FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2087968013> ?p ?o ?g. }

• W2087968013 endingPage "117" @default.
• W2087968013 startingPage "95" @default.
• W2087968013 abstract "The distribution of deep-sea benthonic foraminifera in core top samples from the southwest Indian Ocean is examined. Principal component analysis reveals two major assemblages. One assemblages between 3600 and 4800-m water depth is dominated by Episominella umbonifera and is associated with cold (θ = −0.3 to 0.8°C), low salinity (34.66 to 34.72 × 10−3) Antarctic Bottom Water in the Crozet Basin, in fracture zones, and on the flanks of the Southwest Indian Ridge. A second assemblage, dominated by Planulina wuellerstorfi, Globocassidulina subglobasa, Astrononion echolsi and Pullenia bulloides, is between 1600 and 3800 m on the Crozet Plateau, Madagascar Ridge, Central Indian Ridge, and Southwest Indian Ridge and is associated with relatively warm (θ = 0.8 to 2.6°C), high salinity (34.72 to 34.76 × 10−3) North Atlantic Deep Water. The third principal component divides the P. wuellerstorfi assemblage into two subgroups. One is dominated by Epistominella exigua, P. bulloides, P. wuellerstorfi, and A. echolsi and a second is dominated by G. subglobosa. The distribution of the E. umbonifera assemblage and previous hydrographic studies suggest that AABW flows as a western boundary contour current in the Crozet Basin and penetrates fracture zones in the Southwest Indian Ridge between 55 and 57°E and near 66°E as it travels northward into the Madagascar and Mascarene basins. The faunal-water mass associations from the southeast Indian Ocean are compared; the most notable faunal difference is the absence of Uvigerina as a dominant taxon in the southwest Indian Ocean. A comparison of dissolved oxygen and Uvigerina data shows that oxygen is not a major influence upon the distribution of Uvigerina. A correlation analysis of the faunal data and water depth, potential temperature, in situ temperature, salinity, dissolved oxygen, and 1 − Ω, an index of calcium carbonate undersaturation, was carried out to determine the relationships between fauna and hydrography. The second principal component has a significant positive correlation at the 99.9% level with temperature and negative correlations with water depth and 1 − Ω. A general faunal-water mass correlation exists, but it is not possible to determine which variable controls the faunal distributions." @default.
• W2087968013 created "2016-06-24" @default.
• W2087968013 creator A5044132854 @default.
• W2087968013 date "1983-02-01" @default.
• W2087968013 modified "2023-09-27" @default.
• W2087968013 title "Distribution of Holocene deep-sea benthonic foraminifera in the southwest Indian Ocean" @default.
• W2087968013 cites W1966087894 @default.
• W2087968013 cites W1971776270 @default.
• W2087968013 cites W1974152132 @default.
• W2087968013 cites W1981319527 @default.
• W2087968013 cites W1985217750 @default.
• W2087968013 cites W1986321210 @default.
• W2087968013 cites W1987139609 @default.
• W2087968013 cites W1990266576 @default.
• W2087968013 cites W1991122201 @default.
• W2087968013 cites W1997582396 @default.
• W2087968013 cites W1998112941 @default.
• W2087968013 cites W2007086229 @default.
• W2087968013 cites W2007144211 @default.
• W2087968013 cites W2018631606 @default.
• W2087968013 cites W2032945081 @default.
• W2087968013 cites W2033823888 @default.
• W2087968013 cites W2042823304 @default.
• W2087968013 cites W2060216496 @default.
• W2087968013 cites W2062023725 @default.
• W2087968013 cites W2062045651 @default.
• W2087968013 cites W2071763271 @default.
• W2087968013 cites W2072166221 @default.
• W2087968013 cites W2080665863 @default.
• W2087968013 cites W2089727487 @default.
• W2087968013 cites W2089938349 @default.
• W2087968013 cites W2090349353 @default.
• W2087968013 cites W2090785312 @default.
• W2087968013 cites W2114779017 @default.
• W2087968013 cites W2145742014 @default.
• W2087968013 cites W2328519808 @default.
• W2087968013 cites W2329203376 @default.
• W2087968013 doi "https://doi.org/10.1016/0198-0149(83)90064-x" @default.
• W2087968013 hasPublicationYear "1983" @default.
• W2087968013 type Work @default.
• W2087968013 sameAs 2087968013 @default.
• W2087968013 citedByCount "66" @default.
• W2087968013 countsByYear W20879680132012 @default.
• W2087968013 countsByYear W20879680132013 @default.
• W2087968013 countsByYear W20879680132014 @default.
• W2087968013 countsByYear W20879680132015 @default.
• W2087968013 countsByYear W20879680132016 @default.
• W2087968013 countsByYear W20879680132017 @default.
• W2087968013 countsByYear W20879680132021 @default.
• W2087968013 countsByYear W20879680132022 @default.
• W2087968013 countsByYear W20879680132023 @default.
• W2087968013 crossrefType "journal-article" @default.
• W2087968013 hasAuthorship W2087968013A5044132854 @default.
• W2087968013 hasConcept C109007969 @default.
• W2087968013 hasConcept C111368507 @default.
• W2087968013 hasConcept C127313418 @default.
• W2087968013 hasConcept C140302290 @default.
• W2087968013 hasConcept C140345934 @default.
• W2087968013 hasConcept C151730666 @default.
• W2087968013 hasConcept C157485413 @default.
• W2087968013 hasConcept C2780275952 @default.
• W2087968013 hasConcept C2780368712 @default.
• W2087968013 hasConcept C2988134249 @default.
• W2087968013 hasConcept C32277403 @default.
• W2087968013 hasConcept C6582778 @default.
• W2087968013 hasConcept C76256466 @default.
• W2087968013 hasConcept C83042747 @default.
• W2087968013 hasConceptScore W2087968013C109007969 @default.
• W2087968013 hasConceptScore W2087968013C111368507 @default.
• W2087968013 hasConceptScore W2087968013C127313418 @default.
• W2087968013 hasConceptScore W2087968013C140302290 @default.
• W2087968013 hasConceptScore W2087968013C140345934 @default.
• W2087968013 hasConceptScore W2087968013C151730666 @default.
• W2087968013 hasConceptScore W2087968013C157485413 @default.
• W2087968013 hasConceptScore W2087968013C2780275952 @default.
• W2087968013 hasConceptScore W2087968013C2780368712 @default.
• W2087968013 hasConceptScore W2087968013C2988134249 @default.
• W2087968013 hasConceptScore W2087968013C32277403 @default.
• W2087968013 hasConceptScore W2087968013C6582778 @default.
• W2087968013 hasConceptScore W2087968013C76256466 @default.
• W2087968013 hasConceptScore W2087968013C83042747 @default.
• W2087968013 hasIssue "2" @default.
• W2087968013 hasLocation W20879680131 @default.
• W2087968013 hasOpenAccess W2087968013 @default.
• W2087968013 hasPrimaryLocation W20879680131 @default.
• W2087968013 hasRelatedWork W1965372156 @default.
• W2087968013 hasRelatedWork W1983909472 @default.
• W2087968013 hasRelatedWork W1986954636 @default.
• W2087968013 hasRelatedWork W2018858958 @default.
• W2087968013 hasRelatedWork W2073026692 @default.
• W2087968013 hasRelatedWork W2076839274 @default.
• W2087968013 hasRelatedWork W2163410276 @default.
• W2087968013 hasRelatedWork W2775775372 @default.
• W2087968013 hasRelatedWork W3012224338 @default.
• W2087968013 hasRelatedWork W3093015563 @default.
• W2087968013 hasVolume "30" @default.
• W2087968013 isParatext "false" @default.
• W2087968013 isRetracted "false" @default.

• next