FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4312864605> ?p ?o ?g. }

• W4312864605 endingPage "8" @default.
• W4312864605 startingPage "1" @default.
• W4312864605 abstract "AbstractThe history of research on Ponto-Caspian Quaternary foraminifera at the end of the nineteenth century to the present is introduced. The earliest report from the Crimean region was by Pereialsvtseva (Novorossiysk.ob-va yestestvoisp 10(2):79–114 (in Russian), 1886), who noted nine species. At the very beginning of the twentieth century, Zernov (Yezhegodnik zool. muzeya AN, Sankt Petresburg 13(4):28–35 (in Russian), 1906) wrote that foraminifera are scarce in the Black Sea. In contrast, Dolgoplskaya and Pauli (Trudy Karadagskoy nauchnoy stantsii imeni T.I. Vyazemskogo 4:23–48 (in Russian), 1931) found foraminifera to be abundant and contribute a significant proportion of recent benthic assemblages. Research carried out in the Black Sea, the Kerch Strait, and the Sea of Azov, as well as near the Bosphorus outlet, was conducted by researchers from the USSR, Bulgaria, Romania, and Georgia. The first data on Caspian foraminifera were presented by Ehrenberg in 1873, who reported 23 species. The earliest observations from the Aral Sea found only two species. Intensive study of taxonomy, quantitative distribution, and ecology of live (Rose Bengal stained) foraminifera in the Caspian and Aral Seas and their comparison with recent foraminifera from other basins was carried out by Mayer (Vertikal’noye raspredeleniye foraminifer v Kaspiyskom more. In: Maev YeG (ed) Kompleksnye issledovaniya Kaspiyskogo morya 6, pp 101–107 (in Russian), 1974a, Foraminifery Kaspiyskogo i Aral’skogo morey (Foraminifera of the Caspian and Aral seas). Avtoref. Dis. kand. biol. Nauk. Moscow State University, 24 pp (in Russian), 1979b).In addition to, and often in collaboration with, a variety of other researchers working in the region, the author has carried out more than 50 years of research on the taxonomy, ecology/paleoecology, paleogeography, and biostratigraphy of Ponto-Caspian benthic foraminifera. This chapter introduces extensive exploration of the northwestern Black Sea, along the Ukrainian, Bulgarian, and Caucasian shelves, as well as the northern exit of the Bosphorus Strait, the Sea of Azov, the Caspian Sea, and the Mediterranean Sea. Fossil assemblages from numerous Pleistocene stratotypes were studied in the coastal zone of the Ponto-Caspian region. The application of benthic foraminifera to reconstruction of sea-level change and coastline migration in regard to the Great Flood Hypotheses in the Black Sea was also investigated. Most recently, the focus has been on the use of benthic foraminifera and other meiobenthic organisms (nematodes, ostracods) to contour reservoirs of methane stored under the seabed.Altogether, 173 benthic and 7 planktonic species and subspecies (i.e., lower taxa) have been recorded, with 18 previously reported species not found. Thirty lower taxa belong to agglutinated foraminifera; the rest are calcareous. A vast majority of them are described, illustrated, and supplemented by the data on biostratigraphy and paleoecology in subsequent chapters.KeywordsPonto-CaspianQuaternaryBenthic foraminiferaHistory of study" @default.
• W4312864605 created "2023-01-05" @default.
• W4312864605 creator A5060163844 @default.
• W4312864605 date "2022-01-01" @default.
• W4312864605 modified "2023-10-02" @default.
• W4312864605 title "State-of-the-Art" @default.
• W4312864605 cites W1584728166 @default.
• W4312864605 cites W1986798229 @default.
• W4312864605 cites W2032557290 @default.
• W4312864605 cites W2092258640 @default.
• W4312864605 cites W2120392029 @default.
• W4312864605 cites W2228978586 @default.
• W4312864605 cites W2506028550 @default.
• W4312864605 cites W2613475959 @default.
• W4312864605 cites W2912710710 @default.
• W4312864605 cites W3015152763 @default.
• W4312864605 cites W3084561665 @default.
• W4312864605 cites W4231678884 @default.
• W4312864605 doi "https://doi.org/10.1007/978-3-031-12374-0_1" @default.
• W4312864605 hasPublicationYear "2022" @default.
• W4312864605 type Work @default.
• W4312864605 citedByCount "0" @default.
• W4312864605 crossrefType "book-chapter" @default.
• W4312864605 hasAuthorship W4312864605A5060163844 @default.
• W4312864605 hasConcept C111368507 @default.
• W4312864605 hasConcept C127313418 @default.
• W4312864605 hasConcept C18903297 @default.
• W4312864605 hasConcept C205649164 @default.
• W4312864605 hasConcept C2780368712 @default.
• W4312864605 hasConcept C2986842804 @default.
• W4312864605 hasConcept C58642233 @default.
• W4312864605 hasConcept C83042747 @default.
• W4312864605 hasConcept C86803240 @default.
• W4312864605 hasConceptScore W4312864605C111368507 @default.
• W4312864605 hasConceptScore W4312864605C127313418 @default.
• W4312864605 hasConceptScore W4312864605C18903297 @default.
• W4312864605 hasConceptScore W4312864605C205649164 @default.
• W4312864605 hasConceptScore W4312864605C2780368712 @default.
• W4312864605 hasConceptScore W4312864605C2986842804 @default.
• W4312864605 hasConceptScore W4312864605C58642233 @default.
• W4312864605 hasConceptScore W4312864605C83042747 @default.
• W4312864605 hasConceptScore W4312864605C86803240 @default.
• W4312864605 hasLocation W43128646051 @default.
• W4312864605 hasOpenAccess W4312864605 @default.
• W4312864605 hasPrimaryLocation W43128646051 @default.
• W4312864605 hasRelatedWork W1491450025 @default.
• W4312864605 hasRelatedWork W2042183090 @default.
• W4312864605 hasRelatedWork W2141291900 @default.
• W4312864605 hasRelatedWork W2244958959 @default.
• W4312864605 hasRelatedWork W2331521214 @default.
• W4312864605 hasRelatedWork W2360341140 @default.
• W4312864605 hasRelatedWork W2553798744 @default.
• W4312864605 hasRelatedWork W2597935636 @default.
• W4312864605 hasRelatedWork W3028473695 @default.
• W4312864605 hasRelatedWork W4221135464 @default.
• W4312864605 isParatext "false" @default.
• W4312864605 isRetracted "false" @default.
• W4312864605 workType "book-chapter" @default.