FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000533128> ?p ?o ?g. }

• W2000533128 endingPage "466" @default.
• W2000533128 startingPage "455" @default.
• W2000533128 abstract "Abstract Danian (Paleocene) reefs formed by ahermatypic scleractinian corals in relatively deep water are known in a few localities in southern Scandinavia. Reflection and shallow seismic profiles, and samples from drilling and scuba diving in bridge pier excavations in Oresund, the strait between Denmark and Sweden, for the first time allow interpretation of the factors that controlled the localisation of the reefs. After the mass-extinction at the K/T boundary, reef-building scleractinian corals were absent in the Boreal early Danian in the Danish basin. Faunal evolution after the biotic crisis and a rise in relative sea level are interpreted to have favoured formation of deep-water coral reefs in the Oresund region in mid-Danian time. The reefs were 6–20 m high and 20–200 m long on the seafloor and have a patchy distribution within a bryozoan mound-dominated setting in an area of about 10 km 2 . They are composed of the framework-building ahermatypic scleractinian coral Dendrophyllia candelabrum with minor occurrences of bryozoans, echinoderms, gastropods and bivalves. It has been suspected that the reefs were located over contemporaneous seafloor highs but this notion was only based on comparison with similar modern deep-water reefs offshore Norway. The data from Oresund indicate that the Danian reef complex was formed over a late Maastrichtian palaeo-seafloor high, the Saltholm-Malmo High, supporting this interpretation and thus adding fundamentally to the understanding of the factors controlling the formation and localisation of these deep and cool-water coral reefs. Individual reefs were initiated and grew on eroded crests and steep south-dipping flanks of bryozoan mounds and were predominantly situated on the southern part of the high and are interpreted as growing towards NW-flowing bottom currents rich in particulate nutrients." @default.
• W2000533128 created "2016-06-24" @default.
• W2000533128 creator A5018315054 @default.
• W2000533128 creator A5030571673 @default.
• W2000533128 creator A5031199375 @default.
• W2000533128 creator A5076681556 @default.
• W2000533128 creator A5089509070 @default.
• W2000533128 date "2010-02-01" @default.
• W2000533128 modified "2023-09-26" @default.
• W2000533128 title "Danian cool-water coral reefs in southern Scandinavia localised over seafloor highs" @default.
• W2000533128 cites W1999883999 @default.
• W2000533128 cites W2036401343 @default.
• W2000533128 cites W2038826154 @default.
• W2000533128 cites W2045492996 @default.
• W2000533128 cites W2067137281 @default.
• W2000533128 cites W2076875320 @default.
• W2000533128 cites W2082773656 @default.
• W2000533128 cites W2085464640 @default.
• W2000533128 cites W2093113660 @default.
• W2000533128 cites W2094077212 @default.
• W2000533128 cites W2098423553 @default.
• W2000533128 cites W2100734663 @default.
• W2000533128 cites W2110312429 @default.
• W2000533128 cites W2130901770 @default.
• W2000533128 cites W2136031301 @default.
• W2000533128 cites W2137258492 @default.
• W2000533128 cites W2138464736 @default.
• W2000533128 cites W2323750115 @default.
• W2000533128 cites W3022909864 @default.
• W2000533128 cites W3124267817 @default.
• W2000533128 cites W3153317005 @default.
• W2000533128 cites W3169696856 @default.
• W2000533128 cites W3171602761 @default.
• W2000533128 cites W4248419086 @default.
• W2000533128 doi "https://doi.org/10.1016/j.marpetgeo.2009.09.008" @default.
• W2000533128 hasPublicationYear "2010" @default.
• W2000533128 type Work @default.
• W2000533128 sameAs 2000533128 @default.
• W2000533128 citedByCount "11" @default.
• W2000533128 countsByYear W20005331282012 @default.
• W2000533128 countsByYear W20005331282014 @default.
• W2000533128 countsByYear W20005331282017 @default.
• W2000533128 countsByYear W20005331282019 @default.
• W2000533128 countsByYear W20005331282020 @default.
• W2000533128 countsByYear W20005331282021 @default.
• W2000533128 countsByYear W20005331282022 @default.
• W2000533128 crossrefType "journal-article" @default.
• W2000533128 hasAuthorship W2000533128A5018315054 @default.
• W2000533128 hasAuthorship W2000533128A5030571673 @default.
• W2000533128 hasAuthorship W2000533128A5031199375 @default.
• W2000533128 hasAuthorship W2000533128A5076681556 @default.
• W2000533128 hasAuthorship W2000533128A5089509070 @default.
• W2000533128 hasConcept C111368507 @default.
• W2000533128 hasConcept C117485682 @default.
• W2000533128 hasConcept C127313418 @default.
• W2000533128 hasConcept C143020374 @default.
• W2000533128 hasConcept C151730666 @default.
• W2000533128 hasConcept C77044568 @default.
• W2000533128 hasConcept C79367842 @default.
• W2000533128 hasConceptScore W2000533128C111368507 @default.
• W2000533128 hasConceptScore W2000533128C117485682 @default.
• W2000533128 hasConceptScore W2000533128C127313418 @default.
• W2000533128 hasConceptScore W2000533128C143020374 @default.
• W2000533128 hasConceptScore W2000533128C151730666 @default.
• W2000533128 hasConceptScore W2000533128C77044568 @default.
• W2000533128 hasConceptScore W2000533128C79367842 @default.
• W2000533128 hasIssue "2" @default.
• W2000533128 hasLocation W20005331281 @default.
• W2000533128 hasOpenAccess W2000533128 @default.
• W2000533128 hasPrimaryLocation W20005331281 @default.
• W2000533128 hasRelatedWork W1607533721 @default.
• W2000533128 hasRelatedWork W1975854548 @default.
• W2000533128 hasRelatedWork W2004491920 @default.
• W2000533128 hasRelatedWork W2013326444 @default.
• W2000533128 hasRelatedWork W2091881906 @default.
• W2000533128 hasRelatedWork W2144990865 @default.
• W2000533128 hasRelatedWork W2495550683 @default.
• W2000533128 hasRelatedWork W2950132429 @default.
• W2000533128 hasRelatedWork W2981465667 @default.
• W2000533128 hasRelatedWork W3094060008 @default.
• W2000533128 hasVolume "27" @default.
• W2000533128 isParatext "false" @default.
• W2000533128 isRetracted "false" @default.
• W2000533128 magId "2000533128" @default.
• W2000533128 workType "article" @default.