Arthropleuridea

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Arthropleuridea
Temporal range: Late Silurian - Sakmarian 423–290  Ma
Arthropleura 1914.jpg
Arthropleura fossil illustration
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Subphylum: Myriapoda
Class: Diplopoda
Subclass: Arthropleuridea
Waterlot, 1934
Orders

Arthropleuridea is an extinct subclass of myriapod arthropods that flourished during the Carboniferous period, having first arisen during the Silurian, and perishing in the Early Permian. [1] Members are characterized by possessing diplosegement (fused "double segments", as in modern-day millipedes) paranotal tergal lobes separated from the body axis by a suture, and by sclerotized plates buttressing the leg insertions. Despite their unique features, recent phylogenetic research suggests Arthropleuridea be included among millipedes in the class Diplopoda. [2] [3] The subclass contains three recognized orders, each with a single genus. [4]

Paleobiology

Arthropleurids lived in the moist coal swamps that were common at the time and may have burrowed in the undergrowth. They were either herbivores or detritivores. Besides their size, their most distinguishing features were their legs with eight segments (as many as 30 pairs) and extremely tough exoskeletons. There is no evidence of spiracles, so the animals must have used lungs or gills for respiration. [3]

Most arthropleurideans are thought to have been terrestrial, although, without any known respiratory structure, terrestriality is assumed only by analogy to modern arthropods. [5] Early forms, however, including Eoarthropleura (order Eoarthropleurida), appear to have been aquatic.[ citation needed ] For this reason, some question Arthropleuridea's inclusion among millipedes because no modern aquatic myriapods are known. [3]

Distribution and size

Arthropleuridea is most famous for Arthropleura (order Arthropleurida). Tracks from Arthropleura up to 50 cm wide have been found at Joggins, Nova Scotia. [6] Reaching over 2 meters in length, arthropleurids are among the largest arthropods ever to have lived. The lack of large terrestrial vertebrate predators and the highly oxygenic atmosphere at that time probably enabled them to grow so large. [7] It was previously believed that Arthropleura became extinct as the coal swamps dried out. [3] However, many fossils have been discovered after the Carboniferous rainforest collapse. A more recent proposal is that predation by tetrapods and the aridification of the equator caused it to become extinct. [1] [8] Arthropleura has been found from the Upper Carboniferous of Europe and North America.

Eoarthropleura has been found from the Upper Silurian through the Upper Devonian of Europe and North America. [9]

Microdecemplex , of the order Microdecemplicida, was dwarfed by the other Arthropleurideans, at just a few millimeters long. The genus is known from the Middle through Upper Devonian of New York state, USA. [4]

Classification and placement

After several decades of uncertainty, Arthropleuridea was placed within the Diplopoda in the year 2000. [10] However, there is still controversy regarding the relationships of the three orders to living millipede groups. [2] [11] Some authors place Arthropleuridea within the Chilognatha, as a sister group to all living Chilognathan millipedes (Pentazonia + Helminthomorpha). [10] [12] An alternate hypothesis breaks up the subclass: placing the orders Arthropleurida and Eoarthropleurida within the basal Penicillata (as sister to the living Polyxenida), and leaving only Microdecemplicida as a sister group to the living Chilognatha. [13] Under this hypothesis, Arthropleuridea would be paraphyletic.

See also

Related Research Articles

<span class="mw-page-title-main">Millipede</span> Class of arthropods

Millipedes are a group of arthropods that are characterised by having two pairs of jointed legs on most body segments; they are known scientifically as the class Diplopoda, the name derived from this feature. Each double-legged segment is a result of two single segments fused together. Most millipedes have very elongated cylindrical or flattened bodies with more than 20 segments, while pill millipedes are shorter and can roll into a tight ball. Although the name "millipede" derives from Latin for "thousand feet", no species was known to have 1,000 or more until the discovery in 2020 of Eumillipes persephone, which can have over 1,300 legs. There are approximately 12,000 named species classified into 16 orders and around 140 families, making Diplopoda the largest class of myriapods, an arthropod group which also includes centipedes and other multi-legged creatures.

<span class="mw-page-title-main">Chilognatha</span> Subclass of millipedes

Chilognatha is a subclass of the class Diplopoda, which includes the vast majority of extant millipedes, about 12,000 species.

<span class="mw-page-title-main">Myriapoda</span> Subphylum of arthropods

Myriapods are the members of subphylum Myriapoda, containing arthropods such as millipedes and centipedes. The group contains about 13,000 species, all of them terrestrial.

<span class="mw-page-title-main">Pill millipede</span> Order of millipedes

Pill millipedes are any members of two living orders of millipedes, often grouped together into a single superorder, Oniscomorpha. The name Oniscomorpha refers to the millipedes' resemblance to certain woodlice (Oniscidea), also called pillbugs or "roly-polies". However, millipedes and woodlice are not closely related ; rather, this is a case of convergent evolution.

<i>Arthropleura</i> Extinct genus of many-legged arthropods

Arthropleura is an extinct genus of massive millipedes that lived in what is now North America and Europe around 345 to 290 million years ago, from the Viséan stage of the lower Carboniferous Period to the Sakmarian stage of the lower Permian Period. The species of the genus are the largest known land invertebrates of all time, and would have had few, if any, predators.

Euphoberia is an extinct genus of millipede from the Pennsylvanian epoch of the Late Carboniferous, measuring up to 15 centimetres (5.9 in) in length, that is small in Euphoberiidae which contains species with length about 30 centimetres (12 in). Fossils have been found in Europe and North America.

<i>Pneumodesmus</i> Genus of millipedes

Pneumodesmus newmani is a species of myriapod that lived during the late Wenlock epoch of the Silurian period around 428 million years ago. Although a 2017 study dates its occurrence based on zircon data analysis as the Early Devonian (Lochkovian), the 2023 study confirmed the age identification of the 2004 study through palynological, palaeobotanical and ziron analyses incorporating newly discovered additional data. It is one of the first myriapods, and among the oldest creatures to have lived on land. It was discovered in 2004, and is known from a single specimen from Stonehaven, Aberdeenshire, Scotland.

Eoarthropleura was a genus of millipede-like creatures which lived between the Late Silurian and Late Devonian periods. It reached 100 mm (3.9 in) in length. Fossils, mainly of cuticle fragments, have been found in Europe and North America. It is the earliest known member of the Arthropleuridea, and the oldest known terrestrial animal of North America.

<span class="mw-page-title-main">Euthycarcinoidea</span> Extinct order of arthropods

Euthycarcinoidea are an enigmatic group of extinct possibly amphibious arthropods that ranged from Cambrian to Triassic times. Fossils are known from Europe, North America, Argentina, Australia and Antarctica.

<span class="mw-page-title-main">Polyxenida</span> Order of millipedes

Polyxenida is an order of millipedes readily distinguished by a unique body plan consisting of a soft, non-calcified body ornamented with tufts of bristles – traits that have inspired the common names "bristly millipedes" or "pincushion millipedes". There are at least 86 species in four families worldwide, and are the only living members of the subclass Penicillata.

<span class="mw-page-title-main">Archipolypoda</span> Extinct group of millipedes

Archipolypoda is an extinct group of millipedes known from fossils in Europe and North America and containing the earliest known land animals. The Archipolypoda was erected by Scudder (1882) but redefined in 2005 with the description of several new species from Scotland. Distinguishing characteristics include relatively large eyes with densely packed ocelli, and modified leg pairs on the 8th body ring. Some species had prominent spines while others had a flattened appearance.

<span class="mw-page-title-main">Zosterogrammidae</span> Extinct family of millipedes

Zosterogrammidae is an extinct family of millipedes containing three genera, each with a single species. Fossils are known from the Czech Republic, Scotland, and the USA. Zosterogrammidae constitutes the sole family of the order Zosterogrammida.

The Panther Mountain Formation is a geologic formation in New York. It preserves fossils dating back to the Devonian period. It is located in the counties of Albany, Madison, Oneida, Otsego, and Schoharie. It is well known for its fossil arthropods preserved as flattened cuticles, including Attercopus and Dracochela.

<i>Microdecemplex</i> Genus of millipedes

Microdecemplex rolfei is the only known species of the extinct, small-bodied millipede order Microdecemplicida, a member of the extinct subclass Arthropleuridea. Fossils, measuring less than 5 mm in length, are known from the Panther Mountain Formation of New York State, dating to the Middle Devonian. This species apparently lacks antennae and shows sexual dimorphism in its hind legs, which may be similar in function to the telopods of male living pill-millipedes that are used to grasp females during mating.

<span class="mw-page-title-main">Euphoberiidae</span> Extinct family of millipedes

Euphoberiidae is an extinct family of archipolypodan millipedes known from the Upper Pennsylvanian of Europe and North America. The family includes relatively large millipedes measuring up to 30 cm (12 in) long bearing distinctive spines and were the dominant millipedes of the Pennsylvanian.

<span class="mw-page-title-main">Juliformia</span> Suborder of millipedes

Juliformia is a taxonomic superorder of millipedes containing three living orders: Julida, Spirobolida, and Spirostreptida, and the extinct group Xyloiuloidea known only from fossils.

William Albert Shear is Trinkle Professor Emeritus at Hampden-Sydney College, Virginia. He is a spider and myriapod expert who has published more than 200 scientific articles primarily on harvestman and millipede taxonomy.

<i>Necrogammarus</i> Extinct genus of arthropods

Necrogammarus salweyi is the binomial name applied to an arthropod fossil discovered in Herefordshire, England. The fossil represents a fragmentary section of the underside and an appendage of a pterygotid eurypterid, a group of large and predatory aquatic arthropods that lived from the late Silurian to the late Devonian. The Necrogammarus fossil is Late Silurian in age and its generic name means "dead lobster", deriving from Ancient Greek νεκρός and Latin gammarus ("lobster").

<i>Kampecaris</i> Extinct genus of myriapod

Kampecaris is an extinct genus comprising the Kampecarida, an enigmatic group of millipede-like arthropods, from the Silurian and early Devonian periods of Scotland and England. They are among the oldest known land-dwelling animals. They were small, short-bodied animals with three recognizable sections: an oval head divided along the midline, ten limb-bearing segments forming a cylindrical trunk that tapered slightly towards the front, and a characteristic swollen tail formed by a modified segment that tapers at its rear into an "anal segment". The cuticle forming their exoskeletons was thick, heavily calcified, and composed of two layers.

References

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  2. 1 2 Shear, William A.; Edgecombe, Gregory D. (2010). "The geological record and phylogeny of the Myriapoda". Arthropod Structure & Development. 39 (2–3): 174–190. doi:10.1016/j.asd.2009.11.002. PMID   19944188.
  3. 1 2 3 4 Kazlev, M. Alan. "Class? and Order Arthropleurida". Palaeos. Archived from the original on 13 March 2006. Retrieved 2006-04-12.
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  5. Fortey, Richard; R. H. Thomas (1998). Arthropod Relationships. Springer. ISBN   0-412-75420-7.
  6. "The Excitement of Discovery". Virtual Museum of Canada. Archived from the original on February 4, 2012. Retrieved 2006-04-17.
  7. M. G. Lockley & Christian Meyer (2013). "The tradition of tracking dinosaurs in Europe". Dinosaur Tracks and Other Fossil Footprints of Europe. Columbia University Press. pp. 25–52. ISBN   9780231504607.
  8. Schneider, Joerg; Lucas, Spencer; Werneburg, Ralf; Rößler, Ronny (2010-05-01). "Euramerican Late Pennsylvanian/Early Permian arthropleurid/tetrapod associations – implications for the habitat and paleobiology of the largest terrestrial arthropod". New Mexico Museum of Natural History and Science Bulletin. 49: 49–70.
  9. William Shear & Paul Selden (1995). "Eoarthropleura (Arthropoda, Arthropleurida) from the Silurian of Britain and the Devonian of North America" (PDF). Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen. 196 (3): 347–375. doi:10.1127/njgpa/196/1995/347.
  10. 1 2 Wilson, Heather M.; Shear, William A. (2000). "Microdecemplicida, a new order of minute arthropleurideans (Arthropoda: Myriapoda) from the Devonian of New York State, U.S.A.". Transactions of the Royal Society of Edinburgh: Earth Sciences. 90 (4): 351–375. doi:10.1017/S0263593300002674. S2CID   129597005.
  11. Sierwald, Petra; Bond, Jason E. (2007). "Current Status of the Myriapod Class Diplopoda (Millipedes): Taxonomic Diversity and Phylogeny". Annual Review of Entomology. 52 (1): 401–420. doi:10.1146/annurev.ento.52.111805.090210. PMID   17163800.
  12. Hoffman, RL (1969). "Myriapoda, exclusive of Insecta". In RC Moore (ed.). Treatise on Invertebrate Paleontology, Pt. R, Arthropoda 4. Lawrence: Geol. Soc. Am./Univ. Kans. Press. pp. R572–606.
  13. Kraus, O; C. Brauckman (2003). "Fossil giants and surviving dwarfs. Arthropleurida and Pselaphognatha (Ateolocerata, Diplopoda): characters, phylogenetic relationships and construction". Verh. Naturwiss. Ver. Hamburg. 40 (5): 5–50.