14,172 Works
(Table 2) Chemical composition of airborne material from yellow snow fallen in the Russian North on March 25-26, 2008
Vladimir P Shevchenko, V B Korobov, Alexander P Lisitzin, A S Aleshinskaya, Olga Yu Bogdanova, V B Goryunova, I V Grishchenko, O M Dara & N N Zavernina
These data have been additionally sent by Dr. Vladimir Shevchenko.
(Table 1) Mean grain sizes and standard deviations of gas hydrate samples, supplement to: Klapp, Stephan A; Hemes, H; Klein, Helmut; Bohrmann, Gerhard; MacDonald, Ian R; Kuhs, Werner F (2010): Grain size measurements of natural gas hydrates. Marine Geology, 274(1-4), 85-94
Stephan A Klapp, H Hemes, Helmut Klein, Gerhard Bohrmann, Ian R MacDonald & Werner F Kuhs
Methane hydrates are present in marine seep systems and occur within the gas hydrate stability zone. Very little is known about their crystallite sizes and size distributions because they are notoriously difficult to measure. Crystal size distributions are usually considered as one of the key petrophysical parameters because they influence mechanical properties and possible compositional changes, which may occur with changing environmental conditions. Variations in grain size are relevant for gas substitution in natural hydrates...
(App. Table II-3) Wind parameters and volumes of air filtered through Whatman-41 filters in the Kara Sea in September 1993
Vladimir P Shevchenko
Filter square was 175 sq.cm.
(Table T1) Revised composite depth scale for ODP Site 199-1218
Heiko Pälike, Theodore C Moore, Jan Backman, Isabella Raffi, Luca Lanci, Josep M Parés & Thomas R Janecek(Table T5) Depth mapping pairs from ODP Site 119-1219 to 119-1218
Heiko Pälike, Theodore C Moore, Jan Backman, Isabella Raffi, Luca Lanci, Josep M Parés & Thomas R Janecek
Sediment depth is given in rmcd.
(Table S2) Stable oxygen isotope record and Mg/Ca ratios of Globigerinoides sacculifer from ODP Site 138-847
Michael W Wara, Ana Christina Ravelo & Margaret Lois Delaney
Sediment depth is given in mcd.
(Table S3) Stable oxygen isotope record Globorotalia tumida from ODP Site 138-847
Michael W Wara, Ana Christina Ravelo & Margaret Lois Delaney
Sediment depth is given in mcd.
(Table 7.13) Indicator ratios of tracer elements in Arctic aerosols
Vladimir P Shevchenko(Table 1) Cell number of three size groups of algae and their percentage in total cell number of phytoplankton in the water column in the northern subtropical Pacific
Galina I Semina, A S Mikaelyan & Galina A Belyaeva(Table 4) 40Ar/39Ar total fusion ages of ODP Hole 120-750B
Hubert Whitechurch, R Montigny, James H Sevigny, Michael Storey & Vincent J M Salters
J = 0.0095548, incremental heating
Physical oceanography during HEINCKE cruise HE355
Boris P Koch, Bela Hieronymus Buck & Gerd Rohardt(Table 1) Geotechnical stratigraphic units of ODP Hole 120-751A
Frank R Rack & Amanda Palmer-JulsonBasic measurements of radiation at station Ilorin (1996-03)
T O Aro
Some additional quality control will be performed during summer 2013 for the LW data. For further infos contact Rachel T. Pinker
Documentation of sediment core MD95-2005
Franck C Bassinot & Laurent D LabeyrieDocumentation of sediment core MD95-2010
Franck C Bassinot & Laurent D LabeyrieDocumentation of sediment core MD95-2011
Franck C Bassinot & Laurent D LabeyrieDocumentation of sediment core MD95-2022
Franck C Bassinot & Laurent D LabeyrieDocumentation of sediment core MD95-2025
Franck C Bassinot & Laurent D LabeyrieDocumentation of sediment core MD95-2033
Franck C Bassinot & Laurent D LabeyrieDocumentation of sediment core MD95-2034
Franck C Bassinot & Laurent D LabeyrieDocumentation of sediment core MD95-2039
Franck C Bassinot & Laurent D LabeyrieDocumentation of sediment core MD95-2043
Franck C Bassinot & Laurent D Labeyrie(Table 2) Biomass of the key groups of phytoplankton in the Black Sea in June 1991
T V Yuneva, L S Svetlichnyi, Oleg A Yunev, L V Georgieva & Ludmila G Senichkina
Biomass is average for the 0-100 m layer.
(Table 3) Biomass of dominant species of Peridinea in the Black Sea in June 1991
T V Yuneva, L S Svetlichnyi, Oleg A Yunev, L V Georgieva & Ludmila G Senichkina
Biomass is average for the 0-100 m layer.
Affiliations
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French National Centre for Scientific Research38
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Duke University21
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University of British Columbia20
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The University of Texas at Austin16
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Centre for Ecology & Hydrology13
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UK Centre for Ecology & Hydrology13
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University of Montpellier10
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University of Sheffield10
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University of Cambridge9
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Indiana University9