Results 251 to 260 of about 187,427 (307)

Domestication-Admixed Atlantic Salmon (Salmo salar) Establish a Productive Population in the Wild. [PDF]

Ecol Lett
Harvey AC, Skaala Ø, Besnier F, Østebø BI, Sørvik AG, Fjeldheim PT, Unneland L, Brieuc MSO, Ayllon F, Utne KR, Solberg MF, Glover KA.   +11 more
europepmc   +1 more source

Deep-sea gas hydrate mounds and chemosynthetic fauna discovered at 3640 m on the Molloy Ridge, Greenland Sea. [PDF]

Nat Commun
Panieri G, Copley JT, Linse K, Nye V, Ramirez-Llodra E, Argentino C, Ferré B, Arctic Deep - Extreme24 consortium, Rogers AD.   +8 more
europepmc   +1 more source

Intensification of extreme cold events in East Asia in response to global mean sea-level rise. [PDF]

Nat Commun
Dong C, Zhang Z, Keenlyside N, Sobolowski SP, Otterå OH, Bonaduce A, Xie J, Raj RP, Liu Y, Liu B, Wu M.   +10 more
europepmc   +1 more source

Prokaryotic viability and active metabolism across a Greenland Sea transect (75°N latitude). [PDF]

AIMS Microbiol
Rappazzo AC, Caruso G, Cosenza A, Giudice AL, Maimone G, Papale M, Bensi M, Kovacevic V, Azzaro M.   +8 more
europepmc   +1 more source

Annual Reports to the ESA Council ESA 110th Annual Meeting July, 2025

The Bulletin of the Ecological Society of America, EarlyView.
wiley   +1 more source

Norwegische See 1969 = Norwegian Sea 1969

, 1969
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Lofoten Composite Tectono-Sedimentary Element, Norwegian Rifted Margin, Norwegian Sea

Geological Society, London, Memoirs, 2022
The Lofoten Rifted Margin is a composite tectono-sedimentary element (CTSE), located offshore northern Norway, and comprises the northernmost part of the Norwegian Sea margin at its transition to the West Barents Sea margin. We refine the late Paleozoic–early Cenozoic evolution of the margin with emphasis on the late Mesozoic–early Cenozoic rift phases,
Filippos Tsikalas, Juan Camilo Meza-Cala, Mohamed Mansour Abdelmalak, Jan Inge Faleide, Harald Brekke   +4 more
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The Lofoten Drift, Norwegian Sea

Geological Society, London, Memoirs, 2002
Abstract The Lofoten Contourite Drift is located below c . 1000 m water depth on the continental slope off northern Norway. It has a maximum thickness of about 360 m and correlation to published seismic stratigraphy implies a Neogene age.
Jan Sverre Laberg, Tore O. Vorren, Stig-Morten Knutsen   +2 more
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The Andøya Canyon, Norwegian Sea

Geological Society, London, Memoirs, 2016
The relatively steep continental slope offshore north Norway (3–7°) is dissected by several valleys (e.g. Taylor et al. 2000; Rise et al. 2013), none of which is related to coastal rivers opening into the fjords dominating the coast (Corner 2005). Two end-member valley forms have been identified: (1) classical submarine canyons characterized by a V ...
J. S. Laberg, H. B. Amundsen, T. A. Rydningen   +2 more
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Norwegian-Greenland Sea thermal field

Geological Society, London, Special Publications, 2000
Abstract Thermal gradient and thermal conductivity measurements carried out in the Norwegian-Greenland Sea and in the western Eurasia Basin from 1967 to 1996 have yielded 436 heat-flow values which have been stored on a UNIX-platform database, heat , to facilitate retrieval, documentation and display.
Eirik Sundvor, Olav Eldholm, Tadeusz P Gladczenko, Sverre Planke   +3 more
openaire   +1 more source