Carbotubulus

Carbotubulus
Temporal range: Moscovian
Scientific classification Edit this classification
Kingdom: Animalia
Clade: Panarthropoda
Phylum: †Lobopodia
Clade: †Hallucishaniids
Family: †Hallucigeniidae
Genus: †Carbotubulus
Haug et al., 2012
Species:
†C. waloszeki
Binomial name
†Carbotubulus waloszeki
Haug et al., 2012

Carbotubulus is a genus of aquatic lobopodian known from the Carboniferous Carbondale Formation of the Mazon Creek area from the state of Illinois, in the United States. A monotypic genus, it contains one species: Carbotubulus waloszeki, and is known from a single fossil. Overall, the animal had a very tubular body. Its head, trunk, and 10 pairs of limbs (9 of them being legs) all resembled long thin tubes.

Lazarus taxon that demonstrated that Hallucigeniidae persisted into the carboniferous

Discovery and naming

Carbotubulus is known from only a single fossil, the holotype ROM 47514, and is composed of two halves, a part and counterpart. The fossil was found in the Francis Creek Shale of Illinois's Carbondale Formation. More specifically, it was recovered from Pit 11 of the Mazon Creek fossil beds. Carbotubulus was discovered and described by Joachim T. Haug, Georg Mayer, Carolin Haug, and Derek E.G. Briggs in 2012. Currently, the animal is being held in the Invertebrate Palaeontology Collection at the Royal Ontario Museum of Toronto, Canada.

Carbotubulus's genus name is derived from two words. The first, "carbo", is Latin and references it living in Carboniferous. The second, "tubulus", is also Latin and means "small pipe", a reference to the animal's narrow pipe-like legs. The species name "waloszeki" honors Dieter Waloszek for his work on arthropod evolution.

Description

The Carbotubulus holotype was preserved in 3D, with the animal being nearly 7 times longer than wide (35 mm in length vs 4.8 mm in width). In general, Carbotubulus had a smooth body. It lacked any annulations (rings of skin) or dermal papillae other than a few longitudinal wrinkles.

At the front of its body, Carbotubulus had a long cylindrical head that made up 1/3rd of the animal's total length. While the front-most part was chipped off, most of the head was encased in the fossil concretion. Near the beginning of the head were two pairs of dark circular spots. The first were positioned more towards the sides of the head while the second were located behind it, were slightly fainter, and positioned higher up, being closer to the animal's midline. The paper never suggested what these might be, including if they were eyes. However, the authors dismissed them being artifacts due to their symmetrical arrangement. Behind the dots, Carbotubulus had a small pair of lobopods situated on the bottom of the head towards the sides, being separated from and significantly tinier than the animal's legs. In Knecht et al's 2025 redescription of Palaeocampa, these were considered tentacular lobopods, much like those on the head region of Hallucigenia and typical of Hallucigeniidae.

On its trunk section, Carbotubulus had 9 pairs of long, narrow, tube-like lobopods that would have functioned as legs. The legs were more than twice as long as the body's diameter and were more than 5 times longer than wide. As with the head, not all of these were fully incorporated into the fossil concretion, the ends of pairs 8 and 10 being clipped off. The legs were preserved in different lengths and sizes, with the largest (pair 8) being 11 mm long and 2 mm in diameter. The diameter of pairs 7 and 9 are somewhat wider, though the authors considered this an artifact of preservation from a sloped break when the fossil was cut open. At the end of the animal, the trunk merges with the last pair of limbs rather than continuing further. Knecht et al wondered if Carbotubulus had spines on its back in life, but admitted this had yet to be thoroughly investigated.

Classification

When Carbotubulus was first described, where it sit on the tree of life was not analyzed, and it was loosely assigned to the group Panarthropoda (or in the original description, Arthropoda sensu lato) A study on Hallucigenia's mouth in 2015 and discovery of the Cambrian lobopod Ovatiovermis cribratus from the Burgess Shale in 2017 led to a reanalysis of lobopodian classification, and Carbotubulus was confidently labeled a panarthropod, specifically assigned the family Hallucigeniidae The 2015 study recovered it as a sister group to Hallucigenia sparsa, while the 2017 study found it to be the basalmost definite Hallucigeniid.

This placement was challenged after the discovery of the another post-Cambrian (Silurian) long-legged lobopodian, Thanahita distos, from the Herefordshire Lagerstätte at the England–Wales border in UK in 2018. The new interpretation suggested that Carbotubulus may lie outside the hallucigeniid family. A later study from 2024 disagreed with this, placing Carbotubulus along with Thanahita and Microdictyon back in Hallucigeniidae.

A year later, another paper describing Palaeocampa anthrax found Carbotubulus to be in a polytomy with a variety of traditional Hallucigeniids (though Cardiodictyon and Hallucigenia hongmeia were outside the group). A phylogeny of this can be found below.

†Diania

†Lenisambulatrix

Evolutionary implications

is an aquatic lobopodian

There are other lineages that persisted for longer than originally thought, for example Mimetaster hexagonalis (a marrellomorph) and Schinderhannes bartelsi (a radiodont) from the Early Devonian. Still, the survival of Carbotubulus is much more extreme.

similar thing occurs with Palaeocampa anthrax, a freshwater Aysheaiid lobopodian that lived in the carboniferous during the same general time as carbotubulus.

References

  1. 1 2 3 4 5 6 7 8 Haug, Joachim T.; Mayer, Georg; Haug, Carolin; Briggs, Derek E. G. (2012). "A Carboniferous Non-Onychophoran Lobopodian Reveals Long-Term Survival of a Cambrian Morphotype". Current Biology. 22 (18): 1673–1675. Bibcode:2012CBio...22.1673H. doi:10.1016/j.cub.2012.06.066. PMID 22885062.
  2. 1 2 3 4 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.
  3. 1 2 Smith, Martin R.; Caron, Jean-Bernard (July 2015). "Hallucigenia's head and the pharyngeal armature of early ecdysozoans". Nature. 523 (7558). Nature Publishing Group: 75–78. Bibcode:2015Natur.523...75S. doi:10.1038/nature14573. ISSN 1476-4687. PMID 26106857.
  4. 1 2 Caron, Jean-Bernard; Aria, Cédric (2017). "Cambrian suspension-feeding lobopodians and the early radiation of panarthropods". BMC Evolutionary Biology. 17 (1): 29. Bibcode:2017BMCEE..17...29C. doi:10.1186/s12862-016-0858-y. PMC 5282736. PMID 28137244.
  5. ↑ Siveter, Derek J.; Briggs, Derek E. G.; Siveter, David J.; Sutton, Mark D.; Legg, David (2018). "A three-dimensionally preserved lobopodian from the Herefordshire (Silurian) Lagerstätte, UK". Royal Society Open Science. 5 (8) 172101. Bibcode:2018RSOS....572101S. doi:10.1098/rsos.172101. PMC 6124121. PMID 30224988.
  6. ↑ Aria, Cédric; Caron, Jean-Bernard (2024-12-31). "Deep origin of articulation strategies in panarthropods: evidence from a new luolishaniid lobopodian (Panarthropoda) from the Tulip Beds, Burgess Shale". Journal of Systematic Palaeontology. 22 (1) 2356090. Bibcode:2024JSPal..2256090A. doi:10.1080/14772019.2024.2356090. ISSN 1477-2019.
  7. ↑ Murdock, Duncan J. E.; Gabbott, Sarah E.; Purnell, Mark A. (2016-01-22). "The impact of taphonomic data on phylogenetic resolution: Helenodora inopinata (Carboniferous, Mazon Creek Lagerstätte) and the onychophoran stem lineage". BMC Evolutionary Biology. 16 (1): 19. Bibcode:2016BMCEE..16...19M. doi:10.1186/s12862-016-0582-7 (inactive 24 October 2026). ISSN 1471-2148. PMC 4722706. PMID 26801389.{{cite journal}}: CS1 maint: DOI inactive as of October 2026 (link)