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Belinurus Bronn, 1839 (Chelicerata, Xiphosura) has priority over Bellinurus Pictet, 1846

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Abstract

In the first half of the nineteenth century, a marked shift occurred in our understanding and treatment of the chelicerate fossil record, with the differentiation and recognition of entirely extinct genera for the first time. At the heart of this taxonomic revolution were the Eurypterida (sea scorpions) and Xiphosura (horseshoe crabs), although both groups were in fact considered crustaceans until Lankester's (1881) seminal comparative anatomical study of the extant xiphosuran Limulus Müller, 1785 and modern scorpions. The oldest available eurypterid genus is Eurypterus deKay, 1825; the oldest available fossil arachnid genus name is that of the scorpion Cyclophthalmus Corda, 1835. However, there has been considerable historical confusion over the oldest available fossil xiphosuran genus name, which has been recognized alternately as Belinurus König (with a publication date of either 1820 or 1851) or the synonymous Bellinurus Pictet, 1846. Most recent treatments (e.g., Selden and Siveter, 1987; Anderson and Selden, 1997; Anderson et al., 1997; Lamsdell, 2016, 2021; Bicknell and Pates, 2020) have favored Bellinurus Pictet, 1846 as the available name; however, Haug and Haug (2020) recently argued that Belinurus König, 1820 is valid and has priority, a position then followed by Lamsdell (2020), prompting a reinvestigation of the taxonomic history of the genus. Upon review, it is clear that neither of the previously recognized authorities for Belinurus are accurate and that the two candidate type species for each genus are, in fact, synonyms. Given the convoluted and at times almost illogical history of the competing names, along with the most recent controversy as to which has priority, we present a complete history of the treatment of the genus to resolve the issue.
Belinurus Bronn, 1839 (Chelicerata, Xiphosura) has priority over
Bellinurus Pictet, 1846
James C. Lamsdell1and Matthew E. Clapham2
1
Department of Geology and Geography, West Virginia University, Morgantown, West Virginia 26501, USA <james.lamsdell@mail.wvu.edu>
2
Department of Earth and Planetary Sciences, UC Santa Cruz, Santa Cruz, California 95064, USA <mclapham@ucsc.edu>
In the rst half of the nineteenth century, a marked shift occurred
in our understanding and treatment of the chelicerate fossil
record, with the differentiation and recognition of entirely
extinct genera for the rst time. At the heart of this taxonomic
revolution were the Eurypterida (sea scorpions) and Xiphosura
(horseshoe crabs), although both groups were in fact considered
crustaceans until Lankesters(1881) seminal comparative ana-
tomical study of the extant xiphosuran Limulus Müller, 1785
and modern scorpions. The oldest available eurypterid genus
is Eurypterus deKay, 1825; the oldest available fossil arachnid
genus name is that of the scorpion Cyclophthalmus Corda,
1835. However, there has been considerable historical confusion
over the oldest available fossil xiphosuran genus name, which
has been recognized alternately as Belinurus König (with a pub-
lication date of either 1820 or 1851) or the synonymous Belli-
nurus Pictet, 1846. Most recent treatments (e.g., Selden and
Siveter, 1987; Anderson and Selden, 1997; Anderson et al.,
1997; Lamsdell, 2016,2021; Bicknell and Pates, 2020)have
favored Bellinurus Pictet, 1846 as the available name; however,
Haug and Haug (2020) recently argued that Belinurus König,
1820 is valid and has priority, a position then followed by Lams-
dell (2020), prompting a reinvestigation of the taxonomic history
of the genus. Upon review, it is clear that neither of the previously
recognized authorities for Belinurus are accurate and that the two
candidate type species for each genus are, in fact, synonyms.
Given the convoluted and at times almost illogical history of
the competing names, along with the most recent controversy
as to which has priority, we present a complete history of the
treatment of the genus to resolve the issue.
The issue arises from the partial publication of Königs
(1825)Icones Fossilium Sectiles. This volume (Centuria
Prima) was bound and published, comprising one hundred
gures across eight plates with associated descriptions. Planned
further volumes of Icones Fossilium Sectiles beyond the rst
were never published (Urban, 1851); however, it is apparent
that a limited number of lithographs for the plates for the second
and third volumes were produced and shared by König among
interested parties (Woodward, 1830). Among these plates (g-
ure 230, on plate 18) was a single specimen of a small horseshoe
crab labeled simply Belinurus bellulus.
The informal proliferation of these plates created a scenario
in which the proposed name was widely known among research-
ers but explicitly recognized as unpublished (see Woodward,
1830) and presumably therefore unavailable. Buckland (1837),
in his contribution to the Bridgewater Treatise series, gured
and described a new horseshoe crab species as Limulus trilobi-
toides, explicitly stating that this new species was the same as
Königs unpublished Belinurus bellulus and Martins(1809)
Entomolithus Monoculites?Lunatus (a non-binomial name
that has been suppressed by the International Commission on
Zoological Nomenclature along with all other names within Pet-
ricata Derbiensia). Subsequently, Louis Agassiz, in his Ger-
man translation of Bucklands(1839)Bridgewater Treatise,
followed Bucklands description of Limulus trilobitoides with
a note that the genus Bellinurus König [sic] is deserving of rec-
ognition as a distinct genus from Limulus (pl. 46; it is worth not-
ing that this is the rst recorded occurrence of the alternative
Bellinurus spelling and that it follows an accurate transcription
of the spelling of Belinurus from Bucklands text on the same
page). In the same year, a summary list of fossil horseshoe
crabs appeared in the Neues Jahrbuch für Mineralogie, Geogno-
sie, Geologie und Petrefaktenkunde, which was edited by Karl
von Leonhard and Heinrich Bronn. The summary itself is not
attributed to either editor; however, the article stated that it
was done at the request of van der Hoeven. In turn, van der Hoe-
ven (1838) stated that he had been in contact with Bronn regard-
ing the status of the fossil xiphosuran species, and so Bronn
(1839) can be reliably ascribed as the author of the article. In
it, Bronn directly assigned the species Entomolithus Monocu-
lites? Lunatus Martin, 1809 (as Entomolites monoculites)
and Limulus trilobitoides Buckland to the genus Belinurus
König, with no reference to B. bellulus König. However, the
species reappeared in Morriss(1843)A Catalogue of British
Fossils, where it was listed as a synonym of Limulus trilobi-
toides Buckland.
Later, in his Traité élémentaire de paléontologie, Pictet
(1846) included the genus Bellinurus Königonce again mis-
spelledto which he assigned the species Limulus trilobitoides,
with the erroneous taxonomic authority of König (notably, there
was again no reference to B. bellulus König), although the
second edition listed B. bellulus König as a senior synonym of
Limulus trilobitoides (Pictet, 1854). Matters were further com-
plicated by Baily (1859ac), who in a series of papers utilized
the name Bellinurus König, recognizing B. bellulus König as
a synonym of B. trilobitoides (Buckland) and proposing the
genus Steropis to accommodate a variety of species, including
B. trilobitoides (Buckland). Baily (1863) later recognized Ster-
opis as a junior synonym of Belinurus König, 1820 (potentially
the year that the unpublished lithographs were rst made avail-
able), stating that Pictet (1846) had made the genus name
Journal of Paleontology, page 1 of 4
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original work is properly cited.
0022-3360/21/1937-2337
doi: 10.1017/jpa.2021.53
1
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available. Baily also here treated B. bellulus König, 1820 as a
valid and available species for the rst time and considered it
to have priority over B. trilobitoides (Buckland). Henry Wood-
ward, in his extensive works on British fossil chelicerates, was
inconsistent in his treatment of the genus, at rst attributing
Baily (1863) as the authority for Belinurus König with B. trilo-
bitoides (Buckland) as the type species (Woodward, 1867)
before later following Baily (1863) in recognizing Bellinurus
König, 1820 with B. bellulus König, 1820 as the valid type spe-
cies (Woodward, 1872,1907).
Moving into the twentieth century, there appeared to be a
consensus that Belinurus König, 1820 was the accurate name
and authority, with B. trilobitoides (Buckland) being a junior
synonym of the type species B. bellulus König (Dix and Pringle,
1929; Eller, 1938; Størmer, 1952). Uncertainties regarding the
taxonomic history of the species continued, however, with
Størmer (1952) erroneously listing Woodward (18661878)as
the taxonomic authority for B. bellulus. Størmer (1955) later
compounded this error in the Treatise on Invertebrate Paleon-
tology, which continued to recognize Belinurus König, 1820,
but incorrectly listing Meek and Worthen (1865) as the authority
of the junior synonym Bellinurus.
This situation changed dramatically with the publication of
Morriss(1980)Catalogue of the type and gured specimens of
fossil Crustacea (excl. Ostracoda), Chelicerata, Myriapoda and
Pycnogonida in the British Museum (Natural History). In it,
Morris reported that the second part of Königs work had
become available only after his death and that the earliest the
genus and species could date to is 1851. This would render Bel-
linurus, made available by Pictet in 1846, as having priority over
Belinurus König, c. 1851. Similarly, B. trilobitoides (Buckland,
1837) would have priority over B. bellulus König, c. 1851. The
next treatment of the group, by Selden and Siveter (1987), fol-
lowed Morris in recognizing Bellinurus Pictet as having priority
but considered B. bellulus König, c. 1851 the valid type species.
Subsequent workers all recognized Bellinurus Pictet, 1846 as
the appropriate taxon name and authority (Schultka, 1994;
Anderson and Selden, 1997; Anderson et al., 1997; Lamsdell,
2016,2021; Bicknell and Pates, 2020). Very few of these treat-
ments considered the issue of the appropriate type species,
although Bicknell and Pates (2020) listed both B. bellulus
(ascribed to Pictet, 1846) and B. trilobitoides (Buckland) as dis-
tinct, valid species. Then Haug and Haug (2020) argued on the
basis of an available scan of Icones Fossilium Sectiles from the
Biodiversity Heritage Library that Königs plates were pub-
lished in 1820 and that Belinurus König had priority over Belli-
nurus Pictet, which Lamsdell (2020) then followed in a
comprehensive revision of xiphosurid taxonomy.
With such a turbulent taxonomic history, the question
remains: what is the correct formulation of the genus name,
and what is the correct taxonomic authority? To determine
this, it must rst be ascertained whether the plates for Königs
second volume were published before 1851, or if not, which
publication rst made Belinurus available and whether it pre-
or post-dated Pictets making Bellinurus available in 1846.
With regard to the publication of Königs plates, all contempor-
ary sources (Woodward, 1830; Urban, 1851) are clear in stating
that the later volumes of Icones Fossilium Sectiles were not pub-
lished and the plates were not publicly available. The fact that
the plates for the second and third volumes were distributed
and appended to bindings of the rst volume after Königs
death, as stated by Sherborn (1902) and Lang et al. (1940),
explains the undated binding from the Natural History Museum,
London, that led Haug and Haug (2020) to believe that these
plates were published before 1851. The matter then becomes
when Belinurus and Bellinurus each rst became available.
Although Buckland (1837) stated his Limulus trilobitoides is
the same as KönigsBelinurus bellulus, he did so with reference
to the unpublished plates and so did not make the genus or spe-
cies available as per Article 12.3 of the International Code of
Zoological Nomenclature (International Commission on Zoo-
logical Nomenclature, 1999). Similarly, Agassizs note in his
translation of Buckland (1839) was the rst reference to Belli-
nurus in the literature but did not include an assignation of an
available species name and so did not make that spelling of
the genus available. However, Bronns(1839) summary of fossil
horseshoe crabs explicitly listed Belinurus König as a valid
genus including the valid species Limulus trilobitoides Buck-
land by indication. This satises Article 12.2.5 of the Inter-
national Code of Zoological Nomenclature (International
Commission on Zoological Nomenclature, 1999) and is suf-
cient for the genus name to become available, whereby its taxo-
nomic authority is Bronn (1839) following Article 50.1
(International Commission on Zoological Nomenclature,
1999). Bellinurus was rst made available by Pictet, and so
Belinurus Bronn, 1839 is the valid senior synonym of Bellinurus
Pictet, 1846. Pictet, however, made no reference to B. bellulus,
which Morris (1980) stated was rst made available by the dis-
tribution of Königs plates in or after 1851. If the plates were dis-
tributed after 1854, B. bellulus would be attributable to Pictet
(1854), who gured a specimen alongside a diagnosis of the
species. Irrespective as to whether the species was made avail-
able in 1851 or 1854, as B. trilobitoides (Buckland, 1839) and
B. bellulus König, c. 1851/Pictet, 1854 are subjective synonyms,
B. trilobitoides has seniority and is the valid name.
To clarify these issues for future paleontologists, we present
a revised systematic paleontology for Belinurus Bronn, 1839,
including all currently valid species assignable to the genus.
Systematic paleontology
Xiphosurida Latreille, 1802
Belinurina von Zittel in von Zittel and Eastman, 1913
Family Belinuridae von Zittel in von Zittel and Eastman, 1913
(= Euproopidae Eller, 1938; = Liomesaspidae Raymond, 1944)
Genus Belinurus Bronn, 1839
(= Bellinurus Pictet, 1846;=Steropis Baily, 1859a)
Type species.Belinurus trilobitoides (Buckland, 1837)
(lectotype: BNMH 34889; paralectotype: BMNH 46393)
(= Belinurus bellulus König, c. 1851/Pictet, 1854) from the
clay-ironstone of the Coalbrookdale Coal Measures, Telford,
Shropshire, by subsequent designation.
Other species.Belinurus carwayensis Dix and Pringle, 1929;
Belinurus concinnus Dix and Pringle, 1929;Belinurus
grandaevus Jones and Woodward, 1899;Belinurus
kiltorkensis Baily, 1869;Belinurus morgani Dix and Pringle,
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1930;Belinurus pustulosus Dix and Pringle, 1929;Belinurus
silesiacus (Roemer, 1883); Belinurus sustai (Prantl and Pr
̌ibyl,
1956); Belinurus trechmanni Woodward, 1918.
Diagnosis.Belinurid with axis of rst thoracetron tergite
medially inated; thoracetron ovoid to semicircular in outline;
thoracetron xed tergopleural spines elongate, needle-like
(after Lamsdell, 2020).
Occurrence.Carboniferous: Canada, Czech Republic,
Germany, and United Kingdom.
Remarks.Morris (1980) listed two syntypes for Belinurus
trilobitoides, one gured by Buckland (1837) and the other
not. No lectotype has been subsequently designated, and so
here we select Bucklandsgured specimen, BMNH 34889,
as the lectotype for the species following Article 74.1 of the
International Code of Zoological Nomenclature (International
Commission on Zoological Nomenclature, 1999). According
to Morris, this is also the specimen gured by König (c.
1851). There is no indication as to the identity of the
specimen gured by Pictet (1854).
Acknowledgments
JCL thanks A. Baumgartner and D. Lamsdell for reading
through an early draft of the manuscript and helping ensure
the convoluted taxonomic history was presented in an under-
standable format. We thank R. Plotnick and C. Haug for their
reviews of the manuscript.
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Accepted: 21 June 2021
Journal of Paleontology:144
https://doi.org/10.1017/jpa.2021.53
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... Phylogenetic analysis of Xiphosura was conducted on the basis of a modified matrix derived from Lamsdell (2021a), which is itself an evolution of the matrices presented in Lamsdell (2013Lamsdell ( , 2020, Lamsdell and McKenzie (2015), Selden et al. (2015), and . Five taxa (Belinurus lunatus [Baldwin, 1905], Belinurus arcuatus [Baily, 1859], Belinurus reginae Baily, 1863, Belinurus truemanii [Dix and Pringle, 1929], and Belinurus bellulus König, 1851) were removed from the analysis as they have been shown to represent synonyms of Belinurus trilobitoides (Lamsdell and Clapham, 2021;Lamsdell, 2022). The outgroup taxa included in the analysis were also revised on the basis of recent reinterpretations of a variety of Cambrian taxa as putative stem chelicerates Caron, 2017, 2019); as such, Fuxianhuia protensa Hou, 1987, Leanchoilia illecebrosa Hou, 1987, Alalcomenaeus cambricus Simonetta, 1970, Emeraldella brocki Walcott, 1912, Sydneyia inexpectans Walcott, 1911, and Olenoides serratus (Rominger, 1887) were removed from the matrix, with Yohoia tenuis Walcott, 1912 retained as the new outgroup taxon and Sanctacaris uncata Collins, 1988, Habelia optata Walcott, 1912, and Mollisonia plenovenatrix Aria and Caron, 2019 included to aid in resolving character polarity at the base of Xiphosura. ...
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Xiphosuran chelicerates, also known as horseshoe crabs, are a long-lived clade characterized by a highly distinctive morphology and are a classic example of supposed evolutionary stasis. One key feature of horseshoe crabs is the fusion of the opisthosomal segments into a single sclerite referred to as a thoracetron. There has been historical uncertainty as to whether the thoracetron originated once or multiple times within the clade. Here we review criteria for determining whether segments are fused and apply them to a broad census of taxa for which their ontogeny is known or the adult status of specimens can be reasonably asserted to explore the evolution of the thoracetron within a developmental framework. Our findings indicate that the thoracetron evolved once in the common ancestor to Xiphosura. However, subsequent independent loss of the thoracetron segment boundaries is identified and shown to be the result of heterochronic processes acting on a shared developmental pathway. The multiple cases of effacement of the thoracetron within Limuloidea are cases of peramorphically driven parallelism, while the effacement of the thoracetron in the pedomorphic Belinurina is a case of convergence. Xiphosurids therefore represent an interesting case study for recognizing parallelism and convergence on the same structure within closely related lineages. We also demonstrate that somite VII has been incorporated into the prosoma multiple times within the chelicerate lineage, which has implications for interpreting the ground pattern of the group.
... Including multiple ontogenetic stages of the same species within a phylogenetic analysis can lead to unstable tree topologies, with the species in question resolving in disparate positions across the tree rather than as a clade (Lamsdell and Selden, 2013), which may have implications for interpreting heterochronic trends within lineages if juveniles are incorrectly interpreted as adults (Lamsdell and Selden, 2013;Sharma et al., 2017). In total 14 speciesof which five (Belinurus bellulus, Koenigiella truemanii, Koenigiella reginae, Macrobelinurus arcuatus, and Parabelinurus lunatus) were included in the initial analysiscan be synonymized with the species Belinurus trilobitoides (Lamsdell and Clapham, 2021;Lamsdell, 2021c). This includes the type species of the genera Koenigiella, Macrobelinurus, and Parabelinurus, all three of which are subsumed within Belinurus. ...
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Much of the focus of palaeobiological studies in the last century can be summarized as seeking to understand how evolutionary lineages occupy new regions of morphological, ecological, and geographic space, or are excluded from those spaces. A desire to understand the processes that lead to morphological change unites a variety of biological disciplines focusing on topics ranging from studies of organism genomics to broad scale macroevolutionary analyses. There is increasing recognition that a hierarchical approach, incorporating both intrinsic genealogical processes and external ecological factors, is necessary to understand the mechanisms behind the drivers of phenotypic change. One of the most important issues that remains to be resolved regards the generation and fixation of morphological changes within evolutionary lineages, including whether the evolution of novel morphologies facilitates expansion to previously unoccupied environments (a developmental push mechanism) or whether a shift in ecological occupation results in subsequent morphologic change (an ecological pull mechanism). The geological record affords a unique perspective on morphological change, preserving both evidence of environmental change through shifts in sedimentology and the changing morphology of evolutionary lineages; as such, palaeontology provides a long-term view of the relationship between ecological and morphological shifts. This review focuses on the ways that phylogenetic palaeoecology, which utilizes phylogenetic frameworks in concert with palaeoecological data, can be leveraged to explore these questions. It begins by reviewing the literature on novelty and innovation – the origination of new morphologies and their proliferation within ecosystems – within a hierarchical framework and the role of heterochrony as the primary mechanism by which phenotypic change occurs before exploring evidence for developmental push and ecological pull as competing drivers of morphological shifts. Drivers of morphological shifts are examined through analysis of heterochronic trends in horseshoe crab evolution and comparison with case studies on angiosperm plants, giant ground sloths, and megatooth sharks.
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One of the oldest fossil horseshoe crabs figured in the literature is Entomolithus lunatus Martin, 1809, a Carboniferous species included in his Petrificata Derbiensia . While the species has generally been included within the genus Belinurus Bronn, 1839, it was recently used as the type species of the new genus Parabelinurus Lamsdell, 2020. However, recent investigation as to the appropriate authority for Belinurus (see Lamsdell and Clapham, 2021) revealed that all the names in Petrificata Derbiensia were suppressed in Opinion 231 of the International Commission on Zoological Nomenclature (1954) for being consistently nonbinomial under Article 11.4 of the International Code of Zoological Nomenclature (ICZN) (International Commission on Zoological Nomenclature, 1999). Despite the validation of several species names for anthozoans, brachiopods, and cephalopods described in Petrificata Derbiensia in subsequent rulings (International Commission on Zoological Nomenclature, 1956a, b), Belinurus lunatus has not been the subject of any subsequent Commission ruling or opinion, and so its use in Petrificata Derbiensia remains suppressed. The Belinurus lunatus species name was used in several subsequent publications during the 1800s, none of which made the name available under ICZN article 11.5; Parkinson (1811) is also suppressed for being nonbinomial, while Woodward (1830), Buckland (1837), Bronn (1839), and Baily (1859) refer to the species only as a synonym of Belinurus trilobitoides (Buckland, 1837) through citation to the suppressed Pretificata Derbiensia . The first author to make Belinurus lunatus an available name was Baldwin (1905), who used the name in reference to a new figured specimen from Sparth Bottoms, Rochdale, UK, but again as an explicit junior synonym of Belinurus trilobitoides (Buckland, 1837). Therefore, it was not until Eller (1938) treated B. lunatus as a distinct species from B. trilobitoides that B. lunatus became an available name as per ICZN Article 11.6.1 under the authorship of Baldwin (1905) following ICZN Article 50.7.
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Xiphosurans are aquatic chelicerates with a fossil record extending into the Early Ordovician and known from a total of 88 described species, four of which are extant. Known for their apparent morphological conservatism, for which they have gained notoriety as supposed ‘living fossils’, recent analyses have demonstrated xiphosurans to have an ecologically diverse evolutionary history, with several groups moving into non-marine environments and developing morphologies markedly different from those of the modern species. The combination of their long evolutionary and complex ecological history along with their paradoxical patterns of morphological stasis in some clades and experimentation among others has resulted in Xiphosura being of particular interest for macroevolutionary study. Phylogenetic analyses have shown the current taxonomic framework for Xiphosura—set out in the Treatise of Invertebrate Paleontology in 1955—to be outdated and in need of revision, with several common genera such as Paleolimulus Dunbar, 1923 and Limulitella Størmer, 1952 acting as wastebasket taxa. Here, an expanded xiphosuran phylogeny is presented, comprising 58 xiphosuran species as part of a 158 taxon chelicerate matrix coded for 259 characters. Analysing the matrix under both Bayesian inference and parsimony optimisation criteria retrieves a concordant tree topology that forms the basis of a genus-level systematic revision of xiphosuran taxonomy. The genera Euproops Meek, 1867, Belinurus König, 1820, Paleolimulus , Limulitella , and Limulus are demonstrated to be non-monophyletic and the previously synonymized genera Koenigiella Raymond, 1944 and Prestwichianella Cockerell, 1905 are shown to be valid. In addition, nine new genera ( Andersoniella gen. nov. , Macrobelinurus gen. nov. , and Parabelinurus gen. nov. in Belinurina; Norilimulus gen. nov. in Paleolimulidae; Batracholimulus gen. nov. and Boeotiaspis gen. nov. in Austrolimulidae; and Allolimulus gen. nov., Keuperlimulus gen. nov., and Volanalimulus gen. nov. in Limulidae) are erected to accommodate xiphosuran species not encompassed by existing genera. One new species, Volanalimulus madagascarensis gen. et sp. nov., is also described. Three putative xiphosuran genera— Elleria Raymond, 1944, Archeolimulus Chlupáč, 1963, and Drabovaspis Chlupáč, 1963—are determined to be non-xiphosuran arthropods and as such are removed from Xiphosura. The priority of Belinurus König, 1820 over Bellinurus Pictet, 1846 is also confirmed. This work is critical for facilitating the study of the xiphosuran fossil record and is the first step in resolving longstanding questions regarding the geographic distribution of the modern horseshoe crab species and whether they truly represent ‘living fossils’. Understanding the long evolutionary history of Xiphosura is vital for interpreting how the modern species may respond to environmental change and in guiding conservation efforts.
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Horseshoe crabs are an iconic group of extant chelicerates, with a stunning fossil record that extends to at least the Lower Ordovician (~480 million years ago). As such, the group has retained significant biological and palaeontological interest. The sporadic nature of descriptive and systematic research into fossil horseshoe crabs over the last two centuries has spread information on the group across more than 200 texts dating from the early nineteenth century to the present day. We present the most comprehensive pictorial atlas of horseshoe crabs to date to pool these important data together. This review highlights taxa such as Bellinurus lacoei and Limulus priscus that have never been documented with photography. Furthermore, key morphological features of the true horseshoe crab (Xiphosurida) families—Austrolimulidae, Belinuridae, Limulidae, Paleolimulidae, and Rolfeiidae—are described. The evolutionary history of horseshoe crabs is reviewed and the current issues facing any possible biogeographic work are presented. Four major future directions that should be adopted by horseshoe crab researchers are outlined. We conclude that this review provides the basis for innovative geographic and geometric morphometric studies needed to uncover facets of horseshoe crab evolution.
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The occupation of new environments by evolutionary lineages is frequently associated with morphological changes. This covariation of ecotype and phenotype is expected due to the process of natural selection, whereby environmental pressures lead to the proliferation of morphological variants that are a better fit for the prevailing abiotic conditions. One primary mechanism by which phenotypic variants are known to arise is through changes in the timing or duration of organismal development resulting in alterations to adult morphology, a process known as heterochrony. While numerous studies have demonstrated heterochronic trends in association with environmental gradients, few have done so within a phylogenetic context. Understanding species interrelationships is necessary to determine whether morphological change is due to heterochronic processes; however, research is hampered by the lack of a quantitative metric with which to assess the degree of heterochronic traits expressed within and among species. Here I present a new metric for quantifying heterochronic change, expressed as a heterochronic weighting, and apply it to xiphosuran chelicerates within a phylogenetic context to reveal concerted independent heterochronic trends. These trends correlate with shifts in environmental occupation from marine to nonmarine habitats, resulting in a macroevolutionary ratchet. Critically, the distribution of heterochronic weightings among species shows evidence of being influenced by both historical, phylogenetic processes and external ecological pressures. Heterochronic weighting proves to be an effective method to quantify heterochronic trends within a phylogenetic framework and is readily applicable to any group of organisms that have well-defined morphological characteristics, ontogenetic information, and resolved internal relationships.
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The group Xiphosurida (horseshoe “crabs”) is today only represented by four species. However, in the fossil record, several dozen species have been described, especially from the Carboniferous (about 300 million years ago). Several species have been interpreted as representatives of Euproops or Belinurus, but there is ongoing discussion which of these species are valid and how they can be differentiated. Recent studies suggested that differences in the timing of individual development could provide information for species distinction, exemplified by studies on Euproops danae (Mazon Creek, USA) and Euproops sp. (“Piesproops”; Piesberg, Germany). For this study, we reinvestigated all Carboniferous xiphosurids from the British Coal Measures stored in the collections of the Natural History Museum London. Size comparisons of the specimens revealed nine size groups; the smaller specimens were originally labelled as Belinurus, the larger ones as Euproops. The nine size groups exhibit five different morphotypes differing in structures surrounding the posterior shield (= thoracetron): spines of different lengths and, in larger specimens, a more or less developed flange. Two of these morphotypes show significantly longer spines than the remaining specimens and could be conspecific as E. anthrax. The remaining specimens are interpreted as growth series of another species, presumably of E. rotundatus. An ontogenetic flange formation is also known from E. danae and the “Piesproops”, but the timing differs between all three species. In E. rotundatus, the flange develops rather late, but then comparably abruptly, which makes this development more metamorphic in relation to development in the other species.
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So long since as 1849* Professor M'Coy made the proposition to unite in one tribe of the order Entomostraca the recent and fossil Limulidæ and the extinct species of Pterygotus and Eurypterus . “The tribe Pœcilopoda,” he observes, “are to be distinguished from other Entomostraca by having crustaceous, didactyle, ambulatory thoracic feet, as well as membranous, respiratory abdominal ones.” Professor M'Coy divides the Pœcilopoda into two divisions:—1. Limulidæ— Limulus ; and 2. Eurypteridæ— Eurypterus, Pterygotus , and Belinurus . He subsequently furnished a restoration of Pterygotus problematicus , in illustration of his view of the anatomy of this ancient fossil remain†. It is not surprising that Professor M'Coy should have failed to establish this order, since it was shown by Professor Huxley‡ to be founded upon an erroneous interpretation of the fossil remains; nor can it be doubted that the arrangement was based on conjecture rather than upon any minute acquaintance with the anatomy of these extinct forms of Pterygotus and Eurypterus , then only known in England by extremely fragmentary remains. The researches, too, of Professor Huxley§ into the anatomy and affinities of the genus Pterygotus (in 1859) do not favour M'Coy's view of their classification under a common order or tribe with Limulus , although he does admit that they possess several very important points of structure in common with the latter. “The Pœcilopoda” (i. e. Limulidæ), observes Professor Huxley§, “are, I believe, the only Crustacea which possess antennary organs like those of Pterygotus , and, like them, have the gnathites converted into locomotive organs, want the appendages
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