Results 241 to 250 of about 53,826 (301)

Millennial-to-orbital-scale subsurface ocean warming and Polynya formation off Dronning Maud Land during the last glacial. [PDF]

Nat Commun
Pinho TML, Nürnberg D, Nele Meckler A, Mollenhauer G, Müller J, Lohmann G, Lembke-Jene L, Hidayat S, Rigalleau V, Lamy F, Tiedemann R.   +10 more
europepmc   +1 more source

Deglacial stratification of the polar Southern Ocean. [PDF]

Proc Natl Acad Sci U S A
Fripiat F, Sigman DM, Ai XE, Dumoulin C, Moretti S, Studer AS, Diekmann B, Esper O, Frederichs T, Lamy F, Liu L, Pattyn F, Schmitt M, Tiedemann R, Haug GH, Martínez-García A.   +15 more
europepmc   +1 more source

Phyllosilicate adsorption limited phosphorus bioavailability in early ferruginous oceans. [PDF]

Nat Commun
Cui X, Zhang Z, Li Q, Knoll AH, Zhao G, Sun M, Huang F, Lu X, Li J, Ju P, Hao J.   +10 more
europepmc   +1 more source

A Submarine Landslides Database of Calabrian Continental Margins (Central Mediterranean Sea). [PDF]

Sci Data
Bianchini M, Chiocci FL, Ceramicola S.
europepmc   +1 more source

Reduced N2 fixation in the Atlantic Ocean during the Warm Late Pliocene

Yehudai M, Farmer J, Straub M, Studer A, Oesch L, Creel R, Schiebel R, Auderset A, Lawrence K, Ogretmen N, Haug G, Sigman D, Martinez-Garcia A.   +12 more
europepmc   +1 more source

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Physical oceanography of continental shelves

Reviews of Geophysics, 1983
Knowledge of the physical oceanography of continental shelves has increased tremendously in recent years, primarily as a result of new current and hydrographic measurements made in locations where no comparable measurements existed previously. In general, observations from geographically distinct continental shelves have shown that the nature of the ...
J. S. Allen, Robert C. Beardsley, J. O. Blanton, William C. Boicourt, Bradford Butman, L. K. Coachman, Adriana Huyer, Thomas H. Kinder, Thomas C. Royer, James D. Schumacher, Robert L. Smith, W. Sturges, Clinton D. Winant   +12 more
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Do continental shelves export organic matter?

Nature, 1986
It has been suggested that biological production and consumption of organic matter is not balanced in coastal marine ecosystems1,2. If, as suggested, 90% of the phytoplankton produced during the spring bloom period were exported, excess organic carbon would be sequestered on the continental slope below the permanent thermocline.
G T, Rowe, S, Smith, P, Falkowski, T, Whitledge, R, Theroux, W, Phoel, H, Ducklow   +6 more
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Continental shelves in the Quaternary

Quaternary International, 2002
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Yim, W. W.-S., Rogers, J., Tovey, N. K.
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Origin of Continental Shelves

AAPG Bulletin, 1946
In order to explain the common occurrence of a shelf edge at the isobath of 200 meters, a widespread subsidence of the shelf area in the order of 100 meters has to be assumed, apart from the influence of eustatic changes of sea-level. Spasmodically a warping or tilting movement has taken place along the continental border, causing a submergence of what
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Continental Slopes and Shelves

The Geographical Journal, 1941
AROUND every continent is a relatively flat but gradually shelving sub-?~^-marine belt running out from the low tide mark. Its width varies greatly, but it is usually between 50 and 150 miles; its outer edge is arbitrarily but conveniently defined by the 100-fathom line.
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