New Pareiasaur Material and the Reestablishment of Honania Complicidentata
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Sauropareion Anoplus, with a Discussion of Possible Life History
The postcranial skeleton of the Early Triassic parareptile Sauropareion anoplus, with a discussion of possible life history MARK J. MACDOUGALL, SEAN P. MODESTO, and JENNIFER BOTHA−BRINK MacDougall, M.J., Modesto, S.P., and Botha−Brink, J. 2013. The postcranial skeleton of the Early Triassic parareptile Sauropareion anoplus, with a discussion of possible life history. Acta Palaeontologica Polonica 58 (4): 737–749. The skeletal anatomy of the Early Triassic (Induan) procolophonid reptile Sauropareion anoplus is described on the basis of three partial skeletons from Vangfontein, Middelburg District, South Africa. Together these three specimens preserve the large majority of the pectoral and pelvic girdles, articulated forelimbs and hindlimbs, and all but the caudal portion of the vertebral column, elements hitherto undescribed. Our phylogenetic analysis of the Procolophonoidea is consonant with previous work, positing S. anoplus as the sister taxon to a clade composed of all other procolophonids exclusive of Coletta seca. Previous studies have suggested that procolophonids were burrowers, and this seems to have been the case for S. anoplus, based on comparisons with characteristic skeletal anatomy of living digging animals, such as the presence of a spade−shaped skull, robust phalanges, and large unguals. Key words: Parareptilia, Procolophonidae, phylogenetic analysis, burrowing, Induan, Triassic, South Africa. Mark J. MacDougall [[email protected]], Department of Biology, Cape Breton University, Sydney, Nova Scotia, B1P 6L2, Canada and Department of Biology, University of Toronto at Mississauga, 3359 Mississauga Road, Ontario, L5L 1C6, Canada; Sean P. Modesto [[email protected]], Department of Biology, Cape Breton University, Sydney, Nova Scotia, B1P 6L2, Canada; Jennifer Botha−Brink [[email protected]], Karoo Palaeontology, National Museum, P.O. -
Ontogenetic Change in the Temporal Region of the Early Permian Parareptile Delorhynchus Cifellii and the Implications for Closure of the Temporal Fenestra in Amniotes
RESEARCH ARTICLE Ontogenetic Change in the Temporal Region of the Early Permian Parareptile Delorhynchus cifellii and the Implications for Closure of the Temporal Fenestra in Amniotes Yara Haridy*, Mark J. Macdougall, Diane Scott, Robert R. Reisz Department of Biology, University of Toronto Mississauga, Mississauga, Ontario, Canada * [email protected] a11111 Abstract A juvenile specimen of Delorhynchus cifellii, collected from the Early Permian fissure-fill deposits of Richards Spur, Oklahoma, permits the first detailed study of cranial ontogeny in this parareptile. The specimen, consisting of a partially articulated skull and mandible, exhib- OPEN ACCESS its several features that identify it as juvenile. The dermal tuberosities that ornament the dor- Citation: Haridy Y, Macdougall MJ, Scott D, Reisz sal side and lateral edges of the largest skull of D. cifellii specimens, are less prominent in RR (2016) Ontogenetic Change in the Temporal the intermediate sized holotype, and are absent in the new specimen. This indicates that the Region of the Early Permian Parareptile new specimen represents an earlier ontogenetic stage than all previously described mem- Delorhynchus cifellii and the Implications for bers of this species. In addition, the incomplete interdigitation of the sutures, most notably Closure of the Temporal Fenestra in Amniotes. PLoS ONE 11(12): e0166819. doi:10.1371/journal. along the fronto-nasal contact, plus the proportionally larger sizes of the orbit and temporal pone.0166819 fenestrae further support an early ontogenetic stage for this specimen. Comparisons Editor: Thierry Smith, Royal Belgian Institute of between this juvenile and previously described specimens reveal that the size and shape of Natural Sciences, BELGIUM the temporal fenestra in Delorhynchus appear to vary through ontogeny, due to changes in Received: July 18, 2016 the shape and size of the bordering cranial elements. -
Analysis of Millerettid Parareptile Relationships in the Light of New Material of BROOMIA PERPLEXA Watson, 1914, from the Permian of South Africa
Journal of Systematic Palaeontology 6 (4): 453–462 Issued 24 November 2008 doi:10.1017/S147720190800254X Printed in the United Kingdom C The Natural History Museum ! Analysis of millerettid parareptile relationships in the light of new material of BROOMIA PERPLEXA Watson, 1914, from the Permian of South Africa Juan Carlos Cisneros Departamento de Paleontologia† e Estratigrafia, Universidade Federal do Rio Grande do Sul, Porto Alegre, CP 15001, 91501-970, Brazil; and Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, WITS 2050, Johannesburg, South Africa Bruce S. Rubidge Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, WITS 2050, Johannesburg, South Africa Richard Mason Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, WITS 2050, Johannesburg, South Africa Charlton Dube Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, WITS 2050, Johannesburg, South Africa SYNOPSIS A second specimen of the poorly known millerettid Broomia perplexa is reported. It consists of a cranium and partially articulated postcranium. As indicated by its small size (ca.35% shorter skull than the holotype) and unfused pelvis and limbs, the new specimen is a sub-adult indi- vidual. Comparison with the holotype reveals only minor differences that are ascribed to ontogenetic or individual variation. Accordingly we consider the new specimen to represent the second record of Broomia,discovered90yearsafterthedescriptionoftheholotype.Apreliminaryphylogenetic analysis of millerettid inter-relationships identifies Broomia as a millerettid related to the genus Millerosaurus.TheenigmaticparareptileEunotosaurus africanus is nested within Millerettidae as the sister taxon of Milleretta rubidgei.WhereasmillerettidsarewellknownfromthelatestPermian Dicynodon Assemblage Zone of the Beaufort Group of South Africa, Broomia and Eunotosaurus are found in the Middle Permian Tapinocephalus Assemblage Zone. -
Jiyuan: Landscape, Inscriptions and the Past
Jiyuan: landscape, inscriptions and the past Barend J. ter Haar (Oxford University) With the support of the SSHRC a small group of scholars and graduate students went to Jiyuan 濟源, in western Henan, to collect inscriptions. The group was certainly successful, both in obtaining better versions of inscriptions that we already knew about and collecting a wealth of inscriptions whose existence had gone unnoticed even by the local staff of the Cultural Affairs Bureau. Our principal purpose was collecting inscriptions on and in the Temple of River Ji (jidu miao 濟瀆廟) and on the Daoist sites of Wangwu Mountain 王屋山. I focus here on doing research and the importance of imagining the past, rather than more concrete (and hopefully original) analytical results. To me thinking through the problem of imagining the past and the wonderful conversations with colleagues, students and local people —as well as some 200 or so late sixteenth century votive inscriptions containing names, places and amounts of the donations—were the most important results of our expedition. Since this kind of experience is rarely preserved, but remains part of our oral lore destined for direct colleagues, local student and relatives, I thought should write down some of my impressions during and after this visit, organized topically. The field team (photograph by Liu Jie) Our lost sense of historical distances and physical effort In terms of modern transport, the city of Jiyuan and its surroundings can no longer be considered peripheral. One can fly into Beijing, Shanghai and Guangzhou from most major airports in the world. From there one changes planes to Zhengzhou, the capital of Henan province, and a further bus or taxi drive of several hours brings one safely to any hotel in Jiyuan. -
Reptile Family Tree
Reptile Family Tree - Peters 2015 Distribution of Scales, Scutes, Hair and Feathers Fish scales 100 Ichthyostega Eldeceeon 1990.7.1 Pederpes 91 Eldeceeon holotype Gephyrostegus watsoni Eryops 67 Solenodonsaurus 87 Proterogyrinus 85 100 Chroniosaurus Eoherpeton 94 72 Chroniosaurus PIN3585/124 98 Seymouria Chroniosuchus Kotlassia 58 94 Westlothiana Casineria Utegenia 84 Brouffia 95 78 Amphibamus 71 93 77 Coelostegus Cacops Paleothyris Adelospondylus 91 78 82 99 Hylonomus 100 Brachydectes Protorothyris MCZ1532 Eocaecilia 95 91 Protorothyris CM 8617 77 95 Doleserpeton 98 Gerobatrachus Protorothyris MCZ 2149 Rana 86 52 Microbrachis 92 Elliotsmithia Pantylus 93 Apsisaurus 83 92 Anthracodromeus 84 85 Aerosaurus 95 85 Utaherpeton 82 Varanodon 95 Tuditanus 91 98 61 90 Eoserpeton Varanops Diplocaulus Varanosaurus FMNH PR 1760 88 100 Sauropleura Varanosaurus BSPHM 1901 XV20 78 Ptyonius 98 89 Archaeothyris Scincosaurus 77 84 Ophiacodon 95 Micraroter 79 98 Batropetes Rhynchonkos Cutleria 59 Nikkasaurus 95 54 Biarmosuchus Silvanerpeton 72 Titanophoneus Gephyrostegeus bohemicus 96 Procynosuchus 68 100 Megazostrodon Mammal 88 Homo sapiens 100 66 Stenocybus hair 91 94 IVPP V18117 69 Galechirus 69 97 62 Suminia Niaftasuchus 65 Microurania 98 Urumqia 91 Bruktererpeton 65 IVPP V 18120 85 Venjukovia 98 100 Thuringothyris MNG 7729 Thuringothyris MNG 10183 100 Eodicynodon Dicynodon 91 Cephalerpeton 54 Reiszorhinus Haptodus 62 Concordia KUVP 8702a 95 59 Ianthasaurus 87 87 Concordia KUVP 96/95 85 Edaphosaurus Romeria primus 87 Glaucosaurus Romeria texana Secodontosaurus -
Maria Khayutina • [email protected] the Tombs
Maria Khayutina [email protected] The Tombs of Peng State and Related Questions Paper for the Chicago Bronze Workshop, November 3-7, 2010 (, 1.1.) () The discovery of the Western Zhou period’s Peng State in Heng River Valley in the south of Shanxi Province represents one of the most fascinating archaeological events of the last decade. Ruled by a lineage of Kui (Gui ) surname, Peng, supposedly, was founded by descendants of a group that, to a certain degree, retained autonomy from the Huaxia cultural and political community, dominated by lineages of Zi , Ji and Jiang surnames. Considering Peng’s location right to the south of one of the major Ji states, Jin , and quite close to the eastern residence of Zhou kings, Chengzhou , its case can be very instructive with regard to the construction of the geo-political and cultural space in Early China during the Western Zhou period. Although the publication of the full excavations’ report may take years, some preliminary observations can be made already now based on simplified archaeological reports about the tombs of Peng ruler Cheng and his spouse née Ji of Bi . In the present paper, I briefly introduce the tombs inventory and the inscriptions on the bronzes, and then proceed to discuss the following questions: - How the tombs M1 and M2 at Hengbei can be dated? - What does the equipment of the Hengbei tombs suggest about the cultural roots of Peng? - What can be observed about Peng’s relations to the Gui people and to other Kui/Gui- surnamed lineages? 1. General Information The cemetery of Peng state has been discovered near Hengbei village (Hengshui town, Jiang County, Shanxi ). -
A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes
GENERAL COMMENTARY published: 03 December 2018 doi: 10.3389/feart.2018.00220 Response: Commentary: A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes Michel Laurin 1* and Graciela Piñeiro 2 1 CR2P (UMR 7207), CNRS/MNHN Sorbonne Université, “Centre de Recherches sur la Paléobiodiversité et les Paléoenvironnements”, Muséum National d’Histoire Naturelle, Paris, France, 2 Departamento de Paleontología, Facultad de Ciencias, Montevideo, Uruguay Keywords: Mesosauridae, Parareptilia, Synapsida, Sauropsida, Amniota, Paleozoic, temporal fenestration A Commentary on Commentary: A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes by MacDougall, M. J., Modesto, S. P., Brocklehurst, N., Verrière, A., Reisz, R. R., and Fröbisch, J. (2018). Front. Earth Sci. 6:99. doi: 10.3389/feart.2018.00099 INTRODUCTION Edited by: Corwin Sullivan, University of Alberta, Canada Mesosaurs, known from the Early Permian of southern Africa, Brazil, and Uruguay, are the oldest known amniotes with a primarily, though probably not strictly, aquatic lifestyle (Nuñez Demarco Reviewed by: et al., 2018). Despite having attracted the attention of several prominent scientists, such as Wegener Tiago Simoes, University of Alberta, Canada (1966), who used them to support his theory of continental drift, and the great anatomist and paleontologist von Huene (1941), who first suggested the presence of a lower temporal fenestra *Correspondence: Michel Laurin in Mesosaurus, several controversies still surround mesosaurs. One concerns the presence of the [email protected] lower temporal fenestra in mesosaurs, which we accept (Piñeiro et al., 2012a; Laurin and Piñeiro, 2017, p. 4), contrary to Modesto (1999, 2006) and MacDougall et al. -
An Indian Journal FULL PAPER BTAIJ, 10(24), 2014 [15149-15157]
[Type text] ISSN : [Type0974 -text] 7435 Volume 10[Type Issue text] 24 2014 BioTechnology An Indian Journal FULL PAPER BTAIJ, 10(24), 2014 [15149-15157] Adaptability between agricultural water use and water resource characteristics Zhongpei Liu, Yuting Zhao, Yuping Han* College of Water Resources, North China University of Water Resources and Electric Power, Zhengzhou, 450045, (CHINA) E-mail: [email protected] ABSTRACT Based on analysis of characteristic of agricultural water, water requirement characteristic of main water-intensive crops and effective precipitation throughout each city in Henan Province, agricultural water deficit and crop irrigation water productivity under the condition of natural precipitation and manual irrigation are calculated and the adaptability between agricultural water and water resources characteristic are revealed. The results show that under the condition of natural precipitation, water deficit in Henan Province is 240.5mm and falls to 76.3 mm after manual irrigation. The deficit period is concentrated mostly in March ~ June, accounting for more than 65% of annual water deficit. Spatially water deficit is gradually decreasing from north to south, and agricultural irrigation water productivity is relatively high in central China and relatively low in the south and north. Thereby, the region with full irrigation (the south) and the region with large crop water deficit (the north) have a relatively low irrigation water productivity; a certain degree of water deficit (in central China) is conductive to improvement of crop irrigation water productivity. And then the adaptability between regional agricultural water and water resource characteristic shall not be balanced simply based on the degree of crop water deficit, instead, it shall be closely combined with irrigation water productivity. -
Simulation of Mining-Induced Ground Damage Using Orthogonal
applied sciences Article Simulation of Mining-Induced Ground Damage Using Orthogonal Experiments to Determine Key Parameters of Super-Large Coalface: A Case Study in Shendong Coalfield in China Yinfei Cai 1,* , Xiaojing Li 2, Wu Xiao 3,* and Wenkai Zhang 4 1 College of Mining Engineering, Taiyuan University of Technology, Taiyuan 030024, China 2 School of Public Administration, Shanxi University of Finance and Economics, Taiyuan 030024, China; [email protected] 3 School of Public Affairs, Zhejiang University, Hangzhou 310058, China 4 Institute of land reclamation and ecological restoration, China University of Mining & Technology (Beijing), Beijing 100083, China; [email protected] * Correspondence: [email protected] (Y.C.); [email protected] (W.X.) Received: 29 February 2020; Accepted: 23 March 2020; Published: 26 March 2020 Abstract: High-strength mining of super-large coalfaces in the Shendong coalfield causes significant damage to the ground surface. To study the key parameters of undermined coalfaces that affect ground damage, 25 numerical simulation models were designed using an orthogonal experimental method based on the geological and mining conditions of the Bulianta Mine. In the orthogonal design, four factors (the lengths in both the dip and strike directions, the thickness and the mining speed of the coalface) were considered, with five levels designed for each factor. The subsidence displacements and deformations caused by the excavation were then simulated and verified using field surveying data. A damage extent index (DEI) was introduced and used to assess the extent of global ground damage caused by each simulative excavation. Analysis of variance (ANOVA) method was then employed to determine the key parameters of the coalface that significantly influence the ground damage. -
Effects of Land Use Change on Ecosystem Services in Arid Area Eco- Logical Migration
Chin. Geogra. Sci. 2018 Vol. 28 No. 5 pp. 894–906 Springer Science Press https://doi.org/10.1007/s11769-018-0971-5 www.springerlink.com/content/1002-0063 Effects of Land Use Change on Ecosystem Services in Arid Area Eco- logical Migration LIU Xiaopeng1, 2, CHEN Xiao1, 2, HUA Kaiping1, 3, WANG Yajuan1, 2, WANG Peng1, 2, HAN Xiaojia1, 2, YE Junyan1, 2, 1, 2 WEN Shengqiang (1. School of Resources and Environment, Ningxia University, Yinchuan 750021, China; 2. Key Laboratory (China-Arab) of Resource Evaluation and Environmental Regulation of Arid Region in Ningxia, Yinchuan 750021, China; 3. School of Tourism and Environment, Shaanxi Normal University, Xi’an 710062, China) Abstract: Ecological migration is the process of increasing the population density in the immigration area and transferring the ecologi- cal pressure from emigration area to immigration area. This process may result in significant changes in land use and land cover in the area of immigration and have an important effect on ecosystem services. Therefore, scientifically revealing the effects and differentia- tion mechanisms of ecological migration on ecosystem services is becoming an important issue related to the implementation of the national ecological migration strategy in China. This study employed the Hongsibu District as a typical example of ecological migration. Hongsibu District is located in the central Ningxia steppe and desert steppe areas. Remote sensing data covering five periods from the period before ecological migration in 1995 and after migration in 2000, 2005, 2010, and 2015 was used to measure the value of ecosys- tem services (ESV). A geographical detector model and the value of ecosystem services model were used to diagnose the dynamic mechanism of the effects of land use change on ecosystem services. -
Permian Tetrapods from the Sahara Show Climate-Controlled Endemism in Pangaea
letters to nature 6. Wysession, M. et al. The Core-Mantle Boundary Region 273–298 (American Geophysical Union, faunas that dominated tropical-to-temperate zones to the north Washington, DC, 1998). 13–15 7. Sidorin, I., Gurnis, M., Helmberger, D. V.& Ding, X. Interpreting D 00 seismic structure using synthetic and south . Our results show that long-standing theories of waveforms computed from dynamic models. Earth Planet. Sci. Lett. 163, 31–41 (1998). Late Permian faunal homogeneity are probably oversimplified as 8. Boehler, R. High-pressure experiments and the phase diagram of lower mantle and core constituents. the result of uneven latitudinal sampling. Rev. Geophys. 38, 221–245 (2000). For over 150 yr, palaeontologists have understood end-Palaeozoic 9. Alfe`, D., Gillan, M. J. & Price, G. D. Composition and temperature of the Earth’s core constrained by combining ab initio calculations and seismic data. Earth Planet. Sci. Lett. 195, 91–98 (2002). terrestrial ecosystems largely on the basis of Middle and Late 10. Thomas, C., Kendall, J. & Lowman, J. Lower-mantle seismic discontinuities and the thermal Permian tetrapod faunas from southern Africa. The fauna of these morphology of subducted slabs. Earth Planet. Sci. Lett. 225, 105–113 (2004). rich beds, particularly South Africa’s Karoo Basin, has provided 11. Thomas, C., Garnero, E. J. & Lay, T. High-resolution imaging of lowermost mantle structure under the fundamental insights into the origin of modern terrestrial trophic Cocos plate. J. Geophys. Res. 109, B08307 (2004). 16 12. Mu¨ller, G. The reflectivity method: A tutorial. Z. Geophys. 58, 153–174 (1985). structure and the successive adaptations that set the stage for the 13 13. -
Table of Codes for Each Court of Each Level
Table of Codes for Each Court of Each Level Corresponding Type Chinese Court Region Court Name Administrative Name Code Code Area Supreme People’s Court 最高人民法院 最高法 Higher People's Court of 北京市高级人民 Beijing 京 110000 1 Beijing Municipality 法院 Municipality No. 1 Intermediate People's 北京市第一中级 京 01 2 Court of Beijing Municipality 人民法院 Shijingshan Shijingshan District People’s 北京市石景山区 京 0107 110107 District of Beijing 1 Court of Beijing Municipality 人民法院 Municipality Haidian District of Haidian District People’s 北京市海淀区人 京 0108 110108 Beijing 1 Court of Beijing Municipality 民法院 Municipality Mentougou Mentougou District People’s 北京市门头沟区 京 0109 110109 District of Beijing 1 Court of Beijing Municipality 人民法院 Municipality Changping Changping District People’s 北京市昌平区人 京 0114 110114 District of Beijing 1 Court of Beijing Municipality 民法院 Municipality Yanqing County People’s 延庆县人民法院 京 0229 110229 Yanqing County 1 Court No. 2 Intermediate People's 北京市第二中级 京 02 2 Court of Beijing Municipality 人民法院 Dongcheng Dongcheng District People’s 北京市东城区人 京 0101 110101 District of Beijing 1 Court of Beijing Municipality 民法院 Municipality Xicheng District Xicheng District People’s 北京市西城区人 京 0102 110102 of Beijing 1 Court of Beijing Municipality 民法院 Municipality Fengtai District of Fengtai District People’s 北京市丰台区人 京 0106 110106 Beijing 1 Court of Beijing Municipality 民法院 Municipality 1 Fangshan District Fangshan District People’s 北京市房山区人 京 0111 110111 of Beijing 1 Court of Beijing Municipality 民法院 Municipality Daxing District of Daxing District People’s 北京市大兴区人 京 0115