cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.15135087
title: Table 2 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA

description: Table 2. Conch ontogeny of Girtyoceras meslerianum (Girty, 1909); based on material from Jackfork Creek, Oklahoma (Fig. 7).
dmConch shapeWhorl cross section shapeAperture1.5 mmthickly discoidal; subevolutemoderately depressed; moderately embracinglow(ww / dm = 0.45–0.60; uw / dm = 0.40–(ww / wh 1.80–2.00; IZR = 0.20–0.25)(WER ∼ 1.65)0.45)5 mmthickly discoidal; evolutestrongly depressed; moderately embracinglow(ww / dm = 0.55–0.50; uw / dm = 0.50–(ww / wh = 2.25–2.50; IZR = 0.25–0.30)(WER = 1.50–1.60)0.55)10 mmthickly discoidal; subevoluteweakly depressed; strongly embracingmoderate(ww / dm = 0.50; uw / dm = 0.35)(ww / wh = 1.25; IZR = 0.35–0.40)(WER = 1.75–1.90)20 mmthinly discoidal; subinvoluteweakly compressed; strongly embracinghigh(ww / dm ∼ 0.45; uw / dm ∼ 0.20)(ww / wh = 0.80; IZR ∼ 0.40)(WER ∼ 2.10)
description: Published as part of Titus, A. L., Korn, D., Harrell, J. E. & Lambert, L. L., 2015, Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA, pp. 89 in Fossil Record 18 (2) on page 89, DOI: 10.5194/fr-18-81-2015, http://zenodo.org/record/11585625
DOI: 10.5281/zenodo.15135088
title: Table 3 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA

description: Table 3. Conch dimensions (in millimetres) and proportions for Girtyoceras meslerianum (Girty, 1909) from the type area and the Sierra Diablo.
Specimendmwwwhuwahww / dmww / whuw / dmWERIZRUSNM 119594 (holotype)16.06.07.63.94.60.380.790.242.000.40NPL 683649.55.14.53.12.50.541.100.331.850.44NPL 683656.83.81.92.5–0.561.900.37––
description: Published as part of Titus, A. L., Korn, D., Harrell, J. E. & Lambert, L. L., 2015, Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA, pp. 89 in Fossil Record 18 (2) on page 89, DOI: 10.5194/fr-18-81-2015, http://zenodo.org/record/11585625
DOI: 10.5281/zenodo.15135089
title: Table 3 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA

description: Table 3. Conch dimensions (in millimetres) and proportions for Girtyoceras meslerianum (Girty, 1909) from the type area and the Sierra Diablo.
Specimendmwwwhuwahww / dmww / whuw / dmWERIZRUSNM 119594 (holotype)16.06.07.63.94.60.380.790.242.000.40NPL 683649.55.14.53.12.50.541.100.331.850.44NPL 683656.83.81.92.5–0.561.900.37––
description: Published as part of Titus, A. L., Korn, D., Harrell, J. E. & Lambert, L. L., 2015, Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA, pp. 89 in Fossil Record 18 (2) on page 89, DOI: 10.5194/fr-18-81-2015, http://zenodo.org/record/11585625
DOI: 10.5281/zenodo.15135090
title: Table 4 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA

description: Table 4. Conch dimensions (in millimetres) and proportions for reference specimens of Goniatites eganensis Korn and Titus, 2011 from the Sierra Diablo.
Specimendmwwwhuwahww / dmww / whuw / dmWERIZRNPL 6843147.331.723.92.910.60.671.330.061.660.56NPL 6847137.526.418.42.07.10.701.430.051.520.61NPL 6849326.921.513.81.95.70.801.560.071.610.59NPL 6838918.415.59.70.93.90.841.600.051.610.60Paratype-UT 1203250.029.026.04.0–0.581.120.08––Holotype-UT 1203120.814.611.51.84.70.701.270.091.670.59NPL 6850219.814.511.41.64.50.731.270.081.670.61NPL 6849719.614.610.72.04.30.741.360.101.640.60NPL 6850317.613.59.61.93.90.771.410.111.650.59NPL 6849817.212.98.91.94.10.751.450.111.720.54NPL 6850415.312.58.41.8–0.821.490.12––NPL 6850514.811.98.01.83.50.801.490.121.720.56NPL 6850014.511.67.72.13.30.801.510.141.680.57NPL 6849912.49.86.01.42.80.791.630.111.670.53NPL 685016.96.2–––0.90––––
description: Published as part of Titus, A. L., Korn, D., Harrell, J. E. & Lambert, L. L., 2015, Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA, pp. 90-99 in Fossil Record 18 (2) on page 90, DOI: 10.5194/fr-18-81-2015, http://zenodo.org/record/11585625
DOI: 10.5281/zenodo.15135091
title: Table 4 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA

description: Table 4. Conch dimensions (in millimetres) and proportions for reference specimens of Goniatites eganensis Korn and Titus, 2011 from the Sierra Diablo.
Specimendmwwwhuwahww / dmww / whuw / dmWERIZRNPL 6843147.331.723.92.910.60.671.330.061.660.56NPL 6847137.526.418.42.07.10.701.430.051.520.61NPL 6849326.921.513.81.95.70.801.560.071.610.59NPL 6838918.415.59.70.93.90.841.600.051.610.60Paratype-UT 1203250.029.026.04.0–0.581.120.08––Holotype-UT 1203120.814.611.51.84.70.701.270.091.670.59NPL 6850219.814.511.41.64.50.731.270.081.670.61NPL 6849719.614.610.72.04.30.741.360.101.640.60NPL 6850317.613.59.61.93.90.771.410.111.650.59NPL 6849817.212.98.91.94.10.751.450.111.720.54NPL 6850415.312.58.41.8–0.821.490.12––NPL 6850514.811.98.01.83.50.801.490.121.720.56NPL 6850014.511.67.72.13.30.801.510.141.680.57NPL 6849912.49.86.01.42.80.791.630.111.670.53NPL 685016.96.2–––0.90––––
description: Published as part of Titus, A. L., Korn, D., Harrell, J. E. & Lambert, L. L., 2015, Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA, pp. 90-99 in Fossil Record 18 (2) on page 90, DOI: 10.5194/fr-18-81-2015, http://zenodo.org/record/11585625
DOI: 10.5281/zenodo.15135092
title: Table 5 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA

description: 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
description: Published as part of Titus, A. L., Korn, D., Harrell, J. E. & Lambert, L. L., 2015, Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA, pp. 92 in Fossil Record 18 (2) on page 92, DOI: 10.5194/fr-18-81-2015, http://zenodo.org/record/11585625
DOI: 10.5281/zenodo.15135093
title: Table 5 in Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA

description: 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
description: Published as part of Titus, A. L., Korn, D., Harrell, J. E. & Lambert, L. L., 2015, Late Viséan (late Mississippian) ammonoids from the Barnett Shale, Sierra Diablo Escarpment, Culberson County, Texas, USA, pp. 92 in Fossil Record 18 (2) on page 92, DOI: 10.5194/fr-18-81-2015, http://zenodo.org/record/11585625