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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"Cooper, Alan"

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Abstracts

Kristoffersen, Y., Goodwin, I. D., & Cooper, A. K. (2000). Effort explores 130 Million years of Antarctic paleoenvironment. Eos, Transactions American Geophysical Union, 81(4), 36–37. https://doi.org/https://doi.org/10.1029/00EO00024

Antarctic climate history has been dominated by events and turning points with causes that are poorly understood. To fill the gaps in our knowledges new effort is underway in the international geologic community to acquire and coordinate the circum-Antarctic geologic data needed to derive and model paleoenvironments of the past 130 m.y. The effort, which focuses principally on using shallow (<100 m) stratigraphic drilling and coring to acquire the geologic data, is being led by the Antarctic Offshore Stratigraphy Project (ANTOSTRAT), a group that works under the aegis of the Scientific Committee on Antarctic Research (SCAR). About 40 scientists from 12 countries met this past summer in Wellington, New Zealand, at an ANTOSTRAT meeting to discuss strategies for implementing the desired paleoenvironmental field and modeling studies. The meeting was held in conjunction with the 8th International Symposium on Antarctic Earth Sciences.

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Engvik, A. K., Elvevold, S., Jacobs, J., Tveten, E., de Azevedo, S., & Njange, F. (2007). Pan-African granulites of central Dronning Maud Land and Mozambique: a comparison within the East-African-Antarctic orogen. In A. Cooper & C. Raymond (Eds.), Antarctica - a keystone in a changing world: online proceedings for the 10th International Symposium on Antarctic Earth Sciences (pp. 1–5). National Academic Press.

Granulite-facies metamorphism is extensively reported in Late Neoproterozoic/Early Palaeozoic time during formation of the East-African-Antarctic orogen (EAAO). Metamorphic data acquired from the Pan-African orogen of central Dronning Maud Land (cDML) are compared with data from northern Mozambique. The metamorphic rocks of cDML are characterised by Opx±Grt-bearing gneisses and Sil+Kfs-bearing metapelites which indicate medium-P granulite-facies metamorphism. Peak conditions, which are estimated to 800-900ºC at pressures up to 1.0 GPa, were followed by near-isothermal decompression during late Pan-African extension and exhumation. Granulite-facies lithologies are widespread in northern Mozambique, and Grt+Cpx-bearing assemblages show that high-P granulitefacies conditions with PT reaching 1.55 GPa and 900ºC were reached during the Pan-African orogeny. Garnet is replaced by symplectites of Pl+Opx+Mag indicating isothermal decompression, and the subsequent formation of Pl+amphibole-coronas suggests cooling into amphibolite facies. It is concluded that high-T metamorphism was pervasive in EAAO in Late Neoproterozoic/Early Paleozoic time, strongly overprinting evidences of earlier metamorphic assemblages.
Barker, P., Barrett, P., Camerlenghi, A., Cooper, A., Davey, F., Domack, E., Escutia, C., Kristoffersen, Y., & O’Brien, P. (1998). Ice sheet history from Antarctic Continental Margin sediments: The ANTOSTRAT approach. Terra Antarctica, 5(4), 737–760. http://pubs.er.usgs.gov/publication/70020442

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Cooper, A. K., Brancolini, G., Escutia, C., Kristoffersen, Y., Larter, R., Leitchenkov, G., O’Brien, P., & Jokat, W. (2008). Cenozoic Climate History from Seismic Reflection and Drilling Studies on the Antarctic Continental Margin. In F. Florindo & M. Siegert (Eds.), Developments in Earth and Environmental Sciences (Vol. 8, pp. 115–234). Elsevier. https://doi.org/https://doi.org/10.1016/S1571-9197(08)00005-0

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Cooper, A., Barker, P., Barrett, P., Behrendt, J., Brancolini, G., Childs, J., Escutia, C., Jokat, W., Kristoffersen, Y., Leitchenkov, G., Stagg, H., Tanahashi, M., Wardell, N., & Webb, P. (2011). The ANTOSTRAT Legacy: Science Collaboration and International Transparency in Potential Marine Mineral Resource Exploitation of Antarctica. In P. A. Berkman, M. A. Lang, D. W. H. Walton, & O. R. Young (Eds.), Science Diplomacy: Antarctica, Science, and the Governance of International Spaces (pp. 223–229). Smithsonian Institution Scholarly Press. https://doi.org/10.5479/si.9781935623069.223

Last update from database: 11/1/24, 3:10 AM (UTC)