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==Discovery and naming==
==Discovery and naming==
[[File:Anthrapalaemon parki.jpg|thumb|left|upright|Illustrations of the original ''Perimecturus parki'' fossils from Peach's 1882 paper, originally labeled as ''Anthrapalaemon parki'']]
[[File:Anthrapalaemon parki.jpg|thumb|left|upright|Illustrations of the original ''Perimecturus parki'' fossils from Peach's 1882 paper, originally labeled as ''Anthrapalaemon parki'']]
The first fossil of ''Perimecturus'' known to science was discovered by A. Macconochie, with additional specimens found by Walter Park. These specimens were collected near the [[River Esk, Dumfries and Galloway|River Esk]] in [[Glencartholm]], Scotland, and turned in to the Geological Survey of Scotland. In 1882, [[Ben Peach]] became the first person to study these fossils, which he believed represented a new species of ''[[Anthrapalaemon]]'', naming it ''Anthrapalaemon parki'' after Park.<ref>{{Cite journal |last=Peach |first=Ben N. |date=1882 |title=IV.—On some new Crustaceans from the Lower Carboniferous Rocks of Eskdale and Liddesdale |url=https://archive.org/details/transactionsofro301883roy/page/73/mode/1up |journal=Earth and Environmental Science Transactions of The Royal Society of Edinburgh |language=en |volume=30 |issue=1 |pages=73–91 |doi=10.1017/S0080456800028982 |issn=2053-5945}}</ref> Later, Peach would work alongside J. Horne in 1903 to move this species to a separate genus which they called ''Palaesquilla'', however they did not formally rename it and thus ''Palaesquilla'' is deemed a [[Nomen nudum|''nomen nudum'']].<ref>{{Cite journal |last=Peach |first=B. N. |last2=Horne |first2=J. |date=1905 |title=The Canonbie Coalfield: its Geological Structure and Relations to the Carboniferous Rocks of the North of England and Central Scotland |url=https://archive.org/details/transactionsofro40roya/page/835/mode/1up |journal=Earth and Environmental Science Transactions of The Royal Society of Edinburgh |language=en |volume=40 |issue=4 |pages=835–878 |doi=10.1017/S0080456800034815 |issn=2053-5945}}</ref> A formal reassignment would be published by Peach in 1908, in which he erected the new genus ''Perimecturus'' with this species (now renamed as ''Perimecturus parki'') as its [[type species]]. Furthermore, he also studied several other specimens which he named as a [[subspecies]], ''P. parki duplicarinatus'', and additional species which he assigned to the genus, including ''P. stocki'' and ''P. communis''.<ref name=":0">{{Cite book |last=Peach |first=B. N. |url=https://www.biodiversitylibrary.org/item/41415 |title=Monograph on the higher Crustacea of the Carboniferous rocks of Scotland |date=1908 |publisher=Printed for H.M. Stationery off., by J. Hedderwick & sons, ltd |location=Glasgow}}</ref>
The first fossil of ''Perimecturus'' known to science was discovered by A. Macconochie, with additional specimens found by Walter Park. These specimens were collected near the [[River Esk, Dumfries and Galloway|River Esk]] in [[Glencartholm]], Scotland, and turned in to the Geological Survey of Scotland. In 1882, British paleontologist [[Ben Peach]] became the first person to study these fossils, which he believed represented a new species of ''[[Anthrapalaemon]]'', naming it ''Anthrapalaemon parki'' after Park.<ref>{{Cite journal |last=Peach |first=Ben N. |date=1882 |title=IV.—On some new Crustaceans from the Lower Carboniferous Rocks of Eskdale and Liddesdale |url=https://archive.org/details/transactionsofro301883roy/page/73/mode/1up |journal=Earth and Environmental Science Transactions of The Royal Society of Edinburgh |language=en |volume=30 |issue=1 |pages=73–91 |doi=10.1017/S0080456800028982 |issn=2053-5945}}</ref> Later, Peach would work alongside J. Horne in 1903 to move this species to a separate genus which they called ''Palaesquilla'', however they did not formally rename it and thus ''Palaesquilla'' is deemed a [[Nomen nudum|''nomen nudum'']].<ref>{{Cite journal |last=Peach |first=B. N. |last2=Horne |first2=J. |date=1905 |title=The Canonbie Coalfield: its Geological Structure and Relations to the Carboniferous Rocks of the North of England and Central Scotland |url=https://archive.org/details/transactionsofro40roya/page/835/mode/1up |journal=Earth and Environmental Science Transactions of The Royal Society of Edinburgh |language=en |volume=40 |issue=4 |pages=835–878 |doi=10.1017/S0080456800034815 |issn=2053-5945}}</ref> A formal reassignment would be published by Peach in 1908, in which he erected the new genus ''Perimecturus'' with this species (now renamed as ''Perimecturus parki'') as its [[type species]]. Furthermore, he also studied several other specimens which he named as a [[subspecies]], ''P. parki duplicarinatus'', and additional species which he assigned to the genus, including ''P. stocki'' and ''P. communis''.<ref name=":0">{{Cite book |last=Peach |first=B. N. |url=https://www.biodiversitylibrary.org/item/41415 |title=Monograph on the higher Crustacea of the Carboniferous rocks of Scotland |date=1908 |publisher=Printed for H.M. Stationery off., by J. Hedderwick & sons, ltd |location=Glasgow}}</ref>


In 1979, a review of the Carboniferous-aged [[malacostraca]]ns of Britain written by [[Frederick Schram]] was published. The review found that ''P. parki'' was the only valid species of ''Perimecturus'' named by Peach, and that ''P. p. duplicarinatus'', ''P. stocki'' and ''P. communis'' were all [[junior synonym]]s of it. The specimen GSE 5896 was designated as the [[lectotype]] of this species. Schram stated that Peach's idea of the fossils as separate species was due to incorrect interpretation of the fossils preserved in different modes: the original ''P. parki'' [[holotype]] showed the animal in a top-down view, the ''P. p. duplicarinatus'' specimen clearly preserved the longitudinal ridges, the ''P. stocki'' fossil is an individual in a slanted angle and the ''P. communis'' remains are displayed from the side.<ref name=":1">{{Cite book |last1=Schram |first1=Frederick R. |url=https://www.biodiversitylibrary.org/bibliography/3360 |title=British Carboniferous Malacostraca |date=1979 |publisher=Field Museum of Natural History |location=Chicago |language=}}</ref>
In 1979, a review of the Carboniferous-aged [[malacostraca]]ns of Britain written by American paleontologist [[Frederick Schram]] was published. The review found that ''P. parki'' was the only valid species of ''Perimecturus'' named by Peach, and that ''P. p. duplicarinatus'', ''P. stocki'' and ''P. communis'' were all [[junior synonym]]s of it. The specimen GSE 5896 was designated as the [[lectotype]] of this species. Schram stated that Peach's idea of the fossils as separate species was due to incorrect interpretation of the fossils preserved in different modes: the original ''P. parki'' [[holotype]] showed the animal in a top-down view, the ''P. p. duplicarinatus'' specimen clearly preserved the longitudinal ridges, the ''P. stocki'' fossil is an individual in a slanted angle and the ''P. communis'' remains are displayed from the side.<ref name=":1">{{Cite book |last1=Schram |first1=Frederick R. |url=https://www.biodiversitylibrary.org/bibliography/3360 |title=British Carboniferous Malacostraca |date=1979 |publisher=Field Museum of Natural History |location=Chicago |language=}}</ref>


A second species of ''Perimecturus'' was erected by Schram in 1978 and named ''P. rapax'', the specific name being a [[Latin]] word meaning "to grasp" (in reference to the animal's predatory lifestyle and [[raptorial]] appendages). The holotype for this species, UM 6141, is held in the collection of the [[University of Montana]] and was discovered in the [[Bear Gulch Limestone]] of [[Fergus County, Montana]].<ref name=":2">{{Cite journal |last=Schram |first=Frederick R. |last2=Horner |first2=John |date=1978 |title=Crustacea of the Mississippian Bear Gulch Limestone of Central Montana |url=https://www.jstor.org/stable/1303712 |journal=Journal of Paleontology |volume=52 |issue=2 |pages=394–406 |issn=0022-3360}}</ref>
A second species of ''Perimecturus'' was erected by Schram in 1978 and named ''P. rapax'', the specific name being a [[Latin]] word meaning "to grasp" (in reference to the animal's predatory lifestyle and [[raptorial]] appendages). The holotype for this species, UM 6141, is held in the collection of the [[University of Montana]] and was discovered in the [[Bear Gulch Limestone]] of [[Fergus County, Montana]].<ref name=":2">{{Cite journal |last=Schram |first=Frederick R. |last2=Horner |first2=John |date=1978 |title=Crustacea of the Mississippian Bear Gulch Limestone of Central Montana |url=https://www.jstor.org/stable/1303712 |journal=Journal of Paleontology |volume=52 |issue=2 |pages=394–406 |issn=0022-3360}}</ref> In 1985, David Factor and Rodney Feldmann published a redescription of ''P. rapax'', after a detailed reanalysis of the fossils which found that Schram had misinterpreted some of their features.<ref name=":5">{{Cite journal |last=Factor |first=David F. |last2=Feldmann |first2=Rodney M. |date=1985 |title=Systematics and paleoecology of malacostracan arthropods in the Bear Gulch Lilmestone (Namurian) of central Montana |url=https://www.biodiversitylibrary.org/part/330776 |journal=Annals of the Carnegie Museum |volume=54 |pages=319–356 |doi=10.5962/p.330776 |issn=0097-4463}}</ref>


===Reassigned species===
===Reassigned species===
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The body of ''Perimecturus'' is distinctively flat and almost rectangular. With the largest specimen (GSE 5897) measuring {{convert|15|cm|abbr=on|in}} in total length, ''P. parki'' is among the biggest Paleozoic mantis shrimps, though most specimens measure just {{convert|1.28|-|3.37|cm|abbr=on|in}} in [[carapace]] length and {{convert|1.50|-|4.65|cm|abbr=on|in}} in [[abdomen]] length.<ref name=":1" /> ''P. rapax'' is a smaller species, reaching only {{convert|1.22|-|2.59|cm|abbr=on|in}} in carapace length and {{convert|1.45|-|2.83|cm|abbr=on|in}} in abdomen length.<ref name=":2" />
The body of ''Perimecturus'' is distinctively flat and almost rectangular. With the largest specimen (GSE 5897) measuring {{convert|15|cm|abbr=on|in}} in total length, ''P. parki'' is among the biggest Paleozoic mantis shrimps, though most specimens measure just {{convert|1.28|-|3.37|cm|abbr=on|in}} in [[carapace]] length and {{convert|1.50|-|4.65|cm|abbr=on|in}} in [[abdomen]] length.<ref name=":1" /> ''P. rapax'' is a smaller species, reaching only {{convert|1.22|-|2.59|cm|abbr=on|in}} in carapace length and {{convert|1.45|-|2.83|cm|abbr=on|in}} in abdomen length.<ref name=":2" />


The [[Rostrum (anatomy)|rostrum]] is very broad and blunt, with a rounded tip in ''P. rapax'', though it is slightly more pointed in ''P. parki''. The [[Antenna (biology)|antennae]] are short and flagellated, each with an elongated and pointed scaphocerite ([[exopod]] of the antenna). The large, subrectangular carapace covers the entire [[Thorax (arthropod anatomy)|thorax]] and has a marked furrow all around its margins, as well as short keels extending from the base of the antennae. The carapace has five prominent ridges (one down the middle of the carapace and two on either side) stretching across its latter half.<ref name=":5">{{Cite journal |last=Factor |first=David F. |last2=Feldmann |first2=Rodney M. |date=1985 |title=Systematics and paleoecology of malacostracan arthropods in the Bear Gulch Lilmestone (Namurian) of central Montana |url=https://www.biodiversitylibrary.org/part/330776 |journal=Annals of the Carnegie Museum |volume=54 |pages=319–356 |doi=10.5962/p.330776 |issn=0097-4463}}</ref> Though Schram (1978) claims ''P. parki'' has only four such ridges and ''P. rapax'' has only three, detailed reanalysis by Factor and Feldmann (1985) and Jenner ''et al.'' (1998) confirms both species actually have five.<ref name=":2" /><ref name=":5" /><ref name=":4">{{Cite journal |last=Jenner |first=Ronald A. |last2=Hof |first2=Cees H.J. |last3=Schram |first3=Frederick R. |date=1998 |title=Palaeo- and archaeostomatopods (Hoplocarida, Crustacea) from the Bear Gulch Limestone, Mississippian (Namurian), of central Montana |url=https://brill.com/view/journals/ctoz/67/3/article-p155_1.xml |journal=Contributions to Zoology |volume=67 |issue=3 |pages=155–185 |doi=10.1163/18759866-06703001 |issn=1383-4517}}</ref> The compound eyes are preserved in ''P. rapax'', showing that they are stalked and oval in shape.<ref name=":2" />
The [[Rostrum (anatomy)|rostrum]] is very broad and blunt, with a rounded tip in ''P. rapax'', though it is slightly more pointed in ''P. parki''. The [[Antenna (biology)|antennae]] are short and flagellated, each with an elongated and pointed scaphocerite ([[exopod]] of the antenna). The large, subrectangular carapace covers the entire [[Thorax (arthropod anatomy)|thorax]] and has a marked furrow all around its margins, as well as short keels extending from the base of the antennae. The carapace has five prominent ridges (one down the middle of the carapace and two on either side) stretching across its latter half.<ref name=":5" /> Though Schram (1978) claims ''P. parki'' has only four such ridges and ''P. rapax'' has only three, detailed reanalysis by Factor and Feldmann (1985) and Jenner ''et al.'' (1998) confirms both species actually have five.<ref name=":2" /><ref name=":5" /><ref name=":4">{{Cite journal |last=Jenner |first=Ronald A. |last2=Hof |first2=Cees H.J. |last3=Schram |first3=Frederick R. |date=1998 |title=Palaeo- and archaeostomatopods (Hoplocarida, Crustacea) from the Bear Gulch Limestone, Mississippian (Namurian), of central Montana |url=https://brill.com/view/journals/ctoz/67/3/article-p155_1.xml |journal=Contributions to Zoology |volume=67 |issue=3 |pages=155–185 |doi=10.1163/18759866-06703001 |issn=1383-4517}}</ref> The [[compound eye]]s are preserved in ''P. rapax'', showing that they are stalked and oval in shape.<ref name=":2" />


Like all mantis shrimps, ''Perimecturus'' had [[raptorial]] appendages attached to the thorax. Because the raptorial appendages of this genus are rather short and often retracted to overlap with each other, study of them has been difficult and their features often cannot be discerned. However, some ''P. parki'' specimens have shown that most segments of these appendages are approximately equal in length, except the fourth segment from the [[distal]] end which is notably shorter.<ref name=":1" />
Like all mantis shrimps, ''Perimecturus'' had [[raptorial]] appendages attached to the thorax. Because the raptorial appendages of this genus are rather short and often retracted to overlap with each other, study of them has been difficult and their features often cannot be discerned. However, some ''P. parki'' specimens have shown that most segments of these appendages are approximately equal in length, except the fourth segment from the [[distal]] end which is notably shorter.<ref name=":1" />
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==Classification==
==Classification==
''Perimecturus'' gives its name to the family [[Perimecturidae]], of which it is the [[type genus]]. This family was established by Ben Peach in 1908, who placed it within the now defunct order [[Schizopoda]], believing that perimecturids were intermediate forms between [[Lophogastridae]] and [[Anaspididae]].<ref name=":0" /> In 1962, the Perimecturidae family was first recognized as a group of early mantis shrimps by H. K. Brooks, reassigning it to the [[Order (biology)|order]] Palaeostomatopoda (now delisted as a [[suborder]] and named [[Palaeostomatopodea]]).<ref>{{Cite journal |last=Brooks |first=Harold Kelly |date=1962 |title=The Paleozoic Eumalacostraca of North America |url=https://www.biodiversitylibrary.org/page/10667554 |journal=Bulletins of American Paleontology |volume=44 |issue=202 |pages=163–338}}</ref> With the advent of [[cladistic analyses]], the palaeostomatopods as traditionally construed were first recovered as a [[paraphyletic]] grouping by Jenner ''et al.'' (1998), a finding later confirmed by Schram (2007).<ref name=":3" /><ref name=":4" /> Currently, Palaeostomatopodea is still used in a paraphyletic sense to refer to the [[evolutionary grade]].<ref>{{Cite journal |last=Schram |first=Frederick |date=2008 |title=An adjustment to the higher taxonomy of the fossil Stomatopoda |url=https://www.jstor.org/stable/20111439 |journal=Crustaceana |volume=81 |issue=6 |pages=751–754 |doi=10.1163/156854008784513429 |issn=0011-216X |jstor=20111439}}</ref>
''Perimecturus'' gives its name to the family [[Perimecturidae]], of which it is the [[type genus]]. This family was established by Ben Peach in 1908, who placed it within the now defunct order [[Schizopoda]], believing that perimecturids were intermediate forms between [[Lophogastridae]] and [[Anaspididae]].<ref name=":0" /> In 1962, the Perimecturidae family was first recognized as a group of early mantis shrimps by H. K. Brooks, reassigning it to the [[Order (biology)|order]] Palaeostomatopoda (now delisted as a [[suborder]] and named [[Palaeostomatopodea]]).<ref>{{Cite journal |last=Brooks |first=Harold Kelly |date=1962 |title=The Paleozoic Eumalacostraca of North America |url=https://www.biodiversitylibrary.org/page/10667554 |journal=Bulletins of American Paleontology |volume=44 |issue=202 |pages=163–338}}</ref> With the advent of [[cladistic analyses]], the palaeostomatopods as traditionally construed were first recovered as a [[paraphyletic]] grouping by Jenner ''et al.'' (1998), a finding later confirmed by Schram (2007).<ref name=":3" /><ref name=":4" /> Currently, Palaeostomatopodea is still used in a paraphyletic sense to refer to the [[evolutionary grade]].<ref>{{Cite journal |last=Schram |first=Frederick |date=2008 |title=An adjustment to the higher taxonomy of the fossil Stomatopoda |url=https://www.jstor.org/stable/20111439 |journal=Crustaceana |volume=81 |issue=6 |pages=751–754 |doi=10.1163/156854008784513429 |issn=0011-216X |jstor=20111439}}</ref>

Several studies of conducted [[phylogenetic analyses]] on fossil mantis shrimps. While Jenner ''et al.'' (1998) found the genus to be [[monophyletic]], some other authors have questioned its monophyly.<ref name=":4" /> Schram (2007) and Haug ''et al.'' (2010) both recovered ''Perimecturus'' to be paraphyletic, the former finding ''P. rapax'' to be the sister taxon to ''[[Bairdops]] elegans'' within a monophyletic family Perimecturidae, while the latter suggests the family is a paraphyletic grade in which ''P. parki'' is the sister taxon to all other mantis shrimps except ''[[Archaeocaris]]'' and ''Bairdops''.<ref name=":3" /><ref>{{Cite journal |last=Haug |first=Joachim T |last2=Haug |first2=Carolin |last3=Maas |first3=Andreas |last4=Kutschera |first4=Verena |last5=Waloszek |first5=Dieter |date=2010 |title=Evolution of mantis shrimps (Stomatopoda, Malacostraca) in the light of new Mesozoic fossils |url=http://bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-290 |journal=BMC Evolutionary Biology |language=en |volume=10 |issue=1 |pages=290 |doi=10.1186/1471-2148-10-290 |issn=1471-2148 |pmc=PMC2955030 |pmid=20858249}}</ref> On the other hand, Smith ''et al.'' (2023) supports the idea that both ''Perimecturus'' and Perimecturidae are monophyletic. Their results are displayed in the [[cladogram]] below:<ref>{{Cite journal |last1=Smith |first1=C.P.A. |last2=Aubier |first2=P. |last3=Charbonnier |first3=S. |last4=Laville |first4=T. |last5=Olivier |first5=N. |last6=Escarguel |first6=G. |last7=Jenks |first7=J.F. |last8=Bylund |first8=K.G. |last9=Fara |first9=E. |last10=Brayard |first10=A. |date=2023-03-31 |title=Closing a major gap in mantis shrimp evolution – first fossils of Stomatopoda from the Triassic |url=https://www.researchgate.net/publication/369959650 |journal=Bulletin of Geosciences |language=en |pages=95–110 |doi=10.3140/bull.geosci.1864 |issn=1802-8225|doi-access=free }}</ref>

{{Barlabel
|style=font-size:85%; line-height:85%
|size=24
|at1=3.5|label1=Archaeostomatopods|bar1=red
|at2=10|label2=Palaeostomatopods|bar2=green
|at3=17.5|label3=Pseudosculdids|bar3=blue
|cladogram=
{{clade
|label1=[[Stomatopoda]]
|1={{clade
|label1={{extinct}}''[[Archaeocaris]]'' |barbegin1=red
|1={{clade
|1=''[[Archaeocaris|Archaeocaris vermiformis]]''
|2=''[[Archaeocaris|Archaeocaris graffhami]]''}}
|2={{clade
|1={{clade
|1={{extinct}}''[[Bairdops|Bairdops elegans]]'' |bar1=red
|label2={{extinct}}'''''Perimecturus'''''
|2={{clade
|1='''''Perimecturus parki'''''
|2='''''Perimecturus rapax'''''}} |bar2=red}}
|2={{extinct}}''[[Bairdops|Bairdops beargulchensis]]'' |barend2=red
|3={{clade
|1={{extinct}}''[[Daidal|Daidal pattoni]]'' |barbegin1=green
|2={{clade
|1={{clade
|1={{clade
|1={{extinct}}''[[Daidal|Daidal schoellmanni]]''
|2={{extinct}}''[[Daidal|Daidal acanthocercus]]''}} |bar1=green
|label2={{extinct}}''[[Gorgonophontes]]''
|2={{clade
|1=''[[Gorgonophontes|Gorgonophontes fraiponti]]''
|2=''[[Gorgonophontes|Gorgonophontes peleron]]''}} |bar2=green}}
|3={{clade
|1={{extinct}}''[[Chabardella|Chabardella spinosa]]'' }}|bar3=green
|5={{clade
|1={{extinct}}''[[Tyrannophontes|Tyrannophontes theridion]]'' |bar1=green
|2={{clade
|1={{extinct}}''[[Tyrannophontes|Tyrannophontes gigantion]]'' |barend1=green
|label2=[[Unipeltata]]
|2={{clade
|1={{extinct}}''[[Triassosculda|Triassosculda ahyongi]]''
|2={{clade
|1={{extinct}}''[[Tyrannosculda|Tyrannosculda laurae]]''
|2={{clade
|1={{extinct}}''[[Pseudosculda|Pseudosculda laevis]]'' |barbegin1=blue
|2={{clade
|1={{extinct}}''[[Archaeosculda|Archaeosculda phoenicia]]'' |barend1=blue
|2={{clade
|1={{clade
|1={{extinct}}''[[Sculda|Sculda pennata]]''
|2={{extinct}}''[[Sculda|Sculda syriaca]]''}}
|2={{clade
|1={{extinct}}''[[Ursquilla|Ursquilla yehoachi]]''
|2={{clade
|1={{extinct}}''[[Lysiosquilla|Lysiosquilla nkporoensis]]''
|2={{clade
|1={{extinct}}''[[Nodosculda|Nodosculda fisherorum]]''
|2=''[[Squilla mantis]]''}}}}}}}}}}}}}}}}}}}}}}}}}}}}}}}}


==References==
==References==

Revision as of 19:10, 9 March 2024

Perimecturus
Temporal range: Mississippian
Fossil of P. rapax from the Bear Gulch Limestone
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Class: Malacostraca
Order: Stomatopoda
Family: Perimecturidae
Genus: Perimecturus
Peach, 1908
Type species
Anthrapalaemon parki
Peach, 1882
Species
  • P. parki
    Peach, 1882
  • P. rapax
    Schram & Horner, 1978
Synonyms
Synonyms of Perimecturus
Synonyms of P. parki
  • Anthrapalaemon parki Peach, 1882
  • Palaesquilla parki Peach & Horne, 1903 (nomen nudum)
  • Perimecturus communis Peach, 1908
  • Perimecturus parki duplicarinatus Peach, 1908
  • Perimecturus stocki Peach, 1908

Perimecturus is an extinct genus of mantis shrimp that lived during the Early Carboniferous period in what is now Scotland and the United States. Two named species are currently assigned to it.

Discovery and naming

Illustrations of the original Perimecturus parki fossils from Peach's 1882 paper, originally labeled as Anthrapalaemon parki

The first fossil of Perimecturus known to science was discovered by A. Macconochie, with additional specimens found by Walter Park. These specimens were collected near the River Esk in Glencartholm, Scotland, and turned in to the Geological Survey of Scotland. In 1882, British paleontologist Ben Peach became the first person to study these fossils, which he believed represented a new species of Anthrapalaemon, naming it Anthrapalaemon parki after Park.[1] Later, Peach would work alongside J. Horne in 1903 to move this species to a separate genus which they called Palaesquilla, however they did not formally rename it and thus Palaesquilla is deemed a nomen nudum.[2] A formal reassignment would be published by Peach in 1908, in which he erected the new genus Perimecturus with this species (now renamed as Perimecturus parki) as its type species. Furthermore, he also studied several other specimens which he named as a subspecies, P. parki duplicarinatus, and additional species which he assigned to the genus, including P. stocki and P. communis.[3]

In 1979, a review of the Carboniferous-aged malacostracans of Britain written by American paleontologist Frederick Schram was published. The review found that P. parki was the only valid species of Perimecturus named by Peach, and that P. p. duplicarinatus, P. stocki and P. communis were all junior synonyms of it. The specimen GSE 5896 was designated as the lectotype of this species. Schram stated that Peach's idea of the fossils as separate species was due to incorrect interpretation of the fossils preserved in different modes: the original P. parki holotype showed the animal in a top-down view, the P. p. duplicarinatus specimen clearly preserved the longitudinal ridges, the P. stocki fossil is an individual in a slanted angle and the P. communis remains are displayed from the side.[4]

A second species of Perimecturus was erected by Schram in 1978 and named P. rapax, the specific name being a Latin word meaning "to grasp" (in reference to the animal's predatory lifestyle and raptorial appendages). The holotype for this species, UM 6141, is held in the collection of the University of Montana and was discovered in the Bear Gulch Limestone of Fergus County, Montana.[5] In 1985, David Factor and Rodney Feldmann published a redescription of P. rapax, after a detailed reanalysis of the fossils which found that Schram had misinterpreted some of their features.[6]

Reassigned species

Because it was the first Paleozoic mantis shrimp genus to be named, numerous species have been assigned to Perimecturus before better knowledge of early mantis shrimps was developed. The following species were formerly placed in Perimecturus but have since been moved to other genera:

  • P. elegans was erected in 1908 by Peach based on fossils from the River Esk, Scotland.[3] In 1979, Schram established the genus Bairdops to which this species was reassigned and became the type species of.[4]
  • P. ensifer was named by Peach in 1908 from remains found in the Scottish localities of Liddel Water, Newcastleton and Glencartholm.[3] Schram declared it to be a junior synonym of Bairdops elegans in 1979.[4]
  • P. pattoni was described by Peach in 1908 based on a single fossil from the Top Hosie Limestone of the Lower Limestone Formation near East Kilbride, Scotland.[3] It was first noted by Schram in 1979 to not properly belong to Perimecturus, and in 2007 he moved it to the genus Daidal.[4][7]

Description

The body of Perimecturus is distinctively flat and almost rectangular. With the largest specimen (GSE 5897) measuring 15 cm (5.9 in) in total length, P. parki is among the biggest Paleozoic mantis shrimps, though most specimens measure just 1.28–3.37 cm (0.50–1.33 in) in carapace length and 1.50–4.65 cm (0.59–1.83 in) in abdomen length.[4] P. rapax is a smaller species, reaching only 1.22–2.59 cm (0.48–1.02 in) in carapace length and 1.45–2.83 cm (0.57–1.11 in) in abdomen length.[5]

The rostrum is very broad and blunt, with a rounded tip in P. rapax, though it is slightly more pointed in P. parki. The antennae are short and flagellated, each with an elongated and pointed scaphocerite (exopod of the antenna). The large, subrectangular carapace covers the entire thorax and has a marked furrow all around its margins, as well as short keels extending from the base of the antennae. The carapace has five prominent ridges (one down the middle of the carapace and two on either side) stretching across its latter half.[6] Though Schram (1978) claims P. parki has only four such ridges and P. rapax has only three, detailed reanalysis by Factor and Feldmann (1985) and Jenner et al. (1998) confirms both species actually have five.[5][6][10] The compound eyes are preserved in P. rapax, showing that they are stalked and oval in shape.[5]

Like all mantis shrimps, Perimecturus had raptorial appendages attached to the thorax. Because the raptorial appendages of this genus are rather short and often retracted to overlap with each other, study of them has been difficult and their features often cannot be discerned. However, some P. parki specimens have shown that most segments of these appendages are approximately equal in length, except the fourth segment from the distal end which is notably shorter.[4]

Little is known about the thorax as it is completely covered by the carapace, though its hind segments at least are not fused with it. The abdomen is made up of six segments, each approximately the same length. A small backward-pointing spike is present at the edges of every abdominal segment. Schram (1978) wrongly stated that P. parki and P. rapax had four and three abdominal ridges respectively, believing they lined up with the carapace ridges.[5] Reanalysis has found that both species have six keels on each abdominal segment, forming six continuous ridges down the abdomen (two median ridges and four lateral ridges). The ridges run parallel to each other in the first four segments and begin to converge with each other at the fifth segment. Two small wart-like bumps are present on each abdominal segment, one located in each space between the median ridges and innermost lateral ridges.[6][10]

While both species have biramous (two-branched) uropods, spines near the end of the outer margin of the uropodal exopod (outer branch), a subtriangular telson that tapers into a pointed spike at the end and small furcae (spikes forming the tail fork) flanking the base of this spike, other aspects of the tail fan differs greatly between the two Perimecturus species. In P. parki, this spike is less than half the length of the telson base, with delicate bristles around the edges of the telson and uropods. The exopod of the uropod and the hind part of the telson base are smooth.[4] Meanwhile, the telson spike of P. rapax is over half the length of the telson base, no bristles are present on the tail fan, the outer margin of the uropodal exopod is serrated, and the telson is serrated near the furcae.[6]

Classification

Perimecturus gives its name to the family Perimecturidae, of which it is the type genus. This family was established by Ben Peach in 1908, who placed it within the now defunct order Schizopoda, believing that perimecturids were intermediate forms between Lophogastridae and Anaspididae.[3] In 1962, the Perimecturidae family was first recognized as a group of early mantis shrimps by H. K. Brooks, reassigning it to the order Palaeostomatopoda (now delisted as a suborder and named Palaeostomatopodea).[11] With the advent of cladistic analyses, the palaeostomatopods as traditionally construed were first recovered as a paraphyletic grouping by Jenner et al. (1998), a finding later confirmed by Schram (2007).[7][10] Currently, Palaeostomatopodea is still used in a paraphyletic sense to refer to the evolutionary grade.[12]

Several studies of conducted phylogenetic analyses on fossil mantis shrimps. While Jenner et al. (1998) found the genus to be monophyletic, some other authors have questioned its monophyly.[10] Schram (2007) and Haug et al. (2010) both recovered Perimecturus to be paraphyletic, the former finding P. rapax to be the sister taxon to Bairdops elegans within a monophyletic family Perimecturidae, while the latter suggests the family is a paraphyletic grade in which P. parki is the sister taxon to all other mantis shrimps except Archaeocaris and Bairdops.[7][13] On the other hand, Smith et al. (2023) supports the idea that both Perimecturus and Perimecturidae are monophyletic. Their results are displayed in the cladogram below:[14]

Stomatopoda
Archaeostomatopods
Palaeostomatopods
Pseudosculdids

References

  1. ^ Peach, Ben N. (1882). "IV.—On some new Crustaceans from the Lower Carboniferous Rocks of Eskdale and Liddesdale". Earth and Environmental Science Transactions of The Royal Society of Edinburgh. 30 (1): 73–91. doi:10.1017/S0080456800028982. ISSN 2053-5945.
  2. ^ Peach, B. N.; Horne, J. (1905). "The Canonbie Coalfield: its Geological Structure and Relations to the Carboniferous Rocks of the North of England and Central Scotland". Earth and Environmental Science Transactions of The Royal Society of Edinburgh. 40 (4): 835–878. doi:10.1017/S0080456800034815. ISSN 2053-5945.
  3. ^ a b c d e Peach, B. N. (1908). Monograph on the higher Crustacea of the Carboniferous rocks of Scotland. Glasgow: Printed for H.M. Stationery off., by J. Hedderwick & sons, ltd.
  4. ^ a b c d e f g Schram, Frederick R. (1979). British Carboniferous Malacostraca. Chicago: Field Museum of Natural History.
  5. ^ a b c d e Schram, Frederick R.; Horner, John (1978). "Crustacea of the Mississippian Bear Gulch Limestone of Central Montana". Journal of Paleontology. 52 (2): 394–406. ISSN 0022-3360.
  6. ^ a b c d e Factor, David F.; Feldmann, Rodney M. (1985). "Systematics and paleoecology of malacostracan arthropods in the Bear Gulch Lilmestone (Namurian) of central Montana". Annals of the Carnegie Museum. 54: 319–356. doi:10.5962/p.330776. ISSN 0097-4463.
  7. ^ a b c Schram, Frederick R. (2007). "Paleozoic Proto-Mantis Shrimp Revisited". Journal of Paleontology. 81 (5): 895–916. doi:10.1666/pleo05-075.1. ISSN 0022-3360. JSTOR 4498847. S2CID 85606671.
  8. ^ van Straelen, Victor (1922). "Quelques eumalacostracés nouveaux du Westphalien inférieur d'Argenteau près Liége". Annales de la Société Géologique de Belgique (in French). 45: 35–40.
  9. ^ Schöllmann, Lothar (2004). "Archaeostomatopodea (Malacostraca, Hoplocarida) aus dem Namur B (höheres Marsdenium, Karbon) von Hagen-Vorhalle (NRW, Deutschland) und eine Neudefinition einiger Arten und Famile Tyrannophontidaae". Geologie und Paläontololgie in Westfalen. 62: 111–141.
  10. ^ a b c d Jenner, Ronald A.; Hof, Cees H.J.; Schram, Frederick R. (1998). "Palaeo- and archaeostomatopods (Hoplocarida, Crustacea) from the Bear Gulch Limestone, Mississippian (Namurian), of central Montana". Contributions to Zoology. 67 (3): 155–185. doi:10.1163/18759866-06703001. ISSN 1383-4517.
  11. ^ Brooks, Harold Kelly (1962). "The Paleozoic Eumalacostraca of North America". Bulletins of American Paleontology. 44 (202): 163–338.
  12. ^ Schram, Frederick (2008). "An adjustment to the higher taxonomy of the fossil Stomatopoda". Crustaceana. 81 (6): 751–754. doi:10.1163/156854008784513429. ISSN 0011-216X. JSTOR 20111439.
  13. ^ Haug, Joachim T; Haug, Carolin; Maas, Andreas; Kutschera, Verena; Waloszek, Dieter (2010). "Evolution of mantis shrimps (Stomatopoda, Malacostraca) in the light of new Mesozoic fossils". BMC Evolutionary Biology. 10 (1): 290. doi:10.1186/1471-2148-10-290. ISSN 1471-2148. PMC 2955030. PMID 20858249.{{cite journal}}: CS1 maint: PMC format (link) CS1 maint: unflagged free DOI (link)
  14. ^ Smith, C.P.A.; Aubier, P.; Charbonnier, S.; Laville, T.; Olivier, N.; Escarguel, G.; Jenks, J.F.; Bylund, K.G.; Fara, E.; Brayard, A. (2023-03-31). "Closing a major gap in mantis shrimp evolution – first fossils of Stomatopoda from the Triassic". Bulletin of Geosciences: 95–110. doi:10.3140/bull.geosci.1864. ISSN 1802-8225.

External links