Euthycarcinoidea

Extinct order of arthropods From Wikipedia, the free encyclopedia

Euthycarcinoidea are a group of extinct, possibly amphibious arthropods that ranged from the Cambrian to the Triassic.[1] Fossils are known from Europe, North America, Argentina, Australia, and Antarctica. While previously considered enigmatic, they are now widely considered to be members of Mandibulata, and possibly the closest known relatives of Myriapoda (which contains millipedes and centipedes, among others).

Phylum:Arthropoda
Stem group:Myriapoda
Subclass:Euthycarcinoidea
Gall & Grauvogel, 1964
Quick facts Scientific classification, Genera ...
Euthycarcinoidea
Temporal range: Cambrian–Middle Triassic
Life restoration of Apankura
Life restoration of Sottyxerxes
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Arthropoda
Clade: Mandibulata
Stem group: Myriapoda
Subclass: Euthycarcinoidea
Gall & Grauvogel, 1964
Order: Euthycarcinida
Gall & Grauvogel, 1964
Genera

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Description

The euthycarcinoid body was divided into a cephalon (head), preabdomen, and postabdomen. The cephalon consisted of two segments and included mandibles, antennae and presumed eyes. The preabdomen consisted of five to fourteen tergites, each having up to three somites. Each somite had in turn a pair of uniramous, segmented legs. The postabdomen was limbless and consisted of up to six segments and a terminal tail spine.[2]

The Cambrian euthycarcinoid Mosineia macnaughtoni from the Elk Mound Group, Blackberry Hill, central Wisconsin. Cambrian euthycarcinoids such as this one may have been the first animals to walk and survive on land.[3]

Affinities

Due to its particular combination of characteristics, the position of the Euthycarcinoidea within the Arthropoda has been ambiguous; previous authors have allied euthycarcinoids with crustaceans (interpreted as copepods, branchiopods, or an independent group), with trilobites, or the merostomatans (horseshoe crabs and sea scorpions, now an obsolete group[4]).[5] However, due to the general features and the discovery of fossils from this group in Cambrian rocks, a 2010 study suggested that they may have given rise to the mandibulates, the group that includes the myriapods (centipedes, millipedes and the like), crustaceans, and hexapods (insects, etc.).[2]

However, a 2020 study identified several characters, including compound eyes and various details of the preoral chamber, that suggested instead a position as the closest relatives of living myriapods.[6] This would help to close the gap between the earliest body fossils of crown-group myriapods in the Silurian and molecular clock data suggesting a divergence from their closest relatives during the Ediacaran or Cambrian.[2] This had already been suggested by the cladogram of a previous study.[7] Cladogram of Mandibulata after Laville et al. (2025), showing proposed position of Euthycarcinida as sister to Myriapoda:[8]

Mandibulata

Aquilonifer

Tanazios

Euthycarcinida

Myriapoda (including centipedes and millipedes)

Pancrustacea
Allotriocarida

Branchiopoda (tadpole shrimp/Triops, fairy shrimp, clam shrimp, water fleas)

Hexapoda (including springtails and insects)

Xenocarida

Cephalocarida (horseshoe shrimp)

Remipedia

Oligostraca
Multicrustacea

Copepoda

Cirripedia (barnacles)

Cyclida (Americlidae)

Thylacocephala

Malacostraca (shrimp, prawn, lobsters, mantis shrimp, crab, woodlice, etc)

Environment and life habits

Euthycarcinoid fossils have been found in marine, brackish and freshwater deposits.[2] Taxa from the Cambrian are from marine or intertidal sediments, while all specimens from the Ordovician to the Triassic are freshwater or brackish.[5] Fossil impressions of euthycarcinoid postabdomens in association with Protichnites trackways in Cambrian intertidal/supratidal deposits also suggest that euthycarcinoids may have been the first arthropods to walk on land.[9][10] It has been suggested that the biofilms and microbial mats that covered much of the vast tidal flats during the Cambrian Period in North America may have provided the nourishment that lured these arthropods onto the land.[11] Fossil evidence also suggests the possibility that some euthycarcinoids came onto the land to lay and fertilize their eggs via amplexus, as do the modern horseshoe crabs.[10]

Classification

The known species of euthycarcinoids and their distribution were reviewed by Racheboeuf et al. in 2008. Additional species were described by Collette and Hagadorn in 2010.[5][9][12]

More information Family, Genus ...
Family Genus Species Age Type of deposits Location of deposits
Euthycarcinidae
Handlirsch, 1914
Euthycarcinus
Handlirsch, 1914
E. ibbenburensis
Schultka, 1991
Pennsylvanian: Westphalian Freshwater Germany
E. kessleri
Handlirsch, 1914
Triassic Freshwater France
E. martensi
Schneider, 1983
Permian Freshwater Germany
Synaustrus
Riek, 1964
S. brookvalensis
Riek, 1964
Triassic Freshwater Australia
Kottixerxidae
Starobogatov, 1988
Heterocrania
Hirst & Maulik, 1926
H. rhyniensis
Hirst & Maulik, 1926
Lower Devonian[13] Freshwater[13] United Kingdom[13]
Kalbarria
McNamara & Trewin, 1993
K. brimmellae
McNamara & Trewin, 1993
Ordovician or Late Silurian (age is controversial)[14] Freshwater (habitat is controversial)[14] Australia
Kottixerxes
Schram, 1971
K. anglicus
Wilson & Almond, 2001
Pennsylvanian: Westphalian Brackish to freshwater United Kingdom
K. gloriosus
Schram, 1971
Pennsylvanian: Westphalian Brackish to freshwater United States
Schramixerxes
Starobogatov, 1988
S. gerem
(Schram & Rolfe, 1982)
Late Pennsylvanian: Stephanian Freshwater France
Smithixerxes
Schram & Rolfe, 1982
S. juliarum
Schram & Rolfe, 1982
Pennsylvanian: Westphalian Brackish to freshwater United States
S. pustulosus
Wilson & Almond, 2001
Pennsylvanian: Westphalian Brackish to freshwater United Kingdom
Mictomeridae
Collette & Hagadorn, 2010[9]
Mictomerus
Collette & Hagadorn, 2010[9]
M. melochevillensis
Collette & Hagadorn, 2010[9]
Cambrian Intertidal Canada
incertae sedis Antarcticarcinus
Collette, Isbell & Miller, 2017[15]
A. pagoda
Collette, Isbell & Miller, 2017[15]
Upper Carboniferous to Lower Permian Pagoda Formation, Antarctica[15]
Apankura
Vaccari, Edgecombe & Escudero, 2004[16]
A. machu
Vaccari, Edgecombe & Escudero, 2004[16]
Cambrian Marine Argentina
Ericixerxes
Gueriau, Lamsdell, Wogelius, Manning, Egerton, Bergmann, Bertrand & Denayer, 2020
E. potii
Gueriau, Lamsdell, Wogelius, Manning, Egerton, Bergmann, Bertrand & Denayer, 2020
Upper Devonian Brackish Belgium
Mosineia
Collette & Hagadorn, 2010[9]
M. macnaughtoni
Collette & Hagadorn, 2010[9]
Cambrian Intertidal United States
Pieckoxerxes
Starobogatov, 1988
P. pieckoae
(Schram & Rolfe, 1982)
Pennsylvanian: Westphalian Brackish to freshwater United States
Sottyxerxes
Schram & Rolfe, 1982
S. multiplex
Schram & Rolfe, 1982
Late Pennsylvanian: Stephanian Freshwater France
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References

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