Matches in SemOpenAlex for { <https://semopenalex.org/work/W2149658127> ?p ?o ?g. }
- W2149658127 endingPage "181" @default.
- W2149658127 startingPage "157" @default.
- W2149658127 abstract "Biostratigraphic subdivision and correlation of early Neoproterozoic strata is hampered by the limited number of widely distributed and age diagnostic fossils. The acanthomorphic acritarch Trachyhystrichosphaera aimika, among a few other microfossil taxa, has emerged as a potential early Neoproterozoic index fossil, but its temporal and spatial ranges have not been thoroughly documented. To improve our knowledge about early Neoproterozoic biodiversity, we carried out a micropaleontological investigation of the early Neoproterozoic Liulaobei Formation in northern Anhui of North China. Our investigation using a low-manipulation maceration technique revealed a diverse assemblage of organic-walled microfossils dominated by sphaeromorphs and filaments, with relatively few acanthomorph taxa. A total of 23 taxa were recovered, including three new species (Eotylotopalla? grandis n. sp., Siphonophycus gigas n. sp., and Trachyhystrichosphaera botula n. sp.). Also present in the Liulaobei Formation are Trachyhystrichosphaera aimika (a species widely present in pre-Cryogenian Neoproterozoic and latest Mesoproterozoic rocks) and Pololeptus rugosus (a species characterized by an ellipsoidal vesicle with transverse annulations). The new data add to the growing diversity of early Neoproterozoic fossils and strengthen the basis for improved biostratigraphic correlation of early Neoproterozoic strata. Correlation with other geochronologically dated successions that contain Trachyhystrichosphaera confirms Trachyhystrichosphaera and T. aimika as promising index fossils to define and subdivide the pre-Cryogenian Neoproterozoic Era in terms of Global Boundary Stratotype Section and Point (GSSP), as opposed to current system using Global Standard Stratigraphic Age (GSSA). Available biostratigraphic data, including the occurrence of Trachyhystrichosphaera, Chuaria, Tawuia, and Sinosabellidites, suggest that the Liulaobei Formation is of pre-Cryogenian Neoproterozoic age, not Cryogenian–Ediacaran age as some have suggested in the past." @default.
- W2149658127 created "2016-06-24" @default.
- W2149658127 creator A5010683270 @default.
- W2149658127 creator A5022489948 @default.
- W2149658127 creator A5024294177 @default.
- W2149658127 creator A5044402588 @default.
- W2149658127 creator A5063058691 @default.
- W2149658127 creator A5069381791 @default.
- W2149658127 date "2013-10-01" @default.
- W2149658127 modified "2023-10-14" @default.
- W2149658127 title "Organic-walled microfossils from the early Neoproterozoic Liulaobei Formation in the Huainan region of North China and their biostratigraphic significance" @default.
- W2149658127 cites W1689399105 @default.
- W2149658127 cites W1790466839 @default.
- W2149658127 cites W1969783988 @default.
- W2149658127 cites W1973678768 @default.
- W2149658127 cites W1975312370 @default.
- W2149658127 cites W1978011371 @default.
- W2149658127 cites W1978397424 @default.
- W2149658127 cites W1979139211 @default.
- W2149658127 cites W1979883233 @default.
- W2149658127 cites W1986229949 @default.
- W2149658127 cites W1987123223 @default.
- W2149658127 cites W1991310645 @default.
- W2149658127 cites W1998604730 @default.
- W2149658127 cites W2004106740 @default.
- W2149658127 cites W2015448722 @default.
- W2149658127 cites W2019338098 @default.
- W2149658127 cites W2028774388 @default.
- W2149658127 cites W2028940650 @default.
- W2149658127 cites W2029979255 @default.
- W2149658127 cites W2030823545 @default.
- W2149658127 cites W2035008551 @default.
- W2149658127 cites W2037745504 @default.
- W2149658127 cites W2046615969 @default.
- W2149658127 cites W2048240400 @default.
- W2149658127 cites W2053714867 @default.
- W2149658127 cites W2054913174 @default.
- W2149658127 cites W2068437819 @default.
- W2149658127 cites W2069146350 @default.
- W2149658127 cites W2078286339 @default.
- W2149658127 cites W2082689873 @default.
- W2149658127 cites W2089412265 @default.
- W2149658127 cites W2093852568 @default.
- W2149658127 cites W2094623284 @default.
- W2149658127 cites W2099233919 @default.
- W2149658127 cites W2099239324 @default.
- W2149658127 cites W2101394829 @default.
- W2149658127 cites W2102912852 @default.
- W2149658127 cites W2104547506 @default.
- W2149658127 cites W2121104116 @default.
- W2149658127 cites W2124583589 @default.
- W2149658127 cites W2133159913 @default.
- W2149658127 cites W2140350127 @default.
- W2149658127 cites W2150273101 @default.
- W2149658127 cites W2162207442 @default.
- W2149658127 cites W2163043219 @default.
- W2149658127 cites W2164367600 @default.
- W2149658127 cites W2167401654 @default.
- W2149658127 cites W2167911148 @default.
- W2149658127 cites W2170347820 @default.
- W2149658127 cites W2176267207 @default.
- W2149658127 cites W2180486948 @default.
- W2149658127 cites W2317649737 @default.
- W2149658127 cites W2321955940 @default.
- W2149658127 cites W2333070588 @default.
- W2149658127 cites W2333451854 @default.
- W2149658127 cites W2414800980 @default.
- W2149658127 doi "https://doi.org/10.1016/j.precamres.2013.07.019" @default.
- W2149658127 hasPublicationYear "2013" @default.
- W2149658127 type Work @default.
- W2149658127 sameAs 2149658127 @default.
- W2149658127 citedByCount "77" @default.
- W2149658127 countsByYear W21496581272013 @default.
- W2149658127 countsByYear W21496581272014 @default.
- W2149658127 countsByYear W21496581272015 @default.
- W2149658127 countsByYear W21496581272016 @default.
- W2149658127 countsByYear W21496581272017 @default.
- W2149658127 countsByYear W21496581272018 @default.
- W2149658127 countsByYear W21496581272019 @default.
- W2149658127 countsByYear W21496581272020 @default.
- W2149658127 countsByYear W21496581272021 @default.
- W2149658127 countsByYear W21496581272022 @default.
- W2149658127 countsByYear W21496581272023 @default.
- W2149658127 crossrefType "journal-article" @default.
- W2149658127 hasAuthorship W2149658127A5010683270 @default.
- W2149658127 hasAuthorship W2149658127A5022489948 @default.
- W2149658127 hasAuthorship W2149658127A5024294177 @default.
- W2149658127 hasAuthorship W2149658127A5044402588 @default.
- W2149658127 hasAuthorship W2149658127A5063058691 @default.
- W2149658127 hasAuthorship W2149658127A5069381791 @default.
- W2149658127 hasConcept C127313418 @default.
- W2149658127 hasConcept C146357865 @default.
- W2149658127 hasConcept C151730666 @default.
- W2149658127 hasConcept C170434497 @default.
- W2149658127 hasConcept C192797867 @default.
- W2149658127 hasConcept C61721801 @default.
- W2149658127 hasConcept C62476579 @default.
- W2149658127 hasConcept C6494504 @default.