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Relevant bibliographies by topics / Gondwana

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Academic literature on the topic 'Gondwana'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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Journal articles on the topic "Gondwana"

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Chandra, Shaila, and Sun Keqin. "Evolution and comparison of the Gondwana flora and the Cathaysia flora." Journal of Palaeosciences 46, no. 3 (1997): 35–46. http://dx.doi.org/10.54991/jop.1997.1346.

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By the Late Palaeozoic, during the Late Carboniferous and Permian, the global vegetation was distinguishable into four main geobotanical provinces: Euramerican, Angara, Gondwana and Cathaysia. The largest of these four provinces was the Gondwana Supercontinent comprising two segments- (i) Western Gondwana consisting of South America and Africa possibly Iran-Afghanistan, and (ii) Eastern Gondwana consisting of Antarctica, Australia and India. The Cathaysia flora is the main flora of the Carboniferous and the Permian mainly distributed in present-day China, Korea, Japan, Laos, Thailand, Indonesi

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McLoughlin, Stephen. "The breakup history of Gondwana and its impact on pre-Cenozoic floristic provincialism." Australian Journal of Botany 49, no. 3 (2001): 271. http://dx.doi.org/10.1071/bt00023.

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The concept of ‘Gondwana’, an ancient Southern Hemisphere supercontinent, is firmly established in geological and biogeographical models of Earth history. The term Gondwana (Gondwanaland of some authors) derives from the recognition by workers at the Indian Geological Survey in the mid- to late 19th century of a distinctive sedimentary sequence preserved in east central India. This succession, now known to range in age from Permian to Cretaceous, is lithologically and palaeontologically similar to coeval non-marine sedimentary successions developed in most of the Southern Hemisphere continents

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Lakova, Iskra. "Paleobiogeographical affinities of Pridolian and Lochkovian chitinozoans from North Bulgaria." Geologica Balcanica 25, no. 5-6 (1995): 23–28. http://dx.doi.org/10.52321/geolbalc.25.5-6.23.

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Chitinozoan assemblages of Pridolian and Lochkovian Age from the subsurface of North Bulgaria have been compared with coeval chitinozoan faunas from numerous localities in Laurassia and Gondwana. The Pridolian and Lochkovian chitinozoan faunas of NW Bulgaria seem related without any doubt to the North Gondwanian realm, whereas those from NE Bulgaria are not diverse enough to precisely estimate their biogeographic position within the Laurassia - Gondwana interface.

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Lasseron, Maxime, Ronan Allain, Emmanuel Gheerbrant, et al. "New data on the microvertebrate fauna from the Upper Jurassic or lowest Cretaceous of Ksar Metlili (Anoual Syncline, eastern Morocco)." Geological Magazine 157, no. 3 (2019): 367–92. http://dx.doi.org/10.1017/s0016756819000761.

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AbstractThe Middle Jurassic – Early Cretaceous period witnessed the emergence of some major representatives of modern continental vertebrate groups (stem lissamphibians, squamates, therian mammals and birds) and angiosperms, at a time when fragmentation of Pangaea was underway. The successive Moroccan microvertebrate faunas of Ksar Metlili (?Berriasian) and Guelb el Ahmar (Bathonian) from the Anoual Syncline significantly improve our poor knowledge of Gondwanan and especially African palaeobiodiversity at this time. They are among the richest known from the Mesozoic of Gondwana, and are well p

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Acharyya, S. K. "Limits of Greater Indian Plate during Gondwana time." Journal of Palaeosciences 36 (December 31, 1987): 290–301. http://dx.doi.org/10.54991/jop.1987.1588.

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Limits of the Greater Indian Gondwana continent varied with its break-up and collisional episodes. Late Palaeozoic basal Gondwana type glaciogene and associated sediments containing cold-water marine fauna, with or without Glossopteris, Cathaysian floral remains or admixtures occur in and across the Himalaya, in south Pamir, Tibet and in Shan-Tenesserim-Malaysian area, i.e., across the Late Mesozoic peri-Indian ophiolite belts. Cathaysian Flora with or without Glossopteris intercalations also occurs in western Iraq and New Guinea, both representing parts of the Gondwanic shield. Thus during La

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Jong, Rienk de. "Are there butterflies with Gondwanan ancestry in the Australian region?" Invertebrate Systematics 17, no. 1 (2003): 143. http://dx.doi.org/10.1071/is02021.

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A sister-group relationship of endemic taxa in at least two Gondwanan fragments is considered an indication of a possible Gondwanan ancestry. Without a test of the age of the relationship, such an ancestry remains hypothetical. The relationships of all genera and higher taxa endemic to the Australian region with endemic taxa in other fragments of Gondwana are tested. Out of a total of 207 butterfly genera, 96 genera are endemic. Such a relationship is supported by morphological and molecular characters in a number of analyses in only one case(Cressida with Euryades, in South America). Applicat

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Singh, H. P., and B. S. Venkatachala. "Upper Jurassic-Lower Cretaceous spore-pollen assemblages in the peninsular India." Journal of Palaeosciences 36 (December 31, 1987): 168–76. http://dx.doi.org/10.54991/jop.1987.1575.

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The Upper Jurassic-Lower Cretaceous spore-pollen assemblages recovered from the ‘Upper Gondwana’ sediments in the western, central, southern and eastern parts of the country have been reviewed. Palaeontological geological, tectonic and environmental evidences have been used for a reinterpretation of palynological data. Stratigraphically important palynotaxa have been identified. The occurrence of continental Jurassic assemblages has not been considered authentic. The usage of the term ‘Gondwana’ for continental, as well as paralic sediments, has been questioned. The distribution of some signif

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Murphy, J. Brendan, R. Damian Nance, J. Duncan Keppie, and Jaroslav Dostal. "Role of Avalonia in the development of tectonic paradigms." Geological Society, London, Special Publications 470, no. 1 (2018): 265–87. http://dx.doi.org/10.1144/sp470.12.

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AbstractThe geological evolution of Avalonia was fundamental to the first application of plate tectonic principles to the pre-Mesozoic world. Four tectonic phases have now been identified. The oldest phase (760–660 Ma) produced a series of oceanic arcs, some possibly underlain by thin slivers of Baltica crust, which accreted to the northern margin of Gondwana between 670 and 650 Ma. Their accretion to Gondwana may be geodynamically related to the break-up of Rodinia. After accretion, subduction zones stepped outboard, producing the main phase (640–570 Ma) of arc-related magmatism and basin for

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Russell, Dale A. "China and the lost worlds of the dinosaurian era." Paleontological Society Special Publications 6 (1992): 257. http://dx.doi.org/10.1017/s2475262200008170.

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What is known of dinosaurian biogeography suggests a centre of evolution first on a fragmenting Pangea-Gondwana and then on a consolidating Laurasia. By Cretaceous time members of Gondwanan low-latitude abelisaur-titanosaur assemblages often bore “back-fans,” while those in polar latitudes were relictual and/or highly derived. The time of last contact between South America and Africa is not well constrained, but links to Antarctica continued beyond the end of the Cretaceous. Many Gondwanan tetrapods appear to have waif-dispersed to Laurasia across southern Europe; few crossed in the opposite d

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Li, Jun, and Thomas Servais. "Ordovician acritarchs of China and their utility for global palaeobiogeography." Bulletin de la Société Géologique de France 173, no. 5 (2002): 399–406. http://dx.doi.org/10.2113/173.5.399.

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Abstract Since the 1970s, acritarch workers have recognized two distinct geographic acritarch assemblages in the Ordovician. The first assemblage occurs in the late Tremadoc in low latitude areas. This assemblage, recently redefined by Volkova [1997], has been attributed to warm-water environments. A second “Mediterranean” or “peri-Gondwanan” province, attributed to high latitudes in the southern hemisphere, can easily be recognized in late Tremadoc to Arenig acritarch assemblages. This second palaeogeographic “province”, defined by Li [1989] is distributed around the border of Gondwana in a z

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Dissertations / Theses on the topic "Gondwana"

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Sanders, G. J. "Preparation of the Gondwana coals." Thesis, University of Nottingham, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.353930.

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FRASCA, Antônio Augusto Soares. "Amálgamas do W-Gondwana na Província Tocantins." reponame:Repositório Institucional da CPRM, 2015. http://rigeo.cprm.gov.br/xmlui/handle/doc/15296.

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Submitted by Priscila Ururahy (priscila.ururahy@cprm.gov.br) on 2016-01-13T13:02:36Z No. of bitstreams: 1 TD_FRASCA.pdf: 12632683 bytes, checksum: acff258b03a638f17ab8656c83403fe6 (MD5)<br>Approved for entry into archive by Flasleandro Oliveira (flasleandro.oliveira@cprm.gov.br) on 2016-01-13T17:59:29Z (GMT) No. of bitstreams: 1 TD_FRASCA.pdf: 12632683 bytes, checksum: acff258b03a638f17ab8656c83403fe6 (MD5)<br>Approved for entry into archive by Flasleandro Oliveira (flasleandro.oliveira@cprm.gov.br) on 2016-01-13T17:59:55Z (GMT) No. of bitstreams: 1 TD_FRASCA.pdf: 12632683 bytes, checksum: acf

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Frasca, Antonio Augusto Soares. "Amálgamas do W-Gondwana na província Tocantins." reponame:Repositório Institucional da UnB, 2015. http://dx.doi.org/10.26512/2015.06.T.19548.

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Tese (doutorado)—Universidade de Brasília, Instituto de Geociências, Programa de Pós-Graduação em Geologia, 2015.<br>Submitted by Fernanda Percia França (fernandafranca@bce.unb.br) on 2016-02-22T17:19:22Z No. of bitstreams: 1 2015_AntonioAugustoSoaresFrasca.pdf: 12691648 bytes, checksum: 33d6e97f7cb7064989a9fe22496f5393 (MD5)<br>Approved for entry into archive by Raquel Viana(raquelviana@bce.unb.br) on 2016-02-22T19:52:32Z (GMT) No. of bitstreams: 1 2015_AntonioAugustoSoaresFrasca.pdf: 12691648 bytes, checksum: 33d6e97f7cb7064989a9fe22496f5393 (MD5)<br>Made available in DSpace on 2016-02-2

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Scott, James Morfey, and n/a. "Tectonic evolution of the Eastern Fiordland Gondwana margin." University of Otago. Department of Geology, 2008. http://adt.otago.ac.nz./public/adt-NZDU20081003.094325.

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Eastern Fiordland is an eroded Carboniferous to Cretaceous arc assemblage juxtaposed against the Western Fiordland Gondwana continental margin along the Grebe Shear Zone. In the Manapouri region, Eastern Fiordland is composed of scattered metasedimentary and plutonic rocks of Carboniferous, Jurassic and Jurassic-Early Cretaceous age. Quantitative P-T estimates on rare paragneiss assemblages, coupled with LA-ICP-MS analyses of metamorphic overgrowths on detrital zircon grains, demonstrate metamorphism at low to middle amphibolite facies (<6 kbar, c. 600�C) at 145.0 � 2.8 Ma (all quoted errors a

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Hyam, Daniel Mark. "The Falkland Islands and their position within Gondwana." Thesis, University of Southampton, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.388347.

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Gruber, Leonardo. "Geologia isotópica e geocronologia do complexo metamórfico porongos e suíte metamórfica várzea do capivarita, Cinturão Dom Feliciano, Sul do Brasil: i implicações para a evolução do Gondwana em sua margem ocidental." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2016. http://hdl.handle.net/10183/141048.

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Proveniência por métodos isotópicos em duas unidades litodêmicas – o Complexo Metamórfico Porongos (CMP) no domínio central-oriental do Cinturão Dom Feliciano (CDF) e a Suíte Metamórfica Várzea do Capivarita (SMVC), localizada no domínio leste do CDF - apresentou áreas-fonte similares nos dois casos: Os metassedimentos do CMP, na região das Antiformes de Santana da Boa Vista e Serra dos Pedrosas, foram depositados entre 785 e 595 Ma (U-Pb em zircão detrítico por LA-ICP-MS). Apresentam registros de áreas-fonte com predominância de idades de ca. 2.2 – 2.0 Ga, mesmas idades do embasamento da regi

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Webber, Patricia Marie. "Terrane accretion and translation on the western margin of Gondwana." Thesis, University of Iowa, 2018. https://ir.uiowa.edu/etd/6335.

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The timing and kinematics of terrane accretion and translation on the Paleozoic margin of Gondwana remains contentious. Multiple models exist for the accretion of the MARA and Precordillera terranes, but deviate in timing and kinematics of accretion, the nature of involved terranes, Laurentian versus Gondwanan origin, and the extent of translation along the margin. The Valle Fertil Fault Zone (VFFZ) marks the suture zone between the Pampean margin and the MARA terrane, which was accreted and translated via thrusting or transpression between 515-400 Ma. The VFFZ projects northward to the Sierra

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Cury, Leonardo Fadel. "Geologia do Terreno Paranaguá." Universidade de São Paulo, 2009. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-06072009-113335/.

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O Terreno Paranaguá é composto por unidades geológicas pré-cambrianas distribuídas ao longo de uma faixa alongada segundo a direção NE-SW, com cerca de 250 Km de extensão, tendo em média 30 km de largura. Ocupa a porção sul sudeste do território brasileiro, abrangendo os Estados de São Paulo (Terreno Paranaguá Setentrional), Paraná e Santa Catarina (Terreno Paranaguá Meridional). Esse terreno é constituído em grande parte por um complexo ígneo, representado pelas suítes Morro Inglês, Rio do Poço e Canavieiras-Estrela. Como encaixantes desses granitos l.s., ocorrem rochas gnáissicas e gnáissic

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Zobell, Elizabeth A. "Origin and tectonic evolution of Gondwana Sequence units accreted to the Banda Arc : a structural transect through Central East Timor /." Diss., CLICK HERE for online access, 2007. http://contentdm.lib.byu.edu/ETD/image/etd1837.pdf.

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Evans, F. J. (Fiona Jocelyn). "Taxonomy, palaeoecology and palaeobiogeography of some palaeozoic fish of Southern Gondwana." Thesis, Stellenbosch : Stellenbosch University, 2005. http://hdl.handle.net/10019.1/50460.

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Thesis (PhD)--University of Stellenbosch, 2005.<br>ENGLISH ABSTRACT: The fossiliferous Waaipoort Formation (Witteberg Group, Cape Supergroup), Ganikobis Formation (Dwyka Group, Karoo Supergroup) and Whitehill Formation (Ecca Group, Karoo Supergroup) span a protracted period interrupted by a +-45Ma glacial event. This Late Carboniferous glacial event resulted in a prolonged hiatus in sedimentation as well as significant erosion in many southern continents of Gondwana. This study demonstrates how the glacial episode affected faunal composition and changes in palaeoecology in southern Gon

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Books on the topic "Gondwana"

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Grüninger, H. R. V. Genealogie Gondwanas: Die bewegungsmechanische Auflösung der Tektonik Gondwanas = Genealogy of Gondwana : derivation and kinematic resolution of Gondwana tectonics. H.R.V. Grüninger, 1994.

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1933-, Venkatachala B. S., Maheshwari Hari K, Sahni Birbal 1891-1949, and Geological Society of India, eds. Indian gondwana. Geological Society of India, 1991.

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illustrator, Niese Ralph 1983, ed. Gondwana: Roman. Schöffling & Co., 2014.

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Zalba, Patricia Eugenia, Martín Eduardo Morosi, and María Susana Conconi. Gondwana Industrial Clays. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-39457-2.

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Geoffrey, Audley-Charles Michael, Hallam A. 1933-, Geological Society of London, and Palaeontological Association, eds. Gondwana and Tethys. Published for the Geological Society by Oxford University Press, 1988.

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Rich, Pat Vickers. Wildlife of Gondwana. Reed, 1993.

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G, Audley-Charles M., Hallam A, and Geological Society of London, eds. Gondwana and Tethys. Published for the Geological Society by Oxford University Press, 1988.

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Siegesmund, Siegfried, Miguel A. S. Basei, Pedro Oyhantçabal, and Sebastian Oriolo, eds. Geology of Southwest Gondwana. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-68920-3.

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Karasek, Krzysztof. Gondwana i inne wiersze. Wydawnictwo "Iskry", 2006.

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E, White M. The greening of Gondwana. Reed, 1986.

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Book chapters on the topic "Gondwana"

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Arndt, Nicholas. "Gondwana." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_662-3.

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Arndt, Nicholas. "Gondwana." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_662.

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Arndt, Nicholas. "Gondwana." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_662.

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Arndt, Nicholas. "Gondwana." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_662.

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Arndt, Nicholas. "Gondwana." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-642-27833-4_662-4.

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McDowall, R. M. "Galaxias and Gondwana." In New Zealand Freshwater Fishes. Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9271-7_8.

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Zograph, G. A. "The Gondwana Group." In Languages of South Asia. Routledge, 2023. http://dx.doi.org/10.4324/9781003363705-20.

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Zalba, Patricia Eugenia, Martín Eduardo Morosi, and María Susana Conconi. "Overview." In Gondwana Industrial Clays. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-39457-2_1.

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Zalba, Patricia Eugenia, Martín Eduardo Morosi, and María Susana Conconi. "Azul County." In Gondwana Industrial Clays. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-39457-2_2.

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Zalba, Patricia Eugenia, Martín Eduardo Morosi, and María Susana Conconi. "Benito Juárez County." In Gondwana Industrial Clays. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-39457-2_3.

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Conference papers on the topic "Gondwana"

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Wang, Lijun, Shoufa Lin, and Wenjiao Xiao. "POSITION OF SOUTH CHINA IN GONDWANA." In 59th Annual GSA Northeastern Section Meeting - 2024. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024ne-397741.

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Dartora, F., and I. Moretti. "The Paleozoic Source Rock of NW Gondwana." In Fourth EAGE Shale Workshop. EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20140025.

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Gulbranson, Erik, Nathan Sheldon, Isabel Montanez, Neil J. Tabor, and Julia A. McIntosh. "LATE PERMIAN SOIL-FORMING PALEOENVIRONMENTS ON GONDWANA." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-369982.

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Collins*, Alan S., Donnelly Archibald, Morgan Blades, et al. "Towards a Tectonic Geography of Neoproterozoic Australian Gondwana." In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2210934.

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Wu, Guanghui, Xu Chu, Xu Chu, et al. "DISTINCT TECTONO-MAGMATISM ON RODINIA AND GONDWANA MARGINS." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-379722.

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Pastor, Andres, Carlos Villaroel, Peter Isaacson, Jaime Reyes-Abril, Francisco Velandia, and Gustavo Sarmiento. "THE DEVONIAN SYSTEM IN NORTHWESTERN GONDWANA: FOCUS IN COLOMBIA." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358788.

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Murphy, J. Brendan, R. Nance, Karel Schulmann, Yvette Kuiper, and José Ramón Martínez Catalán. "COMPLEX MORPHOLOGY OF COLLIDING MARGINS IN LAURUSSIA-GONDWANA SUPERCOLLISION." In Joint 60th Annual Meeting of the GSA Northeastern Section and 59th Annual Meeting of the GSA North-Central Section - 2025. Geological Society of America, 2025. https://doi.org/10.1130/abs/2025ne-408265.

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Sahoo, Mrutyunjaya. "Palaeoenvironmental reconstruction from a colossal palaeofloral assemblage from a Lower Gondwana outcrop of Talcher Gondwana Basin, Odisha, India: An empirical case study." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.14536.

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Volk, Natalie Ann, and Paul A. Mueller. "FLORIDA WELL REVEALS NEW BASEMENT ORIGINS AND CONNECTIONS TO GONDWANA." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-290492.

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Şengör, A. M. Celâl, Nalan Lom, Cengiz Zabcı, Gürsel Sunal, and Taylan Sançar. "PALAEO-TETHYAN MARGIN OF GONDWANA-LAND WAS AN EXTENSIONAL ARC." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-318141.

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Reports on the topic "Gondwana"

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Moreno Martín, Diana, and Rubén Díez Fernández. El basamento metamórfico en el sector oriental del Sistema Central: evolución tectonotermal varisca. Ilustre Colegio Oficial de Geólogos, 2021. http://dx.doi.org/10.21028/dmm.2021.02.18.

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El basamento metamórfico del sector occidental de la Península Ibérica se configuró durante la Orogenia Varisca, fruto de la colisión entre Gondwana, Laurrusia y otros terrenos peri-continentales adyacentes que dio lugar a Pangea. Este basamento forma parte de la microplaca ibérica y se deformó durante la Orogenia Alpina junto con el resto de rocas sedimentarias del Mesozoico. El análisis tectonometamórfico del registro varisco en el sector oriental del Sistema Central, junto con datos regionales previos, y un análisis de las deformaciones alpinas sobreimpuestas, han permitido la reconstrucció

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