Platykotta Contents Stratigraphy Description Systematics References Navigation menu25°44′N 56°5′E / 25.733°N 56.083°E / 25.733; 56.083"A new Triassic decapod, Platykotta akaina, from the Arabian shelf of the northern United Arab Emirates: earliest occurrence of the Anomura"10.1007/s12542-010-0080-y10.1651/09-3230.120365890172004
AnomuraTriassic crustaceansMonotypic arthropod generaTriassic animals of AfricaNorian first appearancesRhaetian extinctions
speciesdecapodcrustaceanTriassicUnited Arab EmiratesfossilAnomuraholotypeUnited Arab EmiratesMusandam PeninsulaPersian GulfGulf of OmanPermianCretaceousTethys Seacarbonatesedimentary rocksNorianRhaetianburrowsbivalvesMegalodontidaeWallowaconchidaebrachiopodscrinoidsspongescoralsNatural History Museum of GenevaSwitzerlandsternumAstacidealobsterscrayfishGlypheoideaspiny lobstersslipper lobstersAnomuraGalatheidaeChirostylidaesquat lobstersAeglidaecarapacefamilyEocarcinoideacrabcarcinisationAnomura
Platykotta akaina Temporal range: Norian–Rhaetian PreЄ Є O S D C P T J K Pg N | |
|---|---|
Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Arthropoda |
| Subphylum: | Crustacea |
| Class: | Malacostraca |
| Order: | Decapoda |
| Infraorder: | Anomura |
| Superfamily: | Eocarcinoidea |
| Family: | Platykottidae Chablais et al., 2011 |
| Genus: | Platykotta Chablais et al., 2011 |
| Species: | P. akaina |
Binomial name | |
Platykotta akaina Chablais et al., 2011 | |
Platykotta akaina is a species of decapod crustacean from the Triassic of the United Arab Emirates. It is the oldest known fossil from the infraorder Anomura, and is most closely related to Eocarcinus praecursor.[1]
Contents
1 Stratigraphy
2 Description
3 Systematics
4 References
Stratigraphy
The holotype of P. akaina was found in the United Arab Emirates on the Musandam Peninsula – the peninsula which separates the Persian Gulf from the Gulf of Oman. From the Permian to the Cretaceous, the area was near the shore of the Tethys Sea, which produced carbonate sedimentary rocks. The strata that contained Platykotta were part of the Ghalilah Formation, of Norian–Rhaetian age. These rocks contain extensive networks of burrows, and various other fossils, including bivalves of the families Megalodontidae and Wallowaconchidae, brachiopods, crinoids, sponges and corals.[1] The holotype was found at approximately 25°44′N 56°5′E / 25.733°N 56.083°E / 25.733; 56.083 and has been deposited in the Natural History Museum of Geneva, Switzerland.[1]
Description
Platykotta is characterised by a broad, triangular sternum, unlike the very narrow sternum seen in Astacidea (true lobsters and freshwater crayfish) and Glypheoidea. A similar sternal form is seen in the spiny lobsters and slipper lobsters, and also several families of Anomura, including Galatheidae and Chirostylidae (squat lobsters), and Aeglidae. Unlike other anomurans, however, the carapace is considerably longer than wide. The pattern of grooves on the carapace indicates clear affinities with the Anomura.[1]
Systematics
Platykotta is placed in its own family, Platykottidae, which sits alongside Eocarcinidae (containing only Eocarcinus) in the superfamily Eocarcinoidea. Eocarcinus was previously treated as the earliest true crab, but is now thought, like Platykotta, to show too little carcinisation to be a true crab, and is placed instead among the Anomura.[2]
References
^ abcd Jérôme Chablais, Rodney M. Feldmann & Carrie E. Schweitzer (2011). "A new Triassic decapod, Platykotta akaina, from the Arabian shelf of the northern United Arab Emirates: earliest occurrence of the Anomura" (PDF). Paläontologische Zeitschrift. 85: 93–102. doi:10.1007/s12542-010-0080-y..mw-parser-output cite.citationfont-style:inherit.mw-parser-output .citation qquotes:"""""""'""'".mw-parser-output .citation .cs1-lock-free abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .citation .cs1-lock-limited a,.mw-parser-output .citation .cs1-lock-registration abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .citation .cs1-lock-subscription abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registrationcolor:#555.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration spanborder-bottom:1px dotted;cursor:help.mw-parser-output .cs1-ws-icon abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/12px-Wikisource-logo.svg.png")no-repeat;background-position:right .1em center.mw-parser-output code.cs1-codecolor:inherit;background:inherit;border:inherit;padding:inherit.mw-parser-output .cs1-hidden-errordisplay:none;font-size:100%.mw-parser-output .cs1-visible-errorfont-size:100%.mw-parser-output .cs1-maintdisplay:none;color:#33aa33;margin-left:0.3em.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-formatfont-size:95%.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-leftpadding-left:0.2em.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-rightpadding-right:0.2em
^ Rodney M. Feldmann & Carrie E. Schweitzer (2010). "Is Eocarcinus Withers, 1932, a basal brachyuran?". Journal of Crustacean Biology. 30 (2): 241–250. doi:10.1651/09-3230.1.
Anomura, Monotypic arthropod genera, Norian first appearances, Rhaetian extinctions, Triassic animals of Africa, Triassic crustaceansUncategorized
