Liuzhinia Zheng, 1976
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/03FB87D0-D41D-2E4D-F740-FB3CFB115A33 |
treatment provided by |
Felipe |
scientific name |
Liuzhinia Zheng, 1976 |
status |
|
Genus Liuzhinia Zheng, 1976 View in CoL
TYPE SPECIES. — Liuzhinia subovata Zheng,1976 by original designation.
Liuzhinia praeantalyaensis Forel, 2010 ( Fig. 15L, N, O View FIG )
Liuzhinia praeantalyaensis Forel in Crasquin, Forel, Feng, Yuan, Baudin & Collin, 2010a: 253-255, fig. 23Z-B’.
MATERIAL EXAMINED. — Three complete carapaces.
OCCURRENCES. — Kongtongshan section, Fujian Province, China, Late Permian ( Yi 2004); Meishan section, Zhejiang Province, South China, Late Permian ( Crasquin et al. 2010a); sample 08LO02-5, Tham Nam Maholan section, Nam Maholan Formation, Loei Province, northeast Thailand, Early Permian.
DIMENSIONS. — H = 0.29-0.30 mm, L= 0.59- 0.59 mm,H/L = 0.50-0.51
Liuzhinia naramasei Chitnarin , n. sp. ( Figs 13 View FIG A-H; 20)
TYPE MATERIAL. — Holotype, one complete carapace (SUT-09- 2071, Fig.13A View FIG ); paratypes, two complete carapaces (SUT-09-2076, Fig. 13E View FIG and SUT-09-2074, Fig. 13H View FIG ).
ETYMOLOGY. — In honour of Mr Naramase Teerarungsigul, Department of Mineral Resources, Thailand.
MATERIAL EXAMINED. — 29 complete carapaces.
DIMENSIONS. — H = 0.26-0.44 mm, L = 0.52-0.56 mm, H/L = 0.50- 0.58, Holotype: H = 0.26 mm, L = 0.53 mm; Paratype ( Fig. 13E View FIG ): H = 0.26 mm, L = 0.528 mm; Paratype ( Fig. 13H View FIG ): H = 0.27 mm, L = 0.63 mm ( Fig. 20)
TYPE HORIZON. — Sample 07LB09-1, Khao Phu Chong Kho section, Tak Fa Formation, Kungurian, Early Permian.
TYPE LOCALITY. — Khao Phu Chong Kho section (15°22’45’’N, 100°35’12’’E) Tak Fa Formation, Lopburi Province, central Thailand.
OCCURRENCES. — Sample 07 PB03-5 , Khao Kana section, Pha Nok Khao Formation , Phetchabun Province, central Thailand, Early Permian ; sample 08LO07-1, Sak Chai Quarry, Pha Nok Khao Formation , central Thailand, Early Permian ; sample 07LB09-2, Khao Phu Chongko section, Tak Fa Formation , Nakhon Sawan Province, central Thailand, Early Permian ; samples 07LB05-B1 and 07LB05-B2, Ta Kli section, Tak Fa Formation , Nakhon Sawan Province, central Thailand, Early Permian .
DIAGNOSIS. — Species of Liuzhinia with a subtrapezoidal carapace, ADB and PDB straight, AB rounded and laterally flattened, maximum convexity located below mid H, PB acuminate and with maximum of curvature located at VB, ventral area flat.
DESCRIPTION
Carapace small, subtrapezoid; dorsal outline broadly arched; DB straight and gently inclined to posterior; ADB and PDB straight; AB rounded with medium radius of curvature, maximum convexity located below mid H; AVB short and slightly convex;VB straight; AB and AVB laterally flattened;PVB short; PB acuminated and located at VB level; greatest H located anteriorly at one-fourth of length;dorsal outline subfusiform; surface smooth; LV larger and overlap RV all around the carapace;.
REMARKS
The new species differs from Liuzhinia antalyaensis Crasquin- Soleau, 2004 described from the Late Permian-Early Triassic interval of Turkey (Antalya Nappes; Crasquin-Soleau et al. 2004) by having a smaller PB and max H located in front of mid L. It can be compared with L. praeantalyaensis from the latest Permian af Meishan section, Zhejiang Province, South China ( Crasquin et al. 2010a) by having AB located below mid H and the smaller PB but the carapace of L. naramasei Chitnarin , n. sp. is thicker in dorsal view.
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.
Kingdom |
|
Phylum |
|
Class |
|
Order |
|
Family |
Liuzhinia Zheng, 1976
Chitnarin, Anisong, Crasquin, Sylvie, Forel, Marie-Béatrice & Tepnarong, Prachya 2017 |
Liuzhinia praeantalyaensis
CRASQUIN S. & FOREL M. B. & FENG Q. & YUAN A. & BAUDIN F. & COLLIN P. Y. 2010: 253 |