FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023215134> ?p ?o ?g. }

• W2023215134 endingPage "57" @default.
• W2023215134 startingPage "41" @default.
• W2023215134 abstract "The Cape Roberts Project recovered over 1500 m of coastal glaciomarine sediments of Oligocene and Early Miocene age off the Ross Sea margin of Antarctica. The strata are characterised by cyclic repetition of facies in a glaciomarine setting, and are interpreted to be a record of glacial-interglacial episodes involving significant changes in eustatic sea level on Milankovitch frequencies. We have undertaken a detailed study of pollen and spores (miospores) from an Early Oligocene (31 Ma), and a Late Oligocene (24 Ma) cycle. Although miospores are sparse in the core, averaging only ∼1 grain per gram of sediment processed, over 1200 Cenozoic miospores were recovered for this study. Previous studies of miospores from Ross Sea sediments have encountered problems differentiating between reworked and in situ palynomorphs. Here, only samples containing a low relative abundance of an Eocene dinoflagellate cyst assemblage (the Transantarctic Flora) have been used to infer the contemporaneous Oligocene miospore flora. The flora of the Early Oligocene cycle is dominated by three species of Nothofagidites, and four types of Podocarpidites. The assemblage from the Upper Oligocene cycle is also dominated by Nothofagidites and Podocarpidites, but with the addition of two distinctive taxa, an angiosperm pollen and a bryophyte spore. Notwithstanding these additions, there is a slight decrease in floral diversity between the two cycles. While this study confirms that some floristic changes did occur between Early and Late Oligocene time on the Victoria Land coast, the present data suggest that the changes were not extensive. It is likely that the vegetation of both cycles was a low diversity scrub of low stature, consisting of mainly Nothofagus, podocarps, and bryophytes. Modern analogues suggest that this vegetation was growing in a climate significantly warmer (Mean Summer Monthly Temperature 4–12 °C) than is found on the present day Victoria Land (MSMT − 5 °C), although colder that the temperate climate suggested by the diverse flora found in Ross Sea sediments of Eocene age." @default.
• W2023215134 created "2016-06-24" @default.
• W2023215134 creator A5007431607 @default.
• W2023215134 creator A5026275067 @default.
• W2023215134 creator A5038293279 @default.
• W2023215134 creator A5059344618 @default.
• W2023215134 date "2006-02-01" @default.
• W2023215134 modified "2023-10-05" @default.
• W2023215134 title "Vegetation and climate from two Oligocene glacioeustatic sedimentary cycles (31 and 24 Ma) cored by the Cape Roberts Project, Victoria Land Basin, Antarctica" @default.
• W2023215134 cites W1616890799 @default.
• W2023215134 cites W1823431629 @default.
• W2023215134 cites W1973131361 @default.
• W2023215134 cites W1974041571 @default.
• W2023215134 cites W2003571981 @default.
• W2023215134 cites W2005969926 @default.
• W2023215134 cites W2012839069 @default.
• W2023215134 cites W2034514816 @default.
• W2023215134 cites W2054410655 @default.
• W2023215134 cites W2058359525 @default.
• W2023215134 cites W2077539297 @default.
• W2023215134 cites W2094174688 @default.
• W2023215134 cites W2115575384 @default.
• W2023215134 cites W2135452522 @default.
• W2023215134 cites W2154996984 @default.
• W2023215134 cites W2158492007 @default.
• W2023215134 cites W2165473271 @default.
• W2023215134 cites W4238739564 @default.
• W2023215134 cites W564014934 @default.
• W2023215134 doi "https://doi.org/10.1016/j.palaeo.2005.07.025" @default.
• W2023215134 hasPublicationYear "2006" @default.
• W2023215134 type Work @default.
• W2023215134 sameAs 2023215134 @default.
• W2023215134 citedByCount "60" @default.
• W2023215134 countsByYear W20232151342012 @default.
• W2023215134 countsByYear W20232151342013 @default.
• W2023215134 countsByYear W20232151342015 @default.
• W2023215134 countsByYear W20232151342016 @default.
• W2023215134 countsByYear W20232151342017 @default.
• W2023215134 countsByYear W20232151342018 @default.
• W2023215134 countsByYear W20232151342019 @default.
• W2023215134 countsByYear W20232151342021 @default.
• W2023215134 countsByYear W20232151342022 @default.
• W2023215134 countsByYear W20232151342023 @default.
• W2023215134 crossrefType "journal-article" @default.
• W2023215134 hasAuthorship W2023215134A5007431607 @default.
• W2023215134 hasAuthorship W2023215134A5026275067 @default.
• W2023215134 hasAuthorship W2023215134A5038293279 @default.
• W2023215134 hasAuthorship W2023215134A5059344618 @default.
• W2023215134 hasConcept C109007969 @default.
• W2023215134 hasConcept C111368507 @default.
• W2023215134 hasConcept C127313418 @default.
• W2023215134 hasConcept C142724271 @default.
• W2023215134 hasConcept C146588470 @default.
• W2023215134 hasConcept C151730666 @default.
• W2023215134 hasConcept C15739521 @default.
• W2023215134 hasConcept C162501224 @default.
• W2023215134 hasConcept C186240526 @default.
• W2023215134 hasConcept C18903297 @default.
• W2023215134 hasConcept C2776133958 @default.
• W2023215134 hasConcept C2777234453 @default.
• W2023215134 hasConcept C2780204098 @default.
• W2023215134 hasConcept C2780618852 @default.
• W2023215134 hasConcept C523546767 @default.
• W2023215134 hasConcept C71924100 @default.
• W2023215134 hasConcept C86803240 @default.
• W2023215134 hasConceptScore W2023215134C109007969 @default.
• W2023215134 hasConceptScore W2023215134C111368507 @default.
• W2023215134 hasConceptScore W2023215134C127313418 @default.
• W2023215134 hasConceptScore W2023215134C142724271 @default.
• W2023215134 hasConceptScore W2023215134C146588470 @default.
• W2023215134 hasConceptScore W2023215134C151730666 @default.
• W2023215134 hasConceptScore W2023215134C15739521 @default.
• W2023215134 hasConceptScore W2023215134C162501224 @default.
• W2023215134 hasConceptScore W2023215134C186240526 @default.
• W2023215134 hasConceptScore W2023215134C18903297 @default.
• W2023215134 hasConceptScore W2023215134C2776133958 @default.
• W2023215134 hasConceptScore W2023215134C2777234453 @default.
• W2023215134 hasConceptScore W2023215134C2780204098 @default.
• W2023215134 hasConceptScore W2023215134C2780618852 @default.
• W2023215134 hasConceptScore W2023215134C523546767 @default.
• W2023215134 hasConceptScore W2023215134C71924100 @default.
• W2023215134 hasConceptScore W2023215134C86803240 @default.
• W2023215134 hasIssue "1-2" @default.
• W2023215134 hasLocation W20232151341 @default.
• W2023215134 hasOpenAccess W2023215134 @default.
• W2023215134 hasPrimaryLocation W20232151341 @default.
• W2023215134 hasRelatedWork W1592473541 @default.
• W2023215134 hasRelatedWork W1991346619 @default.
• W2023215134 hasRelatedWork W2061649645 @default.
• W2023215134 hasRelatedWork W2064200967 @default.
• W2023215134 hasRelatedWork W2171788477 @default.
• W2023215134 hasRelatedWork W2279183826 @default.
• W2023215134 hasRelatedWork W2321051191 @default.
• W2023215134 hasRelatedWork W2342483968 @default.
• W2023215134 hasRelatedWork W2553408429 @default.
• W2023215134 hasRelatedWork W3082740897 @default.
• W2023215134 hasVolume "231" @default.
• W2023215134 isParatext "false" @default.

• next