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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Abstracts

Billen, G., & Becquevort, S. (1991). Phytoplankton-bacteria relationship in the Antarctic marine ecosystem. Polar Research, 10(1), 245–254. https://doi.org/10.3402/polar.v10i1.6743

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Clarke, A., & Peck, L. S. (1991). The physiology of polar marine zooplankton. Polar Research, 10(2), 355–370. https://doi.org/10.3402/polar.v10i2.6752

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Croxall, J. P., & Briggs, D. R. (1991). Foraging economics and performance of polar and subpolar Atlantic seabirds. Polar Research, 10(2), 561–578. https://doi.org/10.3402/polar.v10i2.6767

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Haftorn, S., Bech, C., & Mehlum, F. (1991). Aspects of the breeding biology of the Antarctic Petrel Thalassoica antarctica and the krill requirement of the chicks, at Svarthamaren in Mühlig-Hofmanfjella, Dronning Maud Land. Fauna Norvegica. Serie C. Cinclus, Norwegian Journal of Ornithology, 14(1), 7–22.
Haftorn, S., Bech, C., & Mehlum, F. (1991). Notes on the south polar skua Catharacta Maccormicki breeding at Svarthamaren in Mühlig-Hofmannfjella, Dronning Maud Land. Fauna Norvegica. Serie C. Cinclus, Norwegian Journal of Ornithology, 14(1), 47–48.
Harrison, W. G., & Cota, G. F. (1991). Primary production in polar waters: relation to nutrient availability. Polar Research, 10(1), 87–104. https://doi.org/10.3402/polar.v10i1.6730

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Hellgren, L., Karlstam, B., Mohr, V., & Vincent, J. (1991). Krill Enzymes. A New Concept for Efficient Debridement of Necrotic Ulcers. International Journal of Dermatology, 30(2), 102–103. https://doi.org/10.1111/j.1365-4362.1991.tb04219.x

The article discusses the new concept for surgery of necrotic ulcers using the krill enzymes. The krill peptide hydrolases represent a new and important alternative to mammalian or microbial enzymes for distinctive medical applications, such as debridemen.

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Hunt Jr, G. L. (1991). Occurrence of polar seabirds at sea in relation to prey concentrations and oceanographic factors. Polar Research, 10(2), 553–560. https://doi.org/10.3402/polar.v10i2.6766

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Kuvaas, B., & Kristoffersen, Y. (1991). The Crary Fan: A trough-mouth fan on the Weddell Sea continental margin, Antarctica. Marine Geology, 97(3), 345–362. https://doi.org/https://doi.org/10.1016/0025-3227(91)90125-N

Multichannel seismic investigations show the presence of a large trough-mouth fan deposit on the continental margin in the southern Weddell Sea. A characteristic feature of the fan is relatively few, but large canyons and/or channels which appear to have been stable for long periods. Levees associated with the channels may reach thicknesses of more than 1 km. Drilling during ODP Leg 113 recorded the presence of glaciers in East Antarctica since early Oligocene time, and the seismic stratigraphic evidence suggests that the submarine fan is largely composed of glacigenic sediments. The channel-levee systems and complexes indicate several growth phases, apparently controlled by glacial/interglacial climate fluctuations, with maximum fan growth during glacial periods. The present interglacial period is characterized by strong and erosive flow of Ice Shelf Water running down the western slope of the fan and carrying only minor amounts of suspended matter. The fan is essentially sediment starved during interglacial periods. The dimensions of the channel-levee complexes and the persistent loci of sediment supply suggest that turbidite sedimentation resulted from melting of wet-based glaciers at or near the shelf edge, which has consequently prograded 70-80 km seaward.

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Mathot, S., Becquevort, S., & Lancelot, C. (1991). Microbial communities from the sea ice and adjacent water column at the time of ice melting in the northwestern part of the Weddell Sea. Polar Research, 10(1), 267–276. https://doi.org/10.3402/polar.v10i1.6745

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Norheim, G., Mehlum, F., Bech, C., & Moksnes, M. T. (1991). Distribution of selenium binding proteins in liver from two species of penguins from Bouvetøya. Polar Research, 9(1), 109–111. https://doi.org/10.3402/polar.v9i1.6783

Chinstrap penguin Pygoscelis antarctica and macaroni penguin Eudyptes chrysolophus were collected at Bouvettfya in the south Atlantic. The average hepatic selenium levels for the two species were 6.6 ± 2.9 and 23.6 ± 3.4 ng/g wet weight (P < 0.001), respectively. The total hepatic glutathione peroxidase (GSH-Px) activity in the two species was 629 ± 58 and 838 ± 88 u.kat/kg (P < 0.001), respectively. The average selenium dependent GSH-Px activity was 96 ± 3.2% of the total activity. All selenium was present in the cytosol. The selenium binding compounds were separated on Sephadex G-75 into three fractions, a high molecular weight fraction, a metallothionein fraction, and a third non-protein selenium containing fraction. There seems to be an agreement between the amount of selenium recovered in the first fraction and the GSH-Px activity. In chinstrap and macaroni penguins, the percentage of hepatic selenium recovered in the third non-protein fraction was 83 ± 2.6 and 94 ± 1.1% (P < 0.001), respectively.

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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

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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

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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.

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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.

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