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70 results for “palaeogeography”
FIGURE 26. A–C in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 26. A–C, Genus and Species indeterminate 1, ESKU-19-LP 4. D, Genus and Species indeterminate 2, ESKU-19-LP 207. Scale bars represent: 2 mm (A–C); 200 μm (D).
FIGURE 22. A–C in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 22. A–C, Strobeus? sp. 1, A–B, ESKU-19-LP 49. C, ESKU-19-LP 90. D–E, Strobeus? sp. 2, D, ESKU-19-LP 217. E, ESKU-19-LP 220. F, Girtyspira? sp., ESKU-19-LP 222. G, Heterosubulites longusapertura sp. nov. ESKU-19-LP 215, holotype. Scale bars represent: 2 mm (A–C); 200 μm (D–G).
FIGURE 18. A–J in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 18. A–J, Yunnania inflata sp. nov. A–B, ESKU-19-LP 9, holotype; C–G, ESKU-19-LP 65, paratype. H–J, juvenile specimens, H–I, ESKU-19-LP 205. J, ESKU-19-LP 215. K, Araeonema cf. tenuistriata (Netchaev, 1894), ESKU-19-LP 99. All scale bars represent 1 mm.
FIGURE 19 A–C in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 19 A–C, Microdoma conicum Meek & Worthen, 1867, ESKU-19-LP 69. All scale bars represent 1 mm.
FIGURE 15 in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 15. Altotomaria reticulata sp. nov. A–E, ESKU-19-LP 83, holotype. All scale bars represent 1 mm.
FIGURE 25. A in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 25. A, Donaldospira sp., ESKU-19-LP 85. B–E, Knightella irregularis (Longstaff, 1933), B–C, ESKU-19-LP 41. D–E, ESKU-19-LP 84. F–H, Protostylus sp., F, ESKU-19-LP 39. G–H, ESKU-19-LP 64. I–N, Trypanocochlea lopburiensis sp. nov. I, M, ESKU-19-LP 210, holotype; oblique view of early whorls to show protoconch. J, ESKU-19-LP 201, paratype. K, ESKU-19-LP 203, paratype. L, ESKU-19-LP 206, paratype; lateral view of early whorls to show protoconch. N, ESKU-19-LP 221, paratype. O–R, Streptacis? khaokhadensis sp. nov., O–P, ESKU-19-LP 214, holotype. Q–R, ESKU-19-LP 213, paratype. Scale bars represent: 2 mm (A–H); 200 μm (I–R).
FIGURE 21. A–D in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 21. A–D, Trachydomia suwanneeae sp. nov., ESKU-19-LP 26, holotype. E–F, Trachydomia cf. nodusum (Meek & Worthen, 1866), ESKU-19-LP 92. G–K, Trachyspira eleganta sp. nov., ESKU-19-LP 28, holotype. Scale bars represent: 2 mm (A–D, G–K); 1 mm (E–F).
FIGURE 14. A–I in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 14. A–I, Worthenia humiligrada sp. nov. A–D, ESKU-19-LP 22. E–F, ESKU-19-LP 33. G–H, ESKU-19-LP 23. I, ESKU-19-LP 34. J–N, Worthenia cf. pagoda Mansuy, 1912, J, ESKU-19-LP 17. K–N, ESKU-19-LP 66. O–S, Worthenia sp., ESKU-19-LP 88. Scale bars represent: 2 mm (A, B, G, H, I, K, L, O); 1 mm (C, D, J, M, N, P–S); 5 mm (E, F).
FIGURE 4 in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 4. Relative species abundances of major clades of Middle Permian gastropod faunas in Thailand. The gastropod faunas from the Khao Khad Formation (this study), Lopburi province (A) from the Tak Fa Formation, Nakhonsawan province (B) as well as from the Ratburi Limestone, Ratchaburi province (C).
FIGURE 3. A, C in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 3. A, C, Limestone outcrops exposed as the lapiés at the west foot hill of Erawan hill; hammer in the right side for scale (C). B, D, Weathered surface limestones represented by bioclastic packstone as an example for preservation that the studied materials were collected; scale bars represent: 10 cm (B); 2 cm (D).
FIGURE 1 in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 1. Geological map of the study location at Erawan Hill, Chong Sarika sub-district, Phatthana Nikhom district, located about 13 km east of Lopburi Province, Central Thailand.
FIGURE 2. A in The Scolopendra species (Chilopoda: Scolopendromorpha: Scolopendridae) of Greece (E-Mediterranean): a theoretical approach on the effect of geography and palaeogeography on their distribution
FIGURE 2. A) The distribution of species of the canidens group in Greece according to Zapparoli (2002). Black circles: S. clavipes, asterisks: S. cretica, black triangles: S. dalmatica, black arrows: S. canidens (the southern black arrow indicates an uncertain data from Gavdos Is.), B) The distribution of Scolopendra cingulata in Greece according to Zapparoli (2002). Black arrows indicate data from the Aegean Islands whereas black circles indicate data from mainland Greece and Ionian Islands.
FIGURE 4 in The Scolopendra species (Chilopoda: Scolopendromorpha: Scolopendridae) of Greece (E-Mediterranean): a theoretical approach on the effect of geography and palaeogeography on their distribution
FIGURE 4. The palaeogeography of Greece from Miocene to present (redrawn after Creutzburg 1963; Dermitzakis and Papanikolaou 1981; Dermitzakis 1990 and recently published by Parmakelis et al. 2005 and Poulakakis et al. 2005b, 2005c). The maps are drawn based on present geography. Gray: land, white: sea, black: lakes.
FIGURE 3. A in The Scolopendra species (Chilopoda: Scolopendromorpha: Scolopendridae) of Greece (E-Mediterranean): a theoretical approach on the effect of geography and palaeogeography on their distribution
FIGURE 3. A) The distribution of species of the Scolopendra canidens group in the Aegean Archipelago based on new data and bibliographic references, B) The distribution of Scolopendra cingulata in the Aegean Archipelago based on new data and bibliographic references.
FIGURE 5 in The Scolopendra species (Chilopoda: Scolopendromorpha: Scolopendridae) of Greece (E-Mediterranean): a theoretical approach on the effect of geography and palaeogeography on their distribution
FIGURE 5. The proposed chronicle of dispersal of S. canidens, S. cretica and S. cingulata in Greece based on schematic views of the palaeogeographic evolution of the Mediterranean and the Paratethys regions during the Miocene (Roegl and Steininger 1983). A: Middle Miocene (16-14.5 Mya), B: Upper Miocene (12-9 Mya). 1: Mainland Greece, 2: Crete, 3: Turkey, 4: Mid-Aegean trench, 5: Disjunction of Crete from mainland Greece and Cyclades Plateau, Scn: Scolopendra canidens, Sci: Scolopendra cingulata, Scr: Scolopendra cretica. Black: evaporitic sea areas, white: land areas, wavelike: sea areas, chesslike: low salinity sea areas.
Data from: Early Pennsylvanian (Langsettian) fish assemblages from the Joggins Formation, Canada, and their implications for palaeoecology and palaeogeography
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FIGURE 12 in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 12. Peruvispira sp., A–C, ESKU-19-LP 10. D, ESKU-19-LP 68. All scale bars represent 1 mm.
Text-fig. 4. Palaeogeographical reconstruction of the Katian (after Popov et al. 2011, modified) showing geographical distribution of the Middle and Late Ordovician craniides and craniopsides. White arrow = Boda Event expansion of craniiates and craniopsides to Perunica; black arrow = Hirnantian low-latitude expansion of the Hirnantia Fauna. in Lingulate And Craniate Brachiopods From The Top Of The Králův Dvůr Formation (Latest Katian) And Their Contribution To Palaeogeography
Text-fig. 4. Palaeogeographical reconstruction of the Katian (after Popov et al. 2011, modified) showing geographical distribution of the Middle and Late Ordovician craniides and craniopsides. White arrow = Boda Event expansion of craniiates and craniopsides to Perunica; black arrow = Hirnantian low-latitude expansion of the Hirnantia Fauna.
FIGURE 20. A–C in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 20. A–C, Naticopsis sp. 1, ESKU-19-LP 47. D–F, Naticopsis sp. 2, ESKU-19-LP 46. G–I, Naticopsis? sp. 3, ESKU- 19-LP 32. J, Naticopsis? sp. 4, ESKU-19-LP 52. K–L, Naticopsis cf. heshanensis Pan & Erwin, 2002, ESKU-19-LP 44. Scale bars represent: 2 mm (A–J); 5 mm (K–L).
FIGURE 17. A–E in Middle Permian (Roadian) gastropods from the Khao Khad Formation, Central Thailand: Implications for palaeogeography of the Indochina Terrane
FIGURE 17. A–E, Anomphalus cf. vanescens Yochelson, 1956, A–C, ESKU-19-LP 30. D–E, ESKU-19-LP 50. F–L, Anomphalus? blancus Kues & Batten, 2001, F–I, ESKU-19-LP 67. J–L, ESKU-19-LP 96. Scale bars represent: 2 mm (A–C); 1 mm (D–L).
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