identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
6A0387BAFFCAFFDA89600198FBDDFDC8.text	6A0387BAFFCAFFDA89600198FBDDFDC8.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Bairdia McCoy 1844	<div><p>Genus Bairdia McCoy, 1844</p><p>TYPE SPECIES. — Bairdia curta McCoy, 1844 .</p></div>	https://treatment.plazi.org/id/6A0387BAFFCAFFDA89600198FBDDFDC8	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFCAFFDF897002FEFDDEFD9E.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Bairdia jeancharlesi Forel 2011	<div><p>Bairdia jeancharlesi Forel n. sp. (Fig. 3 I-L)</p><p>TYPE MATERIAL. — Holotype: one complete carapace (P6M2607; Fig. 3J); paratype: one complete carapace (P6M2603; Fig. 3I).</p><p>ETYMOLOGY. — Dedicated to Jean-Charles Forel, personal dedication.</p><p>MATERIAL EXAMINED. — 26 complete carapaces and 1 single valve.</p><p>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.</p><p>TYPE HORIZON. — Sample 06Ti08, unit IIIb, Tulong Formation, Smithian, Lower Triassic.</p><p>TYPE LOCALITY. — Tulong section, Southern Tibet .</p><p>OCCURRENCE. — Tulong section, southernTibet.Samples 06Ti04, 06Ti08, 06Ti21, 06Ti27-31, 06Ti35, Tulong Formation, units III, V and VI, Smithian to Anisian, Lower-Middle Triassic.</p><p>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.</p><p>DESCRIPTION</p><p>RV: PDB, DB and ADB straight; AB regularly arched with maximum of curvature located in its middle; AVB and PVB regularly convex; VB concave</p><p>complete carapace (P6M2599); F -H, Bairdia finalyi (Méhes, 1911); F, right lateral view of a complete carapace (P6M2601); G, right lateral view of a complete carapace (P6M2602); H, right lateral view of a complete carapace (P6M2606); I -L, Bairdia jeancharlesi Forel n. sp.; I, paratype (P6M2603), right lateral view of a complete carapace; J, holotype (P6M2607), right lateral view of a complete carapace; K, right lateral view of a broken carapace (P6M2604); L, right lateral view of a complete carapace (P6M2605); M, Spinocypris vulgaris Kozur, 1971, right lateral view of a complete carapace (P6M2600). Scale bars: 100 μm.</p><p>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.</p><p>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.</p><p>REMARKS</p><p>Bairdia jeancharlesi Forel n. sp. is close to Bairdia cassiana rotundidorsata Monostori, 1995 from the Anisian of Balaton area (Hungary; Monostori 1995). Here, the carapace is shorter, the overlap is weaker and the DB and PDB are more inclined posteriorly.</p></div>	https://treatment.plazi.org/id/6A0387BAFFCAFFDF897002FEFDDEFD9E	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFCFFFDF8A90023EFC38FD01.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Bairdia letangae Forel 2011	<div><p>Bairdia letangae Forel n. sp. (Fig. 3 A-E)</p><p>TYPE MATERIAL. — Holotype: one complete carapace (P6M2596; Fig. 3A); paratype: one complete carapace (P6M2595; Fig. 3B).</p><p>ETYMOLOGY. — Dedicated to Béatrice Letang, personal dedication.</p><p>MATERIAL EXAMINED. — 7 complete carapaces and 2 single valves.</p><p>DIMENSIONS. — L = 540-785 µm; H = 320-500 µm. Holotype: L = 785 µm; H = 492 µm. Paratype: L = 540 µm; H = 320 µm.</p><p>TYPE HORIZON. — Sample 06Ti30, unit VI, Tulong Formation, Early Anisian, Middle Triassic.</p><p>TYPE LOCALITY. — Tulong section, Southern Tibet .</p><p>OCCURRENCE. — Tulong section, Southern Tibet . Samples 06Ti21, 06Ti30, 06Ti31 and 06Ti34, Tulong Formation, units V and VI, Spathian-Anisian, Early-Middle Triassic.</p><p>DIAGNOSIS. A massive species of ornamented Bairdia with AB and PB flattened, large reticulation on all the carapace except the dorsal margin.</p><p>DESCRIPTION</p><p>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-</p><p>tion, this reticulation is present on all the surface except for dorsal margins of both valves.</p><p>REMARKS</p><p>Bairdia letangae Forel n. sp. is similar to Bairdia ortiseiensis Crasquin, 2008 from the Late Permian of the Tesero section (Northern Italy; Crasquin et al. 2008). Here the DB is longer, the radius of curvature of AB is more important and the overlap is stronger. Compared to Lobobairdia zapfei Kozur, 1971 from the Anisian of Balaton area (Kozur 1971; Monostori 1995), Bairdia letangae Forel n. sp. has a straighter DB and reticulation present all over the carapace surface.</p></div>	https://treatment.plazi.org/id/6A0387BAFFCFFFDF8A90023EFC38FD01	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFCFFFDF888C02BEFC3AFCB0.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Petasobairdia Chen 1982	<div><p>Genus Petasobairdia Chen, 1982</p><p>TYPE SPECIES. — Petasobairdia bicornuta Chen, 1982 (in Chen &amp; Shi 1982).</p></div>	https://treatment.plazi.org/id/6A0387BAFFCFFFDF888C02BEFC3AFCB0	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFCFFFDE897303FDFDFAFC45.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Petasobairdia collini Forel 2011	<div><p>Petasobairdia collini Forel n. sp. (Fig. 4 I-M)</p><p>TYPE MATERIAL. — Holotype: one complete carapace (P6M2615; Fig. 4M); paratype: one complete carapace (P6M2619; Fig. 4J).</p><p>ETYMOLOGY. — Dedicated to Dr Pierre-Yves Collin, Université Pierre et Marie Curie, Paris.</p><p>MATERIAL EXAMINED. — 18 complete carapaces and 20 isolated valves.</p><p>DIMENSIONS. — L = 630-1140 µm; H = 350-700 µm. Holotype: L = 1030 µm; H = 680 µm. Paratype: L = 848 µm; H = 546 µm.</p><p>TYPE HORIZON. — Sample 06Ti30, unit VI, Tulong Formation, Early Anisian, Middle Triassic.</p><p>TYPE LOCALITY. — Tulong section, Southern Tibet .</p><p>OCCURRENCE. — Tulong section, Southern Tibet . Samples 06Ti21, 06Ti25, 06Ti30, 06Ti32, 06Ti33, Tulong Formation, units V and VI, Spathian-Anisian, Early- Middle Triassic.</p><p>DIAGNOSIS. — A species of Petasobairdia with slight dorsal blade at LV, PB with very small radius of curvature and fingerprint ornamentation of fine ribs.</p><p>DESCRIPTION</p><p>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;</p><p>LV: dorsal and ventral parts regularly arched; DB being more or less one third of length; presence of a dorsal blade.</p><p>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.</p><p>REMARKS</p><p>Petasobairdia collini Forel n. sp. is close to two Late Permian species from South China. Petasobairdia nantongensis Chen, 1982 (in Chen &amp; Shi 1982) has a shorter VB, overlap less important on ADB and PDB, AB and PB are smaller. Petasobairdia subnantongensis Chen, 1987 (in Shi &amp; Chen 1987) has a longer DB particularly on LV and has a ventral “blade”.</p></div>	https://treatment.plazi.org/id/6A0387BAFFCFFFDE897303FDFDFAFC45	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFCEFFDE8AC9047DFDD3FBEF.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Bairdiacypris Bradfield 1935	<div><p>Genus Bairdiacypris Bradfield, 1935</p><p>TYPE SPECIES. — Bairdiacypris deloi Bradfield, 1935 .</p></div>	https://treatment.plazi.org/id/6A0387BAFFCEFFDE8AC9047DFDD3FBEF	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFCEFFDE8AB004C0FB08FB04.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Bairdiacypris combeae Forel 2011	<div><p>Bairdiacypris combeae Forel n. sp. (Fig. 5 F-H)</p><p>Fabalicypris reniformis . – Hao 1992: 41, 42, pl. 1, figs 10, 11.</p><p>TYPE MATERIAL. — Holotype: one complete carapace (P6M2624; Fig. 5F); paratype: one complete carapace (P6M2625; Fig. 5H).</p><p>ETYMOLOGY. — Dedicated to Simone Combe, personal dedication.</p><p>MATERIAL EXAMINED. — 9 complete carapaces.</p><p>DIMENSIONS. — L = 495-770 µm; H = 245-375 µm. Holotype: L = 529 µm; H = 245 µm. Paratype: L = 754 µm; H = 360 µm.</p><p>TYPE HORIZON. — Sample 06Ti30, Unit VI, Tulong Formation, Anisian, Middle Triassic.</p><p>TYPE LOCALITY. — Tulong section, Southern Tibet .</p><p>OCCURRENCE. — Tulong section, Southern Tibet . Samples 06Ti21, 06Ti27, 06Ti28, 06Ti30 and 06Ti34, units V and VI, Spathian-Anisian, Early-Middle Triassic.</p><p>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.</p><p>DESCRIPTION</p><p>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.</p><p>REMARKS</p><p>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.</p></div>	https://treatment.plazi.org/id/6A0387BAFFCEFFDE8AB004C0FB08FB04	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFCEFFDE897804A3FB2DFA91.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Liuzhinia Zheng 1976	<div><p>Genus Liuzhinia Zheng, 1976</p><p>TYPE SPECIES. — Liuzhinia subovata Zheng, 1976 .</p></div>	https://treatment.plazi.org/id/6A0387BAFFCEFFDE897804A3FB2DFA91	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFCEFFD089630506FF42F9AA.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Liuzhinia larmae Forel 2011	<div><p>Liuzhinia larmae Forel n. sp. (Fig. 6 C-G)</p><p>TYPE MATERIAL. — Holotype: one complete carapace (P6M2638; Fig. 6C); paratype: one complete carapace (P6M2639; Fig. 6D).</p><p>F, Bairdia anisica Kozur, 1970, right lateral view of a complete carapace (P6M2613); G, Bairdia ? sp. D, left lateral view of a complete carapace (P6M2614); H, Bairdia cf. finalyi (Méhes, 1911), right lateral view of a broken carapace (P6M2620); I -M, Petasobairdia collini Forel n. sp.; I, right lateral view of a complete carapace (P6M2617); J, paratype (P6M2619), right lateral view of a nearly complete carapace (dorsal part of left valve is missing); K, right lateral view of a nearly complete carapace (P6M2613); L, right lateral view of a complete carapace (P6M2618); M, holotype (P6M2615), right lateral view of a complete carapace. Scale bars: 100 μm.</p><p>ETYMOLOGY. — Dedicated to Kriemhilde Larm, personal dedication.</p><p>MATERIAL EXAMINED. — 32 complete carapaces and 1 isolated valve.</p><p>DIMENSIONS. — L = 350-570 µm; H = 175-290 µm. Holotype: L = 406 µm; H = 200 µm. Paratype: L = 388 µm; H = 206 µm.</p><p>TYPE HORIZON. — Sample 06Ti08, Unit IIIb, Tulong Formation, Smithian, Lower Triassic.</p><p>TYPE LOCALITY. — Tulong section, Southern Tibet .</p><p>OCCURRENCE. — Tulong section, Southern Tibet . Samples 06Ti06, 06Ti08, 06Ti13, 06Ti14 and 06Ti32, units III to VI, Smithian-Anisian, Early-Middle Triassic.</p><p>DIAGNOSIS. — A Liuzhinia species with long and straight dorsal border; AB and PB with small radius of curvature.</p><p>DESCRIPTION</p><p>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</p><p>REMARKS</p><p>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.</p><p>NB: in Crasquin-Soleau et al. (2004: 286), there is a printing mistake in the diagnosis of Liuzhinia antalyaensis . It should be as follows:</p><p>DIAGNOSIS. — Species of Liuzhinia with long straight dorsal border and maximum of height located in the anterior third.</p></div>	https://treatment.plazi.org/id/6A0387BAFFCEFFD089630506FF42F9AA	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFC0FFD08976011BFB0EFE49.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Hungarella Mehes 1911	<div><p>Genus Hungarella Méhes, 1911</p><p>TYPE SPECIES. — Hungarella problematica Méhes, 1911 .</p></div>	https://treatment.plazi.org/id/6A0387BAFFC0FFD08976011BFB0EFE49	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFC0FFD288AE0279FE78FC22.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Hungarella tulongensis Forel & Crasquin 2011	<div><p>Hungarella tulongensis Crasquin n. sp. (Fig. 8 A-F)</p><p>TYPE MATERIAL. — Holotype (P6M2662): one complete carapace (Fig. 8A); paratype (P6M2666): one complete carapace (Fig. 8D).</p><p>ETYMOLOGY. — From the Tulong section, type locality.</p><p>MATERIAL EXAMINED. — 230 complete carapaces and 18 isolated valves.</p><p>DIMENSIONS. — L = 380-570 µm; H = 240-350 µm. Holotype: L = 506 µm; H = 316 µm. Paratype: L = 514 µm; H = 308 µm.</p><p>TYPE HORIZON. — Unit V,Tulong Formation, Spathian, lower Triassic.</p><p>TYPE LOCALITY. — Tulong section, Southern Tibet .</p><p>OCCURRENCE. — Tulong section, SouthernTibet. Samples 06Ti20, 06Ti25, 06Ti26, 06Ti28-32 and 06Ti34, units V and VI, Spathian-Anisian, Early-Middle Triassic.</p><p>DIAGNOSIS. — A species of Hungarella with dorsal parts straight and carapace laterally compressed at AB.</p><p>DESCRIPTION</p><p>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;</p><p>lateral view of a complete carapace (P6M2627); E, right lateral view of a broken carapace (P6M2628); F -H, Bairdiacypris combeae Forel n. sp.; F, holotype (P6M2626), right lateral view of a right valve; G, left lateral view of a complete carapace (P6M2625); H, paratype (P6M2624), left lateral view of left valve; I, Microcheilinella sp. A, right lateral view of left valve (P6M2629); J -M, Triassicindivisia tibetinella Crasquin n. gen., n. sp.; J, holotype (P6M2631), left lateral view of a complete carapace; K, paratype (P6M2632), left lateral view of a complete carapace; L, left lateral view of a complete carapace (P6M2636); M, left lateral view of a complete carapace (P6M2637). Scale bars: 100 μm.</p><p>LV overlap of LV on RV very weak all around the margins; surface smooth.</p><p>REMARKS</p><p>Hungarella tulongensis Crasquin n. sp. differs from the Upper Anisian species “ Hungarella ” reniformis Méhes, 1911 from Lake Balaton (Hungary; Méhes 1911; Monostori 1995) by H/L smaller and a maximum of convexity of BP located lower. Hungarella elongata (Blake, 1876) from the Late Triassic (Rhaetian) of Great Britain (Anderson 1964) has the same anterior structure but the dorsal outline is less angular and H/L is smaller. Hungarella ovata Zheng, 1976 from the Rhaetian of South China (Zheng 1976) is also relatively close to the new species but has a concave VB on RV and a PB with smaller radius of curvature ( Hungarella genus needs re-collection and re-description).</p><p>Order PALAEOCOPIDA Henningsmoen, 1953 Superfamily indet. Family indet.</p></div>	https://treatment.plazi.org/id/6A0387BAFFC0FFD288AE0279FE78FC22	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFC2FFD28AD603BDFF68F988.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Triassicindivisia Forel & Crasquin 2011	<div><p>Genus Triassicindivisia Crasquin n. gen.</p><p>TYPE SPECIES. — Triassicindivisia tibetinella Crasquin n. sp. (Fig. 5 J-M).</p><p>ETYMOLOGY. — From the similarity with the Devonian genus Indivisia Zaspelova, 1954 (in Egorov 1954).</p><p>TYPE HORIZON. — Tulong section, Southern Tibet . Sample 06Ti35, unit VI, Anisian, Middle Triassic.</p><p>DISTRIBUTION. — Middle Smithian to Early Anisian, Tulong section, Southern Tibet .</p><p>DIAGNOSIS. — A new Triassic palaeocopid genus with free margins laterally compressed, without observable sulcus, all surface smooth.</p><p>REMARKS</p><p>Triassicindivisia n. gen. is close to the Devonian Indivisia .</p></div>	https://treatment.plazi.org/id/6A0387BAFFC2FFD28AD603BDFF68F988	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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.text	6A0387BAFFC2FFD588A300BAFD16F92F.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Triassicindivisia tibetinella Forel & Crasquin 2011	<div><p>Triassicindivisia tibetinella Crasquin n. sp. (Fig. 5 J-M)</p><p>TYPE MATERIAL. — Holotype: one complete carapace (P6M2631; Fig. 5J); paratype: one complete carapace (P6M2632; Fig. 5K).</p><p>ETYMOLOGY. — From Tibet, type locality.</p><p>MATERIAL EXAMINED. — 8 complete carapaces.</p><p>DIMENSIONS. — L = 460-825 µm; H = 250-420 µm. Holotype: L = 460 µm; H = 253 µm. Paratype: L = 714 µm; H = 385 µm.</p><p>TYPE HORIZON. — Sample 06Ti35, Unit VI, Tulong Formation, Anisian, Middle Triassic.</p><p>TYPE LOCALITY. — Tulong section, Southern Tibet .</p><p>OCCURRENCE. — Tulong section, Southern Tibet . Samples 06Ti07, 06Ti20, 06Ti31, 06Ti33 and 06Ti35, units III to VI, Smithian-Anisian, Early-Middle Triassic.</p><p>DIAGNOSIS. — A species of Triassicindivisia n. gen. with elongated carapace (H/L = 0.52), AB and PB have small radius of curvature.</p><p>DESCRIPTION</p><p>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.</p><p>REMARKS</p><p>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.</p><p>of a complete carapace (P6M2643); I, Microcheilinella sp. B., right lateral view of a broken carapace (P6M2630); J, Acratia goemoeryi Kozur,1970,right lateral view of a complete carapace (P6M2644); K, Urobairdia? sp.,right lateral view of a broken carapace (P6M2645); L, Bairdia cf. cassiana rotundidorsata Monostori, 1995, right lateral view of a complete carapace (P6M2646); M, Bairdia sp. E, right lateral view of a complete carapace (P6M2647). Scale bars: 100 μm.</p></div>	https://treatment.plazi.org/id/6A0387BAFFC2FFD588A300BAFD16F92F	Public Domain	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.		Plazi	Forel, Marie-Béatrice;Crasquin, Sylvie	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
