Matches in SemOpenAlex for { <https://semopenalex.org/work/W2019436618> ?p ?o ?g. }
Showing items 1 to 92 of
92
with 100 items per page.
- W2019436618 endingPage "133" @default.
- W2019436618 startingPage "113" @default.
- W2019436618 abstract "Abstract Shallow intracratonic basins developed across a large area of the central part of the Australian craton during the Neoproterozoic and continued to accumulate marine sedimentary successions until well into the early Palaeozoic—a half billion year sedimentary record. Carbonate successions ranging in age from Neoproterozoic (Cryogenian) to ostensibly Early Ordovician have been sampled at eleven sites across four of the northernmost of these basins (Amadeus, Georgina, Wiso and Daly Basins). A total of 996 samples were then analyzed for stable carbon ( δ 13 C carb ) and oxygen ( δ 18 O carb ) isotopes to develop a regional secular stable carbon isotopic curve. The curve complements earlier work and provides an important framework for global correlation at a critical time in Earth history during which the biosphere and atmosphere were evolving rapidly. At one site in the Amadeus Basin, diagenesis proved to have significantly modified the isotopic composition of the carbonates and the data were eliminated. Analysis of the remaining samples suggests that they reflect the global secular stable carbon isotope curve and tie well with established palaeontological timescales. In particular, key isotopic excursions can be identified in the earliest part of the Neoproterozoic succession, notably the negative excursion following the Sturtian glaciation. In the early Palaeozoic record a major excursion during Ordian–early Templetonian (509–506 Ma) time can be identified across the region as can the so-called SPICE excursion which has been associated globally with the Steptoean Stage of Laurentia (497.5–495 Ma). A smaller late Templetonian–Floran (506–503 Ma) positive excursion has also been recognized. The stable carbon isotope record provides a strong regional correlation in both fossiliferous and unfossiliferous Neoproterozoic and early Palaeozoic successions and allows a global correlation to be established." @default.
- W2019436618 created "2016-06-24" @default.
- W2019436618 creator A5014698038 @default.
- W2019436618 creator A5017929780 @default.
- W2019436618 creator A5020461773 @default.
- W2019436618 creator A5026043895 @default.
- W2019436618 creator A5026048414 @default.
- W2019436618 creator A5026346984 @default.
- W2019436618 creator A5058173727 @default.
- W2019436618 date "2005-12-01" @default.
- W2019436618 modified "2023-10-06" @default.
- W2019436618 title "The Neoproterozoic–Cambrian record in Australia: A stable isotope study" @default.
- W2019436618 cites W1967484492 @default.
- W2019436618 cites W1975010988 @default.
- W2019436618 cites W1978564004 @default.
- W2019436618 cites W1993646426 @default.
- W2019436618 cites W1994356803 @default.
- W2019436618 cites W2004722069 @default.
- W2019436618 cites W2007694132 @default.
- W2019436618 cites W2010710293 @default.
- W2019436618 cites W2023268715 @default.
- W2019436618 cites W2028837424 @default.
- W2019436618 cites W2029050304 @default.
- W2019436618 cites W2031089091 @default.
- W2019436618 cites W2040269188 @default.
- W2019436618 cites W2042155317 @default.
- W2019436618 cites W2047349403 @default.
- W2019436618 cites W2058684541 @default.
- W2019436618 cites W2094524717 @default.
- W2019436618 cites W2105408232 @default.
- W2019436618 cites W2107533036 @default.
- W2019436618 cites W2118459634 @default.
- W2019436618 cites W2131260438 @default.
- W2019436618 cites W2137439859 @default.
- W2019436618 cites W2143615063 @default.
- W2019436618 cites W2146761970 @default.
- W2019436618 cites W2160376258 @default.
- W2019436618 cites W2170926131 @default.
- W2019436618 cites W2741802816 @default.
- W2019436618 cites W2745327383 @default.
- W2019436618 doi "https://doi.org/10.1016/j.precamres.2005.10.002" @default.
- W2019436618 hasPublicationYear "2005" @default.
- W2019436618 type Work @default.
- W2019436618 sameAs 2019436618 @default.
- W2019436618 citedByCount "59" @default.
- W2019436618 countsByYear W20194366182012 @default.
- W2019436618 countsByYear W20194366182013 @default.
- W2019436618 countsByYear W20194366182014 @default.
- W2019436618 countsByYear W20194366182015 @default.
- W2019436618 countsByYear W20194366182016 @default.
- W2019436618 countsByYear W20194366182017 @default.
- W2019436618 countsByYear W20194366182018 @default.
- W2019436618 countsByYear W20194366182019 @default.
- W2019436618 countsByYear W20194366182020 @default.
- W2019436618 countsByYear W20194366182021 @default.
- W2019436618 countsByYear W20194366182022 @default.
- W2019436618 countsByYear W20194366182023 @default.
- W2019436618 crossrefType "journal-article" @default.
- W2019436618 hasAuthorship W2019436618A5014698038 @default.
- W2019436618 hasAuthorship W2019436618A5017929780 @default.
- W2019436618 hasAuthorship W2019436618A5020461773 @default.
- W2019436618 hasAuthorship W2019436618A5026043895 @default.
- W2019436618 hasAuthorship W2019436618A5026048414 @default.
- W2019436618 hasAuthorship W2019436618A5026346984 @default.
- W2019436618 hasAuthorship W2019436618A5058173727 @default.
- W2019436618 hasConcept C127313418 @default.
- W2019436618 hasConcept C151730666 @default.
- W2019436618 hasConcept C173776410 @default.
- W2019436618 hasConceptScore W2019436618C127313418 @default.
- W2019436618 hasConceptScore W2019436618C151730666 @default.
- W2019436618 hasConceptScore W2019436618C173776410 @default.
- W2019436618 hasIssue "1-4" @default.
- W2019436618 hasLocation W20194366181 @default.
- W2019436618 hasOpenAccess W2019436618 @default.
- W2019436618 hasPrimaryLocation W20194366181 @default.
- W2019436618 hasRelatedWork W1984706377 @default.
- W2019436618 hasRelatedWork W1991450372 @default.
- W2019436618 hasRelatedWork W2018270340 @default.
- W2019436618 hasRelatedWork W2022706693 @default.
- W2019436618 hasRelatedWork W2036031600 @default.
- W2019436618 hasRelatedWork W2111001282 @default.
- W2019436618 hasRelatedWork W2152273076 @default.
- W2019436618 hasRelatedWork W2201315897 @default.
- W2019436618 hasRelatedWork W2635376407 @default.
- W2019436618 hasRelatedWork W2746252382 @default.
- W2019436618 hasVolume "143" @default.
- W2019436618 isParatext "false" @default.
- W2019436618 isRetracted "false" @default.
- W2019436618 magId "2019436618" @default.
- W2019436618 workType "article" @default.