FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1902182613> ?p ?o ?g. }

• W1902182613 endingPage "44" @default.
• W1902182613 startingPage "30" @default.
• W1902182613 abstract "The basal Cambrian marks the beginning of an important chapter in the history of life. However, most paleontological work on the basal Cambrian has been focused on skeletal animal fossils, and our knowledge about the primary producers—cyanobacteria and eukaryotic phytoplankton (e.g., acritarchs)—is limited. In this research, we have investigated basal Cambrian acritarchs, coccoidal microfossils, and cyanobacteria preserved in phosphorites and cherts of the Yanjiahe Formation in the Yangtze Gorges area (South China) and the Yurtus Formation in the Aksu area (Tarim Block, northwestern China). Our study confirms the occurrence in these two formations of small acanthomorphic acritarchs characteristic of the basal Cambrian Asteridium–Comasphaeridium–Heliosphaeridium (ACH) assemblage. These acritarchs include abundant Heliosphaeridium ampliatimi (Wang, 1985) Yao et al., 2005, common Yurtusia uniformis n. gen. and n. sp., and rare Comasphaeridium annulare (Wang, 1985) Yao et al., 2005. In addition, these basal Cambrian successions also contain the clustered coccoidal microfossil Archaeophycus yunnanensis (Song in Luo et al., 1982) n. comb., several filamentous cyanobacteria [ Cyanonema majus n. sp., Oscillatoriopsis longa Timofeev and Hermann, 1979, and Siphonophycus robustum (Schopf, 1968) Knoll et al., 1991], and the tabulate tubular microfossil Megathrix longus L. Yin, 1987a, n. emend. Some of these taxa (e.g., H. ampliatum, C. annulare , and M. longus ) have a wide geographic distribution but occur exclusively in basal Cambrian successions, supporting their biostratigraphic importance. Comparison between the stratigraphic occurrences of microfossils reported here and skeletal animal fossils published by others suggests that animals and phytoplankton radiated in tandem during the Cambrian explosion." @default.
• W1902182613 created "2016-06-24" @default.
• W1902182613 creator A5011031703 @default.
• W1902182613 creator A5012510004 @default.
• W1902182613 creator A5024294177 @default.
• W1902182613 creator A5033681211 @default.
• W1902182613 creator A5039392522 @default.
• W1902182613 creator A5053004487 @default.
• W1902182613 date "2009-01-01" @default.
• W1902182613 modified "2023-10-06" @default.
• W1902182613 title "Basal Cambrian microfossils from the Yangtze Gorges area (South China) and the Aksu area (Tarim block, northwestern China)" @default.
• W1902182613 cites W1563855092 @default.
• W1902182613 cites W1634598038 @default.
• W1902182613 cites W1693703638 @default.
• W1902182613 cites W1790466839 @default.
• W1902182613 cites W1829457858 @default.
• W1902182613 cites W1876101421 @default.
• W1902182613 cites W1966913914 @default.
• W1902182613 cites W1976598471 @default.
• W1902182613 cites W1978397424 @default.
• W1902182613 cites W1980935720 @default.
• W1902182613 cites W1992446442 @default.
• W1902182613 cites W1997998520 @default.
• W1902182613 cites W2003823013 @default.
• W1902182613 cites W2004614425 @default.
• W1902182613 cites W2007915553 @default.
• W1902182613 cites W2013146948 @default.
• W1902182613 cites W2018261895 @default.
• W1902182613 cites W2057191919 @default.
• W1902182613 cites W2057260077 @default.
• W1902182613 cites W2059196424 @default.
• W1902182613 cites W2061127293 @default.
• W1902182613 cites W2061310368 @default.
• W1902182613 cites W2085802849 @default.
• W1902182613 cites W2094623284 @default.
• W1902182613 cites W2097949168 @default.
• W1902182613 cites W2130220748 @default.
• W1902182613 cites W2133159913 @default.
• W1902182613 cites W2135959037 @default.
• W1902182613 cites W2143593009 @default.
• W1902182613 cites W2156936098 @default.
• W1902182613 cites W2283161563 @default.
• W1902182613 cites W2505144080 @default.
• W1902182613 cites W2739043173 @default.
• W1902182613 cites W4211128516 @default.
• W1902182613 doi "https://doi.org/10.1666/07-147r.1" @default.
• W1902182613 hasPublicationYear "2009" @default.
• W1902182613 type Work @default.
• W1902182613 sameAs 1902182613 @default.
• W1902182613 citedByCount "63" @default.
• W1902182613 countsByYear W19021826132012 @default.
• W1902182613 countsByYear W19021826132013 @default.
• W1902182613 countsByYear W19021826132014 @default.
• W1902182613 countsByYear W19021826132015 @default.
• W1902182613 countsByYear W19021826132016 @default.
• W1902182613 countsByYear W19021826132017 @default.
• W1902182613 countsByYear W19021826132018 @default.
• W1902182613 countsByYear W19021826132019 @default.
• W1902182613 countsByYear W19021826132020 @default.
• W1902182613 countsByYear W19021826132021 @default.
• W1902182613 countsByYear W19021826132022 @default.
• W1902182613 countsByYear W19021826132023 @default.
• W1902182613 crossrefType "journal-article" @default.
• W1902182613 hasAuthorship W1902182613A5011031703 @default.
• W1902182613 hasAuthorship W1902182613A5012510004 @default.
• W1902182613 hasAuthorship W1902182613A5024294177 @default.
• W1902182613 hasAuthorship W1902182613A5033681211 @default.
• W1902182613 hasAuthorship W1902182613A5039392522 @default.
• W1902182613 hasAuthorship W1902182613A5053004487 @default.
• W1902182613 hasConcept C127313418 @default.
• W1902182613 hasConcept C134018914 @default.
• W1902182613 hasConcept C151730666 @default.
• W1902182613 hasConcept C2778024521 @default.
• W1902182613 hasConcept C2779306644 @default.
• W1902182613 hasConcept C71640776 @default.
• W1902182613 hasConcept C86803240 @default.
• W1902182613 hasConcept C97316735 @default.
• W1902182613 hasConceptScore W1902182613C127313418 @default.
• W1902182613 hasConceptScore W1902182613C134018914 @default.
• W1902182613 hasConceptScore W1902182613C151730666 @default.
• W1902182613 hasConceptScore W1902182613C2778024521 @default.
• W1902182613 hasConceptScore W1902182613C2779306644 @default.
• W1902182613 hasConceptScore W1902182613C71640776 @default.
• W1902182613 hasConceptScore W1902182613C86803240 @default.
• W1902182613 hasConceptScore W1902182613C97316735 @default.
• W1902182613 hasIssue "1" @default.
• W1902182613 hasLocation W19021826131 @default.
• W1902182613 hasOpenAccess W1902182613 @default.
• W1902182613 hasPrimaryLocation W19021826131 @default.
• W1902182613 hasRelatedWork W2020209097 @default.
• W1902182613 hasRelatedWork W2124583589 @default.
• W1902182613 hasRelatedWork W2128154243 @default.
• W1902182613 hasRelatedWork W2138434568 @default.
• W1902182613 hasRelatedWork W2272958795 @default.
• W1902182613 hasRelatedWork W2350949053 @default.
• W1902182613 hasRelatedWork W2358055632 @default.
• W1902182613 hasRelatedWork W2625142760 @default.
• W1902182613 hasRelatedWork W2769074976 @default.

• next