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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Resource type

Journal Article

Results 1,887 resources

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Abstracts

Prestvik, T., & Duncan, R. A. (1991). The geology and age of Peter I Øy, Antarctica. Polar Research, 9(1), 89–98. https://doi.org/10.3402/polar.v9i1.6781

The island Peter I Oy is located in the Bellinghausen Sea 400 km off the coast of West Antarctica. It is situated at the transition between oceanic and contintental crust close to a former transform fault, the Tharp fracture zone. The island is completely volcanic, consisting of predominantly alkali basalt and hawaiite and some more evolved rocks. Sampling done by the Aurora expedition in 1987 has made dating and detailed petrological studies possible. The island appears to be much younger (< 0.5 Ma) than previously believed. However, the volcanic activity responsible for this oceanic island may have lasted for 10-20 Ma. Volcanic activity at the island thus took place at the same time as post-subduction rift-related volcanism took place along the Antarctic Peninsula and in Marie Byrd Land. However, the petrologic data indicate that this may be coincidental and that the Peter I Oy activity is independent and related to transtensional rifting along the Tharp fracture zone.

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Ringstad, J. E. (1991). Hvalfangernes mat til hverdag og fest. Utkikksposten (Sandefjord) : kontaktorgan for Sandefjordmuseene, 4, 31–32. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2018121481070_001 URN:NBN:no-nb_digitidsskrift_2018121481070_001

View on urn.nb.no
Røv, N. (1991). The density of breeding and non-breeding Antarctic petrels at Svarthamaren, Dronning Maud Land, 1990. Fauna Norvegica. Serie C. Cinclus, Norwegian Journal of Ornithology, 14(2), 49–53.
Sakshaug, E., & Slagstad, D. (1991). Light and productivity of phytoplankton in polar marine ecosystems: a physiological view. Polar Research, 10(1), 69–86. https://doi.org/10.3402/polar.v10i1.6729

View on doi.org
Sakshaug, E., Slagstad, D., & Holm-Hansen, O. (1991). Factors controlling the development of phytoplankton blooms in the Antarctic Ocean — a mathematical model. Marine Chemistry, 35(1), 259–271. https://doi.org/https://doi.org/10.1016/S0304-4203(09)90021-4

A mathematical model describing the development of phytoplankton blooms as a function of the depth of the wind-mixed layer, spectral distribution of light, passage of atmospheric low-pressure systems, size of the initial phytoplankton stock and loss rates is presented. Model runs represent shade-adapted, large-celled, bloom-forming diatoms. Periodic deep mixing caused by strong winds may severely retard the development of blooms and frequently abort them before macronutrients are completely exhausted. Moderate depths of mixing (40-50 m) in combination with a moderately large total loss rate (about 0.01 3 h-1) can prevent blooms from developing during the brightest time of the year. Complete exhaustion of macronutrients in the upper waters is likely only if the wind-mixed layer is less than 10 m deep, i.e. in very sheltered waters, and also in the marginal ice zone when ice is melting. We do not exclude the possibility of control of phytoplankton biomass by iron in ice-free, deep-sea parts of the Antarctic Ocean, but the implied enhancement of export production through addition of iron might be restricted because of limitation by light, i.e. vertical mixing.

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Scully, R. T. (1991). The Eleventh Antarctic Treaty Consultative Meeting. International Challenges, 11(1), 77–90.
Smith, R. I. L., & Øvstedal, D. O. (1991). The lichen genus Stereocaulon in Antarctica and South Georgia. Polar Biology, 11(2), 91–102. https://doi.org/10.1007/BF00234271

Six species of Stereocaulon and one unnamed taxon (close to S. glabrum) are reported from South Georgia, the maritime Antarctic islands and Antarctic Peninsula. S. caespitosum is new to the western sub-Antarctic. Variations in morphology and secondary chemistry are provided, and the ecology and geographical distribution in the sub-Antarctic and Antarctic biomes are given for each taxon.

View on doi.org
Stokke, O. S. (1991). Conference report: preservation or exploitation. Marine Policy, 15(2), 137–141.
Stokke, O. S. (1991). Symposium report: “The Antarctic Treaty System in World Politics.” International Challenges, 11(2), 59–66.
Sæther, B.-E. (1991). Antarktispetrellen: på grensen av det mulige. Naturen, 115(6), 249–253. https://urn.nb.no/URN:NBN:no-nb_digitidsskrift_2015071381019_001

View on urn.nb.no
Ursin, H., Bergan, T., Collet, J., Endresen, I. M., Lugg, D., Maki, P., Matre, R., Molvær, O. I., Müller, H. K., Olff, M., Pettersen, R. C., Sandal, G. M., Værnes, R. J., & Warncke, M. (1991). Psychobiological Studies of Individuals in Small, Isolated Groups in the Antarctic and in Space Analogues. Environment and Behavior, 23(6), 766–781. https://doi.org/10.1177/0013916591236007

Mental and physical health are both at risk under conditions of prolonged remoteness from home and removal from normal social support networks. This article examines relevant data from small groups isolated in (a) Antarctic summer stations, (b) a Transantarctic traverse expedition, and (c) a spacecraft simulator capsule.

View on doi.org
Wexelsen, E. (1991). Sandefjord - et naturlig polarforskningssenter. Utkikksposten (Sandefjord) : kontaktorgan for Sandefjordmuseene, 3, 30–32. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2018121481072_001 URN:NBN:no-nb_digitidsskrift_2018121481072_001

View on urn.nb.no
Yen, J. (1991). Predatory feeding behavior of an Antarctic marine copepod, Euchaeta antarctica. Polar Research, 10(2), 433–442. https://doi.org/10.3402/polar.v10i2.6757

View on polarresearch.net
Andersen, R. T. (1990). Negtiationg a new regime: how CRAMRA came into existence. International Challenges, 10(1), 21–23.
Barnes, J. N. (1990). Protection of the environment in Antarctica: are present regimes sufficient? International Challenges, 10(1), 52–55.
Barr, S. (1990). Antarctica’s cultural heritage: can ICOMOS help? Icomos Information, 1990(2), 30–35.
Beck, P. J. (1990). The resource conventions implemented: the consequences for the sovereignty issue. International Challenges, 10(1), 56–60.
Beddington, J. R., Basson, M., & Gulland, J. A. (1990). The practical implications of the eco-system approach in CCAMLR. International Challenges, 10(1), 17–20.
Bos, A. (1990). Consultative status under the Antarctic Treaty: redefining the criteria? International Challenges, 10(1), 73–77.
Brown, A. D. (1990). The design of CRAMRA: how appropriate for the protection of the environment? International Challenges, 10(1), 24–26.

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Last update from database: 12/1/25, 3:10 AM (UTC)