Chasmataspidid

Chasmataspidids, sometime referred to as chasmataspids, are a group of extinct chelicerate arthropods that form the order Chasmataspidida. Chasmataspidids are probably related to horseshoe crabs (Xiphosura) and/or sea scorpions (Eurypterida), with more recent studies suggest that they form a clade (Dekatriata) with Eurypterida and Arachnida. Chasmataspidids are known sporadically in the fossil record through to the mid-Devonian, with possible evidence suggesting that they were also present during the late Cambrian. Chasmataspidids are most easily recognised by having an opisthosoma divided into a wide forepart (preabdomen) and a narrow hindpart (postabdomen) each comprising 4 and 9 segments respectively. There is some debate about whether they form a natural (i.e. monophyletic) group.

Distribution

Chasmataspidids survived at least since Ordovician to mid-Devonian in age. As of 2019, most chasmataspidids (with a total of 9 species) are known from the Devonian strata, while the preceding Silurian and Ordovician period each have 3 and 2 species being described. '' Diploaspis'' is the only genus of chasmataspidids that unambiguously comprises species from different periods (D. ''casteri'' and ''D. muelleri'' from Devonian and ''D. praecursor'' from silurian). There was also trace fossil compose of resting imprints with ''Chasmataspis-''like outline discovered from late-Cambrian stratum, which might suggest an earlier occurrence of chasmataspidids.

Morphology

Most chasmataspidids are small arthropods with body length did not exceed 3 centimeters, with the ordovician species being exceptionally large, ranging between 10 (''Chasmataspis'') and 29 centimeters (''Hoplitaspis'').

File:20210202 Chasmataspidida size comparison.png, Size comparison of various chasmataspidids.
File:20200919 Chasmataspidida dorsal.png, Dorsal morphology of a generalized chasmataspidid.

The streamlined body of chasmataspidid compose of a rigid prosoma and an externally 13-segmented opisthosoma. Like eurypterid, dorsal side of the prosoma was covered by a rigid carapace (prosomal dorsal shield) that bore a pair of larger lateral (presumably compound) eyes and a pair of tiny median ocelli. Chasmataspidid readily distinguish from other chelicerates by the subdivision of the 13 opisthosomal segments into a widen, 4-segmented preabdomen and a slender, 9-segmented postabdomen. the tergite (dorsal exoskeleton) of the first opisthosomal/preabdomimal segment retain as a narrow element known as 'microtergite', which is not observable in eurypterid. The posterior three preabdominal segments are well developed, forming a rigid box-like section called 'buckler'. The postabdominal segments are cylindrical and the last segment terminated with a spine/plate-like telson, which is usually relatively short.

Appendages

File:Hoplitaspis hiawathai life restoration.png, Reconstruction of ''Hoplitaspis hiawathai'' with ventral view (B) showing appendicular structures.
File:Eurypterid and chasmataspidid sixth appendage comparison.png, Comparison of appendage VI between chasmataspidids (left) and eurypterids (right).

Since the appendages of chasmataspidid are rarely preserved in the fossil, most species have only fragile or even no appendicular structures had been described. Based on available materials, the prosoma compose of 6 appendage pairs (appendage I - VI) just like most euchelicerates, which were 1 pair of small chelicerae and 5 pairs of limb-like appendages, although the detail morphology of the former is still unclear. The coxae (basalmost limb segments) of appendage II-VI bore gnathobases. At least the posteriormost appendage pair (appendage VI) of prosoma seems to be differ between families. Appendage of Chasmataspididae known only from 2 disarticulated specimens of appendages which interpreted as appendage VI of ''Chasmataspis''. the appendage bore exopod-like structure on the base and terminated with a chelate (pincer), similar to those of a xiphosuran. On the other hand, Appendage VI modified into a paddle that strikingly resemble to those of an eurypterine (swimming eurypterid) was discovered in some species of Diploaspididae, but the basal diploaspidid '' Loganamaraspis'' possibly did not possess this character on Appendage VI. the limb-like appendage II-V of diploaspidids are either featureless or bore rows of spines.

Opisthosomal appendages are even rarely being observed and only known from a few diploaspidid materials. they are at least present on the ventral side of preabdomen, each pair originated from one preabdominal segment. the anteriormost appendicular structure of opisthosoma was metastoma, a plate-like structure interpreted as a fused appendage pair of first opisthosomal segment, situated between the gnathobase of prosomal appendage VI. Beyond the metastoma were 3 pairs of plate-like opercula originated from the 3 buckler segments, with the first operculum pair (genital operculum) bore a medially positioned genital appendage that extend until the posterior region of second operculum pair. Some of the opercula may have book gills just like those of xiphosurans and eurypterids, but the evidence are equivocal. Previous reports of a large operculum cover the whole ventral surface of buckler are most likely an misinterpretation of the ventral buckler wall (sternites or dorsal surface of gill chamber), which were originally enclosed by the opercula in life. The metastoma, opercula and genital appendage are shared characters between chasmataspidid and eurypterid, but unlike the fused first and second operculum pair of eurypterid, the two operculum pairs seems to be unfused in chasmataspidid. Possible chasmataspidid trace fossil from cambrian have imprints resembling 6 pairs of opercula. If the interpretation is true, chasmataspidid may had extra 3 pairs of opercula on the first 3 postabdominal segment as well.

Representative genera

''Chasmataspis''

The first chasmataspidid to be discovered was ''Chasmataspis laurencii'', described by the American palaeontologists Kenneth E. Caster and H. K. Brooks in 1956. These Ordovician fossils come from the site of the Douglas Dam in Tennessee, USA. They are the most xiphosuran-like of the known chasmataspidid species, with a horseshoe-shaped carapace. Caster & Brooks raised a new family, Chasmataspididae, to accommodate these specimens. The species was redescribed by Jason Dunlop and colleagues in 2004.

''Diploaspis''

The next species to be discovered were '' Diploaspis casteri'' and ''Heteroaspis novojilovi''; both described by the Norwegian palaeontologist Leif Størmer from the early Devonian of Alken an der Mosel in Germany in 1972.

A revision by Markus Poschmann and co-workers in 2005 recognised ''H. novojilovi'' as a synonym of ''D. casteri''. The two species appear to actually be preservational variants of the same species. Poschmann ''et al.'' also described a second species as ''Diploaspis muelleri''.

A third species, ''Diploaspis praecursor'' (Late Silurian, Bertie Group, New York State), was described by Lamsdell and Briggs in 2017.

''Forfarella''

''Forfarella mitchelli'' from the early Devonian of the Forfar region in the Midland Valley of Scotland was described by Jason Dunlop and colleagues in 1999; although the fossil had actually been recognised as a chasmataspidid and provisionally labelled as such some years previously by Charles Waterston. ''Forfarella mitchelli'' is not very well preserved, but does show the characteristic chasmataspidid body plan.

''Achanarraspis''

The stratigraphically youngest chasmataspidid is '' Achanarraspis reedi'', described by Lyall Anderson and colleagues in 2000, from the mid-Devonian Achanarras quarry in Caithness, Scotland, a site rich in fish fossils.

''Octoberaspis''

Well preserved chasmataspidids were recovered from the early Devonian of October Revolution Island, part of the Severnaya Zemlya group in the Russian Arctic. Originally briefly described as eurypterids, they were formally described as '' Octoberaspis ushakovi'' by Jason Dunlop in 2002. ''Octoberaspis'' is one of the few chasmataspidids with well-documented opisthosomal appendages, reveal some characters previously though to be eurypterid-exclusive were also shared by chasmataspidid as well.

''Loganamaraspis''

'' Loganamaraspis dunlopi'' discovered from a famous Silurian fossil locality near Lesmahagow in Scotland. Described by Erik Tetlie and Simon Braddy in 2003, it was placed in Diploaspididae, but interpreted as being somewhat more intermediate in form between the ''Chasmataspis'' and Diploaspidid body plans.

''Dvulikiaspis''

Fossils of ''Dvulikiaspis menneri'' discovered from the Imangda River of Taymyr Peninsula were originally interpreted as a species of eurypterid genus ''Stylonurus'', and formally described as a new genus of chasmataspidid by David J. Marshall and co-authors in 2014. ''Dvulikiaspis menneri'' is one of the few well-preserved chasmataspidid, with distal morphology of appendage II-VI had been revealed.

''Hoplitaspis''

''Hoplitaspis hiawathai'' is the second known species of Ordovician chasmataspidid, discovered from the Big Hill Lagerstätte of Michigan in United States, described by James C. Lamsdell and co-authors in 2019. With nearly complete set of appendages being observable, ''Hoplitaspis hiawathai'' is the most complete chasmataspidid known at that time. Each of the paddle of ''Hoplitaspis hiawathai'' has a claw instead of an intersegmental element like those of other diploaspidids, providing clues on the relationship between the appendage VI of ''Chasmataspis'' and diploaspidids.

Classification

Phylogenetic position

Chasmataspidids have a controversial phylogenetic position within Chelicerata. The first species to be discovered were thought to be unusual fossil xiphosuran, while later species were often based on specimens initially misidentified as eurypterids. Chasmataspidids had been interpreted as relatives/members of either xiphosurans or eurypterids, or forming a clade (Dekatriata) with eurypterids and arachnids. Some studies even suggest that chasmataspidids may not represent a monophyletic taxon - for example as a paraphyletic grade where the eurypterids arose; or a polyphyletic group with ''Chasmataspis'' and diploaspidids more closely related to xiphosuans and eurypterids, respectively. The polyphyletic hypothesis was based on the xiphosuran-like characters of ''Chasmataspis'' (e.g. genal spines, chelate limbs, fused opisthosomal segments) and eurypterid-like characters found on diploaspidid genera (e.g. paddles on appendage VI). However this interpretation could be unreliable, as the characters are either partially shared by both xiphosuans and eurypterids (e.g. genal spines were be found in eurypterid juveniles; some xiphosurans have non-chelate limbs and unfused opisthosoma) or more likely represent a result of parallel evolution (e.g. the paddles of diploaspidids and swimming eurypterids have different component). Additionally, the monophyly of chasmataspidids could be supported by the unique component of 4-segmented preabdomen and 9-segmented postabdomen as well. As of 2010s, many studies supports the monophyly of Chasmataspidida and Dekatriata (Chasmataspidida+Eurypterida+Arachnida).

Interrelationships

As of 2019, up to 12 genera had been associated within Chasmataspidida. With the exception of '' Diploaspis'' which compose of 3 species since 2017, all chasmataspidid genera are monotypic. The order Chasmataspidida subdivided into two families: Chasmataspididae and Diploaspididae. the former consists of ''Chasmataspis'' (and possibly also '' Kiaeria'') while the latter include the remaining genera.Dunlop, J. A., Penney, D. & Jekel, D. 2018. A summary list of fossil spiders and their relatives. In World Spider Catalog. Natural History Museum Bern, online at http://wsc.nmbe.ch, version 18.5 http://www.wsc.nmbe.ch/resources/fossils/Fossils18.5.pdf (PDF). Chasmataspididae is defined by a horseshoe-shaped carapace with distinct genal spines and a completely fused preabdomen; while Diploaspididae is defined by a semicircular to subquadrate carapace and a preabdomen with curved, nontrilobate segments.

†Chasmataspidida Caster & Brooks, 1956
*†'' Kiaeria'' Størmer, 1934 (might belong to Chasmataspididae)
**†''Kiaeria limuloides'' Størmer, 1934—Silurian
*†Chasmataspididae Caster & Brooks, 1956
**†''Chasmataspis'' Caster & Brooks, 1956
***†''Chasmataspis laurencii'' Caster & Brooks, 1956—Ordovician
*† Diploaspididae Størmer, 1972
**†'' Achanarraspis'' Anderson, Dunlop & Trewin, 2000
***†''Achanarraspis reedi'' Anderson, Dunlop & Trewin, 2000—Devonian
**†'' Diploaspis'' Størmer, 1972
***†''Diploaspis casteri'' Størmer, 1972—Devonian
***†''Diploaspis muelleri'' Poschmann, Anderson & Dunlop, 2005—Devonian
***†''Diploaspis praecursor'' Selden, Lamsdell & Liu 2015—Silurian
**†''Dvulikiaspis'' Marshall, Lamsdell, Shpinev & Braddy, 2014
***†''Dvulikiaspis menneri'' (Novojilov, 1959) (formerly known as ''‘Tylopterella’ menneri'')—Devonian
**†''Forfarella'' Dunlop, Anderson & Braddy, 1999
***†''Forfarella mitchelli'' Dunlop, Anderson & Braddy, 1999—Devonian
**†'' Heteroaspis'' Størmer, 1972
***†''Heteroaspis stoermeri'' Størmer, 1972 (formerly known as ''‘Eurypterus’ stoermeri'')—Devonian
**†''Hoplitaspis'' Lamsdell, Gunderson & Meyer, 2019
***†''Hoplitaspis hiawathai'' Lamsdell, Gunderson & Meyer, 2019—Ordovician
**†'' Loganamaraspis'' Tetlie & Braddy, 2004
***†''Loganamaraspis dunlopi'' Tetlie & Braddy, 2004—Silurian
**†'' Nahlyostaspis'' Marshall, Lamsdell, Shpinev & Braddy, 2014
***†''Nahlyostaspis bergstroemi'' Marshall, Lamsdell, Shpinev & Braddy, 2014—Devonian
**†'' Octoberaspis'' Dunlop, 2002
***†''Octoberaspis ushakovi'' Dunlop, 2002—Devonian
**†'' Skrytyaspis'' Marshall, Lamsdell, Shpinev & Braddy, 2014
***†''Skrytyaspis andersoni'' Marshall, Lamsdell, Shpinev & Braddy, 2014—Devonian

References

{{Taxonbar, from=Q1068066

Prehistoric chelicerates
Chasmataspidida
Ordovician arthropods
Silurian arthropods
Devonian arthropods
Arthropod orders