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Lobopodia

For a type of cell projection, see Pseudopod. For an explanation of very similar terms, see Panarthropoda. For Lobopoda, a genus of beetles, see Lobopoda.

Lobopodia
Temporal range: Descendant taxa Onychophora, Tardigrada, and Euarthropoda survive to Recent, possible Ediacaran ichnofossils [2]
Reconstruction of various lobopodians. 1: Microdictyon sinicum, 2: Diania cactiformis, 3: Collinsovermis monstruosus, 4: Luolishania longicruris, 5: Onychodictyon ferox, 6: Hallucigenia sparsa, 7: Aysheaia pedunculata, 8: Antennacanthopodia gracilis, 9: Facivermis yunnanicus, 10: Paucipodia inermis, 11: Jianshanopodia decora, 12: Hallucigenia fortis
Reconstruction of various lobopodians. 1: Microdictyon sinicum, 2: Diania cactiformis, 3: Collinsovermis monstruosus, 4: Luolishania longicruris, 5: Onychodictyon ferox, 6: Hallucigenia sparsa, 7: Aysheaia pedunculata, 8: Antennacanthopodia gracilis, 9: Facivermis yunnanicus, 10: Paucipodia inermis, 11: Jianshanopodia decora, 12: Hallucigenia fortis
Scientific classificationEdit this classification
Domain: Eukaryota
Kingdom: Animalia
Subkingdom: Eumetazoa
Clade: ParaHoxozoa
Clade: Bilateria
Clade: Nephrozoa
(unranked): Protostomia
Superphylum: Ecdysozoa
(unranked): Panarthropoda
Phylum: †"Lobopodia"
Snodgrass 1938
Groups included
Cladistically included but traditionally excluded taxa

Crown-group Euarthropoda

Synonyms

Lobopodians are members of the informal group Lobopodia[3] (from the Greek, meaning "blunt feet"), or the formally erected phylum Lobopoda Cavalier-Smith (1998).[4] They are panarthropods with stubby legs called lobopods,[5] a term which may also be used as a common name of this group as well.[6][7] While the definition of lobopodians may differ between literatures,[8] it usually refers to a group of soft-bodied, marine worm-like fossil panarthropods such as Aysheaia and Hallucigenia.[9][5][10]

The oldest near-complete fossil lobopodians date to the Lower Cambrian; some are also known from Ordovician, Silurian and Carboniferous Lagerstätten.[11][12][13] Some bear toughened claws, plates or spines, which are commonly preserved as carbonaceous or mineralized microfossils in Cambrian strata.[14][15] The grouping is considered to be paraphyletic, as the three living panarthropod groups (Arthropoda, Tardigrada and Onychophora) are thought to have evolved from lobopodian ancestors.

  1. ^ Haug, J.T.; Mayer, G.; Haug, C.; Briggs, D.E.G. (2012). "A Carboniferous non-Onychophoran Lobopodian reveals long-term survival of a Cambrian morphotype". Current Biology. 22 (18): 1673–1675. doi:10.1016/j.cub.2012.06.066. PMID 22885062.
  2. ^ Chen, Zhe; Chen, Xiang; Zhou, Chuanming; Yuan, Xunlai; Xiao, Shuhai (6 June 2018). "Late Ediacaran trackways produced by bilaterian animals with paired appendages". Science Advances. 4 (6). doi:10.1126/sciadv.aao6691. hdl:10919/84444.
  3. ^ Snodgrass, R.E. (1938). "Evolution of the Annelida, Onychophora, and Arthropoda". Smithsonian Miscellaneous Collections. 97 (6): 1–159.
  4. ^ Cavalier-Smith, T. (1998). "A revised six-kingdom system of life". Biological Reviews. 73 (3): 203–266. doi:10.1017/S0006323198005167 (inactive 2024-04-26). PMID 9809012.{{cite journal}}: CS1 maint: DOI inactive as of April 2024 (link)
  5. ^ a b Ortega-Hernández, Javier (2015-10-05). "Lobopodians". Current Biology. 25 (19): R873–R875. doi:10.1016/j.cub.2015.07.028. ISSN 0960-9822. PMID 26439350.
  6. ^ Budd, Graham; Peel, John (1998-12-01). "A new Xenusiid lobopod from the early Cambrian Sirius Passet fauna of North Greenland". Palaeontology. 41: 1201–1213.
  7. ^ Cite error: The named reference Liu2006 was invoked but never defined (see the help page).
  8. ^ Cite error: The named reference :8 was invoked but never defined (see the help page).
  9. ^ Liu, Jianni; Dunlop, Jason A. (2014-03-15). "Cambrian lobopodians: A review of recent progress in our understanding of their morphology and evolution". Palaeogeography, Palaeoclimatology, Palaeoecology. 398: 4–15. Bibcode:2014PPP...398....4L. doi:10.1016/j.palaeo.2013.06.008. ISSN 0031-0182.
  10. ^ Cite error: The named reference :13 was invoked but never defined (see the help page).
  11. ^ van Roy, P.; Orr, P.J.; Botting, J.P.; Muir, L.A.; Vinther, J.; Lefebvre, B.; Hariri, K.E.; Briggs, D.E.G. (2010). "Ordovician faunas of Burgess Shale type". Nature. 465 (7295): 215–218. Bibcode:2010Natur.465..215V. doi:10.1038/nature09038. PMID 20463737. S2CID 4313285.
  12. ^ von Bitter, P.H.; Purnell, M.A.; Tetreault, D.K.; Stott, C.A. (2007). "Eramosa Lagerstätte—Exceptionally preserved soft-bodied biotas with shallow-marine shelly and bioturbating organisms (Silurian, Ontario, Canada)". Geology. 35 (10): 879. Bibcode:2007Geo....35..879V. doi:10.1130/G23894A.1. S2CID 11561169.
  13. ^ Haug, J.T.; Mayer, G.; Haug, C.; Briggs, D.E.G. (2012). "A Carboniferous non-Onychophoran Lobopodian reveals long-term survival of a Cambrian morphotype". Current Biology. 22 (18): 1673–1675. doi:10.1016/j.cub.2012.06.066. PMID 22885062.
  14. ^ 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.
  15. ^ Topper, T.P.; Skovsted, C.B.; Peel, J.S.; Harper, D.A.T. (2013). "Moulting in the lobopodian Onychodictyon from the lower Cambrian of Greenland". Lethaia. 46 (4): 490–495. doi:10.1111/let.12026.
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