Halwaxiida
Halwaxiida or halwaxiids is a proposed clade equivalent to the older orders Sachitida He 1980 and Thambetolepidea Jell 1981, loosely uniting scale-bearing Cambrian animals, which may lie in the stem group to molluscs or lophotrochozoa. Some palaeontologists question the validity of the Halwaxiida clade. Definition and members. The name "halwaxiid" was formed by combining the names of two members of the proposed group, "Halkieria" and "Wiwaxia". The group was defined as a set of Early to Mid Cambrian animals that had: a "chain mail" coat of three concentric bands of small armor plates that are called sclerites; in  some cases, a small cap-like shell at the front end and in some cases both ends. Some scientists are unhappy with this loose definition, arguing that such traits may have arisen convergently rather than being inherited from a common ancestor. This objection implies that the group may not be monophyletic, and that their similarities are not biologically equivalent but evolved separately. In fact the originators of the term "halwaxiid" prefer an evolutionary "family tree" in which the halwaxiids are not monophyletic. The possibility of convergence is reinforced by the presence of a scleritome in a derived gastropod mollusc. Other  fossil organisms became involved in the debate as there were plausible arguments for considering them closely related to the halkieriids or "Wiwaxia" or both. "Orthrozanclus", first described in 2007, looked an intermediate between the halkieriids and "Wiwaxia" as it had a shell like that of halkieriids, and unmineralized sclerites and long spines like those of "Wiwaxia" – in fact the article which first described "Orthrozanclus" introduced the term "halwaxiid". New finds of "Odontogriphus", reported in 2006, put this animal into play as well – despite its lack of sclerites or shells, its feeding apparatus looks very like "Wiwaxia"’s. The siphogonuchitids, a  very Early Cambrian group known only from isolated sclerites among the small shelly fossils, also appear in analyses as their sclerites suggest this group may have been close to the ancestors of halkieriids. Ecology. Halwaxiid sclerites were not able to grow once they had been formed, but must rather have been either moulted or resorbed to make way for new, larger sclerites; the smallest "Wiwaxia" specimens, 3.4 mm in length, appear to bear the same number of sclerites (minus the spines) as adults 5 cm long. The new sclerites cannot simply have poked between existing sclerites; rather they must  have been shed or resorbed, either one at a time or all at once; presumably the latter, as the close-fitting nature of the armour does not seem compatible with the easy loss of individual sclerites. Suggested phylogenies. Since 1995 several phylogenies, or evolutionary "family trees", have been suggested for these organisms. The position of "Wiwaxia" is highlighted, since the position of this organism has been central to the debate since 1990. Not depicted: Sun et al. (2018) propose "Halkieria" as a stem brachiopod, and Wiwaxia as a stem mollusc. Decline. Wiwaxia and Halkieria did not thrive for a long  period of time and were extinct before the Cambrian was over. A possible reason for this is that during the Cambrian substrate revolution, the microbial mat's disappearance triggered an alternating pattern in the fauna that were present for the Halwaxiids to eat. Section::::"Wiwaxia" and "Odontogriphus". Ever since the debate started in 1990, the most intense part has centered round "Wiwaxia". Until 2006 only one, poor-preserved fossil of "Odontogriphus" had been described; but in that year a description of many new, well-preserved specimens highlighted similarities between the two organisms, making the classification of "Odontogriphus" equally controversial. Conway Morris  (1985) originally dismissed the earliest classification of "Wiwaxia" as a polychaete worm, because he thought there was little structural similarity between a polychaete's scale-like elytra and "Wiwaxia"’s sclerites, and because the arrangement of the sclerites, with quite different numbers in each band, showed no sign of the regular segmentation that is a feature of polychaetes. Instead he thought "Wiwaxia" was very similar to shell-less aplacophoran molluscs, that it must have moved on a mollusc-like muscular foot, and that its feeding apparatus looked like a primitive form of the molluscan radula, a tooth-bearing chitinous "tongue . Hence he classified it as a sister" of the molluscs. When he briefly described the first articulated specimens of "Halkieria" in 1990, Conway Morris wrote of "the halkieriid-wiwaxiid body plan" and that the halkieriids might be close relatives of molluscs. Shortly after this in 1990 Butterfield published his first paper on "Wiwaxia". He argued that, since "Wiwaxia"’s sclerites appeared to be solid, they were not similar to the hollow sclerites of halkieriids. In fact he thought they were more similar to the chitinous bristles (setae) that project from the bodies of modern annelids and in some genera form  leaf-like scales that cover the back like roof tiles - in composition, in detailed structure, in how they were attached to the body via follicle-like pockets in the skin, and in overall appearance. He also contended that Wiwaxia’s feeding apparatus, instead of being mounted in the middle of its "head", was just as likely to be mounted in two parts on the sides of the "head", an arrangement that is common in polychaetes. He therefore classified "Wiwaxia" as a polychaete. Conway Morris and Peel (1995) largely accepted Butterfield's arguments and treated "Wiwaxia" as an ancestor or "aunt  of the polychaetes. However they also argued that Wiwaxia was fairly closely related to and in fact descended from the halkieriids, as the sclerites are divided into similar groups, although those of halkieriids were much smaller, more numerous and hollow. They wrote that in 1994 Butterfield had found Wiwaxia" sclerites that were clearly hollow. They noted that one specimen of Wiwaxia showed traces of a small shell, possibly a vestige left over from an earlier stage in the animal's evolution, and noted that one group of modern polychaetes also has what may be a vestigial shell. However they maintained  that Wiwaxia’s feeding apparatus was much more like a molluscan radula. The cladogram they presented showed the halkieriids split into three groups: one as "aunts" of brachiopods, animals whose modern forms have bivalve shells but differ from molluscs in having muscular stalks and a distinctive feeding apparatus, the lophophore; the second group of halkieriids as "aunts" of both "Wiwaxia" and annelid worms; and the earliest halkieriids as "great aunts" of all of these. Marine biologist Amélie H. Scheltema "et al." (2003) argued that "Wiwaxia"’s feeding apparatus was very similar to the radulas of some modern shell-less aplacophoran  molluscs, and that the sclerites of the two groups are very similar. They concluded that "Wiwaxia" was a member of a clade that includes molluscs. Danish zoologist Danny Eibye-Jacobsen (2004) regarded bristles as a feature shared by molluscs, annelids and brachiopods. Hence even if "Wiwaxia"’s sclerites closely resembled bristles, which he doubted, this would not prove that "Wiwaxia"’s closest relative were annelids. He also pointed out that the very different numbers of sclerites in the various zones of "Wiwaxia"’s body do not correspond to any reasonable pattern of segmentation. Since in his opinion "Wiwaxia" lacked other  clearly polychaete features, he regarded this as an argument against classifying "Wiwaxia" as a polychaete. In his opinion there were no strong grounds for classifying "Wiwaxia" as a proto-annelid or a proto-mollusc, although he thought the objections against classification as a proto-annelid were the stronger. Caron, Scheltema "et al." (2006) interpreted "Odontogriphus"’s feeding apparatus as a forerunner of the molluscan radula, on the grounds that: the occasional and less distinct third tooth-row looked like evidence that the animals grew replacement tooth-rows at the rear of their mouths and shed worn-out ones from the  front, as happens with molluscan radulae; the isolated pairs of tooth-rows they found, not associated with body fossils but in the same relative positions as in the more complete fossils, suggested they were mounted on a fairly tough surface, like the chitinous "belt" of a modern radula; they even found signs that discarded tooth-rows were sometimes eaten by the animals. They thought the teeth on the feeding apparatus of both "Wiwaxia" and "Odontogriphus" strongly resembled those of a modern group of molluscs, Neomeniomorpha. On the other hand, they thought "Wiwaxia" bore little resemblance to polychaetes as it showed  no signs of segmentation, appendages in front of the mouth, or "legs" – all of which are typical polychaete features. Hence they classified both "Odontogriphus", and "Wiwaxia" with its "nearly identical" feeding apparatus, as primitive relatives of molluscs. Butterfield (2006) accepted that "Wiwaxia" and "Odontogriphus" were closely related but wrote, "…it certainly does not require that they be shoehorned into the same lineage. …the seemingly trivial distinction between these two taxa is exactly what is expected at the divergence points leading from a last common ancestor to extant phyla." In his opinion the feeding apparatus of these organisms, with consisted of  two or at most four rows of teeth, could not perform the functions of the "belt-like" molluscan radula with its numerous tooth-rows; the different tooth-rows in both "Wiwaxia" and "Odontogriphus" tooth-rows also have noticeably different shapes, while those of molluscan radulae are produced one after the other by the same group of "factory" cells and therefore are almost identical. He also regarded lines running across the middle region of "Odontogriphus" fossils as evidence of external segmentation, since the lines are evenly spaced and run exactly at right angles to the long axis of the body. As  in his earlier papers, Butterfield emphasized the similarities of internal structure between "Wiwaxia"’s sclerites and the bristles of polychaetes, and the fact that polychates are the only modern organisms in which some of the bristles form a covering over the back. He therefore concluded that both "Wiwaxia" and "Odontogriphus" were stem-group polychaetes rather than stem-group molluscs. In 2007 Conway Morris and Caron described a new fossil, "Orthrozanclus", which had a mineralized shell like that of halkieriids, and unmineralized sclerites and long spines like those of "Wiwaxia" – and, like both of these, a soft underside which they interpreted  as a muscular foot, and a similar arrangement of the sclerites into three concentric bands. Some of "Orthrozanclus"’s sclerites appear to have been hollow, as the specimen includes what look like internal castings. They took these features as evidence that the halkieriids, "Wiwaxia" and "Orthrozanclus" were very closely related and formed the group "halwaxiids". However the simplest "family tree" faces an obstacle: the siphogonuchitids appear in earlier rocks and had "mineralized" sclerites. Hence Conway Morris and Caron found it necessary to consider two more complex family trees, concluding that "Hypothesis 1" fitted the available data better, but was sensitive  to minor changes in the characteristics used: In 2008 Butterfield described a set of micro-fossils dated to between and , found in the Mahto Formation in Alberta's Jasper National Park – this fossil bed is 5 – 10 M years older than the Burgess Shale in which the only known specimens of "Odontogriphus" and "Wiwaxia" were found. Some groupings of these micro-fossils showed a consistent arrangement that he interpreted as an "articulated apparatus" with tens of closely spaced tooth rows, apparently mounted on an organic base, and with noticeable signs of wear in the rows at one end. The rows  were not quite identical, but he noted that some modern aplacophoran molluscs show similar variations. He concluded that the "articulated apparatus" was a genuine molluscan radula, most similar to those of modern aplacophorans or gastropods. He then commented on the contrast between this apparatus and the two or rarely three widely spaced and more heterogeneous tooth-rows found in fossils of "Odontogriphus" and "Wiwaxia", and concluded that "Odontogriphus" and "Wiwaxia" were unlikely to be molluscs. He also noted that "Wiwaxia" lacked some polychaete features which he would expect to be easily preserved in fossils, and therefore classified "Wiwaxia" as a  stem-group annelid, in other words an evolutionary "aunt" of modern annelids. Recent finds indicate that "Orthrozanclus" is likely a halkieriid, but has little affinity to Wiwaxia. Halkieriids and siphogonuchitids. Most of the debate has been about halkieriids' relationship to molluscs, annelids and brachiopods. However a paper published in 2008 argued that halkieriids were closely related to chancelloriids, which have been generally regarded as sponges. Relationship to Molluscs, Annelids and Brachiopods. Halkieriid sclerites were known for a long time as elements of the small shelly fossils. The first articulated specimen, with all their hard parts together, were collected in 1989  and were described briefly in 1990 by Conway Morris and Peel (1990). The same authors produced a more detailed analysis in 1995, which divided the halkieriids into three groups: one as "aunts" of brachiopods, animals whose modern forms have bivalve shells but differ from molluscs in having muscular stalks and a distinctive feeding apparatus, the lophophore; the second group of halkieriids as "aunts" of both "Wiwaxia" and annelid worms; and the earliest halkieriids as "great aunts" of all of these. In 2003 Cohen, Holmer and Luter supported the halkieriid-brachiopod relationship, suggesting that brachiopods may have arisen from a halkieriid  lineage that developed a shorter body and larger shells, and then folded itself and finally grew a stalk out of what used to be the back. Vinther and Nielsen (2005) proposed instead that "Halkieria" was a crown group mollusc, in other words more similar to modern molluscs that to annelids, brachiopods or any intermediate groups. They argued that: "Halkieria"’s sclerites resembled those of the modern solenogaster aplacophoran shell-less molluscs (see ), of some modern polyplacophoran molluscs, which have several shell plates, and of the Ordovician polyplacophoran "Echinochiton"; "Halkieria"’s shells are more similar to the shells of conchiferan molluscs , since shells of both of these groups show no trace of the canals and pores seen in polyplacophoran shell plates; the bristles of brachiopods and annelids are similar to each other but not to "Halkieria"’s sclerites. However Conway Morris (2006) criticized Vinther and Nielsen's classification of "Halkieria" as a crown group mollusc, on the grounds that the growth of the spicules in the aplacophorans and polyplacophorans is not similar to the method of growth deduced for the complex halkieriid sclerites; in particular, he said, the hollow spines of various molluscs are not at all like the halkieriid sclerites  with their complex internal channels. Conway Morris repeated his earlier conclusion that halkieriids were close to the ancestors of both molluscs and brachiopods. In their description of the newly discovered "Orthrozanclus" (2007), which has similarities to both "Wiwaxia" and the halkieriids, Conway Morris and Caron also took account of the siphogonuchitids, a group known only from isolated mineralized sclerites that resemble those of the halkieriids. They proposed the two "family trees" described above: Relationship to chancelloriids. Porter (2008) revived an early 1980s idea that the sclerites of "Halkieria" are extremely similar to those of chancelloriids. These were sessile, bag-like , radially symmetric organisms with an opening at the top. Since their fossils show no signs of a gut or other organs, chancelloriids were originally classified as some kind of sponge. Butterfield and Nicholas (1996) argued that they were closely related to sponges on the grounds that the detailed structure of chancellorid sclerites is similar to that of fibers of spongin, a collagen protein, in modern keratose (horny) demosponges. However Janussen, Steiner and Zhu (2002) denied that chancellorids were sponges on the grounds that: chancellorids' hollow sclerites, probably made of aragonite, were quite different from the solid, silica-based spines of  demosponges; sponges have simple skins that are only one cell thick, while chancellorids' thicker, more complex skins resemble those of more complex animals. In their opinion chancellorids were at least members of the Epitheliazoa, a grade more complex than the Porifera, to which sponges belong. Porter (2008) found that the sclerites of halkieriids and chancelloriids resemble each other at all levels: both have an internal "pulp cavity" and a thin external organic layer; the walls are made of the same material, aragonite; the arrangement of the aragonite fibers is in each is the same, running mainly from base to tip  but with each being closer to the surface at the end nearest the tip. It is extremely improbable that totally unrelated organisms could have developed such similar sclerites independently, but the huge difference in the structures of their bodies makes it hard to see how they could be closely related. This dilemma may be resolved in various ways: