FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1966101227> ?p ?o ?g. }

• W1966101227 endingPage "27" @default.
• W1966101227 startingPage "1" @default.
• W1966101227 abstract "Abstract The hemilpelagic sedimentary sequence in the Gulf of Aden has yielded a continuous succession of relatively well preserved late Neogene nannofossils. Detailed quantitative study of the nannofossils recognized forty-two datum planes which are potentially useful in the late Neogene biostratigraphy. A high rate of sedimentation (52.2 mm/k.y.) allowed us to recognize even relatively closely spaced datum planes and locate them within the sequence. Absolute ages of the nannofossil datum planes younger than 4 Ma have been estimated by interpolation between tephra layers, for which ages were determined by correlation with paleomagnetically and radiometrically dated tephra layers exposed in East African terrestrial sequences. Ages of the older late Neogene datum planes are estimated by interpolation between the FOD of D. hamatus and the Moitu Tuff, and by extrapolation below the FOD of D. hamatus . Previously defined and newly introduced datum planes define twenty nannofossil zones, six each in the Quaternary, Pliocene and late Miocene, and two in the middle Miocene, with durations of 0.13 to 0.78, 0.37 to 0.81 and 0.14 to 2.49 m.y. in the Quaternary, Pliocene and late Miocene time period respectively. Nine new zones and five new subzones are proposed in this paper, three zones in the Pleistocene, two zones in the Pliocene, two zones and five subzones in the late Miocene, and two zones in the upper part of the middle Miocene. Six new datum planes are introduced, FOD of P. lacunosa in the Pliocene, FOD and LOD of D. neohamatus , LOD's of D. loeblichii and D. calcaris in the late Miocene and LOD of D. extensus in the latest middle Miocene." @default.
• W1966101227 created "2016-06-24" @default.
• W1966101227 creator A5069143660 @default.
• W1966101227 creator A5080343334 @default.
• W1966101227 date "1989-11-01" @default.
• W1966101227 modified "2023-09-26" @default.
• W1966101227 title "Late Neogene calcareous nannofossil biostratigraphy of the Gulf of Aden region" @default.
• W1966101227 cites W1505582348 @default.
• W1966101227 cites W1523529762 @default.
• W1966101227 cites W1552867039 @default.
• W1966101227 cites W1555033995 @default.
• W1966101227 cites W1966998609 @default.
• W1966101227 cites W1973802327 @default.
• W1966101227 cites W1981505987 @default.
• W1966101227 cites W2014845713 @default.
• W1966101227 cites W2025707219 @default.
• W1966101227 cites W2046713607 @default.
• W1966101227 cites W2047682684 @default.
• W1966101227 cites W2053251789 @default.
• W1966101227 cites W2058905326 @default.
• W1966101227 cites W2065681782 @default.
• W1966101227 cites W2070933681 @default.
• W1966101227 cites W2078464421 @default.
• W1966101227 cites W2082854515 @default.
• W1966101227 cites W2085790365 @default.
• W1966101227 cites W2087950925 @default.
• W1966101227 cites W2101606957 @default.
• W1966101227 cites W2101897237 @default.
• W1966101227 cites W2104951237 @default.
• W1966101227 cites W2109522189 @default.
• W1966101227 cites W2126456782 @default.
• W1966101227 cites W2128478720 @default.
• W1966101227 cites W2129542724 @default.
• W1966101227 cites W2154188414 @default.
• W1966101227 cites W2155876872 @default.
• W1966101227 cites W2187118611 @default.
• W1966101227 cites W2247807006 @default.
• W1966101227 cites W2292532340 @default.
• W1966101227 cites W2316226371 @default.
• W1966101227 cites W2328505916 @default.
• W1966101227 cites W2328664005 @default.
• W1966101227 cites W2336992407 @default.
• W1966101227 cites W2338311415 @default.
• W1966101227 cites W2342336168 @default.
• W1966101227 cites W2476624827 @default.
• W1966101227 cites W2478016614 @default.
• W1966101227 cites W2479042674 @default.
• W1966101227 cites W2484635891 @default.
• W1966101227 cites W2492570026 @default.
• W1966101227 cites W2495767614 @default.
• W1966101227 cites W2497253303 @default.
• W1966101227 cites W2673629650 @default.
• W1966101227 cites W2722196962 @default.
• W1966101227 cites W2725455224 @default.
• W1966101227 cites W2734766532 @default.
• W1966101227 cites W2737831621 @default.
• W1966101227 cites W2742867698 @default.
• W1966101227 cites W2763444528 @default.
• W1966101227 cites W2915910161 @default.
• W1966101227 cites W2916272161 @default.
• W1966101227 cites W2917808547 @default.
• W1966101227 cites W3151938427 @default.
• W1966101227 cites W3152663889 @default.
• W1966101227 cites W586381714 @default.
• W1966101227 cites W591412810 @default.
• W1966101227 cites W2274977929 @default.
• W1966101227 cites W2501251049 @default.
• W1966101227 doi "https://doi.org/10.1016/0377-8398(89)90002-9" @default.
• W1966101227 hasPublicationYear "1989" @default.
• W1966101227 type Work @default.
• W1966101227 sameAs 1966101227 @default.
• W1966101227 citedByCount "13" @default.
• W1966101227 countsByYear W19661012272020 @default.
• W1966101227 countsByYear W19661012272021 @default.
• W1966101227 crossrefType "journal-article" @default.
• W1966101227 hasAuthorship W1966101227A5069143660 @default.
• W1966101227 hasAuthorship W1966101227A5080343334 @default.
• W1966101227 hasConcept C109007969 @default.
• W1966101227 hasConcept C111368507 @default.
• W1966101227 hasConcept C123552892 @default.
• W1966101227 hasConcept C127313418 @default.
• W1966101227 hasConcept C151730666 @default.
• W1966101227 hasConcept C27492601 @default.
• W1966101227 hasConcept C61721801 @default.
• W1966101227 hasConceptScore W1966101227C109007969 @default.
• W1966101227 hasConceptScore W1966101227C111368507 @default.
• W1966101227 hasConceptScore W1966101227C123552892 @default.
• W1966101227 hasConceptScore W1966101227C127313418 @default.
• W1966101227 hasConceptScore W1966101227C151730666 @default.
• W1966101227 hasConceptScore W1966101227C27492601 @default.
• W1966101227 hasConceptScore W1966101227C61721801 @default.
• W1966101227 hasIssue "1-2" @default.
• W1966101227 hasLocation W19661012271 @default.
• W1966101227 hasOpenAccess W1966101227 @default.
• W1966101227 hasPrimaryLocation W19661012271 @default.
• W1966101227 hasRelatedWork W1982105962 @default.
• W1966101227 hasRelatedWork W1985213725 @default.
• W1966101227 hasRelatedWork W2187483395 @default.

• next