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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Sørishavet

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Abstracts

Ellingsen, T. E., & Norges tekniske høgskole Institutt for teknisk, biokjemi. (1982). Biokjemiske studier over antarktisk krill [Institutt for teknisk biokjemi]. https://www.nb.no/items/URN:NBN:no-nb_digibok_2015062508118

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Fossum, B. A., Maisey, G. H., & Torsen, H. O. (1982). Marine geophysical research in the Weddell Sea during the Norwegian Antarctic research expedition of 1976-77. In Craddock, Campbell (Ed.), Antarctic geoscience : Symposium on Antarctic Geology and Geophysics, Madison, Wisconsin, U.S.A., August 22-27, 1977: Vol. Series B-Number 4 (pp. 397–405). The University of Wisconsin Press Madison.
Haugland, K. (1982). Seismic reconnaissance survey in the Weddell Sea. In Craddock, Campbell (Ed.), Antarctic geoscience: Vol. Series B-Number 4 (pp. 405–413). The University of Wisconsin Press Madison.
Jacobsen, A. R. (1982). Eventyret Anders Jahre. Oktober. https://doi.org/oai:nb.bibsys.no:998320987794702202 URN:NBN:no-nb_digibok_2013092407005

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Orheim, O. (1982). Vil noen satse formuen på isfjelltauing i Sørishavet? Polarboken, 1981/82, 81–87.
Orheim, O., & Govorukha, L. S. (1982). Present-day glaciation in the South Shetland Islands. Annals of Glaciology, 3, 233–238. https://doi.org/10.3189/S0260305500002834

This paper presents mass-balance results from Deception Island for 1968–69 to 1973–74, from King George Island for the balance years 1969–70 and 1970–71, and from Livingston Island from 1971–72 to 1973–74. The accumulation areas of all localities are in the soaked fades, with a firn/ice transition at King George Island at 12 to 20 m depth. Of the glaciers studied, only “Gl” on Deception Island terminates wholly on land and has a relatively large ablation area. The mass-balance curves are similar for King George Island and Livingston Island, with equilibrium lines at around 150 m elevation. “Gl“ on Deception Island has more negative summer balances, and the equilibrium line ranged from 275 to 370 m during the six balance years. Here, there were no years of positive net mass balance, and large negative net values during the 1970–71 to 1972–73 balance years. This resulted from a lowered albedo caused by ash from the August 1970 eruption. Ash layers from the Deception Island eruptions are also observed on Livingston Island and King George Island, where they form stratigraphic markers in the accumulation areas of the glaciers. Annual balance variations from 1957–58 to 1970–71, based on stratigraphic studies at Deception Island and King George Island, show good correlations, indicating that the variations reflect changes in regional climate.
Orheim, O., Wadhams, P., & Kristensen, M. (1982). Iceberg response to sea state. Iceberg Research, 1, 10–15.
Orheim, O., Wadhams, P., & Kristensen, M. (1982). Iceberg response to sea state (abstract only). Annals of Glaciology, 3, 357. https://doi.org/10.3189/S0260305500003360
Sakshaug, E. (1982). Krill: mat i mengder i Sørishavet. Syn og segn, 88(8), 482–489. https://urn.nb.no/URN:NBN:no-nb_digitidsskrift_2014092382254_001

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Tønnessen, J. N., & Johnsen, A. O. (1982). The history of modern whaling. C. Hurst.
Elverhøi, A. (1981). Evidence for a late Wisconsin glaciation of the Weddell Sea. Nature, 293(5834), 641–642. https://doi.org/10.1038/293641a0

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Elverhøi, A., & Roaldset, E. (1981). Glaciomarine sediments and suspended particulate matter, Weddell sea, Antarctica (abstract only). Annals of Glaciology, 2, 142. https://doi.org/10.3189/172756481794352234

Samples of glaciomarine sediments and suspended particulate matter filtered from sea-water were collected in the Weddell Sea during the Norwegian Antarctic Research Expedition (NARE) in 1978–79. Analyses have provided information on the textural and mineralogical composition of shelf sediments, on the nature of biogenic and inorganic suspended particulate matter, and on the total sediment transport to the shelf areas and further into the deeper waters (). The shelf waters contain 0.1 to 1.2 g m–3 of suspended particulate matter, which is close to the range of 0.5 to 1.5 g m–3 reported for suspension concentrations in the oceans, but considerably lower than that found for some other glaciomarine environments such as the Bering Sea {up to 13-15 g m–3 ()) and off Kongsbreen, Spitsbergen {up to 500 g m–3 ()). Suspended particles from the Weddell Sea have maximum sizes of 50 to 70 µm and mean diameters in the range of 10 to 20 µm. In contrast, the bottom sediments on the outer shelf are deficient in the corresponding fractions. This reflects that when floating Antarctic ice supplies material to the Weddell Sea, the coarser fragments (>20-70 µm) are deposited, while the medium silt and finer fractions go into suspension. Considering the suspended-load data and the bottom-current measurements on the shelf break, it is evident that in January 1979 an average of 8.6 × 104tonnes d–1 (or 32 × 106 tonnes a–l) of particulate matter was transported by the current from the central Weddell Sea to the South Atlantic deep water. Morphological (scanning electron microscopy) and chemical analyses show the suspended material to be dominated by silica organisms (diatoms), and also to contain clastic grains of phyllosilicates, feldspar, quartz, zircon, in a few cases Al- and Fe-hydroxides/oxides also; authigenic “Fe-sepiolite” and secondary gypsum. Mineralogical analyses (X-ray diffraction) of the bottom sediments show the fine sand silt fractions to contain mainly clastic materials like illite, smectite-vermiculite, and quartz. Biogenic silica (cristobalite) and carbonate (Mg-calcite) as well as authigenic Fe-silicates (“Fe-sepiolite”) are also present.

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Fevolden, S. E., & Ayala, F. J. (1981). Enzyme polymorphism in Antarctic krill (Euphausiacea); genetic variation between populations and species. Sarsia, 66(3), 167–181. https://doi.org/10.1080/00364827.1981.10414536

By means of enzyme electrophoretical assays three samples of Euphausia superba, all from the Atlantic sector of the Antarctic Ocean, were examined to see whether or not they represent genetically separated populations. The same samples were also compared with E. superba from off the Western coast of the Antarctic Peninsula, representing the Pacific sector. The latter animals have previously been studied by other authors. One sample of a second species of Antarctic krill, E. crystallorophias, was likewise examined. Thirty-five loci were studied in E. superba, and it is concluded that the three samples from the Atlantic sector most probably do not represent reproductively isolated populations. Their average heterozygosity, about 10%, is however greater than the value previously found for the ‘Pacific’ E. superba, 5.8 %. Calculations of the genetic identity and genetic distance between the Atlantic and ‘Pacific’ samples of E. superba suggest they represent separate populations. The average heterozygosity of E. crystallorophias was estimated to be between 9.1 and 9.4 %, from studies of 33 loci. The genetic distance between this species and E. superba was estimated at 0.989. The results are finally discussed in terms of postulated theories on genetic variability versus environmental heterogeneity.

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Fevolden, S. E., & Eidså, G. (1981). Bacteriologigal characteristics of Antarctic krill (Crustacea, Euphausiacea). Sarsia, 66(1), 77–82. https://doi.org/10.1080/00364827.1981.10414524

The bacterial flora of two species of Antarctic krill, Euphausia superba Dana and E. crystallorophias Holt & Tattersall, was studied with the aim of investigating the role played by bacteria during the claimed rapid deterioration of these animals. The number of bacteria on fresh krill was characterized as low, but started to increase exponentially after a few days of storage at low temperatures. Dominant species were of the genera Moraxella, Pseudomonas, and Alteromonas. Comparing the low initial number of bacteria with the high autolytic activity it is suggested that the rapid degradation of krill during the first days of storage is induced by autolysis and not by bacterial activity.

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Gammelsrød, T., & Slotsvik, N. (1981). Hydrographic and current measurements in the southern Weddell Sea 1979/80. Polarforschung, 51(1), 101–111. https://doi.org/10013/epic.29502.d001

During the 1979-1980 expediton with the icebreaker Polarsirkel we had an excellent opportunity to study the physical oceanography of the inner part of the Weddell Sea. The ship followed the ice shelf barrier from Cape Norwegia at about 15 °W, and due to favourable ice conditions, it was able to penetrate all the way to the Antarctic Peninsula (60 0W). In this preliminary report we give a review of the physical oceanography programme which mostly consists of hydrographic (CTD) stations near the barrier, and also sorne current and water level measurernents. The different water masses observed are described and the possibility for a tidal-drlvcn upwelling near the ice shelf barrier is indicated.

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Hodne, F. (1981). Hvalfangst 1868-1914. Hvalfangst blir en ny vekstnæring. In Norges økonomiske historie 1815-1970 (pp. 128–130, 494–498). Cappelen. https://doi.org/oai:nb.bibsys.no:998110569964702202 URN:NBN:no-nb_digibok_2007071004046

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Johnson, G. L., Vanney, J.-R., Elverhøi, A., & LaBrecque, J. L. (1981). Morphology of the Weddell Sea and southwest Indian Ocean. Deutsche Hydrografische Zeitschrift, 34(6), 263–272. https://doi.org/10.1007/BF02226642

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Kristensen, M., Orheim, O., & Wadhams, P. (1981). Field experiments on Antarctic tabular icebergs. Polar Record, 20(128), 445–448. https://doi.org/10.1017/S0032247400003661
Lien, R. (1981). Sea bed feauters in the Blåenga area, Weddell Sea, Antarctica. Université Laval.
Næss, E. D., & Cameron, E. (1981). Shipping - mitt liv : en selvbiografi. A/S Hjemmet Fagpresseforlaget. https://doi.org/oai:nb.bibsys.no:998110912444702202 URN:NBN:no-nb_digibok_2012110206001

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