Zobrazeno 1 - 10
of 33
pro vyhledávání: '"Hurdiidae"'
Publikováno v:
PeerJ, Vol 9, p e11800 (2021)
The Furongian period represents an important gap in the fossil record of most groups of non-biomineralizing organisms, owing to a scarcity of Konservat-Lagerstätten of that age. The most significant of these deposits, the Jiangshanian strata of the
Externí odkaz:
https://doaj.org/article/86bca899e05c47b3878b0691c5f208a1
Publikováno v:
Zoological Letters, Vol 5, Iss 1, Pp 1-11 (2019)
Abstract Background Radiodonta, large Palaeozoic nektonic predators, occupy a pivotal evolutionary position as stem-euarthropods and filled important ecological niches in early animal ecosystems. Analyses of the anatomy and phylogenetic affinity of t
Externí odkaz:
https://doaj.org/article/f8e056bc6ce8410996e7da51a0e3b076
Publikováno v:
Royal Society Open Science, Vol 7, Iss 6 (2020)
Originally considered as large, solely Cambrian apex predators, Radiodonta—a clade of stem-group euarthropods including Anomalocaris—now comprises a diverse group of predators, sediment sifters and filter feeders. These animals are only known fro
Externí odkaz:
https://doaj.org/article/1d2d4601f8c84f05b7fbcb08994230a6
Publikováno v:
Acta Palaeontologica Polonica, Vol 62, Iss 3, Pp 619-625 (2017)
Aysheaia prolata, was described as the only lobopodian from the Drumian (Cambrian) Wheeler Formation in Utah, USA, and the sole representative of this genus besides the type species Aysheaia pedunculata, from the Cambrian (Stage 5) Stephen Formation,
Externí odkaz:
https://doaj.org/article/ec9740463d5c4bf2a1434694d9538e3d
Akademický článek
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Autor:
Caron, J. - B., Moysiuk, J.
3.2. Morphological reinterpretation of Pahvantia hastata Lerosey-Aubril and Pates [22] recently described a fossil assemblage of Pahvantia (KUMIP 314089) showing a well-preserved tripartite carapace complex, identifying it as a radiodont, as well as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::86109340e1e21ed18b23fce8d38e2f8a
Autor:
Caron, J. - B., Moysiuk, J.
Titanokorys gainesi gen. et sp. nov. LSID urn:lsid:zoobank.org:act: F07D43CF-9422-4148-B8E9-AF26E0BC895D LSID urn:lsid:zoobank.org:act: 0EE750AC-FB83-4748-ADD9-013EB53459F1 3.1.1. Etymology Genus name from Titans, a group of powerful Greek deities of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::155b1b598849f77844f7b3bb565ee9fc
Publikováno v:
PeerJ, Vol 9, p e11800 (2021)
PeerJ
PeerJ
The Furongian period represents an important gap in the fossil record of most groups of non-biomineralizing organisms, owing to a scarcity of Konservat-Lagerstätten of that age. The most significant of these deposits, the Jiangshanian strata of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::45e5807f22461197fef393187b869588
https://peerj.com/articles/11800.pdf
https://peerj.com/articles/11800.pdf
Autor:
Allison C. Daley, Enrico Bonino, Stephen Pates, Rudy Lerosey-Aubril, Carlo Kier, Javier Ortega-Hernández
Publikováno v:
PeerJ
PeerJ, vol. 9, pp. e10509
PeerJ, vol. 9, pp. e10509
Radiodonts have long been known from Cambrian deposits preserving non-biomineralizing organisms. In Utah, the presence of these panarthropods in the Spence and Wheeler (House Range and Drum Mountains) biotas is now well-documented. Conversely, radiod
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b25a7f8bc9f229040879c95d89c303b0
https://pubmed.ncbi.nlm.nih.gov/33552709
https://pubmed.ncbi.nlm.nih.gov/33552709
Autor:
Jean-Bernard Caron, J. Moysiuk
Publikováno v:
Royal Society Open Science, Vol 8, Iss 9 (2021)
Royal Society Open Science
Royal Society Open Science
Radiodonts, stem-group euarthropods that evolved during the Cambrian explosion, were among the largest and most diversified lower palaeozoic predators. These animals were widespread geographically, occupying a variety of ecological niches, from benth
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8763f420389e7f1d95f994d0cd51f5db
https://doi.org/10.1098/rsos.210664
https://doi.org/10.1098/rsos.210664