights to land, were finally adopted at the turn of the twenty-first century, in 1999, 2000, and 2001. This article summarizes the rights of aboriginal peoples regarding land ownership/tenure, access to natural resources (renewable and sub-surface), and protection of ancestral lands, in the light of the new federal legislation. It also notes how the federal laws' provisions concur with international requirements for aboriginal land rights.

The ways by which contaminants in freezing ground disperse and interact with associated ecosystems is a new and challenging field of applied research that is crucial to effective assessment, monitoring, and remediation in cold regions. Three key issues have been identified as needing urgent research and development. The first concerns the development and application of meaningful environmental guidelines for cold regions. This usually means that contaminants in freezing ground per se need to be considered in their broadest context by also addressing associated ecosystems, such as the receiving marine environment. The second issue concerns developing best practice for bioremediation of seasonally frozen soils. Of particular concern are the risks, benefits, and costs of using so-called bioproducts, which may not offer substantial improvements over biostimulation of indigenous cold-adapted organisms. The third issue concerns the need for assessment and monitoring protocols and cost-effective analytical tools. In this respect the potential use of field portable instruments deserves careful consideration and on-site testing. Taken together, development of these issues during the coming years will be crucial if the science behind managing contaminants in freezing ground is to catch up with the knowledge that underpins the remediation industry elsewhere.

An article by Walter Sullivan in The New York Times of 30 January 1969 speculated that a note discovered by a Russian party on Rudolf Island, Franz Josef Land, was evidence of defection by three members of the Fiala-Ziegler Polar Expedition, 1903–05. Sullivan indicated that the Soviet Novosti news service had reported that the partially decayed note, which was dated 2 July 1904, started: ‘We the opposition’ and was signed by ‘Tess, Veddy, and Ralliet.’ Examinations of the diaries of a member of the expedition and of expedition leader Anthony Fiala's book Fighting the polar ice show that it was impossible for these men to have been together on 2 July 1904, but that they were together a year later, and that they left a note then, at the place where Novosti reported the Russian party to have found one. Fiala and the diary show that the reported version of the note is not consistent with the circumstances at the purported time of the writing. When the note of 1905 was written, the trio was on a mission to assist Fiala. Defection and dissent by this group are contrary to available documents and publications, as well as the text of what is undoubtedly the original note, newly brought to light. In addition, the foundation for the issue of assassination and defection as raised by William Hunt, who referenced Sullivan's story in his book To stand at the Pole, is challenged.

This article examines current economic practices of the Inuit of Nunavik and the consequences of these practices on social relations. In western societies, recourse to market and increasingly frequent use of money have been identified as major factors related to a decline in household production. These practices are also associated with a reduction of interpersonal dependency and with the emergence of instrumental rationality. In Nunavik, like in many Arctic regions, money and commodities represent an increasing portion of the economic resources of Inuit households. Household production also contributes substantially to their resources. An examination of the Inuit household budget shows a diversity of lifestyles supported by various economic activities and strategies that aim at satisfying material needs of family members. These strategies demonstrate that Inuit are economically rational and make use of monetary calculation. This rationality does not influence all economic behaviours, which are also motivated by traditional values and customary obligations. However, the emergence of diversity in lifestyles indicates the existence of a greater margin of self-determination for individuals.

The medieval King's Mirror describes Iceland and Greenland with a scientific accuracy that is remarkable. One of the very few exceptions is the hafgerdingar in the Greenland Sea. The term translates as ‘sea hedges,’ within which a mariner may become trapped at great peril. Many have believed that a real event was being described, although none of the proposed explanations has been totally satisfactory. The most common view currently is based on Steenstrup (1871), who explained the phenomenon as a tidal wave following a submarine earthquake. A simpler and more consistent theory is developed here: that the hafgerdingar are an optical phenomenon, specifically, a superior mirage. Such mirages, quite common in the polar regions, can produce an appearance fully consistent with the original description, as illustrated by several photographs and a computer simulation. Even the peril to seafarers has been corroborated, in the sense that such a mirage is frequently followed by a storm.

When geographers recommended the exploration of the Antarctic regions at the close of the nineteenth century, Germany and Britain were eager to do their best. The promoters of Antarctic research, such as Georg von Neumayer (1826–1909) in Hamburg and Clements Markham (1830–1916) in London, could finally raise enough money to build national flagships for science. Despite unfavourable political circumstances, due to political rivalry between Germany and Great Britain, the leaders of the expeditions — Erich von Drygalski (1865–1949) and Robert Falcon Scott (1868–1912) — agreed to a scientific collaboration with regard to meteorological and magnetic measurements in Antarctica during 1901–1903, which later was extended until 1904. This paper reveals that favourable circumstances such as the International Geographical Congresses in London (1895) and Berlin (1899) played a major role in increasing scientific interest in and public support of Antarctic research, ultimately leading to international collaboration.

In recent years, pioneer photographers in the Arctic have been researched. The last was W.J.A. Grant, who sailed as a photographer with Sir Allen Young in Pandora in 1876. Grant made another seven photographic trips to the Arctic. Four voyages were in the Dutch Arctic schooner Willem Barents, the others in British yachts. Grant's photographic legacy is considerable, but little known. The majority of his work was done for the Dutch and is still preserved in the Netherlands. Recently it has been possible to identify photographs by Grant in British collections. This article examines Grant and his work as an Arctic photographer.

The behaviour of Antarctic soils towards contaminant materials depends on the nature of the contaminant and the properties of the soil. Relevant properties are: depth to permafrost, whether the permafrost is ice-cemented or dry frozen; the active layer depth, active layer moisture content, and frequency of liquid water; soil salinity characteristics; and the geological composition of the soil materials.

Soil contaminations in the McMurdo region have been investigated through several years in a number of studies, including site surveys, field investigations, and experiments. Results of these studies are summarized in this paper and the significance of the contaminations is discussed. The behaviour of contaminants at the sites investigated conforms to existing knowledge of the soil properties. In the presence of some summer water or occasional moisture influxes from snowmelt, soluble contaminants may be transported variable distances through soils, both downwards and laterally, depending on the amount of water available. Ice-cemented permafrost restricts the downward movement of most contaminants but may aid distribution via lateral flow, especially low-freezing-point contaminants such as hydrocarbons. In dry-frozen soils, low-freezing-point contaminants may penetrate deeply into the soil.

With respect to the sites investigated, the heavy metal contaminations were typically above the values from undisturbed sites, but there may at times be appreciable natural variation. The presence of solid materials in soils — such as particles of plastics, wood, fibre, etc — represents a widespread and pernicious form of contamination, because they are foreign to the environment and are non-degradable.

There is an urgent need to develop new technologies to address the problem of soil remediation in high-latitude regions. A field study was initiated in January 1997 in two contaminated soils in Terre Adélie (Antarctica) with the objective of determining the long-term effectiveness of two bioremediation agents on total and hydrocarbon-degrading microbial assemblages under severe Antarctic conditions. This study was conducted in two steps, from January to July 1997 and from February to November 1999 in the Géologie Archipelago (Terre Adélie, 66°40′S, 140°01′E). Changes in bacterial communities were monitored in situ after crude oil or diesel addition in a series of 600 cm2 soil sectors (20×30 cm). Four contaminated sectors were used for each experiment: diesel oil (10 ml), diesel oil (10 ml) + fertilizer (1 ml), Arabian light crude oil (10 ml), and crude oil (10 ml) + fertilizer (1 ml). Two different bioremediation agents were used: a slow release fertilizer Inipol EAP-22 (Elf Atochem) in 1997 and a fish compost in 1999. Plots were sampled on a regular basis during a three-year period. All samples were analysed for total, saprophytic psychrophilic, and hydrocarbon-utilising bacteria. A one order of magnitude increase of saprophytic and hydrocarbon-utilising micro-organisms occurred during the first month of the experiment in most of the contaminated enclosures, but no clear differences appeared between fertilized and unfertilized plots. Diesel-oil contamination induced a significant increase of all bacterial parameters in all contaminated soils. Crude-oil contamination had no clear effects on microbial assemblages. It was clear that the microbial response could be rapid and efficient in spite of the severe weather conditions. However, microbial growth was not clearly improved in the presence of bioremediation agents.

We used a top–down, multidisciplinary approach to examine the physical and biological environment of the pack ice of the eastern Ross Sea (approximately 125–170°W) during the austral summer of 1999/2000 from RVIB Nathaniel B. Palmer and its ship-based helicopters. The approach focused on pack-ice seals while incorporating studies of biotic and abiotic factors that may influence the distribution and abundances of these apex predators in the Ross Sea to yield a holistic understanding of the structure and function of this complex, large marine ecosystem. This research represented the US component of the international Antarctic Pack Ice Seal (APIS) program, which was designed to document the circumpolar distribution and abundance of Antarctic pack-ice seals. The eastern Ross Sea is one of the two major areas in the Southern Ocean where substantial pack ice exists throughout summer. We found that vast multi-year ice floes (>20 km diameter) and smaller floes north of the shore-fast ice front provide a unique habitat for seals and penguins (apex predators) to forage and haul out while molting in late summer. Farther north, more Ross seals were observed than in any previous surveys in the circumpolar pack ice, perhaps because they are attracted to the area in summer to molt on large stable first-year ice floes. Extensive fast ice along the coastline and drifting pack ice in the shelf–slope boundary zone provided haul-out areas for seals and penguins with access to feeding in the coastal shelf region. Distributions of potential prey for seals and penguins varied over the study area, as determined by nets, acoustics, and diving surveys. Antarctic krill (Euphausia superba) were found throughout the survey region, overlapping the distributions of two smaller species, Thysanoëssa macrura (primarily off-shelf) and E. crystallorophias (primarily found on-shelf). In some locations, E. superba occurred at high densities underneath ice floes, where they foraged on the sea-ice microbial community. Two general fish communities, oceanic and shelf, were distinguished. Off-shelf fishes were members of the classic oceanic midwater fish fauna, whereas on-shelf fishes were Antarctic endemics. The abundance of pelagic fishes was relatively low throughout the study area compared with other Southern Ocean ecosystems. In contrast, benthic fish biomass and diversity on-shelf were high (41 species, 6 families). Hydroacoustic analyses indicated that densities of potential prey were highest in the coastal shelf region where large aggregations of euphausiids (primarily E. crystallorophias) and individual juvenile Antarctic silverfish (Pleuragramma antarcticum) occurred.

The strenuous and costly measures undertaken by the British Admiralty and others to find the missing expedition of Sir John Franklin during the period 1847–59 were hindered by malicious deceptions, misleading rumours, corrupted translations, unfortunate misunderstandings, and premature conclusions. The false leads included fake messages from Franklin, invented reports of his safety or death in various places, clairvoyant statements that placed him in several widely separated locations, discoveries of objects supposedly associated with his expedition, and distorted reports from Indians and Eskimos. The Admiralty had to investigate all leads, and this took time away from the planning and execution of more important measures.

Although there is increasing recognition that traditional ecological knowledge can make important contributions to environmental and resource-management issues, there are also indications that its use in co-management committees has not been straightforward. Three main sets of challenges have been documented — differences in knowledge systems between western scientific and traditional ecological knowledge, the relatively powerful position of western science and scientists in comparison to traditional ecological knowledge and its users, and challenges in documenting and presenting traditional ecological knowledge. This paper reports the results of a study that surveyed members of co-management committees established in Nunavik, northern Quebec, pursuant to the James Bay and Northern Quebec Agreement to explore their perspectives on these issues. Three elements emerged from this study. They are the complex and sometimes contradictory nature of the views that committee members held about traditional ecological knowledge, the active role of the Inuit in attempting to shape how traditional ecological knowledge is used in decision-making, and the need for documentation of, and research funding for, the collection of traditional ecological knowledge.

‘Microbiologist who took part in ten Antarctic expeditions’

‘Biologist who studied the life of the hardy polar microbe and from it evolved theories of life on Mars’

‘Scientist and astronomer fascinated by the possibility of life on Mars’

‘Applying the lessons of Antarctica to the study of the stars’

This is the third in a series of biographies entitled ‘Children of the Golden Age,’ the purpose of which is to describe the background and contributions of significant living figures in polar research who began their scientific careers following World War II. Born on 17 January 1921 in Melbourne, Gordon de Quetteville Robin was educated at Wesley College and the University of Melbourne, graduating in physics with an MSc in 1942. Following submarine training in Scotland, he served in HMS Stygian in the Pacific. Soon after commencing as a research student in nuclear physics at Birmingham University, he joined the Falkland Islands Dependencies Survey and was the first base commander at Signy Station in the South Orkney Islands (1947–48). In 1949–52 he was third-in-command on the Norwegian–British–Swedish Antarctic Expedition responsible for the successful oversnow seismic ice thickness campaign. In 1958, following a brief sojourn in Canberra, he was appointed the first full-time director of the Scott Polar Research Institute in Cambridge. During the next 24 years he developed SPRI into a world-class research institute. In the austral summer 1959–60 he undertook research operating from RRS John Biscoe in the Weddell Sea into the penetration of ocean waves into pack ice. During the early 1960s he stimulated development of radio echo sounding (RES) with Dr Stan Evans, which remains the standard technique for ice-thickness measurement. He undertook experimental fieldwork in Northwest Greenland in 1964 and airborne sounding in Canada in 1966. He was responsible for organising international collaborative programmes of airborne RES in Antarctica with American air support, leading fieldwork in 1967–68, 1969–70, and 1974–75. He was elected secretary of the Scientific Committee on Antarctic Research in 1958, serving for 12 years, and was president between 1970 and 1974. In 1975 he developed with Dr Terence Armstrong a postgraduate course in Polar Studies at SPRI. He retired as director in 1982 and continues his interests in glaciology as a senior research associate at SPRI.

The Larsemann Hills provide a unique opportunity for studying the environmental impacts of four research facilities run by three nations (Australia, China, and Russia). Soil and water samples collected from the vicinity of each station approximately 10 years after their establishment were analysed for a variety of hydrocarbons, metals, and nutrients. Results confirm that hydrocarbon contamination is the most common impact of the stations. Nutrient enrichment of soil was identified within small areas of each station, and water samples obtained from several local tarns and meltpools revealed low-level contamination by metals and polyaromatic hydrocarbons (PAH). Faecal coliforms were present in intertidal pools adjacent to sewage effluent discharge but not in any other water bodies tested. The cumulative impact of the four facilities was an increase in the number of sites contaminated, rather than increased contamination at specific locations due to the additive effect of overlapping sources. The highest levels of contamination were extremely localised and the footprint of contamination arising from each of the facilities remained discrete from that of neighbouring stations. These data provide a baseline to compare environmental conditions at these locations in the Larsemann Hills before and after implementation of the Protocol on Environmental Protection to the Antarctic Treaty.

At the close of 2002, the United Nations (UN), acting in accordance with its 1999 resolution A54/45, returned to the ‘Question of Antarctica,’ which is currently being placed upon the agenda of the General Assembly's First Committee (Disarmament and International Security) every three years. In 2002, the First Committee's discussions, informed yet again by a report produced by the UN Secretary-General (UNSG) updating members about recent Antarctic developments, reaffirmed the varying perspectives existing within the international community about the management of Antarctica. Following statements delivered by the Polish delegate on behalf of the Antarctic Treaty Parties (ATPs) and the Malaysian representative, the First Committee adopted another consensus draft resolution. Subsequently, the UN General Assembly, acting by consensus without a vote, formally adopted the First Committee's draft as resolution A57/51, which basically updated the wording of that adopted in 1999. Thus, the UNSG was instructed to produce another report to guide the next UN session on the ‘Question of Antarctica’ scheduled for 2005. Although the UN discussions on the topic in 2002 proved relatively brief and low key, the actions of Malaysia during the past year or so have raised a number of questions about the future course of the ‘Question of Antarctica,’ given its lead role in first raising the topic at the UN in 1983 and then maintaining pressure upon the Antarctic Treaty System.