A new Bergeria (Flemingitaceae) from the Mississippian of Xinjiang, NW China and its evolutionary implications
Ru Feng1,2, Ashalata D’Rozario3, Jian-Wei Zhang2
1 School of Urban and Environment Science, Huaiying Normal University, Huai’an 223300, Jiangsu Province, China; 2 Xinjiang Institute of Ecology and Geography, Chinese Academy of Science, Urumqi 830011, Xinjiang Uygur Autonomous Region, Chinal; 3 Department of Botany, Narasinha Dutt College, 129 Bellilious Road, Howrah 711101, India
Abstract A new Bergeria (Lepidodendrales, Flemingitaceae), B. wenquanensis sp. nov., is described in this paper, typically characterized by the longest and elongated leaf cushions ever found. The specimen, collected from the Mississippian of Wenquan County, Xinjiang Uygur Autonomous Region, China, is represented by a fossil stem about two meters long, with distinct leaf cushions. The genus Bergeria has usually been assigned to partially decorticated Lepidodendron stems. Although Cathaysian Lepidodendron have been extensively reported in China, most of them were found in the central, eastern and southern parts of the country, rarely in northwestern China. This new species is so far the westernmost record and the most isolated representative from the Cathaysian Lepidodendron center. Based on the distribution of the Cathaysian Lepidodendron during the Mississippian, most of the species were in the South China Plate near the Equator, while the new species is discrete in the north, far from the Equator. According to the spatiotemporal distribution of Cathaysian Lepidodendron, this genus appeared during the Mississippian, a period which was represented by rather few species, it flourished and expanded northwards during the Pennsylvanian, taking the north block of the South China Plate as the center. Since the Cisuralian to the Guadalupian, the genus became gradually sparser in all areas of distribution, probably due to strong climate change. During the Lopingian, the genus migrated southwards to the South China block and had a broader distribution range again, and it became extinct to the end of this interval. The new species is also significant for the evolution of Lepidodendron leaf cushions. During the Mississippian, the primitive species of Lepidodendron usually had narrow, fusiform leaf cushions, while the Pennsylvanian or Permian species were more variable in shape of leaf cushions, from inverted water-drop, rhomboidal, hexagonal, trapeziform to horizontal rhomboidal.
Fund:This research was supported by the National Natural Science Foundation of China under the Grant 41271070 and the West Light Foundation of Chinese Academy of Sciences under Grant 2015-XBQN-B-25.
Corresponding Authors:*zhangjianwei@ms.xjb.ac.cn
Cite this article:
. A new Bergeria (Flemingitaceae) from the Mississippian of Xinjiang, NW China and its evolutionary implications[J]. , 2019, 8(1): 89-98.
. A new Bergeria (Flemingitaceae) from the Mississippian of Xinjiang, NW China and its evolutionary implications[J]. Journal of Palaeogeography, 2019, 8(1): 89-98.
Álvarez-Vázquez C.,R.H. Wagner.2014. Lycopsida from the lower Westphalian (Middle Pennsylvanian) of the Maritime Provinces, Canada.Atlantic Geology 50: 167-232.
[2]
Bateman R.M.,W.A. DiMichele, and D.A. Willard.1992. Experimental cladistic analysis of anatomically preserved arborescent lycopsids from the Carboniferous of Euramerica: An essay on paleobotanical phylogenetics.Annals of the Missouri Botanical Garden 79(3): 500-559.
[3]
Bercovici A.,S. Bourquin,J. Broutin,J. Steyer,B. Battail,M. Véran,R. Vacant,B. Khenthavong, and S. Vongphamany.2012. Permian continental paleoenvironments in southeastern Asia: New insights from the Luang Prabang Basin (Laos).Journal of Asian Earth Sciences 60: 197-211.
[4]
Booi M.,I.M. van Waveren,J.H.A. van Konijnenburg-van Cittert, and P.L. de Boer.2008. New material ofMacralethopteris from the Early Permian Jambi flora (Middle Sumatra, Indonesia) and its palaeoecological implications. Review of Palaeobotany and Palynology 152(3): 101-112.
[5]
Cleal C.J.,B.A. Thomas.2005. Palaeozoic tropical rainforests and their effect on global climates: is the past the key to the present?Geobiology 3(1): 13-31.
[6]
Cleal C.J.,Z.Q. Wang.2002. A new and diverse plant fossil assemblage from the upper Westphalian Benxi Formation, Shanxi, China, and its palaeofloristic significance.Geological Magazine 139(2): 107-130.
[7]
Cleal C.J.,S. Opluštil B.A. Thomas,Y. Tenchov,O.A. Abbink,J. Bek,T. Dimitrova,J. Drábková C. Hartkopffröder, and T.V. Hoof.2009. Late Moscovian terrestrial biotas and palaeoenvironments of Variscan Euramerica.Netherlands Journal of Geosciences 88(4): 181-278.
[8]
Compile Team of Paleozoic Plant in China of Institute of Botany, Chinese Academy of Sciences (CTPP). 1974. Fossil Flora of China, Volume 1: Paleozoic Plant in China. Beijing: Science Press (in Chinese).
[9]
DiMichele W.A.1985. Diaphorodendron, gen. nov., a segregate from Lepidodendron(Pennsylvanian age). Systematic Botany 10(4): 453-458.
[10]
DiMichele W.A.2014. Wetland-dryland vegetational dynamics in the Pennsylvanian ice age tropics.International Journal of Plant Sciences 175(2): 123-164.
[11]
DiMichele W.A.,R.M. Bateman.1992. Diaphorodendraceae, fam. nov. (Lycopsida: Carboniferous): Systematics and evolutionary relationships ofDiaphorodendron and Synchysidendron, gen. nov. American Journal of Botany 79(6): 605-617.
[12]
DiMichele, W.A., C.B. Cecil, D.S. Chaney, S.D. Elrick, S.G. Lucas, R. Lupia, W.J. Nelson, and N.J. Tabor. 2011. Pennsylvanian-Permian vegetational changes in tropical Euramerica. In: J.A. Harper (ed.). Geology of the Pennsylvanian Permian in the Dunkard Basin: Guidebook. 76th Annual Field Conference of Pennsylvania Geologists, Washington, PA, pp. 60-102.
[13]
Fluteau F.,J. Besse,J. Broutin, and M. Berthelin.2001. Extension of Cathaysian Fora during the Permian: Climatic and paleogeographic constraints.Earth and Planetary Science Letters 193(3-4): 603-616.
[14]
Hilton J.,C.J. Cleal.2007. The relationship between Euramerican and Cathaysian tropical floras in the Late Palaeozoic: Palaeobiogeographical and palaeogeographical implications.Earth-Science Reviews 85(3-4): 85-116.
[15]
Leclercq S.1960. Réfendage dùne roche fossilifère et dégagement de ses fossiles sous binoculaire.Senckenbergiana Lethaea 41: 483-487.
[16]
Li X.X.1963. Yuemengou Group plant fossil in North China. Palaeontologia Sinica 148 (6): 1-185; 45 plates (in Chinese).
[17]
Li X.X.1997. The origin, evolution and distribution of the Cathaysian Flora in East Asia.Acta Palaeontologica Sinica 36(4): 411-422 (in Chinese with English abstract).
[18]
Li X.X.,X.Y. Wu.1996. Late Paleozoic phytogeographic provinces in China and its adjacent regions.Review of Palaeobotany and Palynology 90(1): 41-62.
[19]
Moore L.C.,J. Wittry, and W.A. DiMichele.2014. The Okmulgee, Oklahoma fossil flora, a Mazon Creek equivalent: Spatial conservatism in the composition of Middle Pennsylvanian wetland vegetation over 1100 km.Review of Palaeobotany and Palynology 200: 24-52.
[20]
Naugolnykh S.V.,J.H. Jin.2014. An Early Carboniferous flora of the Huadu locality from South China: Its taxonomic composition, paleophytogeographical position and paleoecological interpretation.Acta Geologica Sinica (English Edition) 88(5): 1341-1351.
[21]
Phillips T.L.,W.A. DiMichele.1992. Comparative ecology and life-history biology of arborescent lycopsids in Late Carboniferous swamps of Euramerica.Annals of the Missouri Botanical Garden 79(3): 560-588.
[22]
Presl K.B.1838. The genus Bergeria. In: K.M. Sternberg (ed.). Versuch einer geognostisch-botanischer Darstellung der Flora der Vorwelt, Volume 2. Johann Spurny, Prague, pp. 81-220 (in German).
[23]
Rees P.M.2002. Land-plant diversity and the end-Permian mass extinction.Geology 30(9): 827-830.
[24]
Rigby J. F.,1998. Upper Palaeozoic floras of SE Asia. Biogeography and geological evolution of SE Asia. In: Biogeography and Geological Evolution of SE Asia, Edition 1. Backhuys Publishers, pp. 73-82.
[25]
Sternberg K.M.1820. Versuch einer geognostisch-botanischer Darstellung der Flora der Vorwelt, Volume 1. Prague: Johann Spurny (in German).
[26]
Stevens L.G.,J. Hilton,D.P.G. Bond,I.J. Glasspool, and P.E. Jardine.2011. Radiation and extinction patterns in Permian floras from North China as indicators for environmental and climate change.Journal of the Geological Society 168(2): 607-619.
[27]
Sun K.Q.1999. Origin, evolution and extinction of Cathaysia flora.Chinese Science Bulletin 44(2): 100-107.
[28]
Sun K.Q.2002. The Cathaysia flora and its comparison with global contemporaneous floras.Earth Science Frontiers 9(3): 73-84 (in Chinese with English abstract).
[29]
Sun K.Q.,J.Z. Cui, and S.J. Wang. 2010. Fossil Flora of China, Volume 2: Fossil Pteridophytes in China. Beijing: Higher Education Press (in Chinese).
[30]
Taylor T.N.,E.L. Taylor, and M. Krings. 2009. Paleobotany: The Biology and Evolution of Fossil Plants (Second Edition). London: Academic Press, pp. 265-293.
[31]
Thomas B.A.1970. Epidermal studies in the interpretation ofLepidodendron species. Palaeontology 13(1): 145-173.
[32]
Wang J.2010. Late Paleozoic macrofloral assemblages from Weibei Coalfield, with reference to vegetational change through the Late Paleozoic Ice-age in the North China Block.International Journal of Coal Geology 83(2): 292-317.
[33]
Wang J.,H.W. Pfefferkorn.2013. The Carboniferous-Permian transition on the North China microcontinent — Oceanic climate in the tropics.International Journal of Coal Geology 119: 106-113.
[34]
Wang J.,H.W. Pfefferkorn,Y. Zhang, and Z. Feng.2012. Permian vegetational Pompeii from Inner Mongolia and its implications for landscape paleoecology and paleobiogeography of Cathaysia.Proceedings of the National Academy of Sciences of the United States of America 109(13): 4927-4932.
[35]
Wang Z.Q.,A.S. Chen.2001. Traces of arborescent lycopsids and dieback of the forest vegetation in relation to the terminal Permian mass extinction in North China.Review of Palaeobotany and Palynology 117(4): 217-243.
[36]
Xinjiang Bureau of Geology and Mineral Resources (XBGMR). 1993. Regional Geology of Xinjiang Uygur Autonomous Region (Geological Memoirs of Ministry of Geology and Mineral Resources of the People’s Republic of China, (1) Regional Geology, no. 32). Beijing: Geological Publishing House, pp. 145-147 (in Chinese).
[37]
Yang G.X.,H.S. Wang.2012. Yuzhou Flora — A hidden gem of the Middle and Late Cathaysian Flora.Science China Earth Sciences 55(10): 1601-1619.