FishBase | Search | All Living Things


Onychophora
VELVET WORMS; WALKING WORMS; SPITTING WORMS
Life   Onychophora

IDnature guide

Links
Overview
Elongate, segmented ecdysozoans with many pairs of soft, unjointed, claw-bearing legs. Also known as velvet worms.

Phylogeny

Links to other sites

Acknowledgements

Supported by
go to Discover Life's Facebook group

Following modified from Museum of Paleontology University of California, Berkeley
   Top | See original

http://www.ucmp.berkeley.edu/onychoph/onychophora.html ---> https://ucmp.berkeley.edu/onychoph/onychophora.html

Introduction to the Onychophora

"Velvet worms" with an ancient history indeed

The average resident of the Northern Hemisphere is probably not familiar with the Onychophora; they are restricted to forest regions of South America, Africa, the Caribbean, and Oceania. Shy creatures, able to hide in incredibly tight crevices, these "velvet worms" (about ninety living species known) are rarely seen even in their natural habitat. Yet onychophorans are of great interest to biologists, because they seem to be related to arthropods , and give us an idea of what the ancestors of the arthropods may have been like. Although they are rare as fossils, a number that have been found from the Cambrian period. These fossils show that abundant marine relatives of the Onychophora flourished in the seas 520 million years ago.


Click on the buttons below to learn more about Onychophora.



Following modified from Peripatus
   Top | See original

  Peripatus Home Page  pix1Black.gif (807 bytes)   Paleontology >> Onychophora Updated: 25-May-2020 

Onychophora


Abstract

This page presents a brief overview of the Onychophora, from Cambrian to Recent.

Keywords:  Onychophora, velvet worm, Peripatus , Peripatoides , Aysheaia , fossil history, systematics

Introduction

Onychophorans, of which there are several endemic species in New Zealand, share a number of characteristics with both annelids (segmented worms) and arthropods, although they are more closely related to the latter and are sometimes, as here, regarded as a class within the Arthropoda. Other authors (e.g. Nielsen 2001) regard the Onychophora as a phylum in its own right.

Currently there are around 10 genera and 110 species recognised within two extant families: the Peripatidae (known from the circumtropical regions of Mexico, Central and northern South America, equatorial West Africa, and South East Asia) and the Peripatopsidae (found in Chile, South Africa, Australia including Tasmania, and New Zealand).

Description

[Some of the following is not my writing. Unfortunately, I cannot remember where it came from. My apologies to the unknown author whom I have failed to cite. I’ll rewrite it as soon as I can.]

Onychophorans are small, caterpillar-like animals with a segmented body plan. The Onychophoran dermis lacks a chitinous cuticle or exoskeleton (Jacobs et al. 2000, p. 343). The anterior end is indicated by the antennae and by the ventrally directed mouth, while the posterior end, projecting behind the last pair of walking legs, bears the terminal anus. There are many pairs of legs attached latero-ventrally, these being the only external signs of segmentation. The body is ringed by annuli on which are tubercles set in rows. Each tubercle ends in a tiny chitinous spine.

The body itself is not segmented except for the head, which is divided into three segments. The first contains the two large antennae with an eye at the base (Jamaica and South Africa have cave dwelling species which do not have eyes). Some males also have other appendages believed to be involved in sperm transfer.

The first pair of appendages are the antennae, these are tactile and the chief sense organs. A small eye is situated dorsally behind the base of each antenna and has a spherical lens. The mouth is directed ventrally and surrounded by ridged lips. In the sides of the mouth cavity are a pair of jaws, the appendages of segment 2.

The second segment contains the jaw like mouth which is used for rasping into prey and then sucking out the nutrients. The third segement holds the first pair of parapodia-like legs.

Each jaw is a low papilla with a pair of chitinous teeth. The roof of the anterior end of the mouth cavity is thickened to form the tongue which has a row of small chitinous teeth on its surface. Oral papillae, located lateral to the mouth, are presumed to have a sensory funtion. Defensive slime-glands open through the ends of the oral papillae.

Each of the legs bears a pair of chitinous claws for gripping, although on smooth substrate they walk on walking pads. Variously, the body between the limb insertion points, and the limbs themselves, may be finely annulated.

The legs are conical in shape and terminate distally in a plantigrade foot. The foot is retractable and is usually raised if the going is easy, being brought into play on slippery surfaces. The foot terminates distally in a pair of retractable claws and bears 3 prominent tubercles. Ventrally on the distal ridges of the leg proper are spinous pads; the shape and number of pads are helpful in recognising some species. Basally on the leg a groove runs along the ventral surface of the leg at right angles to the body axis. On all legs except 4 and 5 the excretory pore may be found at the basal end of this groove. If crural glands are present they will be found distal to the end of the groove.

Contemporary Onycophorans are ceolomates and have haemocoel, which means they have a lined body cavity filled with blood, rather than a vascular system. They have a muscular tubular heart which pumps the colorless blood around the body cavity. Locomotion is essentially annelid-like, with the body cavity functioning as a hydrostatic skeleton. The parapodia-like legs are also filled with blood and a valve at the base keeps them firm and muscular coordination can extend them or retract them and make them move forward or make them move backward.

Onycophorans have a cuticle with a-chitin but lacking collagen, which is periodically shed to permit growth (ecdysis). New cuticle is secreted underneath the old one by the ectodermal cells which develop microvilli that are subsequently withdrawn. Ecdysteroids have been found in various tissues but their function remains unknown (Hoffmann 1997; Nielsen 2001, p. 198). Unlike insect dermis, the cuticle of modern representatives is non-articulated, thin and soft and covered in hundreds of papillae and sensory hairs giving them a velvety texture, hence the common name ‘velvet worm.’ However, a characteristic feature of several fossil species is the paired internal sclerotic plates above the limb insertions, which may be variously developed into (presumeably defensive) spikes.

Like insects the Onycophora breathe through spiracles. Spiracles open out to the enviroment and oxygen enters through a system of tubules (trachae) and is absorbed into the tissues across the moist surfaces. However, unlike the insects, onycophorans have no control on the spiracles and they are always open, making the animal extremely vulnerable to dessication, so high levels of humidity are required.

Contemporary onycophorans are able to predate organisms several times larger than themselves by immobilising it with a gluey secretion from glands in its head, projected up to 30cm. The secretion holds the prey while the animal approaches it, bites through the cuticle, and injects a toxic, digestive saliva into the wound.

The animal preys on small arthropods by squirting and entrapping them in a glue fired from openings beside the mouth. It then injects saliva into the prey, dissolving the inner contents, and thus enabling the Peripatus to suck them out.

Onychophorans themselves have few predators, except perhaps insect carnivores such as centipedes, birds and rodents.

Phylogeny and Evolution

“Onychophorans are thought to be the sister taxon of [eu]arthropods and are segmented. However, onychophorans lack engrailed expression in their dermis. Instead, expression is observed in the posterior half of the developing limb and in a segmental pattern in the lateral mesoderm. The limb staining suggests shared ancestry of the onychophoran and arthropod limbs. However, given the close relationship of Arthropoda and Onychophora, and their segmented body plans, the lack of segmental ectodermal expression in Onychophora suggests that the ancestral role of engrailed was not segmentation; this absence may be a consequence of evolutionary loss of skeletons. Onychophoran dermis lacks a chitinous cuticle; thus Onychophora lack an exoskeleton” (Jacobs et al. 2000, p. 343).

Much has been written about enigmatic lobopodan taxa from the great Cambrian lagerstätten, especially the Burgess Shale and Chengjiang sites, and it is probably the most widely held view that many of these are stem-group onychophorans, as asserted by (for example) Jacobs et al. 2000:

“Furthermore, Cambrian fossils thought to be stem group onychophorans, such as Microdictyon , Hallucinogenia , and Xenusion , bear skeletal elements above the limb on each segment. Therefore, the absence of engrailed transcription in the ectoderm of modern Onychophora could well be a consequence of evolutionary loss of exoskeletal elements...” (p. 343-345).

However, it would be wrong to say this view is held universally. The Cambrian lobopods are exclusively marine, whereas all modern representatives are exclusively terrestrial, and their integument seems poorly suited to undertaking the transition from sea to land. The earliest known terrestrial onychophoran(s) is/are Carboniferous ( Antennipatus montceauensis from Montceau-les-Mines, France, and, less convincingly, Helenodora inopinata , from the Mazon Creek lagerstätte of the USA), and there are no putative onychophoran fossils of Ordovician to Devonian age. At least some of us are still highly sceptical that the Cambrian lobopods (“priapulids on legs”, in the words of Dzik & Krumbiegel 1989) have anything to do with modern onychophorans.

Nevertheless, they will be included here, though only because readers will be expecting it.

Fossil History

A number of fossils from the Cambrian have been described which look more or less like onychophorans. The Cambrian forms are marine, however, and are incompletely understood. It is possible they are not really related closely at all. Some, such as the Middle Cambrian form Aysheaia are rather similar to living forms (but see Whittington [find REF] for a contrary view). Others were armored with various plates and spines which, disarticulated, contribute substantially to the “small shelly fauna.” All of these Cambrian forms differed from living onychophorans in being marine.

Hallucigenia is most widely known from the Middle Cambrian, Burgess Shale form, Hallucigenia sparsa (Walcott), famously misinterpreted by Conway Morris (and later commentators) upside-down and back-to-front. Subsequently, another species, Hallucigenia fortis , has been described from the Lower Cambrian Chengjiang fauna.

Maas & Waloszek 2001, reports an undescribed “lobopodian” from the Upper Cambrian ‘Orsten’ beds of Sweden. Although only about a tenth the size of the better-known Cambrian onychophorans, the Swedish “‘Orsten’ lobopodian shares with the Lower to Middle Cambrian lobopodians not only the annulated segmental limbs but also the segmental paired dorsal outgrowths on the finely annulated tubular body, which has a diameter of about 100 to 120 mm. ... The body and limbs are virtually cylindrical, and the limbs were apparently stretched virtually laterally due to a thicker bridge linking right and left legs. [The cuticle] shows a cell-like surface microstructure that resembles the onychophoran condition” (Maas & Waloszek 2001, p. 457).

Another Cambrian fossil organism which might belong within this clade is Kerygmachela , known from the Lower Cambrian Sirius Passet locality (Budd 1993).

The earliest candiate terrestrial onychophorans are two fossils of Late Carboniferous (Pennsylvanian) age. They are Antennipatus montceauensis from Montceau-les-Mines, France (Garwood et al. 2016) and Helenodora inopinata , from the Mazon Creek lagerstätte near Chicago, USA, a locality that has yielded a great many fossils of soft-bodied organisms (Thompson & Jones 1980). The onychophoran affinity of both is contentious, though it is probably fair to say that advocates for one or other of these taxa outnumber those who are sceptical of both.

Systematics

The systematics adopted here mostly follows Hou & Bergström 1995, though with some minor changes as noted.

Phylum Gnathopoda Lankester 1877

  1877 Gnathopoda Lankester  
  1979 Lobopoda Boudreaux  
  1995 Panarthropoda Nielsen  
  1996 Podophora Waggoner  
  1998 Lobopoda de Haro  
  2001a Arthropoda, Budd  
2001 Arthropoda s.l. Maas & Waloszek
  2006 Aiolopoda Hou & Bergstrom  

Discussion: Three groups within the ecdysozoans, the onychophora, tardigrades and “euarthropods”, have received variable treatment over time. Probably most often, today, they are treated as separate phyla (e.g., Nielsen 2001). However, they are obviously closely related, and various taxa have been erected to group them, one of the best known being the Panarthropoda of Nielsen 1995, probably because that work is comparatively recent. An alternative approach, adopted here, is to consider all three to be a single phylum and separate them at the class level.

The relationships between these classes are still controversial. The name Arthropoda was coined by von Siebold (1848) but, despite common usage to the contrary, it is clear from his diagnosis that he intended this group to include only the tardigrades and euarthropods; not onychophorans (see Ortega-Hernández 2016). Other names intended for the same purpose, and therefore junior synonyms, include Arthropoidea [de Haro 1999] and Tactopoda [Budd 2001c].

Sister relationships have also been also proposed for onychophorans+euarthropods (e.g. the names Arthropoda sensu Lankester 1904 and Antennopoda [de Haro 1998] were intended for this purpose) and, finally, for onychophorans+tardigrades (e.g. Pararthropoda [Vandel 1949] and Oncopoda [Weber 1954]).

The three together are most likely monophyletic, so for the present we will simply treat them as a polytomy. Common characteristics of the Gnathopoda include the presence of legs and claws, a ventral nervous system, and a segmented body.

Class Onychophora Grube 1853

  1853 Onychophora Grube  
1904 Onychophora Lankester, p. 529

Discussion: The class Onychophora was used by Hou & Bergström 1995 to include the terrestrial forms: the modern onychophorans and the single known fossil terrestrial species, Helenodora . These authors also noted their belief that the fossil marine form, Onychodictyon , “is closer to modern onychophorans than any of the other Cambrian lobopodians” (p. 11). Their cladogram (Hou & Bergström 1995, fig. 7) depicts Onychodictyon , Helenodora , and modern onychophorans together comprising a well-formed clade. Yet in their systematic section (p. 17) Onychodictyon is left outside Onychophora, in the class Xenusia, on morphologic grounds. This seems appropriate, given the still rather weak evidence that the Cambrian marine forms are Onychophorans at all.

Order Euonychophora Hutchinson 1930, p. 23

Family Peripatidae Evans 1901

Type: Peripatus Guilding 1826

Discussion: The members of this family are generally coloured red-brown and possess 22 to 43 pairs of legs.

Genus Peripatus Guilding 1826

...

Family Peripatopsidae Bouvier 1907

This family contains organisms which are generally coloured blue-green and possess 14 to 25 pairs of legs.

Genus Peripatoides Pocock 1894

Peripatoides novaezealandiae

Description: Peripatoides novaezealandiae has 15 pairs of legs with hooks at the end, two robust feelers, and is velvety in appearance and comes in colours of blue, green, grey and brown; and may reach 80 mm in length.

Occurence: Never abundant but “not uncommon” at Titirangi, near Auckland (Gill 1998).

Habit: Peripatus live in damp areas such as under moss, in rotting logs, behind the bark of trees, and in leaf litter.

Order incertae sedis

Genus Antennipatus Garwood et al. 2016, p. 183

Description: Vermiform taxon with annulated paired appendages resembling lobopods (maximum length is 2.8 mm), serially repeated along a body covered by an annulated cuticle; each segment with eight plicae; each plica with papillae, their size and spacing similar to onychophoran primary papillae. Head with long onychophoran-like antennae (with alternation of wide and narrow annuli) and possible slime papillae represented by ventrolateral appendages shorter than the other appendages. Length and total number of trunk segments not available; a maximum of five trunk segments preserved. (Claws and spinous pads of legs not observed; jaws not observed; genital opening and anal pore not preserved).

Antennipatus montceauensis Garwood et al. 2016, p. 184-185

Discussion: The onychophoran affinities of Antennipatus montceauensis … are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem-group as a whole. Nevertheless, A. montceauensis is the most compelling candidate to date for a terrestrial Paleozoic onychophoran (after Garwood et al. 2016, Abstract).

Class Xenusia Dzik & Krumbiegel 1989

Order Protonychophora Hutchinson 1930, p. 23

Family Aysheaiidae Walcott 1911

Genus Aysheaia Walcott 1911

Aysheaia pedunculata Walcott 1911

This problematical fossil was first described from the Burgess Shale by Walcott in 1911.

Family Xenusiidae Dzik & Krumbiegel 1989

Description: [VERIFY] >20 leg-bearing segments; paired, rounded sclerites on each segment; spiny legs.

Genus Xenusion Pompeckj 1927

Xenusion auerswaldae Pompeckj 1927

Xenusion , from early Cambrian sandstones of eastern Europe. This form was also armed with spines, although they were shorter than those of Hallucigenia. Only two specimens have been found so far.

Order Paronychophora Hou & Bergström 1995

Family Onychodictyidae Hou & Bergström 1995

Genus Onychodictyon Hou et al. 1991

Type Species: Onychodictyon ferox Hou et al. 1991

Order Scleronychophora Hou & Bergström 1995

Family Eoconchariidae Hao & Shu 1987

  1987 Eoconchariidae Hao & Shu  
  1988 Eoconchariidae Shu & Chen  
  1989 Microdictyonidae Chen et al.  

Genus Microdictyon Bengtson et al. 1981 emend. Chen et al. 1989

Species: Microdictyon effusum (type?), M. rhomboidale, M. robisoni, M. sinicum (Chen et al. 1989), M. sphaeroides, M. tenuiporatum

Fig. 1: Microdictyon sp. specimen from Chengjiang region. Image courtesy of The Natural Canvas.

Family Hallucigeniidae Conway Morris 1977

Genus Hallucigenia Conway Morris 1977, p. 624

Type Species: Hallucigenia sparsa (Walcott 1911) Conway Morris 1977

Other Species: Hallucigenia fortis Hou & Bergström 1995

Family Cardiodictyidae Hou & Bergström 1995

Genus Cardiodictyon Hou et al. 1991

Type Species: Cardiodictyon catenulum Hou et al. 1991

Class incertae sedis

Order Archonychophora Hou & Bergström 1995

Hou & Bergström 1995 retain Archonychophora within the Xenusia. However, they also note their belief that Luoishania , is a sister taxon to all other onychophorans (e.g. their fig. 7). If correct, then a cladistic approach to onychophoran taxonomy suggests removing the Archonychophora to a new class.

Family Luolishaniidae Hou & Bergström 1995

Genus Luolishania Hou & Chen 1989

Type Species: Luolishania longicruris Hou & Chen 1989

Genus Antennacanthopodia Ou et al. 2011, p. 588

Type Species: Antennacanthopodia gracilis Ou et al. 2011, p. 588

Order incertae sedis

Family incertae sedis

Genus Helenodora Thompson & Jones 1980

Helenodora inopinata Thompson & Jones 1980

References

Bengtson, S.; Matthews, S.C.; Missarzhevsky, V.V. 1981: . In Missarzhevsky, V.V.; Mambetov, A.M. 1981: Stratigrafiya I fauna pogranichnykh sloev kembriya I dok embriya Malogo Karatau [Stratigraphy and fauna of the Precambrian-Cambrian boundary beds of Malyj Karatau] [in Russian]. Trudy Geologicheskogo Instituta AN SSSR 326 .

Boudreaux, H.B. 1979: Significance of the intersegmental tendon system in arthropod phylogeny and monophyletic classification of Arthropoda. In Gupta, A.P. 1979: Arthropod phylogeny. Van Nostrand Reinhold Company, New York : 551-586.

Bouvier, E.-L. 1907: Crustacés décapodes nouveaux recueillis à Païta (Pérou) par M. le Dr Rivet. Bulletin du Muséum national d’Histoire naturelle 13: 113-116.

Budd, G.E. 1993: A Cambrian gilled lobopod from Greenland. Nature 364: 709-711.

— 2001a: Why are arthropods segmented? Evolution and Development 3 (5): 332-342.

— 2001c: Tardigrades as ‘stem-group arthropods’: The evidence from the Cambrian fauna. Zoologischer Anzeiger 240 (3-4): 265-279.

Chen, J.Y.; Hou, X.G.; Lu, H.Z. 1989: Early Cambrian netted scale-bearing worm-like sea animal [in Chinese]. Acta Palaeontologica Sinica 28: 1-16.

Conway Morris, S. 1977: A new metazoan from the Burgess Shale of British Columbia. Palaeontology 20: 623-640.

de Haro 1998: Origen y relaciones filogenéticas entre Artrópodos, Onicóforos, Anélidos y Lofoforados, según datos moleculares y morfológicos. Boletin de la Real Sociedad Espanola de Historia Natural 94: 103-113.

— 1999: Relaciones filogenéticas entre Artrópodos, Onicóforos, Anélidos y Lofoforados. Boletin de la Sociedad Entomologica Aragonesa 26: 161-169.

Dzik, J.; Krumbiegel, G. 1989: The oldest ‘onychophoran’ Xenusion : a link connecting phyla? Lethaia 22: 169-182.

Evans, R. 1901: On two new species of Onychophora from the Siamese Malay States. Quarterly Journal of Microscopical Science 44: 473-538.

Garwood, R.J.; Edgecombe, G.D.; Charbonnier, S.; Chabard, D.; Sotty, D.; Giribet, G. 2016: Carboniferous Onychophora from Montceau-les-Mines, France, and onychophoran terrestrialization. Invertebrate Biology 135 (3): 179-190.

Gill, B.J. (ed) 1998: Powell’s native animals of New Zealand. 4th ed. Original text by A.W.B. Powell, updated by W.O. Cernohorsky, B.J. Gill, A.B. Stephenson, and K.A.J. Wise. Bateman, Auckland: 1-94.

Grube, E. 1853: Über den Bau von Peripatus edwardsii . Müller‘s Archives of Anatomy and Physiology [1853]: 322-360.

Guilding, L. 1826: Mollusca Caribbaeana. Zoological Journal 2: 437-449.

Hao, Y.; Shu, D. 1987: The oldest known well preserved Pheodaria (Radiolaria) from Southern Shaanxi [in Chinese]. Geoscience 1 (3-4): 301-310.

Hoffmann, K. 1997: Ecdysteroids in adult females of a 'walking worm' Euperipatoides leuckartii (Onychophora, Peripatopsidae). Invert. Reprod. Dev. 32: 27-30.

Hou, X.; Bergström, J. 1995: Cambrian lobopodians - ancestors of extant onychophorans. Zoological Journal of the Linnaean Society 114: 3-19.

Hou, X.; Bergströom, J. 2006: Dinocarids - anomalous arthropods or arthropod-like worms. In Rong, J.; Fang, Z.; Zhou, Z.; Zhan, R.; Wang, X.; Yuan, X. (ed.) 2006: Originations, Radiations and Biodiversity Changes - Evidences from the Chinese Fossil Record. Science Press, Beijing : 139-158.

Hou, X.G.; Chen, J.Y. 1989: Early Cambrian arthropod- annelid intermediate sea animal, Luolishania gen. nov. from Chengjiang, Yunnan. [In Chinese with English summary.]. Acta Palaeont. Sin. 28 (2): 207-213.

Hou, X.G.; Ramsköld, L.; Bergström, J. 1991: Composition and preservation of the Chengjiang fauna - a Lower Cambrian soft-bodied biota. Zool. Scripta 20 (4): 395-411.

Hutchinson, G.E. 1930: Restudy of some Burgess Shale fossils. Proceedings of the United States National Museum 78 (11): 1-24.

Jacobs, D.K.; Wray, C.G.; Wedeen, C.J.; Kostriken, R.; DeSalle, R.; Staton, J.L.; Gates, R.D.; Lindberg, D.R. 2000: Molluscan engrailed expression, serial organization, and shell evolution. Evolution & Development 2 (6): 340-347.

Lankester, E.R. 1877: Notes on the embryology and classification of the Animal kingdom: comprising a revision of speculations relative to the origin and significance of germ-layers. Quarterly Journal of Microscopical Science 68: 399-454.

— 1904: The structure and classification of the Arthropoda. Microscopical Society (London) Quarterly Journal n.s. 47 (188): 523-582.

Maas, A.; Waloszek, D. 2001: Cambrian Derivatives of the Early Arthropod Stem Lineage, Pentastomids, Tardigrades and Lobopodians - An 'Orsten' Perspective. Zoologischer Anzeiger 240: 451-459.

Nielsen, C. 1995: Animal evolution: Interrelationships of the living phyla (first edition). Oxford University Press.

— 2001: Animal evolution: Interrelationships of the living phyla (second edition). Oxford University Press: 1-378.

Ortega-Hernández, J. 2016: Making sense of ‘lower’ and ‘upper’ stem-group Euarthropoda, with comments on the strict use of the name Arthropoda von Siebold, 1848. Biological Reviews 91: 255-273.

Ou, Q.; Liu, J.; Shu, D.; Han, J.; Zhang, Z.; Wan, X.; Lei, Q. 2011: A rare onychophoran-like lobopodian from the Lower Cambrian Chengjiang lagerstätte, southwestern China, and its phylogenetic implications. Journal of Paleontology 85 (3): 587-594.

Pocock, R.I. 1894: Contributions to our knowledge of the arthropod fauna of the West Indies - Part III. Diplopoda and Malacopoda, with a supplement on the Arachnida of the class Pedipalpi. Journal of the Linnean Society - Zoology 24: 473-544.

Pompeckj, J.F. 1927: Ein neues Zeugnis uralten Lebens. Paläontologische Zeitschrift 9: 287-313.

Shu, D.G.; Chen, L. 1988: Discovery of Early Cambrian Radiolaria and its significance [in Chinese]. Scientia Sinica B8: 881-886.

Thompson, I.; Jones, D. 1980: A Possible Onychophoran from the Middle Pennsylvanian Mazon Creek beds of Northern Illinois. Journal of Paleontology 54: 588-596.

Vandel, A. 1949: Embranchment des arthropodes. In Grasse, P.P. (ed.) 1949: Traité de zoologie. Masson, Paris, no. 6: 79-158.

von Siebold, C.T. 1848: Lehrbuch der vergleichenden Anatomie der Wirbellosen Thiere. Erster Theil. In von Siebold, C.T.; Stannius, H. (ed.) 1848: Lehrbuch der vergleichenden Anatomie. Verlag von Veit & Comp., Berlin .

Waggoner, B.M. 1996: Phylogenetic hypotheses of the relationshiops of arthropods to Precambrian and Cambrian problematic fossil taxa. Systematic Biology 45: 190-222.

Walcott, C.D. 1911: Cambrian geology and paleontology, II. 5. Middle Cambrian annelids. Smithsomian Miscellaneous Collections 57: 109-144.

Weber, H. 1954: Grundriss der Insektenkunde (3rd ed.) Fischer, Stuttgart: 1-428.


  Peripatus Home Page  pix1Black.gif (807 bytes)   Paleontology >> Onychophora

Hits counted from 10 Nov 2017:
My Traffic Estimate

Updated: 2020-06-05 19:30:38 gmt
FishBase | Search | All Living Things | Top
© Designed by The Polistes Corporation