taxonID	type	description	language	source
6A0387BAFFCAFFDA89600198FBDDFDC8.taxon	materials_examined	TYPE SPECIES. — Bairdia curta McCoy, 1844.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCAFFDF897002FEFDDEFD9E.taxon	materials_examined	TYPE MATERIAL. — Holotype: one complete carapace (P 6 M 2607; Fig. 3 J); paratype: one complete carapace (P 6 M 2603; Fig. 3 I).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCAFFDF897002FEFDDEFD9E.taxon	etymology	ETYMOLOGY. — Dedicated to Jean-Charles Forel, personal dedication.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCAFFDF897002FEFDDEFD9E.taxon	materials_examined	MATERIAL EXAMINED. — 26 complete carapaces and 1 single valve. DIMENSIONS. — L = 435 to 1120 µm; H = 260 to 680 µm. Holotype: L = 453 µm; H = 276 µm. Paratype: L = 895 µm; H = 535 µm. TYPE HORIZON. — Sample 06 Ti 08, unit IIIb, Tulong Formation, Smithian, Lower Triassic. TYPE LOCALITY. — Tulong section, Southern Tibet. OCCURRENCE. — Tulong section, southernTibet. Samples 06 Ti 04, 06 Ti 08, 06 Ti 21, 06 Ti 27 - 31, 06 Ti 35, Tulong Formation, units III, V and VI, Smithian to Anisian, Lower-Middle Triassic.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCAFFDF897002FEFDDEFD9E.taxon	diagnosis	DIAGNOSIS. — A punctate species of Bairdia with faint overlap, AB and PB with quite small radius of curvature, PDB, BD and ADB straight at RV.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCAFFDF897002FEFDDEFD9E.taxon	description	DESCRIPTION RV: PDB, DB and ADB straight; AB regularly arched with maximum of curvature located in its middle; AVB and PVB regularly convex; VB concave complete carapace (P 6 M 2599); F - H, Bairdia finalyi (Méhes, 1911); F, right lateral view of a complete carapace (P 6 M 2601); G, right lateral view of a complete carapace (P 6 M 2602); H, right lateral view of a complete carapace (P 6 M 2606); I - L, Bairdia jeancharlesi Forel n. sp.; I, paratype (P 6 M 2603), right lateral view of a complete carapace; J, holotype (P 6 M 2607), right lateral view of a complete carapace; K, right lateral view of a broken carapace (P 6 M 2604); L, right lateral view of a complete carapace (P 6 M 2605); M, Spinocypris vulgaris Kozur, 1971, right lateral view of a complete carapace (P 6 M 2600). Scale bars: 100 μm. TABLE 1. — Distribution chart and abundances of Lower and Middle Triassic ostracods in the Tulong section. The global extension of each species within the section is represented with grey parts. Abundances are indicated as follows: z, between 1 and 5 specimens; Ƃ, between 5 and 10 specimens; ¡, between 10 and 20 specimens; ×, more than 20 specimens. in its anterior part; PB with quite small radius of curvature but bairdoid beak poorly expressed. LV: PDB straight, DB regularly arched, ADB straight to gently arched, AB rounded with maximum of curvature in its middle; AVB, VB and PVB arched; PB with quite small radius of curvature. Carapace ornamented by small punctations, flattened laterally in posterior and anterior parts; overlap is small with maximum in anterior part of DB; H / L = 0.61.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCAFFDF897002FEFDDEFD9E.taxon	discussion	REMARKS	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDF8A90023EFC38FD01.taxon	materials_examined	TYPE MATERIAL. — Holotype: one complete carapace (P 6 M 2596; Fig. 3 A); paratype: one complete carapace (P 6 M 2595; Fig. 3 B).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDF8A90023EFC38FD01.taxon	etymology	ETYMOLOGY. — Dedicated to Béatrice Letang, personal dedication.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDF8A90023EFC38FD01.taxon	materials_examined	MATERIAL EXAMINED. — 7 complete carapaces and 2 single valves. DIMENSIONS. — L = 540 - 785 µm; H = 320 - 500 µm. Holotype: L = 785 µm; H = 492 µm. Paratype: L = 540 µm; H = 320 µm. TYPE HORIZON. — Sample 06 Ti 30, unit VI, Tulong Formation, Early Anisian, Middle Triassic. TYPE LOCALITY. — Tulong section, Southern Tibet. OCCURRENCE. — Tulong section, Southern Tibet. Samples 06 Ti 21, 06 Ti 30, 06 Ti 31 and 06 Ti 34, Tulong Formation, units V and VI, Spathian-Anisian, Early-Middle Triassic.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDF8A90023EFC38FD01.taxon	diagnosis	DIAGNOSIS. A massive species of ornamented Bairdia with AB and PB flattened, large reticulation on all the carapace except the dorsal margin.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDF8A90023EFC38FD01.taxon	description	DESCRIPTION At RV, PDB straight, DB long and more or less horizontal, ADB straight to gently concave. At LV all dorsal parts form a regular arch. AB with quite small radius of curvature; AVB and PDB regularly arched; VB straight at LV, gently concave RV; PB with medium radius of curvature; maximum of curvature of PB and AB located at the same H; carapace strongly compressed along free margins and particularly in AB and PB; surface ornamented by a large reticula- tion, this reticulation is present on all the surface except for dorsal margins of both valves.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDF8A90023EFC38FD01.taxon	discussion	REMARKS	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDF888C02BEFC3AFCB0.taxon	materials_examined	TYPE SPECIES. — Petasobairdia bicornuta Chen, 1982 (in Chen & Shi 1982).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDE897303FDFDFAFC45.taxon	materials_examined	TYPE MATERIAL. — Holotype: one complete carapace (P 6 M 2615; Fig. 4 M); paratype: one complete carapace (P 6 M 2619; Fig. 4 J).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDE897303FDFDFAFC45.taxon	etymology	ETYMOLOGY. — Dedicated to Dr Pierre-Yves Collin, Université Pierre et Marie Curie, Paris.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDE897303FDFDFAFC45.taxon	materials_examined	MATERIAL EXAMINED. — 18 complete carapaces and 20 isolated valves. DIMENSIONS. — L = 630 - 1140 µm; H = 350 - 700 µm. Holotype: L = 1030 µm; H = 680 µm. Paratype: L = 848 µm; H = 546 µm. TYPE HORIZON. — Sample 06 Ti 30, unit VI, Tulong Formation, Early Anisian, Middle Triassic. TYPE LOCALITY. — Tulong section, Southern Tibet. OCCURRENCE. — Tulong section, Southern Tibet. Samples 06 Ti 21, 06 Ti 25, 06 Ti 30, 06 Ti 32, 06 Ti 33, Tulong Formation, units V and VI, Spathian-Anisian, Early- Middle Triassic.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDE897303FDFDFAFC45.taxon	diagnosis	DIAGNOSIS. — A species of Petasobairdia with slight dorsal blade at LV, PB with very small radius of curvature and fingerprint ornamentation of fine ribs.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDE897303FDFDFAFC45.taxon	description	DESCRIPTION RV: PDB, DB and ADB straight; DB quite horizontal compared with VB; AB with medium radius of curvature, maximum of curvature at mid-H; VB nearly straight to gently concave; PB with very small radius of curvature and maximum of curvature located at mid H; LV: dorsal and ventral parts regularly arched; DB being more or less one third of length; presence of a dorsal blade. Carapace laterally compressed at AB, AVB, PVB and PB; LV overlaps RV on dorsal and ventral margins with maximum on DB; carapace ornamented by a very fine reticulation organized in fingerprint of fine ribs parallel to margins.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCFFFDE897303FDFDFAFC45.taxon	discussion	REMARKS	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFDE8AC9047DFDD3FBEF.taxon	materials_examined	TYPE SPECIES. — Bairdiacypris deloi Bradfield, 1935.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFDE8AB004C0FB08FB04.taxon	materials_examined	TYPE MATERIAL. — Holotype: one complete carapace (P 6 M 2624; Fig. 5 F); paratype: one complete carapace (P 6 M 2625; Fig. 5 H).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFDE8AB004C0FB08FB04.taxon	etymology	ETYMOLOGY. — Dedicated to Simone Combe, personal dedication.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFDE8AB004C0FB08FB04.taxon	materials_examined	MATERIAL EXAMINED. — 9 complete carapaces. DIMENSIONS. — L = 495 - 770 µm; H = 245 - 375 µm. Holotype: L = 529 µm; H = 245 µm. Paratype: L = 754 µm; H = 360 µm. TYPE HORIZON. — Sample 06 Ti 30, Unit VI, Tulong Formation, Anisian, Middle Triassic. TYPE LOCALITY. — Tulong section, Southern Tibet. OCCURRENCE. — Tulong section, Southern Tibet. Samples 06 Ti 21, 06 Ti 27, 06 Ti 28, 06 Ti 30 and 06 Ti 34, units V and VI, Spathian-Anisian, Early-Middle Triassic.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFDE8AB004C0FB08FB04.taxon	diagnosis	DIAGNOSIS. — A species of Bairdiacypris with maximum of height located in posterior part of the carapace, AB with small radius of curvature and maximum of curvature located high.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFDE8AB004C0FB08FB04.taxon	description	DESCRIPTION DB short and straight at both valves; ADB long and straight; AB with quite small radius of curvature with maximum convexity located high (just below mid-H); VB long, convex at LV and concave at RV; PB with small radius of curvature with maximum of convexity located low (below lower ⅓ of H); carapace long (H / L = 0.46); maximum of H located in posterior third of L.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFDE8AB004C0FB08FB04.taxon	discussion	REMARKS Bairdiacypris combeae Forel n. sp. is close to Bairdiacypris reniformis (Chen, 1958) from the Early Permian of South China. In B. combeae Forel n. sp. the radius of curvature of AB and PB are smaller.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFDE897804A3FB2DFA91.taxon	materials_examined	TYPE SPECIES. — Liuzhinia subovata Zheng, 1976.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFD089630506FF42F9AA.taxon	materials_examined	TYPE MATERIAL. — Holotype: one complete carapace (P 6 M 2638; Fig. 6 C); paratype: one complete carapace (P 6 M 2639; Fig. 6 D). F, Bairdia anisica Kozur, 1970, right lateral view of a complete carapace (P 6 M 2613); G, Bairdia? sp. D, left lateral view of a complete carapace (P 6 M 2614); H, Bairdia cf. finalyi (Méhes, 1911), right lateral view of a broken carapace (P 6 M 2620); I - M, Petasobairdia collini Forel n. sp.; I, right lateral view of a complete carapace (P 6 M 2617); J, paratype (P 6 M 2619), right lateral view of a nearly complete carapace (dorsal part of left valve is missing); K, right lateral view of a nearly complete carapace (P 6 M 2613); L, right lateral view of a complete carapace (P 6 M 2618); M, holotype (P 6 M 2615), right lateral view of a complete carapace. Scale bars: 100 μm.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFD089630506FF42F9AA.taxon	etymology	ETYMOLOGY. — Dedicated to Kriemhilde Larm, personal dedication.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFD089630506FF42F9AA.taxon	materials_examined	MATERIAL EXAMINED. — 32 complete carapaces and 1 isolated valve. DIMENSIONS. — L = 350 - 570 µm; H = 175 - 290 µm. Holotype: L = 406 µm; H = 200 µm. Paratype: L = 388 µm; H = 206 µm. TYPE HORIZON. — Sample 06 Ti 08, Unit IIIb, Tulong Formation, Smithian, Lower Triassic. TYPE LOCALITY. — Tulong section, Southern Tibet. OCCURRENCE. — Tulong section, Southern Tibet. Samples 06 Ti 06, 06 Ti 08, 06 Ti 13, 06 Ti 14 and 06 Ti 32, units III to VI, Smithian-Anisian, Early-Middle Triassic.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFD089630506FF42F9AA.taxon	diagnosis	DIAGNOSIS. — A Liuzhinia species with long and straight dorsal border; AB and PB with small radius of curvature.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFD089630506FF42F9AA.taxon	description	DESCRIPTION DB long and straight; AB with relatively small radius of curvature; VB long and gently convex on both valves; PB with small radius of curvature; AB and PB gently compressed laterally at the extremities of the carapace; maximum of H located in front of L anterior third; H / L = 0.51	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFD089630506FF42F9AA.taxon	discussion	REMARKS Liuzhinia larmae Forel n. sp. is very close from Liuzhinia antalyaensis Crasquin-Soleau, 2004 from the early Induan of the Western Taurus (Turkey, Crasquin-Soleau et al. 2004), Guangxi, South China (Crasquin-Soleau et al. 2006) and Southern Alps, Italy (Crasquin et al. 2008). Here, the radius of curvature of AB is smaller, the DB is shorter, the H / L ratio is smaller and the thickness is less important in posterior part of the carapace. NB: in Crasquin-Soleau et al. (2004: 286), there is a printing mistake in the diagnosis of Liuzhinia antalyaensis. It should be as follows:	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFCEFFD089630506FF42F9AA.taxon	diagnosis	DIAGNOSIS. — Species of Liuzhinia with long straight dorsal border and maximum of height located in the anterior third.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC0FFD08976011BFB0EFE49.taxon	materials_examined	TYPE SPECIES. — Hungarella problematica Méhes, 1911.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC0FFD288AE0279FE78FC22.taxon	materials_examined	TYPE MATERIAL. — Holotype (P 6 M 2662): one complete carapace (Fig. 8 A); paratype (P 6 M 2666): one complete carapace (Fig. 8 D).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC0FFD288AE0279FE78FC22.taxon	etymology	ETYMOLOGY. — From the Tulong section, type locality.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC0FFD288AE0279FE78FC22.taxon	materials_examined	MATERIAL EXAMINED. — 230 complete carapaces and 18 isolated valves. DIMENSIONS. — L = 380 - 570 µm; H = 240 - 350 µm. Holotype: L = 506 µm; H = 316 µm. Paratype: L = 514 µm; H = 308 µm. TYPE HORIZON. — Unit V, Tulong Formation, Spathian, lower Triassic. TYPE LOCALITY. — Tulong section, Southern Tibet. OCCURRENCE. — Tulong section, SouthernTibet. Samples 06 Ti 20, 06 Ti 25, 06 Ti 26, 06 Ti 28 - 32 and 06 Ti 34, units V and VI, Spathian-Anisian, Early-Middle Triassic.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC0FFD288AE0279FE78FC22.taxon	diagnosis	DIAGNOSIS. — A species of Hungarella with dorsal parts straight and carapace laterally compressed at AB.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC0FFD288AE0279FE78FC22.taxon	description	DESCRIPTION PD and AD parts long and straight on RV, straight to gently convex on LV; the two parts are at a 140 - 150 ° angle; AB regularly arched with a clear lateral flattening, maximum of convexity located around mid-H; VB regularly convex on both valves; PB with quite large radius of curvature, maximum of curvature located a little below mid-H; carapace subtriangular with maximum of H at mid-L or a little in front of; H / L = 0.62; lateral view of a complete carapace (P 6 M 2627); E, right lateral view of a broken carapace (P 6 M 2628); F - H, Bairdiacypris combeae Forel n. sp.; F, holotype (P 6 M 2626), right lateral view of a right valve; G, left lateral view of a complete carapace (P 6 M 2625); H, paratype (P 6 M 2624), left lateral view of left valve; I, Microcheilinella sp. A, right lateral view of left valve (P 6 M 2629); J - M, Triassicindivisia tibetinella Crasquin n. gen., n. sp.; J, holotype (P 6 M 2631), left lateral view of a complete carapace; K, paratype (P 6 M 2632), left lateral view of a complete carapace; L, left lateral view of a complete carapace (P 6 M 2636); M, left lateral view of a complete carapace (P 6 M 2637). Scale bars: 100 μm. LV overlap of LV on RV very weak all around the margins; surface smooth.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC0FFD288AE0279FE78FC22.taxon	discussion	REMARKS	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD28AD603BDFF68F988.taxon	materials_examined	TYPE SPECIES. — Triassicindivisia tibetinella Crasquin n. sp. (Fig. 5 J-M).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD28AD603BDFF68F988.taxon	etymology	ETYMOLOGY. — From the similarity with the Devonian genus Indivisia Zaspelova, 1954 (in Egorov 1954).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD28AD603BDFF68F988.taxon	materials_examined	TYPE HORIZON. — Tulong section, Southern Tibet. Sample 06 Ti 35, unit VI, Anisian, Middle Triassic.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD28AD603BDFF68F988.taxon	distribution	DISTRIBUTION. — Middle Smithian to Early Anisian, Tulong section, Southern Tibet.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD28AD603BDFF68F988.taxon	diagnosis	DIAGNOSIS. — A new Triassic palaeocopid genus with free margins laterally compressed, without observable sulcus, all surface smooth.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD28AD603BDFF68F988.taxon	discussion	REMARKS Triassicindivisia n. gen. is close to the Devonian Indivisia.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD588A300BAFD16F92F.taxon	materials_examined	TYPE MATERIAL. — Holotype: one complete carapace (P 6 M 2631; Fig. 5 J); paratype: one complete carapace (P 6 M 2632; Fig. 5 K).	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD588A300BAFD16F92F.taxon	etymology	ETYMOLOGY. — From Tibet, type locality.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD588A300BAFD16F92F.taxon	materials_examined	MATERIAL EXAMINED. — 8 complete carapaces. DIMENSIONS. — L = 460 - 825 µm; H = 250 - 420 µm. Holotype: L = 460 µm; H = 253 µm. Paratype: L = 714 µm; H = 385 µm. TYPE HORIZON. — Sample 06 Ti 35, Unit VI, Tulong Formation, Anisian, Middle Triassic. TYPE LOCALITY. — Tulong section, Southern Tibet. OCCURRENCE. — Tulong section, Southern Tibet. Samples 06 Ti 07, 06 Ti 20, 06 Ti 31, 06 Ti 33 and 06 Ti 35, units III to VI, Smithian-Anisian, Early-Middle Triassic.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD588A300BAFD16F92F.taxon	diagnosis	DIAGNOSIS. — A species of Triassicindivisia n. gen. with elongated carapace (H / L = 0.52), AB and PB have small radius of curvature.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD588A300BAFD16F92F.taxon	description	DESCRIPTION Carapace with long straight to gently convex DB; cardinal angles clearly expressed, equivalent and very obtuse (≈ 145 to 150 °); AB with small radius of curvature, maximum of convexity located at mid-H or a little below; VB regularly curved with maximum of convexity (H maximum) in front of mid-L; BP with small radius of curvature, maximum located high at upper ⅓ of H; free margins compressed laterally; RV overlaps LV all along free margins; surface smooth, no primary nor secondary ornamentation; H / L = 0.52.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
6A0387BAFFC2FFD588A300BAFD16F92F.taxon	discussion	REMARKS This new genus and the type species are reminiscent of Paraparchitoidea by the absence of primary and secondary ornamentation. Internal characters, e. g., muscle scars, were not observed so the superfamily is uncertain for the time being. of a complete carapace (P 6 M 2643); I, Microcheilinella sp. B., right lateral view of a broken carapace (P 6 M 2630); J, Acratia goemoeryi Kozur, 1970, right lateral view of a complete carapace (P 6 M 2644); K, Urobairdia? sp., right lateral view of a broken carapace (P 6 M 2645); L, Bairdia cf. cassiana rotundidorsata Monostori, 1995, right lateral view of a complete carapace (P 6 M 2646); M, Bairdia sp. E, right lateral view of a complete carapace (P 6 M 2647). Scale bars: 100 μm.	en	Forel, Marie-Béatrice, Crasquin, Sylvie (2011): In the aftermath of Permian-Triassic boundary mass-extinction: new ostracod (Crustacea) genus and species from South Tibet. Geodiversitas 33 (2): 247-263, DOI: 10.5252/g2011n2a3, URL: http://dx.doi.org/10.5252/g2011n2a3
