Antarktis-bibliografi er en database over den norske Antarktis-litteraturen.

Hensikten med bibliografien er å synliggjøre norsk antarktisforskning og annen virksomhet/historie i det ekstreme sør. Bibliografien er ikke komplett, spesielt ikke for nyere forskning, men den blir oppdatert.

Norsk er her definert som minst én norsk forfatter, publikasjonssted Norge eller publikasjon som har utspring i norsk forskningsprosjekt.

Antarktis er her definert som alt sør for 60 grader. I tillegg har vi tatt med Bouvetøya.

Det er ingen avgrensing på språk (men det meste av innholdet er på norsk eller engelsk). Eldre norske antarktispublikasjoner (den eldste er fra 1894) er dominert av kvalfangst og ekspedisjoner. I nyere tid er det den internasjonale polarforskninga som dominerer. Bibliografien er tverrfaglig; den dekker både naturvitenskapene, politikk, historie osv. Skjønnlitteratur er også inkludert, men ikke avisartikler eller upublisert materiale.

Til høyre finner du en «HELP-knapp» for informasjon om søkemulighetene i databasen. Mange referanser har lett synlige lenker til fulltekstversjon av det aktuelle dokumentet. For de fleste tidsskriftartiklene er det også lagt inn sammendrag.

Bibliografien er produsert ved Norsk Polarinstitutts bibliotek.

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Topic

polarområdene

Resource type

Book Section

Results 29 resources

Abstracts

Mancilla, A. (2021). Decolonising Antarctica. In D. Bunikowski & A. D. Hemmings (Eds.), Philosophies of polar law (pp. 49–61). Routledge.
Summerhayes, C., Zalasiewicz, J., Vidas, D., & Williams, M. (2020). Polar Regions in the Anthropocene. In K. N. Scott & D. L. VanderZwaag (Eds.), Research handbook on polar law (pp. 18–39). Edward Elgar Publishing.
Kovacs, K. M. (2011). Seler brukt som “forskningsassistenter” for å utforske polhavene. In O. Orheim & K. Ulstein (Eds.), Polaråret 2007-2008 : det norske bidraget (pp. 101–103). Norges forskningsråd. https://doi.org/oai:nb.bibsys.no:991122954014702202 URN:NBN:no-nb_digibok_2014120907592

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Kovacs, K. M., & Coulthard, A. (2011). Seals used as “research assistants” in the polar oceans. In O. Orheim & K. Ulstein (Eds.), International Polar Year 2007-2008 : the Norwegian contribution (pp. 101–103). Research Council of Norway.
Lund, H. Ø., & Berg, S. F. (2011). Bildeberetninger. Mediebegivenheter. Polprospekter. In Norske polarheltbilder : 1888-1928 (pp. 150–155, 208–211, 256–287). Nasjonalbiblioteket Press.
Rike, A. G., Schiewer, S., & Filler, D. M. (2008). Temperature effects on biodegradation of petroleum contaminants in cold soils. In D. L. Barnes, D. M. Filler, & I. Snape (Eds.), Bioremediation of Petroleum Hydrocarbons in Cold Regions (pp. 84–108). Cambridge University Press. https://doi.org/10.1017/CBO9780511535956.007

Bioremediation in cold climates is frequently regarded with skepticism. Owners of polluted sites and regulatory agencies may doubt the effectiveness of biological degradation at near freezing temperatures. While it is true that biodegradation rates decrease with decreasing temperatures, this does not mean that bioremediation is inappropriate for cold regions. Microbial degradation of hydrocarbons occurs even around 0 °C (Chapter 4). In remote alpine, Arctic, and Antarctic locations, excavation and shipping of contaminated soil may be prohibitively expensive. Bioremediation may be the most cost-effective alternative. This chapter discusses microbial adaptation to cold temperatures as well as results of laboratory and field studies of bioremediation at low temperatures.Microorganisms can grow at temperatures ranging from subzero to more than 100 °C. Microbes are divided into four groups based on the range of temperature at which they can grow. The psychrophiles grows at temperatures below 20 °C, the mesophiles between 20 °C and 44 °C, the thermophiles between 45 °C and 70 °C, and the hyperthermophiles require growth temperatures above 70 °C to over 110 °C. The term “cold-adapted microorganisms” (CAMs) is frequently used for describing bacteria growing at or close to zero degrees Celsius. Depending on the cardinal temperatures (the minimal, the optimal, and the maximum growth temperature), CAMs can be classified as psychrophiles or psychrotrophs. Morita's (1975) definition, which holds that psychrophiles have a maximum growth temperature of less than 20 °C and an optimal growth temperature of less than 15 °C, while psychrotrophs have a maximum temperature of 40 °C and an optimal growth temperature higher than 15 °C, is widely accepted.

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Snape, I., Acomb, L., Barnes, D. L., Bainbridge, S., Eno, R., Filler, D. M., Plato, N., Poland, J. S., Raymond, T. C., Rayner, J. L., Riddle, M. J., Rike, A. G., Rutter, A., Schafer, A. N., Siciliano, S. D., & Walworth, J. L. (2008). Contamination, regulation, and remediation: an introduction to bioremediation of petroleum hydrocarbons in cold regions. In D. L. Barnes, D. M. Filler, & I. Snape (Eds.), Bioremediation of Petroleum Hydrocarbons in Cold Regions (pp. 1–37). Cambridge University Press. https://doi.org/10.1017/CBO9780511535956.003

Oil and fuel spills are among the most extensive and environmentally damaging pollution problems in cold regions and are recognized as potential threats to human and ecosystem health. It is generally thought that spills are more damaging in cold regions, and that ecosystem recovery is slower than in warmer climates (AMAP 1998; Det Norske Veritas 2003). Slow natural attenuation rates mean that petroleum concentrations remain high for many years, and site managers are therefore often forced to select among a range of more active remediation options, each of which involves a trade-off between cost and treatment time (Figure 11). The acceptable treatment timeline is usually dictated by financial circumstance, perceived risks, regulatory pressure, or transfer of land ownership.In situations where remediation and site closure are not urgent, natural attenuation is often considered an option. However, for many cold region sites, contaminants rapidly migrate off-site (Gore et al. 1999; Snape et al. 2006a). In seasonally frozen ground, especially in wetlands, a pulse of contamination is often released with each summer thaw (AMAP 1998; Snape et al. 2002). In these circumstances natural attenuation is likely not a satisfactory option. Simply excavating contaminants and removing them for off-site treatment may not be viable either, because the costs are often prohibitive and the environmental consequences of bulk extraction can equal or exceed the damage caused by the initial spill (Filler et al. 2006; Riser-Roberts 1998).

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Arndt, C. E., & Swadling, K. M. (2006). Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies. In Advances in Marine Biology (Vol. 51, pp. 197–315). Academic Press. https://doi.org/10.1016/S0065-2881(06)51004-1

This review concerns crustaceans that associate with sea ice. Particular emphasis is placed on comparing and contrasting the Arctic and Antarctic sea ice habitats, and the subsequent influence of these environments on the life history strategies of the crustacean fauna. Sea ice is the dominant feature of both polar marine ecosystems, playing a central role in physical processes and providing an essential habitat for organisms ranging in size from viruses to whales. Similarities between the Arctic and Antarctic marine ecosystems include variable cover of sea ice over an annual cycle, a light regimen that can extend from months of total darkness to months of continuous light and a pronounced seasonality in primary production. Although there are many similarities, there are also major differences between the two regions: The Antarctic experiences greater seasonal change in its sea ice extent, much of the ice is over very deep water and more than 80% breaks out each year. In contrast, Arctic sea ice often covers comparatively shallow water, doubles in its extent on an annual cycle and the ice may persist for several decades. Crustaceans, particularly copepods and amphipods, are abundant in the sea ice zone at both poles, either living within the brine channel system of the ice‐crystal matrix or inhabiting the ice–water interface. Many species associate with ice for only a part of their life cycle, while others appear entirely dependent upon it for reproduction and development. Although similarities exist between the two faunas, many differences are emerging. Most notable are the much higher abundance and biomass of Antarctic copepods, the dominance of the Antarctic sea ice copepod fauna by calanoids, the high euphausiid biomass in Southern Ocean waters and the lack of any species that appear fully dependent on the ice. In the Arctic, the ice‐associated fauna is dominated by amphipods. Calanoid copepods are not tightly associated with the ice, while harpacticoids and cyclopoids are abundant. Euphausiids are nearly absent from the high Arctic. Life history strategies are variable, although reproductive cycles and life spans are generally longer than those for temperate congeners. Species at both poles tend to be opportunistic feeders and periods of diapause or other reductions in metabolic expenditure are not uncommon.

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Basberg, B. L. (2004). Whalers, explorers and scientists: historical perspectives on the development of the antarctic whaling industry. In A. Elzinga, T. Nordin, D. Turner, & U. Wråkberg (Eds.), Antarctic challenges : historical and current perspectives on Otto Nordenskjöld’s Antarctic expedition 1901-1903 (Vol. 5, pp. 25–38). Royal Society of Arts and Sciences.
Elstad, Å. (2004). Polarturisme. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 3 : Rikdommene (pp. 477-[519]). Gyldendal.
Eriksen, A. (2004). Polarheltene - minner og monumenter. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 1 : Ekspedisjonene (pp. 345–388). Gyldendal.
Sale, R. (2002). Antarctica. In Polar reaches : the history of Arctic and Antarctic exploration (pp. 146–219). Mountaineers Books.
Barr, S. (1999). Ekspedisjonsfotografi i polare områder. In Bildet lever! : bidrag til norsk fotohistorie. 7 (pp. 57–69). Norsk fotohistorisk forening. https://doi.org/oai:nb.bibsys.no:999908187724702202 URN:NBN:no-nb_digibok_2014072108006

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Eriksen, K. E. (1997). Et større Norge 1949-65. In Kald krig og internasjonalisering, 1949-1965 (Vol. 5, pp. 353–380). Universitetsforl. https://doi.org/oai:nb.bibsys.no:999729211174702202 URN:NBN:no-nb_digibok_2010062508034

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Fure, O.-B. (1996). Territoriell ekspansjonspolitikk. In Mellomkrigstid : 1920-1940 (Vol. 3, pp. 109–147). Universitetsforl. https://doi.org/oai:nb.bibsys.no:999617498904702202 URN:NBN:no-nb_digibok_2009110304155

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Berg, R. (1995). Norges polare interesser. In Norge på egen hånd: Vol. II. (pp. 145–150). Universitetsforl. https://doi.org/oai:nb.bibsys.no:999526034704702202 URN:NBN:no-nb_digibok_2010050308080

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Sømme, L., & Block, W. (1991). Adaptations to alpine and polar environments in insects and other terrestrial arthropods. In R. E. Lee & D. L. Denlinger (Eds.), Insects at low temperature (pp. 318–359). Chapman and Hall.
Huntford, R., & Hoff, T. (1988). Sydpolen 1910-1912. In Roald Amundsens oppdagelsesreiser i bilder (pp. 39–142, ill.). Grøndahl. https://doi.org/oai:nb.bibsys.no:998830791604702202 URN:NBN:no-nb_digibok_2013091638079

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Huntford, R. (1987). The South Pole expedition 1910-1912. In The Amundsen photographs (pp. 39–142). Hodder & Stoughton.
Antonsen, P. (1976). Antarktis. In Norske interesser i polarområdene (pp. 30–32). NRK.

Last update from database: 3/1/25, 3:17 AM (UTC)