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Geographic map showing the location of the study area. Inset map shows the locality of the main map.
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Abundant, very diverse, and well-preserved Nassellarian fauna has been obtained from cherty/clayey limestone levels at the basal part of the Kö seyahya nappe east of the town of Elbistan, Eastern Taurides. A comparison with the radiolarian faunas of Austria, Japan and Turkey allows us to assign a middle Carnian age to this radiolarian fauna from th...
Contexts in source publication
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... study area is located in the Eastern Taurides and at approximately 22 km east of town of Elbistan (Fig. 1). Around this town, there are many allochtho- nous sequences (for brief review see Bedi et al. 2005) and their features have been studied in detail by Ayaslioglu (1970), Perincek & Kozlu (1984), Yilmaz et al. (1987), Pehlivan et al. (1991), Yilmaz et al. (1993) and Bedi et al. (2004Bedi et al. ( , 2005. Binboga metamorphics consti- tute ...
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... 04-ELB-5, side view. 13-16. Paratypes. Fig. 13 is from sample 04-ELB-2, view from apical side. Fig. 14 is from sample 04-ELB-5, side view. Fig. 15 is from sample 04-ELB-5, view from apical side. Furthermore, the ammonoid species Tropites cf. subbulatus, (det. by Leopold Krystyn, Vienna, Austria) found in the sample 06-MYB-10B, in the unit 5 (Fig. 3), indicates a middle Late Carnian ...
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... 04-ELB-5, side view. 13-16. Paratypes. Fig. 13 is from sample 04-ELB-2, view from apical side. Fig. 14 is from sample 04-ELB-5, side view. Fig. 15 is from sample 04-ELB-5, view from apical side. Furthermore, the ammonoid species Tropites cf. subbulatus, (det. by Leopold Krystyn, Vienna, Austria) found in the sample 06-MYB-10B, in the unit 5 (Fig. 3), indicates a middle Late Carnian age (Fig. 5) for unit 5. Based on this fact, it can be ...
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... 04-ELB-5, side view. 13-16. Paratypes. Fig. 13 is from sample 04-ELB-2, view from apical side. Fig. 14 is from sample 04-ELB-5, side view. Fig. 15 is from sample 04-ELB-5, view from apical side. Furthermore, the ammonoid species Tropites cf. subbulatus, (det. by Leopold Krystyn, Vienna, Austria) found in the sample 06-MYB-10B, in the unit 5 (Fig. 3), indicates a middle Late Carnian age (Fig. 5) for unit 5. Based on this fact, it can be suggested that the age of the underlying ...
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... of Pessagno (1969), Foreman (1973), Kozur & Mostler (1979, Dumitrica, Kozur & Mostler (1980), Kozur (1984) Family Bulbocyrtidae Kozur & Mostler, 1981Genus Bulbocyrtium Kozur & Mostler, 1981emend. Tekin, 1999 Type species: Bulbocyrtium reticulatum Kozur & Mostler, 1981. Bulbocyrtium cordevolicum Kozur & Mostler, 1981 Pl fig. 2; pl. 13, fig. 1 Remarks. This specimen differs from the Bulbo- cyrtium globosum Tekin by having a smaller cephalis, two segmented thorax and wider, brimmed distal ...
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... Planum (Latin, adj.), flat, plain. Types. Holotype, HU.JMB.0062 (Pl. 1, Fig. 12); paratypes, HU.JMB.0063 (Pl. 1, Fig. 13), HU.JMB.0064 (Pl. 1, Fig. 14), HU.JMB.0065 (Pl. 1, Fig. 15), HU.JMB.0066 (Pl. 1, Fig. ...
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... Planum (Latin, adj.), flat, plain. Types. Holotype, HU.JMB.0062 (Pl. 1, Fig. 12); paratypes, HU.JMB.0063 (Pl. 1, Fig. 13), HU.JMB.0064 (Pl. 1, Fig. 14), HU.JMB.0065 (Pl. 1, Fig. 15), HU.JMB.0066 (Pl. 1, Fig. ...
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... Planum (Latin, adj.), flat, plain. Types. Holotype, HU.JMB.0062 (Pl. 1, Fig. 12); paratypes, HU.JMB.0063 (Pl. 1, Fig. 13), HU.JMB.0064 (Pl. 1, Fig. 14), HU.JMB.0065 (Pl. 1, Fig. 15), HU.JMB.0066 (Pl. 1, Fig. ...
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... Planum (Latin, adj.), flat, plain. Types. Holotype, HU.JMB.0062 (Pl. 1, Fig. 12); paratypes, HU.JMB.0063 (Pl. 1, Fig. 13), HU.JMB.0064 (Pl. 1, Fig. 14), HU.JMB.0065 (Pl. 1, Fig. 15), HU.JMB.0066 (Pl. 1, Fig. ...
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... Planum (Latin, adj.), flat, plain. Types. Holotype, HU.JMB.0062 (Pl. 1, Fig. 12); paratypes, HU.JMB.0063 (Pl. 1, Fig. 13), HU.JMB.0064 (Pl. 1, Fig. 14), HU.JMB.0065 (Pl. 1, Fig. 15), HU.JMB.0066 (Pl. 1, Fig. ...
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... outline with six to seven rows of pores. Pores on proximal part of abdominal skirt small, subcircular to subelliptical, medium to big pores present at medial and distal parts of abdominal skirt. Distal end of the abdominal skirt not brimmed. Aperture large, mainly covered by a con- vex cap with scattered, circular to subelliptical pores (pl. 1, fig. 16). A circular opening present at one side of the apertural ...
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... Holotype, HU.JMB.0067 (Pl. 1, Fig. 21); paratypes, HU.JMB.0068 (Pl. 1, Fig. 22), HU.JMB.0069 (Pl. 1, Fig. ...
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... bigger cephalis, poreless thorax and longer feet. It differs from Sanfilippoella lengeranlii Tekin, 1999 by having a test without lateral horn and velum at the end. It can be differentiated from Hinedorcus sp. A in possessing a twisted and shorter apical horn, less prominent lateral horn, shorter and poreless thorax and poreless ridges on feet. fig. 1 Description. Test dicyrtid with three long feet. Cephalis small, hemispherical and poreless with short, triradiate lateral horn and proximally wide, solid, dis- tally triradiate, and long apical horn. Thorax pyramidal, sparsely porous with long, slightly inwardly curved trir- adiate feet. Ridges on the feet sparsely porous. Aperture ...
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... electron micrographs of the middle Carnian Nassellaria from the Kö seyahya nappe. Length of scale bar = number of micro- meters (mm) for each figure. -Katroma ? ornata Tekin n. sp. 9. Holotype, sample 04-ELB-4. 10-13. Paratypes. Fig. 10 is from sample 04-ELB-5 and figs. 11, 12, 13 are from sample 04- ELB-4, scale bar for all figures = 120 mm. Figs. 14, 15, 16 -Katroma? proba Tekin n. sp. 14. Holotype, sample 04-ELB-2. 15-16 Paratypes. Fig. 15 is from sample 04-ELB-2 and fig. 16 is from sample 04-ELB-4, scale bar for all figures = 120 mm. Figs. 17, 18, 19, 20 -Katroma? ...
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... electron micrographs of the middle Carnian Nassellaria from the Kö seyahya nappe. Length of scale bar = number of micro- meters (mm) for each figure. -Katroma ? ornata Tekin n. sp. 9. Holotype, sample 04-ELB-4. 10-13. Paratypes. Fig. 10 is from sample 04-ELB-5 and figs. 11, 12, 13 are from sample 04- ELB-4, scale bar for all figures = 120 mm. Figs. 14, 15, 16 -Katroma? proba Tekin n. sp. 14. Holotype, sample 04-ELB-2. 15-16 Paratypes. Fig. 15 is from sample 04-ELB-2 and fig. 16 is from sample 04-ELB-4, scale bar for all figures = 120 mm. Figs. 17, 18, 19, 20 -Katroma? tunoglui Tekin n. sp. 17. Holotype, sam- ple 04-ELB-2. 18-20 Paratypes. Fig. 18 is from sam- ple 04-ELB-2 and figs. 19, ...
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... scale bar = number of micro- meters (mm) for each figure. -Katroma ? ornata Tekin n. sp. 9. Holotype, sample 04-ELB-4. 10-13. Paratypes. Fig. 10 is from sample 04-ELB-5 and figs. 11, 12, 13 are from sample 04- ELB-4, scale bar for all figures = 120 mm. Figs. 14, 15, 16 -Katroma? proba Tekin n. sp. 14. Holotype, sample 04-ELB-2. 15-16 Paratypes. Fig. 15 is from sample 04-ELB-2 and fig. 16 is from sample 04-ELB-4, scale bar for all figures = 120 mm. Figs. 17, 18, 19, 20 -Katroma? tunoglui Tekin n. sp. 17. Holotype, sam- ple 04-ELB-2. 18-20 Paratypes. Fig. 18 is from sam- ple 04-ELB-2 and figs. 19, 20 are from sample 04- ELB-5, scale bar for all figures = 120 ...
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... (mm) for each figure. -Katroma ? ornata Tekin n. sp. 9. Holotype, sample 04-ELB-4. 10-13. Paratypes. Fig. 10 is from sample 04-ELB-5 and figs. 11, 12, 13 are from sample 04- ELB-4, scale bar for all figures = 120 mm. Figs. 14, 15, 16 -Katroma? proba Tekin n. sp. 14. Holotype, sample 04-ELB-2. 15-16 Paratypes. Fig. 15 is from sample 04-ELB-2 and fig. 16 is from sample 04-ELB-4, scale bar for all figures = 120 mm. Figs. 17, 18, 19, 20 -Katroma? tunoglui Tekin n. sp. 17. Holotype, sam- ple 04-ELB-2. 18-20 Paratypes. Fig. 18 is from sam- ple 04-ELB-2 and figs. 19, 20 are from sample 04- ELB-5, scale bar for all figures = 120 ...
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... 04- ELB-4, scale bar for all figures = 120 mm. Figs. 14, 15, 16 -Katroma? proba Tekin n. sp. 14. Holotype, sample 04-ELB-2. 15-16 Paratypes. Fig. 15 is from sample 04-ELB-2 and fig. 16 is from sample 04-ELB-4, scale bar for all figures = 120 mm. Figs. 17, 18, 19, 20 -Katroma? tunoglui Tekin n. sp. 17. Holotype, sam- ple 04-ELB-2. 18-20 Paratypes. Fig. 18 is from sam- ple 04-ELB-2 and figs. 19, 20 are from sample 04- ELB-5, scale bar for all figures = 120 ...
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... Ornata (Latin, adj.), ornate. Types. Holotype, HU.JMB.0070 (Pl. 2, Fig. 9); paratypes, HU.JMB.0071 (Pl. 2, Fig. 10), HU.JMB.0072 (Pl. 2, Fig. 11), HU.JMB.0073 (Pl. 2, Fig. 12), HU.JMB.0074 (Pl. 2, Fig. ...
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... Ornata (Latin, adj.), ornate. Types. Holotype, HU.JMB.0070 (Pl. 2, Fig. 9); paratypes, HU.JMB.0071 (Pl. 2, Fig. 10), HU.JMB.0072 (Pl. 2, Fig. 11), HU.JMB.0073 (Pl. 2, Fig. 12), HU.JMB.0074 (Pl. 2, Fig. ...
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... Ornata (Latin, adj.), ornate. Types. Holotype, HU.JMB.0070 (Pl. 2, Fig. 9); paratypes, HU.JMB.0071 (Pl. 2, Fig. 10), HU.JMB.0072 (Pl. 2, Fig. 11), HU.JMB.0073 (Pl. 2, Fig. 12), HU.JMB.0074 (Pl. 2, Fig. ...
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... Ornata (Latin, adj.), ornate. Types. Holotype, HU.JMB.0070 (Pl. 2, Fig. 9); paratypes, HU.JMB.0071 (Pl. 2, Fig. 10), HU.JMB.0072 (Pl. 2, Fig. 11), HU.JMB.0073 (Pl. 2, Fig. 12), HU.JMB.0074 (Pl. 2, Fig. ...
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... Tekin n. sp. in possessing fewer lateral horns, much inflated post-abdominal segment, more and shorter medial spines on post-abdominal segment, shorter tube with more and shorter distal projections. , Fig. 14); paratypes, HU.JMB.0076 (Pl. ...
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... regularly arranged triangu- lar distal projections. It is also differentiated from Ka- troma ? tunoglui Tekin n. sp. in possessing fewer lateral horns, much inflated post-abdominal segment, more and shorter medial spines on post-abdominal segment, shorter tube with more and shorter distal projections. , Fig. 14); paratypes, HU.JMB.0076 (Pl. 2, Fig. 15), HU.JMB.0077 (Pl. 2, Fig. ...
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... triangu- lar distal projections. It is also differentiated from Ka- troma ? tunoglui Tekin n. sp. in possessing fewer lateral horns, much inflated post-abdominal segment, more and shorter medial spines on post-abdominal segment, shorter tube with more and shorter distal projections. , Fig. 14); paratypes, HU.JMB.0076 (Pl. 2, Fig. 15), HU.JMB.0077 (Pl. 2, Fig. ...
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... Holotype, HU.JMB.0078 (Pl. 2, Fig. 17); paratypes, HU.JMB.0079 (Pl. 2, Fig. 18), HU.JMB.0080 (Pl. 2, Fig. 19), HU.JMB.0081 (Pl. 2, Fig. ...
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... Holotype, HU.JMB.0078 (Pl. 2, Fig. 17); paratypes, HU.JMB.0079 (Pl. 2, Fig. 18), HU.JMB.0080 (Pl. 2, Fig. 19), HU.JMB.0081 (Pl. 2, Fig. ...
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... Holotype, HU.JMB.0078 (Pl. 2, Fig. 17); paratypes, HU.JMB.0079 (Pl. 2, Fig. 18), HU.JMB.0080 (Pl. 2, Fig. 19), HU.JMB.0081 (Pl. 2, Fig. ...
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... Firma (Latin, adj.) -strong, firm. Types. Holotype, HU.JMB.0082 (Pl. 3, Fig. 1); paratypes, HU.JMB.0083 (Pl. 3, Fig. 2), HU.JMB.0084 (Pl. 3, Fig. ...
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... Syringocapsa nuda Tekin n. sp. by having longer test, subspherical to subelliptical, large pores on the post-abdominal segment, medial spines and wider tube. Tekin U.K. & Bedi Y. 180 PLATE 3 Scanning electron micrographs of the middle Carnian Nassellaria from the Kö seyahya nappe. Length of scale bar = number of micrometers (mm) for each figure. Figs. 1, 2, 3 -Syringocapsa firma Tekin n. sp. 1. Holotype, sample 04-ELB-2. 2-3 Paratypes. Fig. 2 is from sample 04- ELB-3 and fig. 3 is from sample 04-ELB-2, scale bar for all figures = 90 mm. Figs. 4, 5, 6 -Syringocapsa nuda Tekin n. sp. 4. Holotype, sample 04-ELB-4. 5-6 Paratypes. Fig. 5 is from sample 04- ELB-3 and fig. 6 is from sample ...
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... Tekin n. sp. 4. Holotype, sample 04-ELB-4. 5-6 Paratypes. Fig. 5 is from sample 04- ELB-3 and fig. 6 is from sample 04-ELB-4, scale bar for all figures = 70 mm. Fig. 7 -Praeprotunuma sp. A. Sample 04-ELB-4, scale bar = 65 mm. Figs. 8, 9, 10 -Nabolella parvispinosa (Kozur & Mock). Fig. 8 is from sample 04-ELB-2, fig. 9 is from sample 04- ELB-5 and fig. 10 is from sample 04-ELB-3, scale bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale ...
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... sample 04- ELB-3 and fig. 6 is from sample 04-ELB-4, scale bar for all figures = 70 mm. Fig. 7 -Praeprotunuma sp. A. Sample 04-ELB-4, scale bar = 65 mm. Figs. 8, 9, 10 -Nabolella parvispinosa (Kozur & Mock). Fig. 8 is from sample 04-ELB-2, fig. 9 is from sample 04- ELB-5 and fig. 10 is from sample 04-ELB-3, scale bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and ...
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... is from sample 04-ELB-4, scale bar for all figures = 70 mm. Fig. 7 -Praeprotunuma sp. A. Sample 04-ELB-4, scale bar = 65 mm. Figs. 8, 9, 10 -Nabolella parvispinosa (Kozur & Mock). Fig. 8 is from sample 04-ELB-2, fig. 9 is from sample 04- ELB-5 and fig. 10 is from sample 04-ELB-3, scale bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and fig. 19 is from sample ...
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... for all figures = 70 mm. Fig. 7 -Praeprotunuma sp. A. Sample 04-ELB-4, scale bar = 65 mm. Figs. 8, 9, 10 -Nabolella parvispinosa (Kozur & Mock). Fig. 8 is from sample 04-ELB-2, fig. 9 is from sample 04- ELB-5 and fig. 10 is from sample 04-ELB-3, scale bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and fig. 19 is from sample 04-ELB-3, scale bar for both figures = ...
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... scale bar = 65 mm. Figs. 8, 9, 10 -Nabolella parvispinosa (Kozur & Mock). Fig. 8 is from sample 04-ELB-2, fig. 9 is from sample 04- ELB-5 and fig. 10 is from sample 04-ELB-3, scale bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and fig. 19 is from sample 04-ELB-3, scale bar for both figures = 90 mm. Fig. 20 - Range. Middle ...
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... & Mock). Fig. 8 is from sample 04-ELB-2, fig. 9 is from sample 04- ELB-5 and fig. 10 is from sample 04-ELB-3, scale bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and fig. 19 is from sample 04-ELB-3, scale bar for both figures = 90 mm. Fig. 20 - Range. Middle ...
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... fig. 9 is from sample 04- ELB-5 and fig. 10 is from sample 04-ELB-3, scale bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and fig. 19 is from sample 04-ELB-3, scale bar for both figures = 90 mm. Fig. 20 - Range. Middle ...
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... scale bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and fig. 19 is from sample 04-ELB-3, scale bar for both figures = 90 mm. Fig. 20 - Range. Middle ...
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... bar for all figures = 130 mm. Figs. 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and fig. 19 is from sample 04-ELB-3, scale bar for both figures = 90 mm. Fig. 20 - Range. Middle ...
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... 11, 12 -Nabolella sp. A. Fig. 11 is from sample 04-ELB-4 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Figs. 13, 14 -Annulopoulpus parviaperturus (Kozur & Mostler). Fig. 13 is from sample 04-ELB-5 and fig. 14 is from sample 04-ELB-4, scale bar for both figures = 110 mm. Fig. 15 - Fig. 18 is from sample 04-ELB-5 and fig. 19 is from sample 04-ELB-3, scale bar for both figures = 90 mm. Fig. 20 - Range. Middle ...
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... Parapoulpus Kozur & Mostler, 1979 Type species: Parapoulpus oertlii Kozur & Mostler, 1979 Parapoulpus sp. A Pl. 3, fig. 15 Description. Monocyrtid test with thick, spongy skeletons. Cephalis hemispherical with three feet. Feet very long, slender, triradiate with wide grooves and shallow furrows, proximally curved outside then curved inside distally. Velum after cephalis long, decreasing in width distally. Aperture large and ...
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... Veghia Kozur & Mostler, 1981 Type species: Veghia goestlingensis Kozur & Mostler, 1981 Veghia goestlingensis Kozur & Mostler, 1981 Pl. 3, figs 18, 19 1981 Veghia goestlingensis Kozur & Mostler, pp. 86-87, pl. 30, fig. 1 Kozur & Mostler, 1979Genus Pseudosaturniforma Kozur & Mostler, 1979 Type species: Pseudosaturniforma latimarginata Kozur & Mostler, 1979 Range. Middle Carnian -early Norian -? late middle ...
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... Holotype, HU.JMB.0088 (Pl. 4, Fig. 1); paratypes, HU.JMB.0089 (Pl. 4, Fig. 2), HU.JMB.0090 (Pl. 4, Fig. ...
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... rare, scattered small pores and basally wider, small feet. Scanning electron micrographs of the middle Carnian Nassellaria from the Kö seyahya nappe. Length of scale bar = number of micro- meters (mm) for each figure. -Sanfilippoella sp. A. Sample 04-ELB-2, scale bar = 165 mm. Fig. 8 -Sanfilippoella sp. B. Sample 04-ELB-2, scale bar = 175 mm. Figs. 9, 10 -Castrum sp. aff. C. perornatum Blome. Fig. 9 is from sample 04-ELB-2 and fig. 10 is from sample 04-ELB-5, scale bar for both figures = 120 mm. Figs. 11, 12 -Castrum sp. A. Fig. 11 is from sample 04-ELB-2 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Sanfilippoella tortilis Kozur & Mostler, 1979 Pl. fig. 7 ...
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... of the middle Carnian Nassellaria from the Kö seyahya nappe. Length of scale bar = number of micro- meters (mm) for each figure. -Sanfilippoella sp. A. Sample 04-ELB-2, scale bar = 165 mm. Fig. 8 -Sanfilippoella sp. B. Sample 04-ELB-2, scale bar = 175 mm. Figs. 9, 10 -Castrum sp. aff. C. perornatum Blome. Fig. 9 is from sample 04-ELB-2 and fig. 10 is from sample 04-ELB-5, scale bar for both figures = 120 mm. Figs. 11, 12 -Castrum sp. A. Fig. 11 is from sample 04-ELB-2 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Sanfilippoella tortilis Kozur & Mostler, 1979 Pl. fig. 7 Description. Cephalis broadly conical with trir- adiate tapering horn and polygonal ...
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... of scale bar = number of micro- meters (mm) for each figure. -Sanfilippoella sp. A. Sample 04-ELB-2, scale bar = 165 mm. Fig. 8 -Sanfilippoella sp. B. Sample 04-ELB-2, scale bar = 175 mm. Figs. 9, 10 -Castrum sp. aff. C. perornatum Blome. Fig. 9 is from sample 04-ELB-2 and fig. 10 is from sample 04-ELB-5, scale bar for both figures = 120 mm. Figs. 11, 12 -Castrum sp. A. Fig. 11 is from sample 04-ELB-2 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Sanfilippoella tortilis Kozur & Mostler, 1979 Pl. fig. 7 Description. Cephalis broadly conical with trir- adiate tapering horn and polygonal pore frames with nodes at pore frame vertices. Thorax subpyramidal with ...
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... micro- meters (mm) for each figure. -Sanfilippoella sp. A. Sample 04-ELB-2, scale bar = 165 mm. Fig. 8 -Sanfilippoella sp. B. Sample 04-ELB-2, scale bar = 175 mm. Figs. 9, 10 -Castrum sp. aff. C. perornatum Blome. Fig. 9 is from sample 04-ELB-2 and fig. 10 is from sample 04-ELB-5, scale bar for both figures = 120 mm. Figs. 11, 12 -Castrum sp. A. Fig. 11 is from sample 04-ELB-2 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Sanfilippoella tortilis Kozur & Mostler, 1979 Pl. fig. 7 Description. Cephalis broadly conical with trir- adiate tapering horn and polygonal pore frames with nodes at pore frame vertices. Thorax subpyramidal with same pore frames as ...
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... -Sanfilippoella sp. A. Sample 04-ELB-2, scale bar = 165 mm. Fig. 8 -Sanfilippoella sp. B. Sample 04-ELB-2, scale bar = 175 mm. Figs. 9, 10 -Castrum sp. aff. C. perornatum Blome. Fig. 9 is from sample 04-ELB-2 and fig. 10 is from sample 04-ELB-5, scale bar for both figures = 120 mm. Figs. 11, 12 -Castrum sp. A. Fig. 11 is from sample 04-ELB-2 and fig. 12 is from sample 04-ELB-5, scale bar for both figures = 130 mm. Sanfilippoella tortilis Kozur & Mostler, 1979 Pl. fig. 7 Description. Cephalis broadly conical with trir- adiate tapering horn and polygonal pore frames with nodes at pore frame vertices. Thorax subpyramidal with same pore frames as cephalis at proximal part and with rare ...
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... sp. B Pl. 4, fig. 13 Description. Test long, spindle-shaped with twelve post-abdominal segments. Cephalothorax dome-shaped, poreless, without horn. Abdomen to last post-abdominal segment inverse subtrapezoidal in out- line. Between circumferential ridges, two different types of pore frames present; smaller, polygonal pore frames with small subcircular ...
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An assemblage of primitive agglutinated foraminifera is reported for the first time from Silurian limestones from the Dingle Peninsula, Ireland. The assemblage is dominated by tubothalamids (Rectoammodiscus and rare Sansabaina), with less abundant monothalamids (Psammosiphonella and Psammosphaera). At the species level, the agglutinated foraminifer...
The phosphate series of Matam (located at the North-East of Senegal) consists of a 10 meters alternation of soft phosphate levels, sand horizons and phosphatic limestones. While they were only mentioned in some preliminary geological works, isolated teeth of selachians are nevertheless common in these phosphate deposits. Detailed fieldwork of 9 new...
At two limestone sites in the vicinity of Rockensüß (Hessen, Germany), the fauna of True Bugs (Insecta: Heteroptera) was recorded between May 2012 and June 2013 mainly by using Malaise traps. A total of 61 species of bugs was discovered. The mirid bugs Capsus pilifer and Strongylocoris leucocephalus are endangered species at federal state and count...
Meghalaya, a small state in North Eastern region of India is abundantly blessed with coal and limestone. About 9% of the country's total limestone reserves are distributed in the state. Mining is carried out by open cast method of mining which is taking place at both large scale and small scale levels. The limestone mined is used chiefly for the ma...
Citations
... Some of the taxa, such as Paraparonaella okuyucui, Ropanaella nitida, R. ygraeca Triassoastrum paratrammeri, Carinacyclia acari, Praeorbiculiformella parvicentrum, Recoarella lahmi, Relindella lenticulata, Tetraporobrachia bedii, Haeckelicyrtium planum from sample Kilek-23 were previously described from the upper Lower Carnian strata from eastern Turkey (Tekin and Bedi, 2007b;Dumitrica et al., 2013aDumitrica et al., , 2013bDumitrica, 2017), corresponding to the Elbistanium gracile Radiolaria Zone by Moix et al. (2007). Some additional taxa belonging to this zone, have also been reported by some studies (e.g., Tekin and Bedi, 2007a;Dumitrica et al., 2010) based on material also from Elbistan, SE Turkey. ...
... Some of the taxa in sample Kilek-23 were previously obtained from the uppermost Lower Carnian (based on the two-fold Carnian subdivision) or the uppermost Middle Carnian strata (based on the three-fold subdivision), indicating the Elbistanium gracile Zone (e.g. Tekin & Bedi 2007b;Dumitrica et al. 2013a, b;Dumitrica 2017). Due to the presence of the index taxon for the Tetraporobrachia haeckeli Zone and the absence of the index taxon for the earlier Elbistanium gracile Zone, the radiolarian fauna from sample Kilek-23 corresponds to the Tetraporobrachia haeckeli Zone (Fig. 4). ...
The Mersin Mélange, located in southern Turkey north-west of the city of Mersin, includes blocks and tectonic slices of different origins. The Kilek section in the Mersin Mélange was sampled for a thorough examination of its lithology, biostratigraphy and fossil content. Two samples from the cherty limestone layers within the Huglu Tuffites at the top of the section yielded a rich silicified ostracod fauna of late Early Carnian (based on a two-fold Carnian subdivision) or middle Middle Carnian age (based on a three-fold Carnian subdivision), deposited in an open marine environment, in the outer platform-upper slope zone. We report 121 ostracod species belonging to 53 genera. Two new genera are described: Edithobairdia Forel gen. nov. and Gencella Forel gen. nov., as well as 16 new species: Acanthoscapha mersinella Forel sp. nov., Bairdia hugluensis Forel sp. nov., Acratia kollmanni Forel sp. nov., Citrella? carniana Forel sp. nov., Cytheropteron? schornikovi Forel sp. nov., Eucytherura lacerata Forel sp. nov., Gencella taurensis Forel sp. nov., Kerocythere dorsidenticulata Forel sp. nov., Kerocythere tricostata Forel sp. nov., Monoceratina praevulsaformis Forel sp. nov., Patellacythere tourkosella Forel sp. nov., Polycope kilekensis Forel sp. nov., Ptychobairdia praekristanae Forel sp. nov., Simeonella daginikella Forel sp. nov., Spinomicrocheilinella reliquiaella Forel sp. nov. and Triassocythere tavuscayiriensis Forel sp. nov. The diagnosis of Acratia goemoeryi Kozur is emended. The Kilek fauna retains primitive characteristics illustrated by the first known occurrence of Palaeocopida and Rectonariidae (typical Palaeozoic forms) in the Late Triassic, associated with typical Triassic–modern elements such as thick-shelled and ornamented Bairdiidae and diverse Cytheroidea known from the Middle and Late Triassic worldwide. The unique composition of Palaeozoic and Mesozoic taxa from the Kilek section illustrates unexpected long-term survival in a deep-sea refuge zone following the end-Permian extinction, and the diachronous character of the ostracod recovery in different environments.
http://zoobank.org/urn:lsid:zoobank.org.pub:662C3D5C–2B86–4D7B–BDB5–8F8B6A1AD1E7
... These similarities prove doubtlessly that both faunas come from the same paleogeographic area. These two faunas have many elements in common with the upper Carnian (Tetraporobrachia haeckeli Zone) fauna from the Köseyahya Nappe in Elbistan (Tekin and Bedi, 2007a, b, Dumitrica et al., 2010, 2013a. In this paper, we continue the taxonomic work of the exceptionally preserved lower Tuvalian radiolarians by the description of several new taxa of Nassellaria from the Sorgun Ophiolitic Mélange and from the Kopría Mélange, Rhodes (Greece). ...
... This Austrian species does not seem at all to be a Silicarmiger species because it shows no segmented postcephalic body. The only species that seems somehow to belong to this new species is that illustrated by Tekin and Bedi (2007a) from the Köseyahya Nappe near Elbistan, but its spines are not yet so long as this species from the Moixi Zone. The upper Julian species from Elbistan seems to be, in fact, the forerunner of the present one. ...
... Recently, Dumitrica et al. (2010Dumitrica et al. ( , 2013aDumitrica et al. ( , 2013b revised the Elbistan radiolarian assemblage and suggested that the E. gracile Zone should be placed at the topmost part of middle Carnian, corresponding to the Austriacum Zone ( fig. 5). When the Turunç radiolarian assemblage is compared with the assemblage in the E. gracile Zone (Tekin andBedi 2007a, 2007b;Dumitrica et al. 2010Dumitrica et al. , 2013aDumitrica et al. , 2013b from the Elbistan region, some of the taxa (e.g., N. parvispinosa and R. goczani) are common in both places. However, the most characteristic taxa (E. ...
... Recently, Dumitrica et al. (2010Dumitrica et al. ( , 2013aDumitrica et al. ( , 2013b revised the Elbistan radiolarian assemblage and suggested that the E. gracile Zone should be placed at the topmost part of middle Carnian, corresponding to the Austriacum Zone ( fig. 5). When the Turunç radiolarian assemblage is compared with the assemblage in the E. gracile Zone (Tekin andBedi 2007a, 2007b;Dumitrica et al. 2010Dumitrica et al. , 2013aDumitrica et al. , 2013b from the Elbistan region, some of the taxa (e.g., N. parvispinosa and R. goczani) are common in both places. However, the most characteristic taxa (E. ...
The Turunç Unit, which represents one of the tectonic slices within the Lycian Nappes in southwestern Anatolia, preserves the remnants derived from the northern branch of Neotethys. The unit includes basalts intercalated with pelagic limestones of middle Carnian age (early Late Triassic) based on the characteristic radiolarian assemblage of the Tetraporobrachia haeckeli Zone. The Turunç lavas reflect trace element signatures resembling those fromsubduction zones, displaying selective enrichment of Th and light rare earth elements over high-field strength elements and heavy rare earth elements. Considering the overall geochemical characteristics of the Turunç basalts and given that they are found to be associated with no continent-derived detritus, the Turunç lavas appear to represent fragments of a Late Triassic island arc formed on the Neotethyan oceanic lithosphere. This result is of particular importance, since it reflects the oldest subduction age obtained from the entire Neotethyan realm to date. It may further indicate that the Neotethyan oceanic lithosphere had already been formed by the early Late Triassic, thus suggesting a pre-early Late Triassic oceanization of the northern branch of Neotethys. On the basis of this, we also suggest that the initial rifting leading to the opening of the northern branch of Neotethys should have taken place during the Middle Triassic or earlier.
... Monod, (1977) dated blocks of debris flow deposits as Anisian which constitute the unit. However, Mahmut tepesi limestones which are in transitional contact with Dedemli formation were dated as middle Carnian (Tekin, 1999;Tekin and Bedi, 2007). Therefore, the age of the formation was accepted as Anisian-middle Carnian. ...
... The unit is composed of brown, orange, pink colored, cherty, fine bedded and folded pelagic limestones (Figure 5c different ages in different parts of the Central Taurides and have been deposited in a broad time period ranging from Middle-Late Triassic to early Senonian (Özgül, 1977). In latter studies, Middle Carnian age was obtained from radiolarians in cherty limestones constituting the unit (Tekin, 1999;Tekin et al., 2001;Tekin and Bedi 2007). The age of the unit was accepted as middle Norian-Santonian. ...
The study area located in Bucakkışla region in Central Taurides consists of rock units of
the melange which form Bozkır unit of the Tauride units and the overlying cover rocks.
There are volcanic, ophiolitic and sedimentary rocks which generated in different
environmental conditions. These rock groups comprise units which formed in Middle-
Upper Triassic-Paleocene periods in Inner Tauride Ocean that had been opened between
Tauride – Anatolide continents. Within the scope of this study, lithostratigraphic
characteristics of Huğlu, Boyalı tepe, Korualan nappes and cover rocks which form Bozkır
Unit and tectono sedimentary evolution of the study area was built up by paleontological
and structural features. Due to rifting, which started in Middle Upper Triassicin the region,
the products of the rift volcanism in rifting center and the carbonate deposition on margins
of basin have occurred. The continuation of extension which initiated rifting caused
collapse in the basin in Middle Upper Triasic – Lower Senonian. Deep marine deposition
has occurred at the center of basin, however pelagic and neritic limestones were deposited
in basin margins during this time. The region has become compressed by the effect of a
new tectonical regime which had been effective starting from Santonian. This compression
caused new melanges to take place due to reverse faults and thrust. The formation of these
melanges has continued until the end of Paleocene period. However, there has not been
observed any formation depending on the compression in post Paleocene. The nappes have
moved southward by the effect of compression until Eocene. But then, these nappes could
not advance forward anymore so, northward back thrusts took place as basin was closured
andreached the collisional stage. Sequences which had become imbricated structures by
back thrusts were subjected to collapsing by the stop of compression and the gravitational
effect. All sequences in the imbricated structure were cut by dip slip normal faults and
lacustrine basins were formed on fallen blocks. The formation of Early Oligocene
terrestrial deposits in these lakes indicates that the collapse occurred in Oligocene or
immediately before this time, and this allows the dating of new tectonical period. Early
Oligocene deposits to become tilted by dip slip faults show that new tectonic period in the
region has also continued after Oligocene.
... Monod, (1977) dated blocks of debris flow deposits as Anisian which constitute the unit. However, Mahmut tepesi limestones which are in transitional contact with Dedemli formation were dated as middle Carnian (Tekin, 1999;Tekin and Bedi, 2007). Therefore, the age of the formation was accepted as Anisian-middle Carnian. ...
... The unit is composed of brown, orange, pink colored, cherty, fine bedded and folded pelagic limestones (Figure 5c different ages in different parts of the Central Taurides and have been deposited in a broad time period ranging from Middle-Late Triassic to early Senonian (Özgül, 1977). In latter studies, Middle Carnian age was obtained from radiolarians in cherty limestones constituting the unit (Tekin, 1999;Tekin et al., 2001;Tekin and Bedi 2007). The age of the unit was accepted as middle Norian-Santonian. ...
The study area located in Bucakk›flla region in Central Taurides consists of rock units of the melange which form Bozk›r unit of the Tauride units and the overlying cover rocks. There are volcanic, ophiolitic and sedimentary rocks which generated in different environmental conditions. These rock groups comprise units which formed in Middle-Upper Triassic-Paleocene periods in Inner Tauride Ocean that had been opened between Tauride – Anatolide continents. Within the scope of this study, lithostratigraphic characteristics of Hu¤lu, Boyal› hill, Korualan nappes and cover rocks which form Bozk›r Unit and tectono sedimentary evolution of the study area was built up by paleontological and structural features. Due to rifting, which started in Middle Upper Triassicin the region, the products of the rift volcanism in rifting center and the carbonate deposition on margins of basin have occurred. The continuation of extension which initiated rifting caused collapse in the basin in Middle Upper Triasic – Lower Senonian. Deep marine deposition has occurred at the center of basin, however pelagic and neritic limestones were deposited in basin margins during this time. The region has become compressed by the effect of a new tectonical regime which had been effective starting from Santonian. This compression caused new melanges to take place due to reverse faults and thrust. The formation of these melanges has continued until the end of Paleocene period. However, there has not been observed any formation depending on the compression in post Paleocene. The nappes have moved southward by the effect of compression until Eocene. But then, these nappes could not advance forward anymore so, northward back thrusts took place as basin was closured andreached the collisional stage. Sequences which had become imbricated structures by back thrusts were subjected to collapsing by the stop of compression and the gravitational effect. All sequences in the imbricated structure were cut by dip slip normal faults and lacustrine basins were formed on fallen blocks. The formation of Early Oligocene terrestrial deposits in these lakes indicates that the collapse occurred in Oligocene or immediately before this time, and this allows the dating of new tectonical period. Early Oligocene deposits to become tilted by dip slip faults show that new tectonic period in the region has also continued after Oligocene.
... Without waiting for the completion of the study of the whole fauna; that is, without knowing its complete content, but based only on the new nassellarians described by Tekin & Bedi (2007b) and especially (we cite) on the ''cooccurrence of the species of Elbistanium Tekin, with species characteristic of the Tetraporobrachia haeckeli Zone along with several other taxa not present below this zone including Castrum spp., Syringocapsa firma Tekin, S. nuda Tekin, Podobursa spp., Spinocapnuchosphaera spp., and the first Unumidae'', Kozur et al. (2009) defined a new biostratigraphic zone for this assemblage, which they called the Elbistanium gracile Zone. According to them, the zone is only known in the Köseyahya section studied in the present paper. ...
The present article is a taxonomic study of all spongy spumellarian radiolarian taxa with three and four coplanar spines or spongy arms occurring in the middle Carnian from the Köseyahya section, near the town of Elbistan, SE Turkey. This fauna is characteristic of the Tetraporobrachia haeckeli radiolarian Zone, and comes from an 8 m thick succession of clayey-cherty limestones occurring at the lower part of the section. In addition, a few species from the Middle and Upper Triassic from other areas have been also included in this study to improve some generic diagnoses, and to better comprehend the diversity and evolutionary trends of some genera, subfamilies and families. The taxonomy at the generic and suprageneric levels is based primarily on the types of microsphere. This new approach allowed new taxonomic arrangements of genera and suprageneric units, and suggested new phylogenetic relationships among these radiolarians and between them and younger radiolarians. The authors discuss and describe 69 species, of which 37 are new, and 14 genera, of which three are new (Paraparonaella, Pseudangulobracchia, and Ropanaella). The genus Triassoastrum and others are reinterpreted. All genera studied are assigned to five subfamilies, of which two are new (Tetrapaurinellinae and Triassocrucellinae), and two families (Tritrabidae and Veghicycliidae). Nine species in open nomenclature are also illustrated.
... Without waiting for the completion of the study of the whole fauna; that is, without knowing its complete content, but based only on the new nassellarians described by Tekin & Bedi (2007b) and especially (we cite) on the ''cooccurrence of the species of Elbistanium Tekin, with species characteristic of the Tetraporobrachia haeckeli Zone along with several other taxa not present below this zone including Castrum spp., Syringocapsa firma Tekin, S. nuda Tekin, Podobursa spp., Spinocapnuchosphaera spp., and the first Unumidae'', Kozur et al. (2009) defined a new biostratigraphic zone for this assemblage, which they called the Elbistanium gracile Zone. According to them, the zone is only known in the Köseyahya section studied in the present paper. ...
This article reports on the few cases of Siamese twins of Mesozoic Radiolaria found by the author during his entire activity as a micropaleontologist and by previous authors. Such cases are extremely rare: a single case is known from the Middle Triassic (late Anisian) nassellarians, while cases of spumellarians have been found from the Middle Triassic (Anisian), the Late Jurassic (early Tithonian) and the Late Cretaceous (Cenomanian), and entactinarian cases are known from the Late Jurassic (early Tithonian) Saturnalidae. The already known case of the Oxfordian nassellarian species Parvicingula dhimenaensis, considered to represent Siamese twins with four joined individuals, has been proved to be a very interesting case of reparation of a damaged specimen during its growth. The author also discusses the different types of Siamese twin radiolarians and the relations between their silicification and binary fission of the central capsule.RésuméL’article présente les rares cas de squelettes siamois de radiolaires mésozoïques trouvés par l’auteur au cours de son activité de micropaléontologue ainsi que par d’autres auteurs. Ces cas sont rarissimes : un seul cas est connu parmi les nassellaires du Trias Moyen (Anisien supérieur), alors que plusieurs cas sont décrits chez les spumellaires du Trias moyen (Anisien), du Jurassique supérieur (Tithonien inférieur) et du Crétacé supérieur (Cénomanien) et d’autres cas encore sont décrits chez des entactinaires de la famille des Saturnalidae du Jurassique supérieur (Tithonien inférieur). Le cas déjà connu de l’espèce oxfordienne Parvicingula dhimenaensis, considéré comme un squelette siamois avec quatre individus accolés au niveau de l’ouverture, s’est révélé être un cas très intéressant de réparation d’un individu brisé pendant sa croissance. L’auteur discute aussi les différents types de squelettes siamois et des relations entre leur silicification et la fission de la capsule centrale.
... P. glaber, P. sp. cf. P. simoni), it can be concluded that this fauna has great similarity to the faunas previously obtained from middle Carnian strata of Austria (Kozur and Mostler, 1978;1979;Lahm, 1984) and Turkey (Tekin, 1999;Tekin and Bedi, 2007a;2007b). Based on these facts, middle a Carnian age is assigned to sample 04-CK-1 from the Cukurkoy section (Fig. 9). ...
The geochemical features of spilitic basalts and the radiolarian fauna of associated pelagic sediments have been studied from two different sections of the Alakirçay Nappe of the Antalya Nappes, SW Turkey. The first section in Cukurkoy is located in the eastern part of the Antalya Gulf and includes thick spilitic basalts, overlain by an alternation of mudstone, marl and pelagic cherty limestone. Radiolarian data from the cherty limestone in this unit reveals a middle Carnian age for this section. The second section in Yaylakuzdere is situated in the western part of the Antalya Gulf. In this section, thick pillow basalts are overlain by a succession of limestone/cherty limestone and shale beds. The age of the limestones interlayered with the pillow basalts was assigned to the late Carnian, whereas the basal part of the overlying cherty limestones was dated as latest Carnian/earliest Norian by conodont and radiolarian faunas. The pillow lavas in the çukurköy and Yaylakuzdere regions consist of within-plate type alkaline basalts and display multi-element pattern similar to typical oceanic island basalts (OIB). Low La/Yb, Zr/Y and La/Nb < 1 ratios are also indicative for an OIB-like deep mantle source. These alkaline basalts have not suffered interactions with a subducted slab and/or continental crust due to presence of high HFSE abundance, the lack of depletion in Nb and Ta that are characteristics of subduction and/or crustal contamination processes. Based on this data, it can be concluded that alkaline volcanism in these two regions of the Antalya Nappes have been probably generated by a small OIBtype mantle plume during the middle - late Carnian time interval, in the advanced stages of rifting of the Antalya Nappes successions in the southern branch of Neotethys. This data reveals the generation of a rift basin before middle Carnian for this ocean.
