Silicified and phosphatized Tianzhushania, spheroidal microfossil of possible animal origin from the Neoproterozoic of South China

• Autorzy: Yin C , Bengtson S. , Yue Z.
• Języki publikacji: EN

Abstrakty

EN

Comparative study of microfossils from two kinds of sediments: chert intercalations (studied in thin section) and phosphorite/phosphatic carbonate (in thin section and maceration), from the upper Neoproterozoic Doushantuo phosphorites in the Weng’an area, Guizhou Province, South China, shows that the phosphatized Megasphaera ornata and the chert−preserved Tianzhushania tuberifera should be regarded as representing the same taxon preserved by different mineralization processes. In phosphatized specimens the outer wall is often peeled off, exposing the ornamented middle wall. Some phosphatized specimens isolated from the rock matrix and specimens seen in thin sections of phosphorites show a partly preserved outer wall with spines, which can be compared to the thin−sectioned specimens from the chert beds. The small pits usually seen on the surface of the ornamented middle wall of phosphatized specimens correspond to the attachment spots of the spines in the outer wall. The presence of a spiny outer wall is a characteristic of Tianzhushania Yin and Li, 1978. Tianzhushania ornata (Xiao and Knoll, 2000) comb. nov. is here proposed as the valid name for the species. The proposed resting−egg nature of T. ornata, mainly based on the ornament type of the middle wall, cannot be excluded. The presence of a spiny outer wall, however, suggests that it is a pelagic rather than a benthic form.

Słowa kluczowe

EN

benthic form; China; Tianzhushania; phosphorite; animal origin; Doushantuo Formation; Megasphaera; Tianzhushania tuberifera; chert; spheroidal microfossil; Metazoa; Tianzhushania ornata; Megasphaera ornata; Neoproterozoic; rock matrix

• Wydawca: -
• Czasopismo: Acta Palaeontologica Polonica
• Rocznik: 2004
• Tom: 49
• Numer: 1
• Opis fizyczny: p.1-12,fig.,ref.

Twórcy

autor

Yin C

• Chinese Academy of Geological Sciences, 100037 Beijing, China

autor

Bengtson S.

autor

Yue Z.

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