identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
302A87B5FFF00D0FFC76FDD9FA2D10BB.text	302A87B5FFF00D0FFC76FDD9FA2D10BB.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Diplopodichnus biformis Brady 1947	<div><p>Diplopodichnus biformis Brady, 1947 (Fig. 3C, D)</p> <p>MATERIAL EXAMINED. — Seven traces; four traces preserved as convex hyporeliefs on slab M486_ 2022.1.1; three traces preserved as convex hyporeliefs on slab M486_ 2022.1.2.</p> <p>DESCRIPTION</p> <p>Traces are horizontal, unbranched, straight to curved, run in different directions and up to 3.0 mm wide. The longest course is 72 mm. The traces consist of two thin and up to 1.4 mm wide parallel hypichnial ridges separated by a central groove that is up to 0.8 mm wide (Fig. 3C, D).</p> <p>REMARKS</p> <p>The ichnogenus Diplopodichnus Brady, 1947 is reported from the Late Proterozoic to the Early Jurassic (Buatois et al. 1998; Uchman et al. 2011 and references therein). D. biformis is widely recorded in Palaeozoic deposits including many occurrences in Permian formations worldwide (e.g. Brady 1947; Lucas et al. 2004, 2005; Contardi &amp; Santi 2009; Avanzini et al. 2011a; Lima &amp; Netto 2012; Moreau et al. 2020).</p> </div>	https://treatment.plazi.org/id/302A87B5FFF00D0FFC76FDD9FA2D10BB	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
302A87B5FFF00D0FFF1EFABFFC5315C4.text	302A87B5FFF00D0FFF1EFABFFC5315C4.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Medusina atava (Pohlig 1892) Walcott 1898	<div><p>Medusina atava (Pohlig, 1892) Walcott, 1898 (Fig. 3A, B)</p> <p>MATERIAL EXAMINED. — One specimen; M486_ 2022.1.9.</p> <p>DESCRIPTION</p> <p>The specimen is umbrella-shaped and 16 mm in diameter. The velum is locally visible, forming an up to 3.3 mm wide marginal thickening. The jellyfish bears 10, thin, quite straight and radially arranged furrows originating from the centre and corresponding to radial canals (Fig. 3A, B). Most furrows join the periphery of the jellyfish. The centre of the jellyfish shows an up to 8 mm wide, star-shaped and concave structure corresponding to the manubrium (Fig. 3A, B).</p> <p>REMARKS Medusina atava was reported in Permian deposits from France (Gand et al. 1996), Germany (Schüppel 1984) and Italy (Ronchi &amp; Santi 2003). In the Saint-Affrique Basin, both species Medusina atava and Medusina limnica Müller, 1978 are known from some Permian sites (Gand et al. 1996). However, Medusina is for the first time reported in the Permian deposits of the Rodez Basin. M. limnica is mainly distinguished from M. atava by showing a maximum of four radial canals. Amongst M. atava the number of radial canals is variable and can reach a number of ten (Schüppel 1984; Gand et al. 1996).</p> </div>	https://treatment.plazi.org/id/302A87B5FFF00D0FFF1EFABFFC5315C4	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
302A87B5FFF00D0FFC1CFA9FFA0A13B9.text	302A87B5FFF00D0FFC1CFA9FFA0A13B9.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Scoyenia gracilis White 1929	<div><p>Scoyenia gracilis White, 1929</p> <p>(Fig. 3C, D)</p> <p>MATERIAL EXAMINED. — Two burrows; one is preserved as concave epirelief on slab M486 _ 2022.1.3; the other is preserved as convex hyporelief on slab M486 _ 2022.1.2.</p> <p>DESCRIPTION</p> <p>Burrows are unbranched, and straight to slightly curved. They are circular to oval in transverse section, up to 15 mm in diameter and horizontally, obliquely to vertically oriented (Fig. 3C, D). The surface of burrows shows longitudinal striations. Longitudinal sections of burrows show prominent meniscate backfills (Fig. 3C, D).</p> <p>REMARKS</p> <p>Scoyenia gracilis is a very common ichnospecies in non-marine Permian deposits (Buatois et al. 1997). This ichnotaxon was abundantly reported from some Permian tracksites of the basins of Saint-Affrique and Lodève (e.g. Lopez et al. 2008).</p> </div>	https://treatment.plazi.org/id/302A87B5FFF00D0FFC1CFA9FFA0A13B9	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
302A87B5FFF30D0DFF2BFA5EFE161258.text	302A87B5FFF30D0DFF2BFA5EFE161258.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Amphisauropus latus Haubold 1970	<div><p>Amphisauropus latus Haubold, 1970</p> <p>(Fig. 4)</p> <p>MATERIAL EXAMINED. — Eight tracks preserved as concave epireliefs on slab M486_ 2022.1.5.</p> <p>DESCRIPTION</p> <p>The trackway is 13 cm long, 6 cm wide and composed of four consecutive pes/manus sets (Fig. 4A, B). Pes and manus stride is 6.4-6.5 cm long. The manus tracks are more internal than pes tracks. Both are small sized and semi-plantigrade. Pes imprints are pentadactyl and wider than long (PL = 1.1 cm, PW = 1.8-2.0 cm; Fig. 4). The PL/PW ratio is equal to 0.6. Digit imprints are short, straight to slightly curved and end in an enlarged rounded tip (Fig. 4 C-E). Pes tracks show a short, large and poorly impressed sole with concave proximal margin. The manus tracks are strongly oriented inward, forming an angle of up to 120° with the trackway axis. Manus imprints are pentadactyl and wider than long (ML = 0.9-1.1 cm; MW = 1.6-1.9 cm; ML/MW = 0.6). Imprints of digits are short and end in a small enlarged rounded tip. The manual digits II-III bent inwards. The divarication angle of digits I-V is up 153°.</p> <p>REMARKS</p> <p>As noted by Gand et al. (2000) Amphisauropus Haubold, 1970 shares similarities with Merifontichnus Gand, Garric, Demathieu &amp; Ellenberger, 2000. Tracks from Le Bousquet differ from this latter by smaller size and the pedal digit I not parallel to the proximal margin of the sole. Although tracks from Le Bousquet share some similarities with Dolomitipes Marchetti, Voigt &amp; Klein, 2017, this ichnogenus differs in showing manus tracks placed in line or slightly external to the pes, and pedal tracks longer than wide or about as wide as long and 40 to 250 mm long (Marchetti et al. 2019). Amphisauropus represents a widespread Permian ichnogenus that has been reported from many areas including Africa (Voigt et al. 2011; Hminna et al. 2012; Moreau et al. 2020); Argentina (Melchor &amp; Sarjeant 2004); Canada (Mossman &amp; Place 1989; van Allen et al. 2005); Europe (e.g. Gand &amp; Haubold 1984; Gand 1987; Haubold 1971; Santi &amp; Krieger 2001; Ptaszyński &amp; Niedźwiedzki 2004; Voigt 2005; Avanzini et al. 2008; Voigt et al. 2012; Marchetti et al. 2015) and the United States (Lucas et al. 2001). In France, Amphisauropus was previously reported from the Lodève Basin (Gand &amp; Durand 2006) and the Rodez Basin (Gand 1987). Although Gand (1987) reported Amphisauropus in several localities near Banassac-Canilhac this ichnogenus is here for the first time reported from Le Bousquet.</p> </div>	https://treatment.plazi.org/id/302A87B5FFF30D0DFF2BFA5EFE161258	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
302A87B5FFF20D02FF04F97EFCA2111B.text	302A87B5FFF20D02FF04F97EFCA2111B.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Batrachichnus salamandroides Geinitz 1861	<div><p>Batrachichnus salamandroides Geinitz, 1861 (Fig. 5)</p> <p>Material examined. — Six tracks; four tracks preserved as concave epireliefs and convex hyporeliefs on slabs M486_ 2022.1.6 A and M486_ 2022.1.6 B, respectively; two tracks preserved as concave epireliefs on slab M486_ 2022.1.7.</p> <p>DESCRIPTION</p> <p>The tracks are small, plantigrade to semi-plantigrade. Pes imprints are pentadactyl and longer (PL = 1.5-4.0 mm) than wide (PW = 1.3-3.8 mm; Fig. 5 A-E) to as long as wide. The ratio PL/PW varies from 1.0-1.2. Digit imprints are straight and end in an enlarged, rounded tip (Fig. 5 C-E). The divarication angle of digits I-V is up 85°. Pes tracks show a large rounded and well-marked sole (Fig. 5 C-E). Manus imprints are tetradactyl, smaller than pes tracks and as long (ML= 1.3-2.3 mm) as wide (MW= 1.3-2.8 mm) to slightly wider than long. The ML/MW ratio varies from 0.8 to1.0. Digit imprints are straight and end in an enlarged, rounded tip. The divarication angle of digits I-IV varies from 46° to 73°. Manus tracks show a short and large sole with a concave proximal margin (Fig. 5A, B).</p> <p>REMARKS</p> <p>The presence of the tetradactyl manus imprints as well as the rounded digit apex are characteristic of the ichnogenera Batrachichnus Woodworth, 1900 and Limnopus Marsh, 1894. The two ichnogenera are distinguished based on their sizes. Manus imprints of Batrachichnus are less than 40 mm in length whereas tracks of Limnopus are larger (up to 200 mm in length; Voigt &amp; Lucas 2018). Regionally, the ichnospecies Batrachichnus salamandroides was reported from the Saint-Affrique Basin (Gand 1987, 1993b; Gand &amp; Haubold 1984), the Lodève Basin (Ellenberger 1983b; Gand &amp; Durand 2006) and the Rodez Basin (Gand 1987). The ichnospecies Batrachichnus salamandroides was also reported from southeastern France, in the Estérel Basin (Provence; Gand &amp; Durand 2006). This ichnospecies is for the first time reported from Le Bousquet.</p> </div>	https://treatment.plazi.org/id/302A87B5FFF20D02FF04F97EFCA2111B	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
302A87B5FFFD0D02FEB0FA3FFB9513BE.text	302A87B5FFFD0D02FEB0FA3FFB9513BE.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Ichniotherium isp. Pohlig 1892	<div><p>Ichniotherium isp.</p> <p>(Fig. 6)</p> <p>MATERIAL EXAMINED. — Two tracks preserved as concave epireliefs and convex hyporeliefs on slabs M486_ 2022.1.4 A and M486_ 2022.1.4 B, respectively.</p> <p>DESCRIPTION</p> <p>The material includes a single pes/manus set (Fig. 6A, B). The tracks are medium sized and plantigrade. The pes track is pentadactyl and as long as wide to wider than long (PL = 5.8 cm, PW = 6.3 cm). The PL/PW ratio is equal to 0.9. On the pes track, digit impressions are only impressed distally, forming a rounded tip (Fig. 6A, B). The manus track is pentadactyl, smaller than pes track and wider than long (ML = 3.8 cm; MW = 5.2 cm; ML/MW = 0.7). Digit impressions increase in length from I to IV. Proximally digits show transverse and thin grooves. The divarication angle of digits I-V is 81°. On the manus track, digit imprints are short, large, straight and end in an enlarged rounded termination. Digits are more impressed distally. The impression of digit IV is the deepest. Both pes and manus tracks show a short and large sole that is distinctly separated from the digit impressions (Fig. 6A, B).</p> <p>REMARKS</p> <p>The presence of: 1) pentadactyl manus and pes tracks showing enlarged digit tips and large soles; 2) pes imprints as long as wide; and 3) manus imprints wider than long, are characteristic of Ichniotherium Pohlig, 1892. This ichnogenus was reported from upper Carboniferous to lower Permian deposits of many localities throughout the world (e.g. Canada, Brink et al. 2012; France, Gand 1987; Germany, Voigt &amp; Ganzelewski 2010; England, Buchwitz &amp; Voigt 2018; Morocco, Lagnaoui et al. 2018; Poland, Voigt et al. 2012; United States, Voigt et al. 2005). In France, Ichniotherium was reported from the Lodève Basin (Gand 1987; Gand &amp; Durand 2006; Mujal &amp; Marchetti 2020), the Rodez Basin (Gand 1987) and the Saint-Affrique Basin (Gand &amp; Haubold 1984). Although Gand (1987) briefly mentioned Ichniotherium at Le Bousquet (based on the private collection of D. Naudin), he did not describe or illustrate the specimens.</p> </div>	https://treatment.plazi.org/id/302A87B5FFFD0D02FEB0FA3FFB9513BE	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
302A87B5FFFC0D03FEBDFBD8FDB813BE.text	302A87B5FFFC0D03FEBDFBD8FDB813BE.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Characichnos isp. Whyte & Romano 2001	<div><p>Characichnos isp.</p> <p>(Fig. 7 A-C)</p> <p>MATERIAL EXAMINED. — M486_ 2022.1.8, slab with numerous tracks preserved as convex hyporeliefs.</p> <p>DESCRIPTION</p> <p>The slab M486_ 2022.1.8 bears numerous swimming tracks of tetrapods (Fig. 7 A-C). They are small, up to 14 mm long and up to 9 mm wide. Some of them are aligned showing a trackway-like pattern (Fig. 7C). Morphology of individual tracks vary a lot. They show two to four parallel, elongated, thin and straight to strongly curved furrows. Some of the tracks seem to bear claw traces. Imprints of sole are absent.</p> <p>REMARKS</p> <p>Characichnos shows a wide stratigraphic range (Carboniferous to Cretaceous) and was reported from several Permian tracksites throughout the world (e.g. Argentina, Melchor &amp; Sarjeant 2004; Spain, Mujal et al. 2016; United States, Lucas &amp; Spielmann 2009; Lerner &amp; Lucas 2015; Morocco, Moreau et al. 2020). This ichnogenus is for the first time reported in the Permian deposits from the Rodez Basin. These tracks can be interpreted as pes and manus imprints of small tetrapods half-floating and swimming in shallow water. Here, only the tips of the digits touched the substrate. On the slab M486_ 2022.1.8, these swimming tracks co-occur with abundant fish trails ascribed to Undichna cf. britannica Higgs, 1988 (Fig. 7 D-G).</p> </div>	https://treatment.plazi.org/id/302A87B5FFFC0D03FEBDFBD8FDB813BE	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
302A87B5FFFC0D00FC72FB9FFCA212B9.text	302A87B5FFFC0D00FC72FB9FFCA212B9.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Undichna britannica Higgs 1988	<div><p>Undichna cf. britannica Higgs, 1988</p> <p>(Fig. 7 A-G)</p> <p>MATERIAL EXAMINED. — M486_ 2022.1.8, slab bearing numerous trails preserved as convex hyporeliefs.</p> <p>DESCRIPTION</p> <p>The slab bears many wavy, horizontal, intermittent, sharp and up to 1.0 mm wide ridges (Fig. 7A, B, D). Some of these ridges form trails consisting of two intertwined and out-of-phase waves (Fig. 7 E-G). The longest trail is 145 mm long. Waves show a wavelength of up to 40 mm and an amplitude of up to 5 mm. In some trails, one of the waves shows a low amplitude, whereas the other shows a greatest amplitude (Fig.7F). Some trails show outer marks that are parallel to central waves (Fig. 7E, G).</p> <p>REMARKS</p> <p>The presence of wavy, intertwined, horizontal, and intermittent, grooves/ridges is characteristic of several Undichna Anderson,1976 ichnospecies (e.g. Undichna quina from the Permian deposits of the Falkland Island, Trewin2000; Undichna britannica from the Carboniferous deposits of England, Higgs 1988). Since ridges are out-of-phase in specimens from Le Bousquet it should be tempting to see similarities with U. britannica (see Higgs 1988 and Minter &amp; Braddy 2006). In contrast, amongst U. quina ridges are in phase (see Trewin 2000). On trails showing strong variation of amplitude between the two waves (Fig.7F), the wave with the lowest amplitude was probably made by the anal fin whereas the wave with a greatest amplitude was probably made by the caudal fin.Outer marks were probably made by pelvic fins.</p> </div>	https://treatment.plazi.org/id/302A87B5FFFC0D00FC72FB9FFCA212B9	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
302A87B5FFFF0D01FE9EF890FEA415E4.text	302A87B5FFFF0D01FE9EF890FEA415E4.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Walchia Sternberg 1825	<div><p>cf. Walchia (Fig. 5A, B)</p> <p>MATERIAL EXAMINED. — M486_ 2022.1.6, slab with one specimen. M486_ 2022.1.10, slab with numerous specimens.</p> <p>DESCRIPTION</p> <p>The longest shoot is 90 mm long. Leafy shoots are up to 17 mm in diameter, and straight to slightly curved (Fig. 5A, B). Leaves are helically arranged. They are quite elongated and show a long free part that forms an angle of up to 45° with the main axis of the shoot (Fig. 5A, B). Leaves are falcate in sagittal section. They are up to 12 mm long. The apex of leaves is acute and commonly slightly curved inward. Occasionally, the apex of leaves is slightly recurved outwards.</p> <p>REMARKS</p> <p>Plant remains are quite common in the fossiliferous bed from Le Bousquet. However, the plant assemblage is only composed of cf. Walchia leafy axes.Regionally, the conifer Walchia Sternberg, 1825 was previously reported from the basins of Saint-Affrique (Gand et al. 1996) and Lodève (Galtier &amp; Broutin 2008; Gand et al. 2013).</p> </div>	https://treatment.plazi.org/id/302A87B5FFFF0D01FE9EF890FEA415E4	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	Moreau, Jean-David;Gand, Georges	Moreau, Jean-David, Gand, Georges (2022): New data on the Permian ecosystem of the Rodez Basin: ichnofauna (traces of protostomians, tetrapods and fishes), jellyfishes and plants from Banassac-Canilhac (Lozère, southern France). Geodiversitas 44 (31): 975-987, DOI: 10.5252/geodiversitas2022v44a31
