Lenisambulatrix

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Lenisambulatrix
Temporal range: Cambrian Stage 3
Three-dimensional reconstruction of Lenisambulatrix humboldti
Diagrammatic reconstruction of Lenisambulatrix humboldti
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
(unranked): Panarthropoda
Phylum: †"Lobopodia"
Genus: †Lenisambulatrix
Species:
†L. humboldti
Binomial name
†Lenisambulatrix humboldti
Ou & Mayer, 2018

Lenisambulatrix (Humboldt lobopodian) is a genus of extinct worm belonging to the group Lobopodia and known from the Lower Cambrian Maotianshan shale of China. It is represented by a single species L. humboldti. The incomplete fossil was discovered and described by Qiang Ou and Georg Mayer in 2018.[1] Due to its missing parts, its relationship with other lobopodians is not clear. It shares many structural features with another Cambrian lobopodian Diania cactiformis, a fossil of which was found alongside it.[2]

Discovery[edit]

Lenisambulatrix humboldti fossils

The fossil of Lenisambulatrix humboldti was discovered by Qiang Ou (China University of Geosciences, Beijing, China) and Georg Mayer (University of Kassel, Kassel, Germany). It was found in the Heilinpu Formation of the Huaguoshan section at Sanjiezi village, Erjie town, Yunnan, South China.[1] The location is dated to Cambrian Series 2, Stage 3 (about 520 million years old).[3][4] The excavation also yielded a fossil of Diania cactiformis, already described by Ou's team in 2011.[5] The specimen was compressed partly with the fossil of a brachiopod Diandongia pista, which was described from the similar Maotianshan shale in 2003.[6] The discovery was reported in the September issue of the Scientific Reports.[7]

The generic name is derived from Latin words, lenis, meaning soft or smooth, or gentle, attributing to the smooth unarmoured body; ambulatrix, meaning walker. The specific name is in honour of the German zoologist Friedrich Wilhelm Heinrich Alexander von Humboldt, after whose name was established the Alexander von Humboldt Foundation, which funded the research.[2]

Description[edit]

Lenisambulatrix is seen as dark, carbonaceous and aluminosilicate films in a worn out mudstone. The original soft tissues and cuticle are represented by deposits of dark red to brown iron(III) oxide fine grains as a result of weathering of microscopic diagenetic pyrite.[2] This fossilisation process is similar to those of other specimens in the Chengjian region.[8] The fossil is oblique-ventrally compressed and the remaining parts are nicely preserved showing details of the body structure. This good preservation is characteristic of Chengjian biota and indicates death due to a catastrophic event.[9]

The worm is a soft-bodied lobopodian without any hard part (sclerotized) surface, thus, appears naked[1] in contrast to most lobopodians which bears spines as body armours.[10][11] It is not preserved in a completely stretched form and many parts are missing. The measurable length of the body is 2.9 cm; with a width varying from 2 to 3.6 mm. The trunk consists of at least eight segments (somites), each of which bears a pair of thick and long legs. The fossil contains only the anterior part and the posterior region remains unknown.[2] The head part is slightly extended and does not show any specific part. It is believed to be closely related to Diania, but with unique differences. The main distinction is numerous sclerotized spines that adorn Diana are completely absent in Lenisambulatrix.[1] Diana's head is also much more rounded and shorter. The general outline of Lenisambulatrix's head more similar to other lobopodians such as Microdictyon sinicum, Paucipodia inermis, and Hallucigenia sparsa.[10][12][13] However, the relatively thick and elongated legs measuring 11.6 to 18 mm long are unique to both Diania and Lenisambulatrix.[7] Their legs also lack claws that are the common features in other lobopods.[11][14] The legs indicate that they were adapted to walking or crawling on the bottom of waters.[7] The simple body structure suggests that Lenisambulatrix is one of the earliest panarthropod animal.[2]

References[edit]

  1. ^ a b c d Geggel, Laura (2018-09-20). "Without Claws or Armor, 520-Million-Year-Old 'Naked' Critter Was Likely a Loner". Live Science. Retrieved 2022-01-15.
  2. ^ a b c d e Ou, Qiang; Mayer, Georg (2018). "A Cambrian unarmoured lobopodian, † Lenisambulatrix humboldti gen. et sp. nov., compared with new material of † Diania cactiformis". Scientific Reports. 8 (1): 13667. Bibcode:2018NatSR...813667O. doi:10.1038/s41598-018-31499-y. PMC 6147921. PMID 30237414.
  3. ^ Liu, Yu; Scholtz, Gerhard; Hou, Xianguang (2015). "When a 520 million-year-old Chengjiang fossil meets a modern micro-CT – a case study". Scientific Reports. 5 (1): 12802. Bibcode:2015NatSR...512802L. doi:10.1038/srep12802. ISSN 2045-2322. PMC 4523851. PMID 26238773.
  4. ^ Yang, Chuan; Li, Xian-Hua; Zhu, Maoyan; Condon, Daniel J.; Chen, Junyuan (2018). "Geochronological constraint on the Cambrian Chengjiang biota, South China". Journal of the Geological Society. 175 (4): 659–666. Bibcode:2018JGSoc.175..659Y. doi:10.1144/jgs2017-103. ISSN 0016-7649. S2CID 135091168.
  5. ^ Liu, Jianni; Steiner, Michael; Dunlop, Jason A.; Keupp, Helmut; Shu, Degan; Ou, Qiang; Han, Jian; Zhang, Zhifei; Zhang, Xingliang (2011). "An armoured Cambrian lobopodian from China with arthropod-like appendages". Nature. 470 (7335): 526–530. Bibcode:2011Natur.470..526L. doi:10.1038/nature09704. ISSN 1476-4687. PMID 21350485. S2CID 4324509.
  6. ^ Zhifei, Zhang; Jian, H. a. N.; Xingliang, Zhang; Jianni, L. I. U.; Degan, S. H. U. (2003). "Pediculate Brachiopod Diandongia pista from the Lower Cambrian of South China". Acta Geologica Sinica. 77 (3): 288–293. doi:10.1111/j.1755-6724.2003.tb00743.x. ISSN 1755-6724. S2CID 129658643.
  7. ^ a b c "Palaeontology: 'Reclusive' fossil worm from the Cambrian identified". www.natureasia.com. 2018-09-21. Retrieved 2022-01-15.
  8. ^ Forchielli, Angela; Steiner, Michael; Kasbohm, Jörn; Hu, Shixue; Keupp, Helmut (2014). "Taphonomic traits of clay-hosted early Cambrian Burgess Shale-type fossil Lagerstätten in South China". Palaeogeography, Palaeoclimatology, Palaeoecology. Cambrian Bioradiation. 398: 59–85. Bibcode:2014PPP...398...59F. doi:10.1016/j.palaeo.2013.08.001. ISSN 0031-0182.
  9. ^ Gaines, Robert R.; Briggs, Derek E.G.; Yuanlong, Zhao (2008). "Cambrian Burgess Shale–type deposits share a common mode of fossilization". Geology. 36 (10): 755. Bibcode:2008Geo....36..755G. doi:10.1130/G24961A.1. ISSN 0091-7613.
  10. ^ a b Caron, Jean-Bernard; Aria, Cédric (2017). "Cambrian suspension-feeding lobopodians and the early radiation of panarthropods". BMC Evolutionary Biology. 17 (1): 29. doi:10.1186/s12862-016-0858-y. PMC 5282736. PMID 28137244.
  11. ^ a b Liu, Jianni; Dunlop, Jason A. (2014). "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.
  12. ^ Ma, Xiaoya; Hou, Xianguang; Aldridge, Richard J.; Siveter, David J.; Siveter, Derek J.; Gabbott, Sarah E.; Purnell, Mark A.; Parker, Andrew R.; Edgecombe, Gregory D. (2012-09-01). "Morphology of Cambrian lobopodian eyes from the Chengjiang Lagerstätte and their evolutionary significance". Arthropod Structure & Development. 41 (5): 495–504. doi:10.1016/j.asd.2012.03.002. ISSN 1467-8039. PMID 22484085.
  13. ^ Xian-Guang Hou; Xiao-Ya Ma; Jie Zhao; Jan Bergström (2004). "The lobopodian Paucipodia inermis from the Lower Cambrian Chengjiang fauna, Yunnan, China". Lethaia. 37 (3): 235–244. doi:10.1080/00241160410006555.
  14. ^ Xianguang, Hou; Ramsköld, Lars; Bergström, Jan (1991). "Composition and preservation of the Chengjiang fauna –a Lower Cambrian soft-bodied biota". Zoologica Scripta. 20 (4): 395–411. doi:10.1111/j.1463-6409.1991.tb00303.x. ISSN 1463-6409. S2CID 85077111.
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