Although molecular studies estimated that cycloneuralians might have originated in the Ediacaran Period and diversified in the early Cambrian, it was not until 2014 that they were first reported from the Cambrian Fortunian Stage. To date only two species and five indeterminate forms have been described. Here, we report new three‐dimensionally phosphatized microfossils of cycloneuralians from the Fortunian Zhangjiagou Lagerstätte, South China. Two new genera and species, Qinscolex spinosus gen. et sp. nov. and Shanscolex decorus gen. et sp. nov., and Indeterminate Forms 1–7 are described and tentatively assigned to total‐group Scalidophora, greatly increasing the diversity of the Fortunian cycloneuralians. These Fortunian cycloneuralians hav...
Markuelia is a vermiform, annulated introvertan animal known as embryonic fossils from the Lower Cam...
Chitinozoans are an enigmatic group of organic-walled marine microfossils with an abundant Lower Ord...
Macro-organisms of the Ediacaran period (635-541 Ma) were large and morphologically complex, with so...
Although molecular studies estimated that cycloneuralians might have originated in the Ediacaran Per...
Although morphology-based phylogenetic analyses and molecular data suggested that the cycloneuralian...
Scalidophoran worms diversified in the Cambrian Fortunian, as indicated by recent reports from this ...
The latest discovery of microfossils from lower Cambrian (Fortunian Stage) Zhangjiagou Lagerstätte i...
The latest discovery of microfossils from lower Cambrian (Fortunian Stage) Zhangjiagou Lagerstätte i...
The latest discovery of microfossils from lower Cambrian (Fortunian Stage) Zhangjiagou Lagerstätte i...
The latest discovery of microfossils from the lower Cambrian (Fortunian Stage) Zhangjiagou Lagerstät...
Twenty years after its proposal, the monophyly of molting protostomes—Ecdysozoa—is a well-corrobora...
The Guanshan Biota (Cambrian Series 2, Stage 4) is a typical Burgess Shale-type biota, and is one of...
The Lophotrochozoa includes disparate tentacle-bearing sessile protostome animals, which apparently ...
Markuelia is a vermiform, annulated introvertan animal known as embryonic fossils from the Lower Cam...
Macro-organisms of the Ediacaran period (635-541 Ma) were large and morphologically complex, with so...
Markuelia is a vermiform, annulated introvertan animal known as embryonic fossils from the Lower Cam...
Chitinozoans are an enigmatic group of organic-walled marine microfossils with an abundant Lower Ord...
Macro-organisms of the Ediacaran period (635-541 Ma) were large and morphologically complex, with so...
Although molecular studies estimated that cycloneuralians might have originated in the Ediacaran Per...
Although morphology-based phylogenetic analyses and molecular data suggested that the cycloneuralian...
Scalidophoran worms diversified in the Cambrian Fortunian, as indicated by recent reports from this ...
The latest discovery of microfossils from lower Cambrian (Fortunian Stage) Zhangjiagou Lagerstätte i...
The latest discovery of microfossils from lower Cambrian (Fortunian Stage) Zhangjiagou Lagerstätte i...
The latest discovery of microfossils from lower Cambrian (Fortunian Stage) Zhangjiagou Lagerstätte i...
The latest discovery of microfossils from the lower Cambrian (Fortunian Stage) Zhangjiagou Lagerstät...
Twenty years after its proposal, the monophyly of molting protostomes—Ecdysozoa—is a well-corrobora...
The Guanshan Biota (Cambrian Series 2, Stage 4) is a typical Burgess Shale-type biota, and is one of...
The Lophotrochozoa includes disparate tentacle-bearing sessile protostome animals, which apparently ...
Markuelia is a vermiform, annulated introvertan animal known as embryonic fossils from the Lower Cam...
Macro-organisms of the Ediacaran period (635-541 Ma) were large and morphologically complex, with so...
Markuelia is a vermiform, annulated introvertan animal known as embryonic fossils from the Lower Cam...
Chitinozoans are an enigmatic group of organic-walled marine microfossils with an abundant Lower Ord...
Macro-organisms of the Ediacaran period (635-541 Ma) were large and morphologically complex, with so...