FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1976582157> ?p ?o ?g. }

• W1976582157 endingPage "77" @default.
• W1976582157 startingPage "63" @default.
• W1976582157 abstract "A 47‐ to 60‐mm‐thick Fe‐Mn crust from Horizon Guyot (water depth 1800–1780 m), central Pacific, was used to evaluate the potential of crusts as recorders of Neogene paleoceanographic and paleoclimatic conditions. The chemical composition was determined by microprobe for 16 elements from a polished thin section. Three analyses were made per millimeter and averaged to give the composition of each millimeter. The age of the crust was determined by measuring the strontium isotope composition of the crust and comparing it with the Tertiary seawater curve. The crust represents 18.5 m.y. of growth of Fe and Mn oxyhydroxides. The crust is composed of alternating botryoidal and laminated layers. The botryoidal layers formed during the same time intervals that widespread Neogene deep‐sea hiatuses were forming in bottom sediments. The botryoidal layers represent growth during times of intensified deepwater flow, whereas the laminated intervals represent more quiescent conditions. The correspondence between the botryoidal layers and the Neogene hiatuses is so strong that we were able to choose a variable growth rate model over a constant growth rate model for the crust. Chemical changes in the crust take two forms. The first is represented by broad changes in the composition defined chiefly by fourth‐order polynomial fits to the chemical profiles of each element with depth in the crust. The second is high‐frequency changes in composition. The broader changes occurred primarily at about 15, 11.5, 7.4, 6.4, 5.2, and 4.6 Ma, which may correlate with major changes in paleoceanographic circulation and development of ice caps at the poles. The periods of the high‐frequency changes may reflect climatic changes that resulted from orbital forcing. These high‐frequency changes may correspond to the high‐order eccentricity periods of 3.47, 2.04, and 1.31 m.y." @default.
• W1976582157 created "2016-06-24" @default.
• W1976582157 creator A5013565235 @default.
• W1976582157 creator A5033390004 @default.
• W1976582157 creator A5036074576 @default.
• W1976582157 creator A5063127534 @default.
• W1976582157 creator A5087453409 @default.
• W1976582157 date "1992-02-01" @default.
• W1976582157 modified "2023-10-14" @default.
• W1976582157 title "Variations in the Fine‐Scale Composition of a Central Pacific Ferromanganese Crust: Paleoceanographic Implications" @default.
• W1976582157 cites W1561453780 @default.
• W1976582157 cites W1963862934 @default.
• W1976582157 cites W1971407642 @default.
• W1976582157 cites W1972538937 @default.
• W1976582157 cites W1974331260 @default.
• W1976582157 cites W1980922211 @default.
• W1976582157 cites W1984101546 @default.
• W1976582157 cites W1984134126 @default.
• W1976582157 cites W1987263569 @default.
• W1976582157 cites W1987349010 @default.
• W1976582157 cites W1987605849 @default.
• W1976582157 cites W1997252211 @default.
• W1976582157 cites W1997297461 @default.
• W1976582157 cites W2001173398 @default.
• W1976582157 cites W2005683769 @default.
• W1976582157 cites W2006982726 @default.
• W1976582157 cites W2012246906 @default.
• W1976582157 cites W2013095501 @default.
• W1976582157 cites W2014392338 @default.
• W1976582157 cites W2015589786 @default.
• W1976582157 cites W2016333946 @default.
• W1976582157 cites W2020420401 @default.
• W1976582157 cites W2022545034 @default.
• W1976582157 cites W2023820712 @default.
• W1976582157 cites W2036604182 @default.
• W1976582157 cites W2039398229 @default.
• W1976582157 cites W2041139363 @default.
• W1976582157 cites W2048274163 @default.
• W1976582157 cites W2048877545 @default.
• W1976582157 cites W2051328300 @default.
• W1976582157 cites W2051590784 @default.
• W1976582157 cites W2054475421 @default.
• W1976582157 cites W2062552134 @default.
• W1976582157 cites W2066008299 @default.
• W1976582157 cites W2069510110 @default.
• W1976582157 cites W2075343565 @default.
• W1976582157 cites W2080403834 @default.
• W1976582157 cites W2081142711 @default.
• W1976582157 cites W2088582413 @default.
• W1976582157 cites W2101051734 @default.
• W1976582157 cites W2116727743 @default.
• W1976582157 cites W2477338288 @default.
• W1976582157 cites W2505323838 @default.
• W1976582157 cites W388075207 @default.
• W1976582157 doi "https://doi.org/10.1029/91pa02936" @default.
• W1976582157 hasPublicationYear "1992" @default.
• W1976582157 type Work @default.
• W1976582157 sameAs 1976582157 @default.
• W1976582157 citedByCount "90" @default.
• W1976582157 countsByYear W19765821572012 @default.
• W1976582157 countsByYear W19765821572013 @default.
• W1976582157 countsByYear W19765821572014 @default.
• W1976582157 countsByYear W19765821572015 @default.
• W1976582157 countsByYear W19765821572016 @default.
• W1976582157 countsByYear W19765821572017 @default.
• W1976582157 countsByYear W19765821572018 @default.
• W1976582157 countsByYear W19765821572019 @default.
• W1976582157 countsByYear W19765821572020 @default.
• W1976582157 countsByYear W19765821572021 @default.
• W1976582157 countsByYear W19765821572022 @default.
• W1976582157 countsByYear W19765821572023 @default.
• W1976582157 crossrefType "journal-article" @default.
• W1976582157 hasAuthorship W1976582157A5013565235 @default.
• W1976582157 hasAuthorship W1976582157A5033390004 @default.
• W1976582157 hasAuthorship W1976582157A5036074576 @default.
• W1976582157 hasAuthorship W1976582157A5063127534 @default.
• W1976582157 hasAuthorship W1976582157A5087453409 @default.
• W1976582157 hasConcept C109007969 @default.
• W1976582157 hasConcept C111368507 @default.
• W1976582157 hasConcept C121332964 @default.
• W1976582157 hasConcept C127313418 @default.
• W1976582157 hasConcept C149849071 @default.
• W1976582157 hasConcept C151730666 @default.
• W1976582157 hasConcept C154200439 @default.
• W1976582157 hasConcept C17409809 @default.
• W1976582157 hasConcept C197248824 @default.
• W1976582157 hasConcept C27492601 @default.
• W1976582157 hasConcept C2776698055 @default.
• W1976582157 hasConcept C58097730 @default.
• W1976582157 hasConcept C77928131 @default.
• W1976582157 hasConcept C97355855 @default.
• W1976582157 hasConceptScore W1976582157C109007969 @default.
• W1976582157 hasConceptScore W1976582157C111368507 @default.
• W1976582157 hasConceptScore W1976582157C121332964 @default.
• W1976582157 hasConceptScore W1976582157C127313418 @default.
• W1976582157 hasConceptScore W1976582157C149849071 @default.
• W1976582157 hasConceptScore W1976582157C151730666 @default.
• W1976582157 hasConceptScore W1976582157C154200439 @default.

• next