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Radiizonates arcuatus , a distinctive new miospore species from the Lower Carboniferous of Western Gondwana

Identifieur interne : 000488 ( Istex/Corpus ); précédent : 000487; suivant : 000489

Radiizonates arcuatus , a distinctive new miospore species from the Lower Carboniferous of Western Gondwana

Auteurs : Stanislas Loboziak ; Geoffrey Playford ; José H. G. Melo

Source :

RBID : ISTEX:197C27D4FABC81B3B50B15240401B1FD16662F51

English descriptors

Abstract

Abstract: A new species of trilete zonate miospores, Radiizonates arcuatus, is established for Lower Carboniferous Western Gondwanan forms hitherto ascribed misguidedly to Radiizonates genuinus (Jushko) Loboziak and Alpern (1978), a Russian Lower Carboniferous species. The latter binomen is, moreover, not a valid combination and is more correctly designated as Vallatisporites genuinus (Jushko) Byvsheva, 1980. R. arcuatus is, from records to date, confined to westerly parts of Gondwana (Brazil, North Africa and Middle East), in which it is characteristic of Early Carboniferous strata, albeit with some slightly older and slightly younger occurrences.

Url:
DOI: 10.1016/S0034-6667(99)00059-7

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ISTEX:197C27D4FABC81B3B50B15240401B1FD16662F51

Le document en format XML

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<div type="abstract" xml:lang="en">Abstract: A new species of trilete zonate miospores, Radiizonates arcuatus, is established for Lower Carboniferous Western Gondwanan forms hitherto ascribed misguidedly to Radiizonates genuinus (Jushko) Loboziak and Alpern (1978), a Russian Lower Carboniferous species. The latter binomen is, moreover, not a valid combination and is more correctly designated as Vallatisporites genuinus (Jushko) Byvsheva, 1980. R. arcuatus is, from records to date, confined to westerly parts of Gondwana (Brazil, North Africa and Middle East), in which it is characteristic of Early Carboniferous strata, albeit with some slightly older and slightly younger occurrences.</div>
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<note type="content">PLATE I: Slides 960566 from well 1-RX-3-AM, 9305348 from well 1-CM-1-PA and 9601772 from well 1-NO-6-AM are housed in the palynological slide collection of the Biostratigraphy and Paleoecology Section of Petrobras Research Centre (Cenpes/Divex/Sebipe), Rio de Janeiro, Brazil. Other slides are housed in the palynological collection of the Laboratory of Paleobotany, University of Lille, France. Miospore locations on slides are based on England Finder graticules. Magnification of illustrated specimens: ×500. 1–18. Radiizonates arcuatus sp. nov. 1. Holotype. Slide A.N.99.142(2): L32/2, well Aoulingen 142, Agadès Coal Basin, Niger. 2. Slide A.N.99.142(1): C51, well Aoulingen 142, Agadès Coal Basin, Niger. 3. Slide A.N.99.142(1): L31, well Aoulingen 142, Agadès Coal Basin, Niger. 4. Slide A.N.99.142(1): E45/3, well Aoulingen 142, Agadès Coal Basin, Niger. 5. Slide R.L.99.16. 1218,7(1): D58, well A1-49, core 16, M'Rar Formation, Hammadah Basin, Libya. 6. Slide R.L.99.16. 1218,7(2): Q46/4, well A1-49, core 16, M'Rar Formation, Hammadah Basin, Libya. 7. Slide I.A.99.34. 1666(1): O42/3, well Tesselit 101, core 34, Issendjel Formation, Illizi Basin, Algeria. 8. Slide I.A.99.34. 1666(3): H49/3, well Tesselit 101, core 34, Issendjel Formation, Illizi Basin, Algeria. 9. Slide I.A.99.34. 1666(3): D62, well Tesselit 101, core 34, Issendjel Formation, Illizi Basin, Algeria. 10. Slide E.I.99.129(2):W43/4, outcrop sample 129, Noh-Deh Section, Mobarak Formation, eastern Elburz, Iran. 11. Slide E.I.99.129(2):H50(1), outcrop sample 129, Noh-Deh Section, Mobarak Formation, eastern Elburz, Iran. 12. Slide E.I.99.129(2): K45, outcrop sample 129, Noh-Deh Section, Mobarak Formation, eastern Elburz, Iran. 13. Slide 960566: H51/2, well 1-RX-3-AM, core 27, Oriximiná Formation, Amazon Basin, Brazil. 14. Slide 960566: X54/1, well 1-RX-3-AM, core 27, Oriximiná Formation, Amazon Basin, Brazil. 15. Slide 9305348: Q59/2, well 1-CM-1-PA, core 9, Oriximiná Formation, Amazon Basin, Brazil. 16. Slide 9601772: F50/1, well 1-NO-6-AM, core 17, Oriximiná Formation, Amazon Basin, Brazil. 17. Slide P.B.99.34(1): G.40/4, well 2-PM-1-AM, core 34, Poti Formation, Parnaı́ba Basin, Brazil. 18. Slide P.B.99.34(1): M33/2, well 2-PM-1-AM, core 34, Poti Formation, Parnaı́ba Basin, Brazil.</note>
<note type="content">Fig. 1: Location of known occurrences of Radiizonates arcuatus in Western Gondwana and respective data sources (palaeogeographic reconstruction after Scotese and Barrett, 1990, fig. 10). 1, Amazon Basin, after Loboziak et al. (1993, fig. 2 and 1998, fig. 2); 2, Parnaı́ba Basin, after Loboziak et al. (1992, figs. 2, 3 and 1998, fig. 2); 3, Grand Erg occidental, after Lanzoni and Magloire (1969, table 1); 4, Illizi Basin, after Attar et al. (1980, table 1) and Abdesselam-Rouighi and Coquel (1997, fig. 4); 5, Tim Mersoı̈ Basin, Arlit Region, after Coquel et al. (1995, fig. 2), Agadès Coal Basin, after Loboziak and Alpern (1978, p. 57); 6, Hammadah (Rhadamès) Basin, after Massa et al. (1980, figs. 4, 5); 7, Cyrenaica, after Loboziak and Clayton (1988, fig. 9); 8, Al Kufra Basin, after Grignani et al. (1991, fig. 4); 9, Northeastern Syria, after Ravn et al. (1994, fig. 2); 10, Northern Saudi Arabia, after Clayton (1995, table 1); 11, Eastern Elburz, after Coquel et al. (1977, p. 64).</note>
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<title level="a">Radiizonates arcuatus , a distinctive new miospore species from the Lower Carboniferous of Western Gondwana</title>
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<forename type="first">José H.G.</forename>
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<p>A new species of trilete zonate miospores, Radiizonates arcuatus, is established for Lower Carboniferous Western Gondwanan forms hitherto ascribed misguidedly to Radiizonates genuinus (Jushko) Loboziak and Alpern (1978), a Russian Lower Carboniferous species. The latter binomen is, moreover, not a valid combination and is more correctly designated as Vallatisporites genuinus (Jushko) Byvsheva, 1980. R. arcuatus is, from records to date, confined to westerly parts of Gondwana (Brazil, North Africa and Middle East), in which it is characteristic of Early Carboniferous strata, albeit with some slightly older and slightly younger occurrences.</p>
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<ce:cross-ref refid="REF19">Loboziak and Alpern (1978)</ce:cross-ref>
, a Russian Lower Carboniferous species. The latter binomen is, moreover, not a valid combination and is more correctly designated as
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(Jushko) Byvsheva, 1980.
<ce:italic>R. arcuatus</ce:italic>
is, from records to date, confined to westerly parts of Gondwana (Brazil, North Africa and Middle East), in which it is characteristic of Early Carboniferous strata, albeit with some slightly older and slightly younger occurrences.</ce:simple-para>
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<abstract lang="en">Abstract: A new species of trilete zonate miospores, Radiizonates arcuatus, is established for Lower Carboniferous Western Gondwanan forms hitherto ascribed misguidedly to Radiizonates genuinus (Jushko) Loboziak and Alpern (1978), a Russian Lower Carboniferous species. The latter binomen is, moreover, not a valid combination and is more correctly designated as Vallatisporites genuinus (Jushko) Byvsheva, 1980. R. arcuatus is, from records to date, confined to westerly parts of Gondwana (Brazil, North Africa and Middle East), in which it is characteristic of Early Carboniferous strata, albeit with some slightly older and slightly younger occurrences.</abstract>
<note type="content">PLATE I: Slides 960566 from well 1-RX-3-AM, 9305348 from well 1-CM-1-PA and 9601772 from well 1-NO-6-AM are housed in the palynological slide collection of the Biostratigraphy and Paleoecology Section of Petrobras Research Centre (Cenpes/Divex/Sebipe), Rio de Janeiro, Brazil. Other slides are housed in the palynological collection of the Laboratory of Paleobotany, University of Lille, France. Miospore locations on slides are based on England Finder graticules. Magnification of illustrated specimens: ×500. 1–18. Radiizonates arcuatus sp. nov. 1. Holotype. Slide A.N.99.142(2): L32/2, well Aoulingen 142, Agadès Coal Basin, Niger. 2. Slide A.N.99.142(1): C51, well Aoulingen 142, Agadès Coal Basin, Niger. 3. Slide A.N.99.142(1): L31, well Aoulingen 142, Agadès Coal Basin, Niger. 4. Slide A.N.99.142(1): E45/3, well Aoulingen 142, Agadès Coal Basin, Niger. 5. Slide R.L.99.16. 1218,7(1): D58, well A1-49, core 16, M'Rar Formation, Hammadah Basin, Libya. 6. Slide R.L.99.16. 1218,7(2): Q46/4, well A1-49, core 16, M'Rar Formation, Hammadah Basin, Libya. 7. Slide I.A.99.34. 1666(1): O42/3, well Tesselit 101, core 34, Issendjel Formation, Illizi Basin, Algeria. 8. Slide I.A.99.34. 1666(3): H49/3, well Tesselit 101, core 34, Issendjel Formation, Illizi Basin, Algeria. 9. Slide I.A.99.34. 1666(3): D62, well Tesselit 101, core 34, Issendjel Formation, Illizi Basin, Algeria. 10. Slide E.I.99.129(2):W43/4, outcrop sample 129, Noh-Deh Section, Mobarak Formation, eastern Elburz, Iran. 11. Slide E.I.99.129(2):H50(1), outcrop sample 129, Noh-Deh Section, Mobarak Formation, eastern Elburz, Iran. 12. Slide E.I.99.129(2): K45, outcrop sample 129, Noh-Deh Section, Mobarak Formation, eastern Elburz, Iran. 13. Slide 960566: H51/2, well 1-RX-3-AM, core 27, Oriximiná Formation, Amazon Basin, Brazil. 14. Slide 960566: X54/1, well 1-RX-3-AM, core 27, Oriximiná Formation, Amazon Basin, Brazil. 15. Slide 9305348: Q59/2, well 1-CM-1-PA, core 9, Oriximiná Formation, Amazon Basin, Brazil. 16. Slide 9601772: F50/1, well 1-NO-6-AM, core 17, Oriximiná Formation, Amazon Basin, Brazil. 17. Slide P.B.99.34(1): G.40/4, well 2-PM-1-AM, core 34, Poti Formation, Parnaı́ba Basin, Brazil. 18. Slide P.B.99.34(1): M33/2, well 2-PM-1-AM, core 34, Poti Formation, Parnaı́ba Basin, Brazil.</note>
<note type="content">Fig. 1: Location of known occurrences of Radiizonates arcuatus in Western Gondwana and respective data sources (palaeogeographic reconstruction after Scotese and Barrett, 1990, fig. 10). 1, Amazon Basin, after Loboziak et al. (1993, fig. 2 and 1998, fig. 2); 2, Parnaı́ba Basin, after Loboziak et al. (1992, figs. 2, 3 and 1998, fig. 2); 3, Grand Erg occidental, after Lanzoni and Magloire (1969, table 1); 4, Illizi Basin, after Attar et al. (1980, table 1) and Abdesselam-Rouighi and Coquel (1997, fig. 4); 5, Tim Mersoı̈ Basin, Arlit Region, after Coquel et al. (1995, fig. 2), Agadès Coal Basin, after Loboziak and Alpern (1978, p. 57); 6, Hammadah (Rhadamès) Basin, after Massa et al. (1980, figs. 4, 5); 7, Cyrenaica, after Loboziak and Clayton (1988, fig. 9); 8, Al Kufra Basin, after Grignani et al. (1991, fig. 4); 9, Northeastern Syria, after Ravn et al. (1994, fig. 2); 10, Northern Saudi Arabia, after Clayton (1995, table 1); 11, Eastern Elburz, after Coquel et al. (1977, p. 64).</note>
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