Table 5 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA

Name: Table 5 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA
Creator: Department of Geological Sciences, The University of Texas at San Antonio, One UTSA Circle, San Antonio, TX 78249, USA; J. E. Harrell & Museum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstrasse 43,; D. Korn & Grand Staircase-Escalante National Monument, 669 S. Highway 89 A, Kanab, UT 84741, USA; L. L. Lambert & Noble Energy Inc., Houston, TX 77070, USA
Published: 2015-06-04 00:00:00
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Zenodo2015-06-04 更新2026-04-07 收录

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Table 5. Character matrix of the genera within the subfamily Dombaritinae for the cladistic analysis presented here. 0. Conch ontogeny of whorl width index: biphasic (0), triphasic (1)1. Distance of prongs of external lobe: very short (0), moderate or wide (1)2. Median saddle higher than 45 % of ventrolateral saddle: no (0), yes (1)3. Median saddle higher than 55 % of ventrolateral saddle: no (0), yes (1)4. Median saddle higher than 65 % of ventrolateral saddle: no (0), yes (1)5. Median saddle higher than 75 % of ventrolateral saddle: no (0), yes (1)6. Median saddle higher than 85 % of ventrolateral saddle: no (0), yes (1)7. External lobe V-shaped (0), Y-shaped (1)8. Ventrolateral saddle subacute: no (0), acute (1)9. Ventrolateral saddle tectiform: no (0), yes (1)10. External lobe wider than 0.60: no (0), yes (1)11. External lobe wider than 0.85: no (0), yes (1)12. External lobe wider than 1.10: no (0), yes (1)13. External lobe wider than 1.35: no (0), yes (1)14. External lobe with tridentate branches: no (0), yes (1)15. Adventive lobe: flanks simple curved (0), sinuous or with deflexion (1)16. Adventive lobe: flanks not angular (0), angular or tridentate (1)17. Adventive lobe tridentate: no (0), yes (1)18. Inner whorls involute (0), subevolute or evolute (1)19. Drastic size reduction of the conch: no (0), yes (1)20. Whorl expansion rate: low (0), moderate (1)21. Preadult whorls triangularly coiled: no (0), yes (1)22. Apertural shape in juveniles: rectiradiate (0), prorsiradiate (1)23. Adult conch shape pachyconic or globular (0), discoidal (1)24. Shell constrictions in intermediate stage: no (0), yes (1)25. Course of growth lines: with projections and sinuses (0), linear (1)Progoniatites pilus000000000000000000000000?0Goniatites crenistria11000000100000000000000000Arnsbergites falcatus11100000001000010010001000Hibernicoceras hibernicum11100000001000010010001000Paraglyphioceras rotundum11100000001000000010000000Lusitanoceras poststriatum11100001011000010010011010Goniatitella agricola?100000?000000010001100001Neogoniatites milleri11111000001000000010000000Hypergoniatites exiguus10000001100000000000100000Dombarites tectus11111101111100011010001010Proshumardites delepinei11111111011100011110011010Platygoniatites molaris11111101111110010010011110Delepinoceras bressoni11111111011111110010011110Choctawites choctawensis11110001011000011010001000Revilloceras granofalcatum11110001111000010010011010Dombarites falcatoides11111001111000010010011010

提供机构：

Department of Geological Sciences, The University of Texas at San Antonio, One UTSA Circle, San Antonio, TX 78249, USA; J. E. Harrell & Museum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstrasse 43,; D. Korn & Grand Staircase-Escalante National Monument, 669 S. Highway 89 A, Kanab, UT 84741, USA; L. L. Lambert & Noble Energy Inc., Houston, TX 77070, USA

创建时间：

2015-06-04