Academic literature on the topic 'NW Barents Sea'
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Journal articles on the topic "NW Barents Sea"
ROBERTS, R. J., T. H. TORSVIK, T. B. ANDERSEN, and E. F. REHNSTRÖM. "The Early Carboniferous Magerøy dykes, northern Norway: palaeomagnetism and palaeogeography." Geological Magazine 140, no. 4 (July 2003): 443–51. http://dx.doi.org/10.1017/s0016756803008082.
Full textKlitzke, P., J. I. Faleide, M. Scheck-Wenderoth, and J. Sippel. "A lithosphere-scale structural model of the Barents Sea and Kara Sea region." Solid Earth Discussions 6, no. 2 (July 10, 2014): 1579–624. http://dx.doi.org/10.5194/sed-6-1579-2014.
Full textZecchin, Massimo, Michele Rebesco, Renata G. Lucchi, Mauro Caffau, Hendrik Lantzsch, and Till J. J. Hanebuth. "Buried iceberg-keel scouring on the southern Spitsbergenbanken, NW Barents Sea." Marine Geology 382 (December 2016): 68–79. http://dx.doi.org/10.1016/j.margeo.2016.10.005.
Full textMidtkandal, Ivar, Jan Inge Faleide, Thea Sveva Faleide, Christopher Sæbø Serck, Sverre Planke, Romain Corseri, Myrsini Dimitriou, and Johan Petter Nystuen. "Lower Cretaceous Barents Sea strata: epicontinental basin configuration, timing, correlation and depositional dynamics." Geological Magazine 157, no. 3 (September 16, 2019): 458–76. http://dx.doi.org/10.1017/s0016756819000918.
Full textJankowski, A. W. "Transfer of Platycola circularis Dons, 1941, symbiont of wood-boring isopod Limnoria, to Lagenophrys (Ciliophora, Peritrichia)." Proceedings of the Zoological Institute RAS 319, no. 1 (March 25, 2015): 23–39. http://dx.doi.org/10.31610/trudyzin/2015.319.1.23.
Full textCaridi, F., A. Sabbatini, M. Bensi, V. Kovačević, R. G. Lucchi, C. Morigi, P. Povea, and A. Negri. "Benthic foraminiferal assemblages and environmental drivers along the Kveithola Trough (NW Barents Sea)." Journal of Marine Systems 224 (December 2021): 103616. http://dx.doi.org/10.1016/j.jmarsys.2021.103616.
Full textJørgensen, Lis Lindal, Pavel Ljubin, Hein Rune Skjoldal, Randi B. Ingvaldsen, Natalia Anisimova, and Igor Manushin. "Distribution of benthic megafauna in the Barents Sea: baseline for an ecosystem approach to management." ICES Journal of Marine Science 72, no. 2 (July 2, 2014): 595–613. http://dx.doi.org/10.1093/icesjms/fsu106.
Full textMurdmaa, Ivar, Leonid Polyak, Elena Ivanova, and Natalia Khromova. "Paleoenvironments in Russkaya Gavan' Fjord (NW Novaya Zemlya, Barents Sea) during the last millennium." Palaeogeography, Palaeoclimatology, Palaeoecology 209, no. 1-4 (July 2004): 141–54. http://dx.doi.org/10.1016/j.palaeo.2004.02.020.
Full textZecchin, Massimo, and Michele Rebesco. "Glacigenic and glacimarine sedimentation from shelf to trough settings in the NW Barents Sea." Marine Geology 402 (August 2018): 184–93. http://dx.doi.org/10.1016/j.margeo.2018.02.014.
Full textSagnotti, Leonardo, Patrizia Macrì, and Renata G. Lucchi. "Geomagnetic palaeosecular variation around 15 ka ago from NW Barents Sea cores (south of Svalbard)." Geophysical Journal International 204, no. 2 (December 10, 2015): 785–97. http://dx.doi.org/10.1093/gji/ggv485.
Full textDissertations / Theses on the topic "NW Barents Sea"
Matteo, Bazzaro. "Past and active biogeochemical processes in the Kveithola trough (NW Barents Sea)." Doctoral thesis, Università di Siena, 2019. http://hdl.handle.net/11365/1089134.
Full textCARIDI, FRANCESCA. "Influence of environmental patterns on the benthic faunal structure in the Kveithola Trough, NW Barents Sea." Doctoral thesis, Università Politecnica delle Marche, 2020. http://hdl.handle.net/11566/274551.
Full textFor the first time, we have documented the Arctic benthic faunal structure in the Kveithola Trough (NW Barents Sea), to improve knowledge gaps existing in this area. The Kveithola is characterized by peculiar morpho-depositional and hydrographic conditions, which allow to distinguish three main areas (the outer, the inner area and Northern channel). In the outer area, high hydrodynamic does not favour the accumulation of the organic matter and low sediment organic carbon bioavailability supports a poorly sediment community oxygen consumption. The inner part and Northern channel represent an eutrophic area, dominated by a detritivores community (subsurface-feeding polychaeta Maldane sarsi, the surface-feeding polychaeta Lenvisenia gracilis, the subsurface lamellibranch bivalve Mendicula cf. pigmea, the subsurface protobranch bivalve genus Yoldiella), predators belonging to Nemertea and foraminifera as calcareous Nonionellina labradorica, Globobulimina auriculata and agglutinated Lagenammina difflugiformis. These taxa indicate the presence of an organic-rich sediment and oxygen-depleted environment possibly linked to a cold seep system and are also responsible for the bioturbation activity. Interestingly, delicate foraminifera monothalamous morphotypes (Micrometula and Cylindrogullmia) were reported from all sites with high abundance percentage, they inhabit typically the detritus layer of Arctic fjords and live in an extremely oxygen-deficient environment. Meanwhile, megafauna results suggest the possibility of the methane emission creating a biomass and diversity hotspot on the site 21 seafloor, characterized by heterogeneous environment with carbonate structures, microbial mats and chemosynthetic worm tufts. To conclude, the distinct geomorphological and environmental feature, supply of organic matter and seep activity of this area, are key drivers of benthic faunal structure and their heterogeneity distribution.
Book chapters on the topic "NW Barents Sea"
Llopart, J., R. Urgeles, A. Camerlenghi, R. G. Lucchi, B. De Mol, M. Rebesco, and M. T. Pedrosa. "Slope Instability of Glaciated Continental Margins: Constraints from Permeability-Compressibility Tests and Hydrogeological Modeling Off Storfjorden, NW Barents Sea." In Submarine Mass Movements and Their Consequences, 95–104. Cham: Springer International Publishing, 2013. http://dx.doi.org/10.1007/978-3-319-00972-8_9.
Full textConference papers on the topic "NW Barents Sea"
Pizzigalli, Claudia, Giancarlo Giovanetti, Lisa Pedinelli, and Roberto Padilla-Hernandez. "NOAA-CFSR Offshore Wind Validation." In ASME 2021 3rd International Offshore Wind Technical Conference. American Society of Mechanical Engineers, 2021. http://dx.doi.org/10.1115/iowtc2021-3547.
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