Acratia chongpani Chitnarin, 2017
publication ID |
https://doi.org/ 10.5252/g2017n4a1 |
publication LSID |
urn:lsid:zoobank.org:pub:DB464417-3EA1-4C4E-9C03-624C1627969C |
persistent identifier |
https://treatment.plazi.org/id/94C48BFA-B847-4D24-A665-B0D5390E476C |
taxon LSID |
lsid:zoobank.org:act:94C48BFA-B847-4D24-A665-B0D5390E476C |
treatment provided by |
Felipe |
scientific name |
Acratia chongpani Chitnarin |
status |
sp. nov. |
Acratia chongpani Chitnarin , n. sp.
( Figs 21 View FIG A-G; 22)
Acratina guseva e Kozur, 1985b: 104, pl. 20, fig. 1. — Crasquin- Soleau & Baud 1998: pl. 3, fig. 1. n. syn.
TYPE MATERIAL. — Holotype, one complete carapace (SUT-09- 2006, Fig.21A View FIG ); paratypes, two complete carapaces (SUT-09-2001, Fig. 21E View FIG and SUT-09-2013, Fig. 21F View FIG ).
ETYMOLOGY. — In honour of Dr Chongpan Chonglakmani, Thailand.
MATERIAL EXAMINED. — 51 complete carapaces.
DIMENSIONS. — H = 0.25-0.51 mm, L = 0.66-1.18 mm, H/L = 0.43- 0.53, Holotype: H = 0.73 mm, L = 1.08 mm; Paratype ( Fig. 21F View FIG ): H = 0.42 mm, L = 0.60 mm; Paratype ( Fig. 21E View FIG ): H = 0.58 mm, L = 0.90 mm ( Fig. 22).
TYPE HORIZON. — Sample 07LB05-6, Ta Kli section, Tak Fa Formation, Early Permian.
TYPE LOCALITY. — Ta Kli section (15°19’05’’N, 100°22’46’’E), Tak Fa Formation, Nakhon Sawan Province, central Thailand.
OCCURRENCES. — Hydra Island , Greece, late Middle Permian (Crasquin-Soleau & Baud 1998) ; sample 08LO07-3, Sak Chai section, Pha Nok Khao Formation, Chiyaphum Province, northeast Thailand, Early Permian ; samples 07 PB03-2 , 07 PB03-3 and 07 PB03-5 , Khao Kana section, Pha Nok Khao Formation, Phetchabun Province, central Thailand, Early Permian ; sample 07LB05-6, Ta Kli section, Tak Fa Formation, Nakhon Sawan Province, central Thailand, Early Permian ; sample 08LB01-1, Khao Som Phot section, Tak Fa Formation, Lopburi Province, central Thailand, Middle Permian .
DIAGNOSIS. — Species of Acratia with a laterally flattened, long, hook-like AB, pointing downward, and located at lower 30% of H, angle between AVB and VB is 150° and PB is located at ventral level. DESCRIPTION
Carapace long and large; dorsal outline broadly arched; DB slightly convex on LV, straight on RV which gently inclined rearward at 15-20°; ADB convex and with an angle of 140° with DB; PDB convex and with an angle of 140° with DB; AB of a hook-like shape, maximum convexity located at lower third of H, AB flattened laterally; AVB long and making an angle of 150°with VB; VB straight to slightly concave; ventral area flat; PVB short in extension of VB; PB bluntly round and located at VB; maximum H located in front of mid L; surface smooth; LV larger and overlapping RV at ADB and PDB; carapace subfusiform in dorsal view.
REMARKS
Acratia chongpani Chitnarin , n. sp. can be compared to A. praetypica Posner, 1951 from the Early Carboniferous of Moscow Basin, Russia ( Posner 1951: 98, pl. 21, fig. 9) in lateral outline. Differences occur at VB which is blunt in A. chongpani but raised upward in A. praetypica , and at the angle between AVB and VB which is of 150° in the former species but of 140° in the latter. Acratina guseva e Kozur sensu Crasquin-Soleau & Baud 1998 is included to A. chongpani Chitnarin , n. sp. due tothe smaller AVB and the shorter PVB than those in Acratina guseva e Kozur, 1985.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Acratia chongpani Chitnarin
Chitnarin, Anisong, Crasquin, Sylvie, Forel, Marie-Béatrice & Tepnarong, Prachya 2017 |
Acratina guseva
KOZUR H. 1985: 104 |