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Data from: The amphibamiform Nanobamus macrorhinus from the early Permian of Texas
Nanobamus macrorhinus is a small amphibamiform temnospondyl from the early Permian Arroyo Formation of Texas. It is most readily characterized by an elongate and partially subdivided naris. This condition is superficially reminiscent of that seen in the coeval trematopids, the group to which N. macrorhinus was originally referred to under an interpretation of the holotype as a larval form. This was discounted by later workers, but the amphibamiform affinities of the specimen were not formalized until recently. The specimen has never been described in the context of its amphibamiform affinities and remains poorly characterized, never having been sampled in a phylogenetic analysis. Here we present a complete, updated osteological description of N. macrorhinus, including an improved characterization of its unique mosaic of plesiomorphic and apomorphic features and clarification of the taxon's autapomorphies. Our analysis of the taxon's phylogenetic position within Amphibamiformes shows that N. macrorhinus is recovered as diverging after basal amphibamiforms such the micropholids and before derived amphibamiforms such as the amphibamids. This is supported by the unique mixture of retained plesiomorphies such as non-foreshortened postparietals and an oval choana and apomorphies such as a narrow interorbital region and slender palatal rami of the pterygoid. These results reflect the complexity of terrestrial amphibamiform diversity and provide further insight into the evolutionary history of the lissamphibian stem in terrestrial environments.
Supplement photos for paper: New genus Navipelta (Peltaspermales, Pteridospermae) from Permian-Triassic boundary of Moscow sineclise
<p>Additional images of ovuliferous organs <em>Navipelta </em>from the terrestrial deposits of the Nedubrovo locality (village of Nedubrovo, Vologda Region, Russia), belonging to the base of Vetlugian Group (Upper Permian–Lower Triassic)</p>
High-resolution oil and gas methane emission inventory for the Permian Basin
<p>This dataset consists of a high-resolution (0.01<sup>o</sup> × 0.01<sup>o</sup>) oil and gas methane emission inventory for the Permian Basin, developed at Environmental Defense Fund (<a href="http://www.edf.org">www.edf.org</a>). The Permian Basin in western Texas and southern New Mexico is the largest oil producing basin in the U.S., accounting for more than 40% of national oil production in 2021. It is also the nation's largest methane emitting basin, with recent measurement-based estimates of more than three million metric tons per year. Here, we develop an improved inventory of oil and gas methane emissions for the Permian Basin, based on recent facility-scale measurements and updated oil and gas activity data for the year 2021.</p> <p>Full details for the oil and gas methane emission inventory development and key results can be found in the following journal paper, which is under review at Earth System Science Data journal.</p> <p>Please cite the paper when using the methane inventory dataset:</p> <p>Omara, M., Gautam, R., O'Brien, M.A., Himmelberger, A., Franco, A., Meisenhelder, K., Hauser, G., Lyon, D.R., Chulakadaba, A., Miller, C.C., Franklin, J., Wofsy, S., and Hamburg, S.P. Developing a spatially explicit global oil and gas infrastructure database for characterizing methane emission sources at high resolution. <em>In review</em>, Earth System Science Data journal (2023).</p> <p>Points of Contact at Environmental Defense Fund: Mark Omara (momara@edf.org) and Ritesh Gautam (rgautam@edf.org).</p>
Data from: The amphibamiform Nanobamus macrorhinus from the early Permian of Texas
Open the record for dataset details and reuse information.
Fig. 15 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 15. (opposite page). Ostracods from the Dajiang section, South China. — A–B. Callicythere postiangusta Wei, 1981. A. Carapace, left lateral view, P6M3126. B. Carapace, left lateral view, P6M3127. — C–E. Callicythere sp. 1. C. Carapace, right lateral view, P6M3128. D. Carapace, right lateral view, P6M3129. E. Carapace, dorsal view, P6M3130. — F. Sulcella sp. 1, carapace, right lateral view, P6M3133. — G. Sulcella? sp. 2, carapace, right lateral view, P6M3134. — H–I. Polycope sp. 1. I. Carapace, right? lateral view, P6M3135. J. Carapace, right? lateral view, P6M3136. — J. Polycope sp. 2, carapace, right? lateral view, P6M3137. — K. Polycope? sp. 3, carapace, right? lateral view, P6M3138. — L–M. Cyathus sp. 1. L. Carapace, right lateral view, P6M3139. M. Carapace, dorsal view, P6M3140. — N. Cyathus sp. 2, carapace, right lateral view, P6M3141. — O. Amphissites? sp. 1, carapace, right lateral view, P6M3142. — P. Amphissites? sp. 2, broken carapace, right lateral view, P6M3143. — Q. Shleesha? sp. 1, broken carapace, right lateral view, P6M3144. — R. Kirkbya? sp. 1, carapace, right lateral view, P6M3145. — S. Kirkbya? sp. 2, carapace, right lateral view, P6M3146. — T. Oliganisus? sp. 1, carapace, left lateral view, P6M3147. — U. Paraparchites sp. 1, carapace, right lateral view, P6M3148. — V. Paraparchitidae indet., carapace, right lateral view, P6M3149. — W. Shemonaella sp. 1, carapace, left lateral view, P6M3150. – Scale = 100 µm.
Fig. 14 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 14. Ostracods from the Dajiang section, South China. — A–B. Paracypris cf. gaetanii Crasquin– Soleau, 2006. A. Carapace, right lateral view, P6M3104. B. Carapace, right lateral view, P6M3105. — C–E. Paracypris sp. 6. C. Carapace, right lateral view, P6M3106. D. Carapace, right lateral view, P6M3107. E. Carapace, right lateral view, P6M3108. — F. Paracypris sp. 1, carapace, right lateral view, P6M3109. — G. Paracypris? sp. 2, carapace, right lateral view, P6M3110. — H. Paracypris? sp. 3, carapace, right lateral view, P6M3111. — I. Paracypris? sp. 4, carapace, right lateral view, P6M3112. — J–M. Paracypris? sp. 5. J. Carapace, right lateral view, P6M3113. K. Carapace, right lateral view, P6M3114. L. Carapace, dorsal view, P6M3151. M. Carapace, right lateral view, P6M3115. — N. Monoceratina? sp. 1, carapace, right lateral view, P6M3116. — O–R. Basslerella tota Chen & Bao, 1986. O. Carapace, right lateral view, P6M3117. P. Carapace, right lateral view, P6M3118. Q. Carapace, right lateral view, P6M3119. R. Carapace, right lateral view, P6M3120. — S. Basslerella? sp. 1, carapace, right lateral view, P6M3121. — T–W. Callicythere postiangusta Wei, 1981. T. Carapace, right lateral view, P6M3122. U. Carapace, right lateral view, P6M3123. V. Carapace, right lateral view, P6M3124. W. Carapace, dorsal view, P6M3125. – Scale = 100 µm.
Fig. 9 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 9. Ostracods from the Dajiang section, South China. — A–D. Bairdia sp. 25. A. Carapace, right lateral view, P6M3011. B. Carapace, right lateral view, P6M3012. C. Carapace, right lateral view, P6M3013. D. Carapace, right lateral view, P6M3014. — E–G. Bairdia sp. 26. E. Carapace, right lateral view, P6M3015. F. Carapace, right lateral view, P6M3016. G. Carapace, right lateral view, P6M3017. — H–I. Bairdia sp. 27. H. Carapace, right lateral view, P6M3018. I. Carapace, right lateral view, P6M3019. — J-K. Bairdia sp. 28. J. Carapace, right lateral view, P6M3020. K. Carapace, right lateral view, P6M3021. — L–N. Bairdia sp. 29. L. Carapace, right lateral view, P6M3022. M. Carapace, right lateral view, P6M3023. N. Carapace, right lateral view, P6M3024. — O–Q. Bairdia sp. 30. O. Carapace, right lateral view, P6M3025. P. Carapace, right lateral view, P6M3026. Q. Carapace, right lateral view, P6M3027. — R-S. Bairdia sp. 31. R. Carapace, right lateral view, P6M3028. S. Carapace, right lateral view, P6M3029. — T–W. Bairdia sp. 32. T. Carapace, right lateral view, P6M3030. U. Carapace, right lateral view, P6M3031. V. Carapace, right lateral view, P6M3032. W. Carapace, left lateral view, P6M3033. – Scale = 100 µm.
Fig. 8 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 8. Ostracods from the Dajiang section, South China. — A. Bairdia sp. 10, carapace, right lateral view, P6M2987. — B. Bairdia sp. 11, carapace, right lateral view, P6M2988. — C. Bairdia sp. 12, carapace, right lateral view, P6M2989. — D. Bairdia sp. 13, carapace, right lateral view, P6M2990. — E. Bairdia sp. 14, carapace, right lateral view, P6M2991. — F. Bairdia sp. 15, carapace, right lateral view, P6M2992. — G. Bairdia sp. 16, carapace, right lateral view, P6M2993. — H. Bairdia sp. 17, carapace, right lateral view, P6M2994. — I–L. Bairdia sp. 18. I. Carapace, right lateral view, P6M2995. J. Carapace, right lateral view, P6M2996. K. Carapace, right lateral view, P6M2997. L. Carapace, dorsal view, P6M2998. — M–N. Bairdia sp. 19. M. Carapace, right lateral view, P6M2999. N. Carapace, right lateral view, P6M3000. — O–P. Bairdia sp. 20. O. Carapace, right lateral view, P6M3001. P. Carapace, right lateral view, P6M3002. — Q. Bairdia sp. 21, carapace, right lateral view, P6M3003. — R–S. Bairdia sp. 22. R. Carapace, right lateral view, P6M3004. S. Carapace, right lateral view, P6M3005. — T. Bairdia sp. 23, carapace, right lateral view, P6M3006. — U–W. Bairdia sp. 24. U. Carapace, right lateral view, P6M3007. V. Carapace, right lateral view, P6M3008. W. Carapace, right lateral view, P6M3009. — X. Bairdia cf. sp. 24, carapace, right lateral view, P6M3010. – Scale = 100 µm.
Fig. 7 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 7. Ostracods from the Dajiang section, South China. — A–B. Bairdia sp. 3. A. Carapace, right lateral view, P6M2963. B. Carapace, dorsal view, P6M2964. — C. Bairdia sp. 4, Carapace, right lateral view, P6M2965. — D–J. Bairdia sp. 5. D. Carapace, right lateral view, P6M2966. E. Carapace, right lateral view, P6M2967. F. Carapace, right lateral view, P6M2968. G. Carapace, right lateral view, P6M2969. H. Carapace, right lateral view, P6M2970. I. Carapace, right lateral view, P6M2971. J. Carapace, right lateral view, P6M2972. — K–M. Bairdia? sp. 6. K. Carapace, left lateral view, P6M2973. L. Carapace, right lateral view, P6M2974. L. Carapace, right lateral view, P6M2975. — N–S. Bairdia sp. 7. N. Carapace, left lateral view, P6M2976. O. Carapace, right lateral view, P6M2977. P. Carapace, right lateral view, P6M2978. Q. Carapace, right lateral view, P6M2979. R. Carapace, right lateral view, P6M2980. S. Carapace, right lateral view, P6M2981. — T–U. Bairdia sp. 8. T. Carapace, right lateral view, P6M2982. U. Carapace, right lateral view, P6M2983. — V–W.?Bairdia sp. 8. V. Carapace, right lateral view, P6M2984. W. Carapace, right lateral view, P6M2985. — X. Bairdia sp. 9, carapace, right lateral view, P6M2986. – Scale = 100 µm.
Fig. 16 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 16. Evolution of the ostracod faunas through the PTB in Dajiang. A. Evolution of the number of species (species richness) and number of specimens (abundance). B. Evolution of the relative proportions of each superfamily/family. C. Evolution of the relative proportions of each palaeoecological group.
Fig. 4 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 4. Ostracods from the Dajiang section, South China. — A–F. Bairdia? huberti sp. nov. A. Carapace, right lateral view, P6M2939. B. Carapace, right lateral view, P6M2940. C. Paratype, carapace, right lateral view, P6M2941. D. Holotype, carapace, right lateral view, P6M2942. E. Carapace, right lateral view, P6M2943. F. Carapace, right lateral view, P6M2944. — G–P. Bairdia jeromei sp. nov. G. Holotype, carapace, right lateral view, P6M2945. H. Carapace, dorsal view, P6M2946. I. Carapace, right lateral view, P6M2947. J. Paratype, carapace, right lateral view, P6M2948. K. Carapace, right lateral view, P6M2949. L. Carapace, right lateral view, P6M2950. M. Carapace, right lateral view, P6M2951. N. Carapace, right lateral view, P6M2952. O. Carapace, right lateral view, P6M2953. P. Carapace, right lateral view, P6M2954. — Q–T. Bairdia limatusformis Forel, 2010. Q. Carapace, right lateral view, P6M2955. R. Carapace, left lateral view, P6M2956. S. Carapace, sub-dorsal view, P6M2957. T. Carapace, right lateral view, P6M2958. — U–V. Bairdia sp. 1. U. Carapace, right lateral view, P6M2959. V. Carapace, right lateral view, P6M2960. — W–X. Bairdia sp. 2. W. Carapace, dorsal view, P6M2961. X. Carapace, right lateral view, P6M2962. – Scale = 100 µm.
Fig. 3 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 3. Ostracods from the Dajiang section, South China. — A–D. Acratia candyae sp. nov. A. Holotype, carapace, right lateral view, P6M2917. B. Carapace, dorsal view, P6M2918. C. Paratype, carapace, right lateral view, P6M2919. D. Carapace, right lateral view, P6M2920. — E–F. Acratia subfusiformis Wang, 1978. E. Carapace, right lateral view, P6M2921. F. Carapace, right lateral view, P6M2922. — G. Acratia? sp. 1, carapace, right lateral view, P6M2923. — H. Acratia? sp. 2, carapace, right lateral view, P6M2924. — I. Acratia? sp. 3, carapace, right lateral view, P6M2925. — J–K. Acratia sp. 4. J. Carapace, left lateral view, P6M2926. K. Carapace, right lateral view, P6M2927. — L. Acratia sp. 5, carapace, right lateral view, P6M2928. — M. Acratiidae indet., carapace, right lateral view, P6M2929. — N–Q. Bairdia adelineae sp. nov. N. Holotype, carapace, right lateral view, P6M2930. O. Carapace, dorsal view, P6M2931. P. paratype, carapace, right lateral view, P6M2932. Q. Carapace, right lateral view, P6M2933. — R–V. Bairdia gaelleae Crasquin, 2010. R. Carapace, dorsal view, P6M2934. S. Carapace, right lateral view, P6M2935. T. Carapace, left lateral view, P6M2936. U. Carapace, right lateral view, P6M2937. V. Carapace, right lateral view, P6M2938. – Scale = 100 µm.
Fig. 2 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 2. Lithostratigraphy of the Dajiang Section, with the location of studied samples and ostracod species distribution through the section.
Fig. 13 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 13. Ostracods from the Dajiang section, South China. — A–B. Petasobairdia sp. 1. A. Carapace, right lateral view, P6M3082. B. Carapace, right lateral view, P6M3083. — C. Petasobairdia sp. 2, carapace, right lateral view, P6M3084. — D–E. Petasobairdia sp. 3. D. Carapace, right lateral view, P6M3085. E. Carapace, right lateral view, P6M3086. — F. Petasobairdia? sp. 4, carapace, right lateral view, P6M3087. — G. Spinocypris sp. 1, carapace, right lateral view, P6M3088. — H–I. Spinocypris? sp. 2. H. Carapace, right lateral view, P6M3089. I. Carapace, right lateral view, P6M3090. — J. Kempfina sp. 1, carapace, right lateral view, P6M3091. — K–L. Silenites sp. 1. K. Carapace, right lateral view, P6M3092. L. Carapace, right lateral view, P6M3093. — M-N. Silenites sp. 2. M. Carapace, right lateral view, P6M3094. N. carapace, right lateral view, P6M3095. — O. Silenites sp. 3, carapace, right lateral view, P6M3096. — P. Silenites sp. 4, carapace, right lateral view, P6M3097. — Q. Microcheilinella cf. venusta Chen, 1958, carapace, dorsal view, P6M3132. — R. Microcheilinella sp. 1, carapace, right lateral view, P6M3131. — S. Cetollina? sp. 1, carapace, right lateral view, P6M3098. — T–X. Paracypris gaetanii Crasquin–Soleau, 2006. T. Carapace, right lateral view, P6M3099. U. Carapace, right lateral view, P6M3100. V. Carapace, left lateral view, P6M3101. W. Carapace, left lateral view, P6M3102. X. Carapace, right lateral view, P6M3103. – Scale = 100 µm.
Fig. 11 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 11. Ostracods from the Dajiang section, South China. — A–B. Bairdiacypris sp. 8. A. Carapace, right lateral view, P6M3058. B. Carapace, right lateral view, P6M3059. — C–D. Bairdiacypris sp. 9. C. Carapace, right lateral view, P6M3060. D. Carapace, right lateral view, P6M3061. — E–F. Bythocypris? sp. 1. E. Carapace, right lateral view, P6M3062. F. Carapace, right lateral view, P6M3063. — G. Bythocypris sp. 2, carapace, right lateral view, P6M3064. — H. Bythocypris? sp. 3, carapace, right lateral view, P6M3065. — I. Fabalicypris parva Wang, 1978, carapace, right lateral view, P6M3066. — J–N. Liuzhinia antalyaensis Crasquin–Soleau, 2004. J. Carapace, right lateral view, P6M3067. K. Carapace, left lateral view, P6M3068. L. Carapace, left lateral view, P6M3069. M. Carapace, right lateral view, P6M3070. N. Carapace, right lateral view, P6M3071. — O.?Liuzhinia antalyaensis Crasquin– Soleau, 2004, carapace, left lateral view, P6M3072. — P. Liuzhinia sp., carapace, right lateral view, P6M3073. — Q–S. Liuzhinia sp. 2. Q. Carapace, right lateral view, P6M3074. R. Carapace, left lateral view, P6M3075. S. Carapace, right lateral view, P6M3076. — T–X. Orthobairdia jeanlouisi sp. nov. T. Holotype, carapace, right lateral view, P6M3077. U. Carapace, left lateral view, P6M3078. V. Paratype, carapace, dorsal view, P6M3079. W. Carapace, right lateral view, P6M3080. X. Carapace, right lateral view, P6M3081. – Scale = 100 µm.
Fig. 10 in Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
Fig. 10. Ostracods from the Dajiang section, South China. — A. Bairdia sp. 33, carapace, right lateral view, P6M3034. — B. Bairdia sp. 34, carapace, right lateral view, P6M3035. — C. Bairdia sp. 35, carapace, right lateral view, P6M3036. — D. Bairdia? sp. 36, carapace, right lateral view, P6M3037. — E–H. Bairdiacypris ottomanensis Crasquin–Soleau, 2004. E. Carapace, right lateral view, P6M3038. F. Carapace, right lateral view, P6M3039. G. Carapace, dorsal view, P6M3040. H. Carapace, right lateral view, P6M3041. — I. Bairdiacypris sp. 1, carapace, right lateral view, P6M3042. — J–K. Bairdiacypris sp. 2. J. Carapace, right lateral view, P6M3043. K. Carapace, right lateral view, P6M3044. — L–M. Bairdiacypris sp. 3. L. Carapace, right lateral view, P6M3045. M. Carapace, dorsal view, P6M3046. — N–Q. Bairdiacypris sp. 4. N. Carapace, right lateral view, P6M3047. O. Carapace, right lateral view, P6M3048. P. Carapace, right lateral view, P6M3049. Q. Carapace, right lateral view, P6M3050. — R–T. Bairdiacypris sp. 5. R. Carapace, right lateral view, P6M3051. S. Carapace, right lateral view, P6M3052. T. Carapace, left lateral view, P6M3053. — U. Bairdiacypris? sp. 6, carapace, right lateral view, P6M3054. — V–X. Bairdiacypris sp. 7. V. Carapace, right lateral view, P6M3055. W. Carapace, right lateral view, P6M3056. X. Carapace, right lateral view, P6M3057. – Scale = 100 µm.
Data from: A new tusked cistecephalid dicynodont (Therapsida, Anomodontia) from the upper Permian Upper Madumabisa Mudstone Formation, Luangwa Basin, Zambia
Cistecephalids are among the most distinctive Permian dicynodonts because of their highly derived skulls and postcrania, which indicate a fossorial ecology. Four cistecephalid species have been described from India, South Africa, and Tanzania; a fifth putative species has been reported from the Luangwa Basin of Zambia but never formally described. Here we present a detailed description of the Luangwa Basin cistecephalid, which we name Kembawacela kitchingi gen. et. sp. nov. The most obvious diagnostic character of K. kitchingi is the presence of caniniform tusks in most specimens. Other important characters include a pineal foramen located at the posterior end of the skull roof; an interparietal that has a pair of anterior processes that extend onto the dorsal surface of the skull, flanking the pineal foramen (but otherwise is restricted to the occipital surface); an undivided nuchal crest; and a trough on the ventral surface of the mid-ventral vomerine plate. Phylogenetic analysis reconstructs Kembawacela as a basal cistecephalid and confirms that Cistecephalidae is a well-supported clade. However, relationships within the clade received low branch support. Increased knowledge of cistecephalid diversity shows that they vary in functionally relevant characters, such as degree of inflation of the bony vestibule and the morphology of the scapula and humerus, indicating the need for a more nuanced approach to the relationship between form, function, and ecology in the clade. The highly allopatric distribution of cistecephalid species suggests that they experienced strong interspecific competition for limited resources and had limited dispersal ability, similar to extant subterranean mammals.
Figs 1-4 in New Genus Of The Family Liomopteridae (Insecta: Grylloblattida) From Lower Permian Of Russia
Figs 1-4. Uralioma variabilis gen. et sp. n. 1) holotype, spec. N 1700/3929; 2-4) paratypes, fore wing: 2) spec. N 1/334; 3) spec. N 1700/824; 4) spec. N 2/377.
Figs 5-8 in New Genus Of The Family Liomopteridae (Insecta: Grylloblattida) From Lower Permian Of Russia
Figs 5-8. Uralioma variabilis gen. et sp. n. 5-7) paratypes, fore wing: 5) spec. N 1700/869; 6) spec. N 1700/823; 7) spec. N 1/362; 8) paratype, hind wing, spec. N 1700/837.
Heterogeneous selectivity and morphological evolution of marine clades during the Permian-Triassic mass extinction
<p>This is a supplementary repository, including the dataset and codes we used in this manuscript. we developed a new method, called DeepMorph to analyze the morphological evolution of six marine clades (i.e., ammonoids, bivalves, brachiopods, gastropods, ostracods, and conodonts ) during the Permian-Triassic mass extinction events. The taxonomy dataset was uploaded and contains 599 genera and 656 images, spanning from the latest Permian (Changhsingian) to the earliest Triassic (Induan). </p>
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