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  • Fuxianospira gyrata Chen and Zhou, 1997


    Images:

    oilshale

    Taxonomy

    ?Macroalgae

    Kingdom: Plantae
    Phylum: Chlorophyta
    Class: incertae sedis
    Order: incertae sedis
    Family: incertae sedis
    Genus: Fuxianospira
    Species: Fuxianospira gyrata
    Author Citation Chen and Zhou, 1997

    Geological Time Scale

    Eon: Phanerozoic
    Era: Paleozoic
    Period: Cambrian
    Sub Period: None
    Epoch: Series 2 Epoch
    International Age: Stage 3

    Stratigraphy

    Heilinpu Formation

    Provenance

    Acquired by: Purchase/Trade

    Dimensions

    Length: 2.5 cm
    Width: 2 cm

    Location

    Jiucun Township
    Chengjiang City
    Yunnan Province
    China

    Comments

    Although originally described as an alga, F. gyrata is now regarded by some authors as a coprolite (e.g., Steiner et al. 2005).
    Taxonomy from GBIF.org.
    Description and remarks by Chen and Zhou 1997., p. 88 : "Thread cylindrical, unbranchial, with a uniform, flattened width of 1.2mm and a preserved length of at least 20cm. Surface bears a tightly and helically coiled structure.
    Remarks: This is the most abundant alga in the Chengjiang biota. Most of the thread are preserved within a microturbidite mud layer and show irregular twisting, indicating that the thread was extremely flexible. Specimens probably sank to the bottom from the overlying water column, in a very low-energy environment, before the incursion of minor mud flow.”

    Restoration by Chen and Zhou 1997., p. 89:

    2015679053_FuxianospiragyrataRestorationchenzhou89.thumb.jpg.650cc637a6dec41c4a01f5df4e51fd8d.jpg

    References:

    Chen, J.Y., and Zhou, G., (1997) Biology of the Chengjiang fauna. Bulletin of the National Museum of Natural Science, v. 10, p. 11–105.
    Hou, X., Aldridge, R., Bergstrom, J., Siveter, D.J., Siveter, D., and Feng, X., (2004) The Cambrian Fossils of Chengjiang, China: The Flowering of Early Animal Life. Malden, Wiley Blackwell, 233 p.
    Maletz, J., Steiner, M., and Fatka, O., (2005) Middle Cambrian pterobranchs and the question: What is a graptolite? Lethaia, v. 38, p. 73–85.
    Fu, X., Wu, M., Zhao, Y., Zhu, W., and Yang, Y., (2012) Discovery of macroalgae from the Cambrian Tsinghsutung Formation of Guizhou. Acta Palaeontologica Sinica, v. 51, p. 56–63.
    Wang, P.L., LoDuca, S. T., Wu, M. Y. et al., (2021) Benthic primary producers in exceptionally preserved Cambrian biotas of North China, Palaeoworld , https://doi.org/10.1016/j.palwor.2021.01.009 




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