Foraminifera source details
Wu, X.; Wang, S. (2004). 贵州晚新元古代陡山沱磷块岩中疑似磷酸盐化原生动物化石 - Possible phosphatized Protozoan fossils from the Late Neoproterozoic Doushantuo phosphorites in Guizhou Province. 微体古生物学报 - Acta Micropalaeontologica Sinica. 21(2): 194-198.
340842
Wu, X.; Wang, S.
2004
贵州晚新元古代陡山沱磷块岩中疑似磷酸盐化原生动物化石 - Possible phosphatized Protozoan fossils from the Late Neoproterozoic Doushantuo phosphorites in Guizhou Province
微体古生物学报 - Acta Micropalaeontologica Sinica
21(2): 194-198
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On the basis of morphological characters and aperture features of these specimens, three new species are described Luxapertus wenganensis, Luxapertus sphaeroidolis and Luxapertus papillaformis for the representatives of possible early stage Protozoa on Earth. The discovery is not only enriching content of Wengan Biota but also providing evidence for possible Protozoa in it. As a general rule, Foraminifera appears in Cambrian, the discovery of a suspicious Foraminifera from Wengan Biota suggests an earlier origin.
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Luxapertus Wu & Wang, 2004 † (original description)
Luxapertus papillaformis Wu & Wang, 2004 † (original description)
Luxapertus sphaeroidolis Wu & Wang, 2004 † (original description)
Luxapertus wenganensis Wu & Wang, 2004 † (original description)
Luxapertus papillaformis Wu & Wang, 2004 † (original description)
Luxapertus sphaeroidolis Wu & Wang, 2004 † (original description)
Luxapertus wenganensis Wu & Wang, 2004 † (original description)