Rhombocorniculum

Rhombocorniculum
Temporal range:
Scientific classification Edit this classification
Kingdom: Animalia
Clade: Panarthropoda
Phylum: †Lobopodia
Family: †Hallucigeniidae
Genus: †Rhombocorniculum
Walliser, 1958[2]

Rhombocorniculum is a species of small shelly fossil comprising twisted ornamented cones. It has been described from the Comley Limestone and elsewhere. R. cancellatum straddles the Atdabanian/Botomian boundary.[1] The structure of its inner layer suggests that its phosphatic fibres formed within a flexible organic matrix.[3]

Description

Three species are recognized — in stratigraphic succession: R. insolutum, R. cancellatum (=R. walliseri), and R. spinosus (=Rushtonites spinosus).[4] Landing (1995) refers R. insolutum to the strictocorniculids, along with Rushtonites.[3] Hinz (1987) considers insolutum to fall within the variability seen in cancellatum.

Classification

Based on details of the ornament and construction, Rhombocorniculum is interpreted as the spines of a Hallucigenia-like lobopodian worm.[5]

The slightly simplified cladogram below is from a paper by Knecht et al. redescribing the lobopodian Palaeocampa anthrax.[6]

†Diania

†Lenisambulatrix

†Paucipodia

†Thanahita

†Eoconchariidae

†Microdictyon

†Fusuchoncharium

†Quadratapora

†Strictocorniculum

†Rhombocorniculum

†Orstenotubulus

†Carbotubulus

†Hallucigenia fortis

†Hallucigenia sparsa

†"Hallucigenia" hongmeia

†Cardiodictyon

Tardigrada (tardigrades)

†Luolishania

†Collinsovermidae

†EBS Collinsovermid (SAM P14848)

See also

References

  1. 1 2 Brasier, M. D. (1986). "The succession of small shelly fossils (especially conoidal microfossils) from English Precambrian–Cambrian boundary beds". Geological Magazine. 123 (3): 237–256. Bibcode:1986GeoM..123..237B. doi:10.1017/S0016756800034737.
  2. ↑ Otto H. Walliser (1958). "Rhombocorniculum comleyense n. gen., n. sp". Paläontologische Zeitschrift. 32 (3–4): 176–180. Bibcode:1958PalZ...32..176W. doi:10.1007/BF02989029.
  3. 1 2 Landing, E. (May 1995). "Upper Placentian-Branchian Series of Mainland Nova Scotia (Middle-Upper Lower Cambrian): Faunas, Paleoenvironments, and Stratigraphic Revision". Journal of Paleontology. 69 (3): 475–495. Bibcode:1995JPal...69..475L. doi:10.1017/S0022336000034879. JSTOR 1306322.
  4. ↑ Brasier, M. D. (1989). Towards a biostratigraphy of the earliest skeletal biotas. In J. W. Cowie & M. D. Brasier (Eds.), The Precambrian-Cambrian boundary (pp. 117–165). Oxford: Clarendon Press.
  5. ↑ Caron, J. -B.; Smith, M. R.; Harvey, T. H. P. (2013). "Beyond the Burgess Shale: Cambrian microfossils track the rise and fall of hallucigeniid lobopodians". Proceedings of the Royal Society B: Biological Sciences. 280 (1767) 20131613. doi:10.1098/rspb.2013.1613. PMC 3735267. PMID 23902914.
  6. ↑ Knecht, Richard J.; McCall, Christian R. A.; Tsai, Cheng-Chia; Rabideau Childers, Richard A.; Yu, Nanfang (23 July 2025). "Palaeocampa anthrax, an armored freshwater lobopodian with chemical defenses from the Carboniferous". Communications Biology. 8 (1) 1080. doi:10.1038/s42003-025-08483-0. PMC 12287526. PMID 40702124.