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Dalmanites

Dalmanites is a genus of trilobite in the order Phacopida. They lived from the Late Ordovician to Middle Devonian.[1]

Dalmanites
Temporal range: Late OrdovicianMiddle Devonian, 449.5–376.1 Ma[1]
Specimen of Dalmanites limulurus
Scientific classification
Kingdom: Animalia
Phylum: Arthropoda
Class: Trilobita
Order: Phacopida
Family: Dalmanitidae
Genus: Dalmanites
Barrande, 1852
Species
  • D. caudatus (Bruennich, 1781) (type) = Trilobus caudatus
  • D. corrugatus (Reed, 1901)
  • D. halli (Weller, 1907)
  • D. limulurus (Green, 1832)
  • D. myops (Koenig, 1825)
  • D. nexilus Salter, 1864
  • D. obtusus (Lindstroem, 1885)
  • D. platycaudatus Weller, 1907
  • D. rutellum Campbell, 1967
  • D. socialis Barrande

The trilobites of this genus have slightly convex exoskeletons with an average length of 4–7 cm (1.5–3 in). The cephalon is semicircular or parabolic. The glabella (center portion of the head) is often pear-shaped, and tapers outward toward the front. The glabella also always contains three pairs of obvious glabellar furrows. Also prominent are the large mosaic (schizochroal) eyes.

The thorax is composed of eleven segments, with the relatively large pygidium with a slender axis of 11 to 16 rings and 6 or 7 pleural ribs. The pygidium ends in a striking tail spike.

Taxonomy

Species previously assigned to Dalmanites

Some species formerly included in Dalmanites have now been reassigned to other genera.

Description

 
Specimen with preserved limbs

Dalmanites is genus of trilobites with an average (about 8 centimetres or 3.1 inches long), moderately vaulted exoskeleton with an inverted egg-shaped outline (about 1.5× longer than wide). Its headshield (or cephalon) is semicircular, with robust (genal) spines extending from the side of the cephalon back to approximately the 8th thorax segment. The frontal margin of the cephalon is semicircular to parabolic, and it may have a simple and short anterior extension. The facial suture lies inside or touches the preglabellar furrow. The frontal lobe of the central raised area of the cephalon (or glabella) is much wider than the other lobes. The frontal lobe is vaulted. The eye is moderate to large, about half as long as the cheek. The "seem" that is visible from the ventral side (or doublure) is wide and flat, and has a deep and wide antennal furrow. The "palate" (or hypostome), also only visible from the ventral side, is subtriangular (about as long as wide) and adorned with three weak denticles at its back rim. To the front the hypostome has weak wings extending sideways. The thorax consists of 11 segments. The tips of the segments are pointed and angle back increasingly from about 30° for the anterior segment to slightly pointing inwards for the posterior segment. The tailshield (or pygidium) is large, subtriangular, and about ⅔-¾× as long as wide. The axis is vaulted and ±35% of the width of the pygidium and consists of 12-15 rings. 9–10 deep and wide pleural furrows have flat or only slightly concave bottoms. The furrows within each pleural rib (or interpleural furrows) are very narrow. The frontal band of each pleural rib is more vaulted and broader than the rear band. The pleural furrows almost reach the margin. The pygidial termination (or mucro) is vaulted and more or less pointed into a spine, which may differ between species. The entire exoskeleton is covered in fine and coarse granules.[8] A specimen of an indeterminate species with preserved soft tissue is known from the Silurian aged Coalbrookdale Formation of England. The antennae are not preserved, though biramous limb pairs are preserved, three are present on the cephalon, 11 on the thorax and at least 3 on the pygidium. The thoracic pairs become smaller posteriorly. The exopods of the limbs bear filamentous structures, which appear to be joined with each other by a membrane.[9]

References

  1. ^ a b Dalmanites at Fossilworks.org
  2. ^ "Dalmanites lapeyrei Bureau 1889". Global Names Index.
  3. ^ Carvalho, M.G.P.; Fonseca, V.M.M. (2007). "The Trilobite "Dalmanites" maecurua (Middle Devonian, Amazon Basin, Brazil) and the New Genus Amazonaspis (Synphoriidae)". American Museum Novitates (3591): 1–14. doi:10.1206/0003-0082(2007)3591[1:TTDMCM]2.0.CO;2. ISSN 0003-0082. S2CID 198159893. Retrieved 2014-01-07.
  4. ^ Edgecombe, G.D. (1993). "Silurian Acastacean trilobites of the Americas" (PDF). Journal of Paleontology. 67 (4): 535–548. doi:10.1017/S0022336000024884. S2CID 132918487. Retrieved 2014-01-09.
  5. ^ Lieberman, B.S.; Kloc, G.J. (1997). "Evolutionary and biogeographical patterns in the Asteropyginae (Trilobita, Devonian) Delo, 1935". Bulletin of the American Museum of Natural History. 232. hdl:2246/1623. Retrieved 16 December 2013.
  6. ^ Corbacho, Joan (2011). (PDF). Batelleria. 16: 16–31. Archived from the original (PDF) on 2014-12-20.
  7. ^ Sandford, Andrew C.; Holloway, David J. (2006). "Early Silurian phacopide trilobites from central Victoria, Australia" (PDF). Memoirs of the Museum of Victoria. 63 (2): 215–255. doi:10.24199/j.mmv.2006.63.17.[permanent dead link]
  8. ^ Budil, Petr; Thomas, Alan Trevor; Hörbinger, František (2008). "Exoskeletal architecture, hypostomal morphology and mode of life of Silurian and Lower Devonian dalmanited trilobites" (PDF). Bulletin of Geosciences. 83 (1): 2–10. doi:10.3140/bull.geosci.2008.01.001. Retrieved 2014-01-07.
  9. ^ Siveter, Derek J.; Fortey, Richard A.; Briggs, Derek E. G.; Siveter, David J.; Sutton, Mark D. (November 2021). Zhang, Xi‐Guang (ed.). "The first Silurian trilobite with three‐dimensionally preserved soft parts reveals novel appendage morphology". Papers in Palaeontology. 7 (4): 2245–2253. doi:10.1002/spp2.1401. ISSN 2056-2799. S2CID 239718706.

dalmanites, genus, trilobite, order, phacopida, they, lived, from, late, ordovician, middle, devonian, temporal, range, late, ordovician, middle, devonian, preꞒ, nspecimen, limulurusscientific, classificationkingdom, animaliaphylum, arthropodaclass, trilobitao. Dalmanites is a genus of trilobite in the order Phacopida They lived from the Late Ordovician to Middle Devonian 1 DalmanitesTemporal range Late Ordovician Middle Devonian 449 5 376 1 Ma 1 PreꞒ Ꞓ O S D C P T J K Pg NSpecimen of Dalmanites limulurusScientific classificationKingdom AnimaliaPhylum ArthropodaClass TrilobitaOrder PhacopidaFamily DalmanitidaeGenus DalmanitesBarrande 1852SpeciesD caudatus Bruennich 1781 type Trilobus caudatusD corrugatus Reed 1901 D halli Weller 1907 D limulurus Green 1832 D myops Koenig 1825 D nexilus Salter 1864D obtusus Lindstroem 1885 D platycaudatus Weller 1907D rutellum Campbell 1967D socialis BarrandeThe trilobites of this genus have slightly convex exoskeletons with an average length of 4 7 cm 1 5 3 in The cephalon is semicircular or parabolic The glabella center portion of the head is often pear shaped and tapers outward toward the front The glabella also always contains three pairs of obvious glabellar furrows Also prominent are the large mosaic schizochroal eyes The thorax is composed of eleven segments with the relatively large pygidium with a slender axis of 11 to 16 rings and 6 or 7 pleural ribs The pygidium ends in a striking tail spike Contents 1 Taxonomy 1 1 Species previously assigned to Dalmanites 2 Description 3 ReferencesTaxonomy EditSpecies previously assigned to Dalmanites Edit Some species formerly included in Dalmanites have now been reassigned to other genera D lapeyrei Zeliszkella torrubiae 2 D maecurua Amazonaspis maecurua 3 D micheli Phacopidina micheli 4 D pleione Bellacartwrightia pleione 5 D torrubiae Zeliszkella torrubiae 6 D weaveri var tenuimucronata Bessazoon tenuimucronata 7 Description Edit Specimen with preserved limbs Dalmanites is genus of trilobites with an average about 8 centimetres or 3 1 inches long moderately vaulted exoskeleton with an inverted egg shaped outline about 1 5 longer than wide Its headshield or cephalon is semicircular with robust genal spines extending from the side of the cephalon back to approximately the 8th thorax segment The frontal margin of the cephalon is semicircular to parabolic and it may have a simple and short anterior extension The facial suture lies inside or touches the preglabellar furrow The frontal lobe of the central raised area of the cephalon or glabella is much wider than the other lobes The frontal lobe is vaulted The eye is moderate to large about half as long as the cheek The seem that is visible from the ventral side or doublure is wide and flat and has a deep and wide antennal furrow The palate or hypostome also only visible from the ventral side is subtriangular about as long as wide and adorned with three weak denticles at its back rim To the front the hypostome has weak wings extending sideways The thorax consists of 11 segments The tips of the segments are pointed and angle back increasingly from about 30 for the anterior segment to slightly pointing inwards for the posterior segment The tailshield or pygidium is large subtriangular and about as long as wide The axis is vaulted and 35 of the width of the pygidium and consists of 12 15 rings 9 10 deep and wide pleural furrows have flat or only slightly concave bottoms The furrows within each pleural rib or interpleural furrows are very narrow The frontal band of each pleural rib is more vaulted and broader than the rear band The pleural furrows almost reach the margin The pygidial termination or mucro is vaulted and more or less pointed into a spine which may differ between species The entire exoskeleton is covered in fine and coarse granules 8 A specimen of an indeterminate species with preserved soft tissue is known from the Silurian aged Coalbrookdale Formation of England The antennae are not preserved though biramous limb pairs are preserved three are present on the cephalon 11 on the thorax and at least 3 on the pygidium The thoracic pairs become smaller posteriorly The exopods of the limbs bear filamentous structures which appear to be joined with each other by a membrane 9 References Edit Paleontology portal Paleozoic portal a b Dalmanites at Fossilworks org Dalmanites lapeyrei Bureau 1889 Global Names Index Carvalho M G P Fonseca V M M 2007 The Trilobite Dalmanites maecurua Middle Devonian Amazon Basin Brazil and the New Genus Amazonaspis Synphoriidae American Museum Novitates 3591 1 14 doi 10 1206 0003 0082 2007 3591 1 TTDMCM 2 0 CO 2 ISSN 0003 0082 S2CID 198159893 Retrieved 2014 01 07 Edgecombe G D 1993 Silurian Acastacean trilobites of the Americas PDF Journal of Paleontology 67 4 535 548 doi 10 1017 S0022336000024884 S2CID 132918487 Retrieved 2014 01 09 Lieberman B S Kloc G J 1997 Evolutionary and biogeographical patterns in the Asteropyginae Trilobita Devonian Delo 1935 Bulletin of the American Museum of Natural History 232 hdl 2246 1623 Retrieved 16 December 2013 Corbacho Joan 2011 Trilobites from the Upper Ordovician of Bou Nemrou El Kaid Errami Morocco Trilobites del Ordovicico Superior de Bou Nemrou El Kaid Errami Marruecos PDF Batelleria 16 16 31 Archived from the original PDF on 2014 12 20 Sandford Andrew C Holloway David J 2006 Early Silurian phacopide trilobites from central Victoria Australia PDF Memoirs of the Museum of Victoria 63 2 215 255 doi 10 24199 j mmv 2006 63 17 permanent dead link Budil Petr Thomas Alan Trevor Horbinger Frantisek 2008 Exoskeletal architecture hypostomal morphology and mode of life of Silurian and Lower Devonian dalmanited trilobites PDF Bulletin of Geosciences 83 1 2 10 doi 10 3140 bull geosci 2008 01 001 Retrieved 2014 01 07 Siveter Derek J Fortey Richard A Briggs Derek E G Siveter David J Sutton Mark D November 2021 Zhang Xi Guang ed The first Silurian trilobite with three dimensionally preserved soft parts reveals novel appendage morphology Papers in Palaeontology 7 4 2245 2253 doi 10 1002 spp2 1401 ISSN 2056 2799 S2CID 239718706 Retrieved from https en wikipedia org w index php title Dalmanites amp oldid 1139847964, wikipedia, wiki, book, books, library,

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