- For a type of cell projection see Pseudopod.
| Lobopodia Fossil range: Early Cambrian–Silurian |
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Lobopodia is a group of poorly understood animals, which mostly fall as a stem group of arthropods. Their fossil range dates back to the Early Cambrian. Lobopods are segmented and typically bear legs with hooked claws on their ends.[1]
The oldest near-complete fossil lobopods date to the Lower Cambrian; some are also known from Silurian lagerstatte.[2] They resemble the modern onychophorans (velvet worms) in their worm-like body shape and numerous stub-legs. They differ in their possession of numerous dorsal armour plates, "sclerita", which often cover the entire body and head. Since they taper off into long, pointed spikes, these probably served a role in defence against predators[citation needed]. Individual sclerita are found among the so-called "small shelly fauna" (SSF) from the early Cambrian period.[1] The "lobopodia" group is considered to include these Cambrian forms in addition to the extant onychophorans.
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Representative taxa
The better-known genera include, for example, Aysheaia, which was discovered among the Canadian Burgess Shale and which is the most similar of the Lobopoda in appearance to the modern velvet worms; a pair of appendages on the head have been considered precursors of today's antennae.[citation needed] Xenusion was apparently able to roll itself up, spines outward, giving insight into the defensive strategies of the Lobopoda. However, by far the most famous[citation needed] of the lobopod genera is Hallucigenia, named on account of its bizarre appearance. It was originally reconstructed by with long, stilt-like legs and mysterious fleshy dorsal protuberances, and was long considered a prime example of the way in which nature experimented with the most diverse and bizarre body designs during the Cambrian.[3] However, further discoveries showed that this reconstruction had placed the animal upside-down: interpreting the "stilts" as dorsal spines made it clear that the fleshy "dorsal" protuberances were actually legs. This second reconstruction also exchanged the front and rear ends of the creature, which further investigation showed to be erroneous.[4]
Morphology
Most lobopods are in the order of inches in length. They are annulated, although the annulation may be difficult to discern on account of their close spacing (~0.2mm) and low relief.[5] Lobopodia and their legs are circular in cross-section.[5] Their legs, technically called lobopods, are loosely conical in shape, tapering from the body to their clawed tips.[5] The longest and most robust legs are at the middle of the trunk, with those nearer the head and tail more spindly.[5] The claws are slightly curved. Their length is loosely proportional to the length of the leg to which they are attached.[5] The eyes are similar to those of modern arthropods as has been shown in Miraluolishania haikouensis (Liu et al., 2004).
Their gut is a straight, undifferentiated tube, which in some fossils is found to be filled with sediment.[5] The gut of the representative Paucipodia is variable in width, being widest towards the centre of the body. Its position in the body cavity is only loosely fixed, and flexibility is possible.
Ecology
The way of life of the Cambrian Lobopoda is to a large extent unknown; some species were apparently carnivorous, feeding on other animals such as, for example, sponges (Porifera) or sea cucumbers (Holothuroidea) of the genus Eldonia.
Diversity
During the Cambrian lobopods displayed a substantial degree of biodiversity. However, only one species is known from each of the Ordovician and Silurian periods,[6][7] with a few more known from the Carboniferous (Mazon Creek).
Phylogeny
The lobopods are closely related to the arthropods; indeed, the arthropods may well have arisen from within the lobopods. They are less closely related to the tardigrades; precise classification is still in flux.[1]
See also
The name Lobopodia is also used for lobose pseudopods, found among certain amoeboids.
References
- ^ a b c Liu (2007). "Origin, diversification, and relationships of Cambrian lobopods". Gondwana Research 14: 277. doi:.
- ^ 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: 879. doi:.
- ^ Gould, S.J. (1989). Wonderful Life: The Burgess Shale and the Nature of History. W.W. Norton & Company.
- ^ Further information and references: See Hallucigenia
- ^ a b c d e f Hou, Xian-Guang (2004). "The lobopodian Paucipodia inermis from the Lower Cambrian Chengjiang fauna, Yunnan, China". Lethaia 37: 235. doi:.
- ^ doi:10.1111/j.1475-4983.2009.00860.x
This citation will be automatically completed in the next few minutes. You can jump the queue or expand by hand - ^ 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: 879. doi:.
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