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  • Elsevier  (2)
  • [Kiel] : Christian-Albrechts-Universität zu Kiel  (1)
  • Exzellenzcluster "Ozean der Zukunft", Christian-Albrechts-Universität
  • The Geological Society of America
  • 2020-2024  (3)
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Year
  • 1
    Keywords: Forschungsbericht ; Forschungsdaten ; Lehre ; Curriculum
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (42 Seiten, 1,99 MB) , Illustrationen, Diagramme
    Language: German
    Note: Paralleltitel dem englischen Berichtsblatt entnommen , Förderkennzeichen BMBF 16FDM025 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Sprache der Zusammenfassung: Deutsch, Englisch
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  • 2
    Publication Date: 2024-02-07
    Description: Highlights • Silicoflagellates include ten Cenozoic genera, starting with Corbisema. • Rotated apical structures begin with Dictyocha byronalis in early Eocene. • Neogene rotation of Dictyocha apical bridge is an independent evolution. • Multi-windowed Stephanopsis are common from early Oligocene. • Paramesocena develops from Stephanopsis and is a possible ancestor of Octactis. Cenozoic silicoflagellate evolution led to ten known genera derived from two groups classified together in Corbisema that may have survived the end-Cretaceous extinction. These underwent rapid diversification and gave rise to at least five genera before the end of the Paleocene, including Dictyocha and Naviculopsis. Important silicoflagellate evolutionary events include the emergence of corner-aligned double skeleton configuration by the early Paleocene and the sinistral rotation of the Dictyocha byronalis apical bridge in early to middle Eocene that evolved into the apically-ringed silicoflagellate genera (e.g., Distephanopsis and Stephanocha). We interpret Paramesocena and Octactis as descended from Stephanocha, although their precise evolutionary paths remain uncertain. The earliest Octactis has thicker apical ring elements than modern O. pulchra, and is here described as the new species O. kosciuszkoi. New combinations are provided for Stephanocha antarctica and Dityocha octangulata. Overall, Cenozoic silicoflagellates show a trend towards more complicated apical geometries and smaller portals. These features enable silicoflagellate double skeletons to form near-spherical skeletal structures that support the external cell boundaries during mitosis. Silicoflagellates employ various strategies to hold double skeletons together and support the cell boundaries across the portal and window openings. Variability is an important feature of the silicoflagellate skeleton and occurs in two broadly different contexts. The first occurs for all silicoflagellate species, with occasional variant skeletal designs distinct from the predominant morphology. The second variability is associated with a single taxon, where multiple unusual skeletal shapes occur in a silicoflagellate plexus over a geologically narrow time interval and limited geographic extent.
    Type: Article , PeerReviewed
    Format: text
    Format: archive
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  • 3
    Publication Date: 2024-02-07
    Description: Highlights: • Silicoflagellates more common and diverse in late Eocene, lower in Oligocene. • Record of new species Corbisema tajmahalii from Late Eocene, with interpreted double skeleton (DS). • First known Bachmannocena DS, has corner-aligned configuration. • Observation of early evolution of Stephanocha raupii, transferred to Distephanopsis. Abstract Study of the South Pacific Ocean sediments from IODP Expedition 378, Holes U1553A and U1553B, shows 19 late Eocene to late Oligocene silicoflagellate species. The late Eocene includes Corbisema tajmahalii n. sp., observed over a ∼ 8.4 m interval and proposed as a new subzone within the Corbisema apiculata Zone. The new species is characterized by the presence of basal ring that has three sides and an arrowhead-shaped outline with the two minor-axis corners more closely spaced. This study has found the first known Bachmannocena double skeleton, in corner-aligned configuration that suggests evolutionary relationship with the Corbisema triacantha group of Cenozoic silicoflagellates. Also observed is the apparent early evolution of Stephanocha raupii at ∼29.6 Ma, derived from a skeletal diversity related to Distephanopsis crux, thus the species is here transferred to Distephanopsis (abbreviated as Ds.). Silicoflagellate skeletal abundance declines after the Eocene-Oligocene boundary, with generally low abundance except for two sediment samples immediately below the Ds. raupii n. comb. first appearance.
    Type: Article , PeerReviewed
    Format: text
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