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Text-fig. 12. Paramblypterus cf. rohani. Arrows indicate directio cranialis. a, b: photograph and drawing of four ridge scales in front of the dorsal fin base, locality Otovice "Chmelnice", P 80178, scale bars 5 mm; c: scale rows from the area between the pectoral and pelvic fins, outer surfaces of the scales bear fine ridges terminating as denticles on the posterior edge of the scales, locality Otovice "Chmelnice", NM-M 4916, scale bar 5 mm; d: isolated scale, from anterior area of the lateral side of the body, with denticulated posterior edge, locality Otovice "Chmelnice", P 30945, scale bar 2 mm; e: isolated scale from the pelvic area of the body, locality Otovice "Chmelnice", P 30945, scale bar 2 mm; f, g: drawing and photograph of the postcleithrum and the scales behind the pectoral girdle (the scales bear conspicuous ridges on their outer surface; well preserved large postcleithrum is without ridges.), locality Otovice "Chmelnice", NM-M 4915, scale bars 5 mm. Abbreviations: Cl – cleithrum, Pcl – postcleithrum, Scl – supracleithrum. in Actinopterygians Of The Broumov Formation (Permian) In The Czech Part Of The Intra-Sudetic Basin (The Czech Republic)
Text-fig. 12. Paramblypterus cf. rohani. Arrows indicate directio cranialis. a, b: photograph and drawing of four ridge scales in front of the dorsal fin base, locality Otovice "Chmelnice", P 80178, scale bars 5 mm; c: scale rows from the area between the pectoral and pelvic fins, outer surfaces of the scales bear fine ridges terminating as denticles on the posterior edge of the scales, locality Otovice "Chmelnice", NM-M 4916, scale bar 5 mm; d: isolated scale, from anterior area of the lateral side of the body, with denticulated posterior edge, locality Otovice "Chmelnice", P 30945, scale bar 2 mm; e: isolated scale from the pelvic area of the body, locality Otovice "Chmelnice", P 30945, scale bar 2 mm; f, g: drawing and photograph of the postcleithrum and the scales behind the pectoral girdle (the scales bear conspicuous ridges on their outer surface; well preserved large postcleithrum is without ridges.), locality Otovice "Chmelnice", NM-M 4915, scale bars 5 mm. Abbreviations: Cl – cleithrum, Pcl – postcleithrum, Scl – supracleithrum.
Text-fig. 11. Paramblypterus cf. rohani. Arrows indicate directio cranialis. Scale bars 5 mm. a: isolated maxilla, cleithrum and supracleithrum in lateral view, locality Otovice "Chmelnice", P 64661; b: left posttemporal in dorsal view, locality Otovice "Chmelnice", P 64664; c: right operculum in lateral view, locality Otovice "Chmelnice", P 64883; d: anal fin, locality Otovice "Stěnava", DP 4529; e: dorsal fin, locality Otovice "Chmelnice", NM-M 4916. Abbreviations: Cl – cleithrum, Mx – maxilla, Scl – supracleithrum. in Actinopterygians Of The Broumov Formation (Permian) In The Czech Part Of The Intra-Sudetic Basin (The Czech Republic)
Text-fig. 11. Paramblypterus cf. rohani. Arrows indicate directio cranialis. Scale bars 5 mm. a: isolated maxilla, cleithrum and supracleithrum in lateral view, locality Otovice "Chmelnice", P 64661; b: left posttemporal in dorsal view, locality Otovice "Chmelnice", P 64664; c: right operculum in lateral view, locality Otovice "Chmelnice", P 64883; d: anal fin, locality Otovice "Stěnava", DP 4529; e: dorsal fin, locality Otovice "Chmelnice", NM-M 4916. Abbreviations: Cl – cleithrum, Mx – maxilla, Scl – supracleithrum.
Text-fig. 15. Aeduellidae. Scale bars 5 mm. a: isolated left maxilla in lateral view, locality Otovice "Chmelnice", P 64678; b: the skull in lateral view, locality Otovice "Stěnava", G 58; c, d: drawing and photograph of the skull roof in dorsal view, locality Otovice, NM-M 4910. Abbreviations: Dpt – dermopterotic, Dsph – dermosphenotic, Ext – extrascapular, Fr – frontal, Io – infraorbital, ioc – infraorbital canal, Md – mandible, mp – medial pit line, Mx – maxilla, Na – nasal, Op – operculum, Pa – parietal, pp – posterior pit line, soc – supraorbital canal, stc – supratemporal canal. in Actinopterygians Of The Broumov Formation (Permian) In The Czech Part Of The Intra-Sudetic Basin (The Czech Republic)
Text-fig. 15. Aeduellidae. Scale bars 5 mm. a: isolated left maxilla in lateral view, locality Otovice "Chmelnice", P 64678; b: the skull in lateral view, locality Otovice "Stěnava", G 58; c, d: drawing and photograph of the skull roof in dorsal view, locality Otovice, NM-M 4910. Abbreviations: Dpt – dermopterotic, Dsph – dermosphenotic, Ext – extrascapular, Fr – frontal, Io – infraorbital, ioc – infraorbital canal, Md – mandible, mp – medial pit line, Mx – maxilla, Na – nasal, Op – operculum, Pa – parietal, pp – posterior pit line, soc – supraorbital canal, stc – supratemporal canal.
Text-fig. 10. Progyrolepis heyleri POPLIN, 1999. a: dorsal lobe of the caudal fin with the fulcral scales along the dorsal edge of the lobe, GMC 55, whitened, scale bar 5 mm; b: basal fulcral scales from the dorsal edge of the caudal peduncle, G 123, whitened, scale bar 5 mm; c: fragment of the body of juvenile specimen with dorsal and anal fins, GMC 11, whitened, scale bar 5 mm; d: isolated scales from lateral side of the body, G 123, whitened, scale bar 5 mm; e: ridges on the scale surface, the frame delineates the area illustrated in (f) at higher magnification, G 123, scale bar 500 µm; f: details of the surface with microtubercles, scale bar 50 µm; g: isolated lepidotrichium of an adult specimen with very short and wide segments and with unsegmented basal part, GMC 101, whitened, scale bar 5 mm; h: large conical teeth from the internal row of the maxilla, G 123, scale bar 2 mm; i: microsculpture formed by elliptical proximo-distally elongated protuberances on the large conical tooth, G 123, scale bar 100 µm; j: large conical tooth from the internal row of the maxilla, G 123, scale bar 2 mm; k: microsculpture formed by elliptical proximo-distally elongated protuberances on the large conical tooth, G 123, scale bar 100 µm. in New Actinopterygians From The Permian Of The Brive Basin, And The Ichthyofaunas Of The French Massif Central
Text-fig. 10. Progyrolepis heyleri POPLIN, 1999. a: dorsal lobe of the caudal fin with the fulcral scales along the dorsal edge of the lobe, GMC 55, whitened, scale bar 5 mm; b: basal fulcral scales from the dorsal edge of the caudal peduncle, G 123, whitened, scale bar 5 mm; c: fragment of the body of juvenile specimen with dorsal and anal fins, GMC 11, whitened, scale bar 5 mm; d: isolated scales from lateral side of the body, G 123, whitened, scale bar 5 mm; e: ridges on the scale surface, the frame delineates the area illustrated in (f) at higher magnification, G 123, scale bar 500 µm; f: details of the surface with microtubercles, scale bar 50 µm; g: isolated lepidotrichium of an adult specimen with very short and wide segments and with unsegmented basal part, GMC 101, whitened, scale bar 5 mm; h: large conical teeth from the internal row of the maxilla, G 123, scale bar 2 mm; i: microsculpture formed by elliptical proximo-distally elongated protuberances on the large conical tooth, G 123, scale bar 100 µm; j: large conical tooth from the internal row of the maxilla, G 123, scale bar 2 mm; k: microsculpture formed by elliptical proximo-distally elongated protuberances on the large conical tooth, G 123, scale bar 100 µm.
FIGURE 4. Isolated left P4 in Endemism and migration in the Kochkor Basin? Identification and description of Adcrocuta eximia (Mammalia: Carnivora: Hyaenidae) and c.f. Paramachaerodus (Mammalia: Carnivora: Felidae) fossils at the Miocene locality of Ortok, Kyrgyzstan
FIGURE 4. Isolated left P4 of UOMNH F-70508, Adcrocuta eximia. A, schematic of preserved features in occlusal view; B, occlusal view of specimen displaying minimal wear on metastylar blade; C, lingual view of specimen. Note reduced protocone that does not extend anterior to the anterior face of the parastyle. Scale bar equals 10 mm.
FIGURE 5 in Genetic differentiation through dispersal and isolation in two freshwater fish species from coastal basins of Northeastern Brazil
FIGURE 5 | Time-calibrated phylogeny for samples of Prochilodus lacustris from Maranhão coastal basins and Tocantins basin. Time is in thousands of years. The color bars in the tree correspond to the populations presented in Fig. 3A.
FIGURE 4 in Genetic differentiation through dispersal and isolation in two freshwater fish species from coastal basins of Northeastern Brazil
FIGURE 4 | Time-calibrated phylogeny for samples of Schizodon dissimilis from coastal basins of northeastern Brazil. Time is in thousands of years. The color bars in the tree correspond to the populations presented in Fig. 2A.
FIGURE 3 in Genetic differentiation through dispersal and isolation in two freshwater fish species from coastal basins of Northeastern Brazil
FIGURE 3 | Distribution and haplotype structure of Prochilodus lacustris. A. Paleodrainage reconstruction of coastal basins from northeastern Brazil and geographic distribution of groups defined by SAMOVA. B. Estimate of the probable groups of populations produced by the BAPS. C. Haplotypes networks of mtDNA control region. All analysis recovered a total of six groups in this area, but the SAMOVA do not identify the same groups that other analysis. The colors used to highlight areas in the network correspond to populations in map.
Fig. 2 in A report of 22 unrecorded bacterial species in Korea, isolated from the North Han River basin in 2017
Fig. 2. Transmission electron micrographs of cells of the strains isolated in the study. Strains: 1, IMCC34522 (0.5 μm); 2, IMCC34590 (0.2 μm); 3, IMCC34630 (0.2 μm); 4, IMCC34661 (0.2 μm); 5, IMCC34666 (0.5 μm); 6, IMCC34578 (0.5 μm); 7, IMCC34610 (0.5 μm); 8, IMCC34605 (1.0 μm); 9, IMCC34726 (0.2 μm); 10, IMCC34658 (0.5 μm); 11, IMCC34655 (0.5 μm); 12, IMCC34711 (0.2 μm); 13, IMCC34728 (0.5 μm); 14, IMCC34689 (0.2 μm); 15, IMCC34713 (0.2 μm); 16, IMCC34644 (0.2 μm); 17, IMCC34656 (0.2 μm); 18, IMCC34688 (0.5 μm); 19, IMCC34510 (0.5 μm); 20, IMCC34659 (0.5 μm); 21, IMCC34607 (0.2 μm); 22, IMCC34525 (0.5 μm). Scale bars are indicated in parenthesis after strain ID.
Text-fig. 2. Condylopyge cf. rex (BARRANDE, 1846), middle Cambrian, latest Cambrian Stage 5 and lower Drumian, Jince Formation, Příbram-Jince Basin. a. internal mould of isolated cephalon (Specimen CGS CW 17), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. b. latex cast of external mould of isolated pygidium (Specimen CGS FK 63), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. c. internal mould of isolated cephalon (Specimen CGS CW 18), foot of the slope known as Vinice near Jince (locality 20 in Fatka and Kordule 1992) in lower levels of the Onymagnostus hybridus Zone. Condylopyge rex (BARRANDE, 1846), middle Cambrian, lower Drumian, Buchava Formation, Paradoxides (Eccaparadoxides) pusillus Zone, Skryje-Týřovice Basin. d. internal mould of isolated cephalon (NM-L43011a), Karáskovská rokle - nad chatami. e. internal mould of isolated pygidium (NM-L43014), Lůmek u Týřovic. f. internal mould of isolated cephalon (NM-L43013), Lůmek u Týřovic. Whitened with ammonium chloride sublimate. All scale bars are 1 mm. Photographs by Martin Valent (National Museum Prague). in Condylopyge Hawle Et Corda, 1847 In The Příbram-Jince Basin (Barrandian Area, The Czech Republic, Agnostida)
Text-fig. 2. Condylopyge cf. rex (BARRANDE, 1846), middle Cambrian, latest Cambrian Stage 5 and lower Drumian, Jince Formation, Příbram-Jince Basin. a. internal mould of isolated cephalon (Specimen CGS CW 17), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. b. latex cast of external mould of isolated pygidium (Specimen CGS FK 63), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. c. internal mould of isolated cephalon (Specimen CGS CW 18), foot of the slope known as Vinice near Jince (locality 20 in Fatka and Kordule 1992) in lower levels of the Onymagnostus hybridus Zone. Condylopyge rex (BARRANDE, 1846), middle Cambrian, lower Drumian, Buchava Formation, Paradoxides (Eccaparadoxides) pusillus Zone, Skryje-Týřovice Basin. d. internal mould of isolated cephalon (NM-L43011a), Karáskovská rokle - nad chatami. e. internal mould of isolated pygidium (NM-L43014), Lůmek u Týřovic. f. internal mould of isolated cephalon (NM-L43013), Lůmek u Týřovic. Whitened with ammonium chloride sublimate. All scale bars are 1 mm. Photographs by Martin Valent (National Museum Prague).
Text-fig. 2. A – First small excavation trench in the newly discovered fossiliferous outcrop area of the Ploužnice lake horizon, locality "Small Ravine" south of the village Ploužnice on the slope of road No. 286. Typical are the red, violet and varicoloured tuffaceous siltstones. Semily Formation, Late Stephanian, Krkonoše Piedmont Basin. B – Basal part of fossiliferous 12 cm to14 cm thick reddish to purple-red tuffaceous siltstone bed from the trench in Text-fig. 2A. Internal bedding is expressed as horizontal but with diffuse changes in grain size from fine silt to coarse, fine sandy silt. Intercalated in places are 3 to 5 mm thick layers (indicated by arrows) with patchy concentrations of isolated fish remains, especially in the first 3 centimetres of this siltstone layer. The large white spot at 2.5 cm is a coprolite fragment. in Fossil Fauna And Flora Of A Re-Discovered Locality In The Late Carboniferous Ploužnice Horizon Of The Krkonoše Piedmont Basin, Bohemian Massif
Text-fig. 2. A – First small excavation trench in the newly discovered fossiliferous outcrop area of the Ploužnice lake horizon, locality "Small Ravine" south of the village Ploužnice on the slope of road No. 286. Typical are the red, violet and varicoloured tuffaceous siltstones. Semily Formation, Late Stephanian, Krkonoše Piedmont Basin. B – Basal part of fossiliferous 12 cm to14 cm thick reddish to purple-red tuffaceous siltstone bed from the trench in Text-fig. 2A. Internal bedding is expressed as horizontal but with diffuse changes in grain size from fine silt to coarse, fine sandy silt. Intercalated in places are 3 to 5 mm thick layers (indicated by arrows) with patchy concentrations of isolated fish remains, especially in the first 3 centimetres of this siltstone layer. The large white spot at 2.5 cm is a coprolite fragment.
Text-fig. 4. Stutzeliastrobus bohemicus (BAYER) J.KVAČEK, Harcov. a – ovuliferous cone showing apical parts of bract-scale complexes, NM-F 4551, scale bar 10 mm, b – shoot with attached ovuliferous cone (Bayer 1914: fig. 21b; 1920: fig. 21b), NM-F 872, scale bar 1 mm, c – SEM of isolated shoot, NM-F 2840, scale bar 0.5 mm, d – LM of abaxial cuticle and hypodermis, NM-F 872b, scale bar 200 µm, e – LM of abaxial cuticle showing two stomatal bands (arrows) and hypodermis, NM-F 872b, scale bar 100 µm, f – LM of abaxial cuticle, detail of e showing stomata (arrows), NM-F 872b, scale bar 50 µm. in Stutzeliastrobus Bohemicus Comb. Nov. - Basal Cupressaceae Conifer From The Cenomanian Of The Bohemian Cretaceous Basin, Central Europe
Text-fig. 4. Stutzeliastrobus bohemicus (BAYER) J.KVAČEK, Harcov. a – ovuliferous cone showing apical parts of bract-scale complexes, NM-F 4551, scale bar 10 mm, b – shoot with attached ovuliferous cone (Bayer 1914: fig. 21b; 1920: fig. 21b), NM-F 872, scale bar 1 mm, c – SEM of isolated shoot, NM-F 2840, scale bar 0.5 mm, d – LM of abaxial cuticle and hypodermis, NM-F 872b, scale bar 200 µm, e – LM of abaxial cuticle showing two stomatal bands (arrows) and hypodermis, NM-F 872b, scale bar 100 µm, f – LM of abaxial cuticle, detail of e showing stomata (arrows), NM-F 872b, scale bar 50 µm.
Text-fig. 3. Stutzeliastrobus bohemicus (BAYER) J.KVAČEK, Harcov. a – surface view of bract-scale complex (arrow) and probably aborted seed, No. NM-F 2746 (lectotype), scale bar 1 mm, b – seed with a wing (arrow) NM-F 872, scale bar 1 mm, c – microCT perpendicular section of bract scale complex showing two seeds with wings (arrows), No. NM-F 2746 (lectotype), scale bar 1 mm, d – microCT longitudinal section of bract scale complex showing three seeds, No. NM-F 2746 (lectotype), scale bar 1 mm, e – microCT longitudinal section of bract scale complex with one seed reconstructed showing micropyle (arrow), No. NM-F 2746 (lectotype), scale bar 1 mm, f – isolated seed with a fragment of wing (arrow), No. NM-F 2746 (lectotype), scale bar 1 mm. in Stutzeliastrobus Bohemicus Comb. Nov. - Basal Cupressaceae Conifer From The Cenomanian Of The Bohemian Cretaceous Basin, Central Europe
Text-fig. 3. Stutzeliastrobus bohemicus (BAYER) J.KVAČEK, Harcov. a – surface view of bract-scale complex (arrow) and probably aborted seed, No. NM-F 2746 (lectotype), scale bar 1 mm, b – seed with a wing (arrow) NM-F 872, scale bar 1 mm, c – microCT perpendicular section of bract scale complex showing two seeds with wings (arrows), No. NM-F 2746 (lectotype), scale bar 1 mm, d – microCT longitudinal section of bract scale complex showing three seeds, No. NM-F 2746 (lectotype), scale bar 1 mm, e – microCT longitudinal section of bract scale complex with one seed reconstructed showing micropyle (arrow), No. NM-F 2746 (lectotype), scale bar 1 mm, f – isolated seed with a fragment of wing (arrow), No. NM-F 2746 (lectotype), scale bar 1 mm.
Data from: Dusky grouse seasonal resource selection in the Great Basin isolated mountain ranges of Nevada, USA
Open the record for dataset details and reuse information.
Data from: Examination of a historic collection of isolated cranial and appendicular hadrosaurid material from the lower Kirtland Formation of the San Juan Basin, New Mexico
The Field Museum of Natural History collection contains several isolated hadrosaurid specimens collected by Charles H. Sternberg from the lower Kirtland Formation of the San Juan Basin, New Mexico, that have been previously overlooked. Cranial elements described herein consist of a dentary and three jugals while appendicular material is limited to two humeri and two pubes. Many of the specimens preserve taxonomically informative characters that show strong affinities with Kritosaurini but are distinct from Kritosaurus navajovius (Brown, 1910) suggesting that the saurolophine-dominated San Juan Basin diversity is greater than currently recognized. Future examination of currently unprepared material will add to our developing understanding of the ambiguous hadrosaurid diversity of the San Juan Basin.
Distribution. Discontinuous and limited to wetland environments in the Congo Basin N and W of the range of the Zambezi Sitatunga in S Benin (Porto Novo), S Nigeria, Cameroon, Central African Republic, Equatorial Guinea, Gabon, Republic of the Congo, N DR Congo; also several isolated populations in W Africa (Senegal, Gambia & Guinea-Bissau), NE Nigeria and W Chad, and perhaps extreme S Ghana. Maps and distributional information here are provisional pending future research. in Bovidae
Distribution. Discontinuous and limited to wetland environments in the Congo Basin N and W of the range of the Zambezi Sitatunga in S Benin (Porto Novo), S Nigeria, Cameroon, Central African Republic, Equatorial Guinea, Gabon, Republic of the Congo, N DR Congo; also several isolated populations in W Africa (Senegal, Gambia & Guinea-Bissau), NE Nigeria and W Chad, and perhaps extreme S Ghana. Maps and distributional information here are provisional pending future research.
Subspecies and Distribution. L. c. cana E. Geoffroy Saint-Hilaire, 1812 — Brazilian Amazon, S of the Rio Amazonas-Solimoes, between the rios Jurua and Tapajos-Juruena, but restricted to the left bank of the Rio Madeira above the mouth of the Rio Jiparana (a right bank tributary), and to the right bank of the Rio Jiparana, S to ¢.12° S, and W along the N (left bank) of the Rio Abuna on the upper Rio Madeira. L. c. tschudii Pucheran, 1857 — SE Peru, its range is poorly known butis believed to extend between the rios Pachitea and Ucayali, S from the Rio Inuya, W as far as the Rio Inambari, and S to both sides of the Rio Madre de Dios into the Rio Tambopata Basin, to the frontier with Bolivia, with an isolated population in Madidi National Park. in Atelidae
Subspecies and Distribution. L. c. cana E. Geoffroy Saint-Hilaire, 1812 — Brazilian Amazon, S of the Rio Amazonas-Solimoes, between the rios Jurua and Tapajos-Juruena, but restricted to the left bank of the Rio Madeira above the mouth of the Rio Jiparana (a right bank tributary), and to the right bank of the Rio Jiparana, S to ¢.12° S, and W along the N (left bank) of the Rio Abuna on the upper Rio Madeira. L. c. tschudii Pucheran, 1857 — SE Peru, its range is poorly known butis believed to extend between the rios Pachitea and Ucayali, S from the Rio Inuya, W as far as the Rio Inambari, and S to both sides of the Rio Madre de Dios into the Rio Tambopata Basin, to the frontier with Bolivia, with an isolated population in Madidi National Park.
Subspecies and Distribution. R.m.minutillaG.S.Miller,1897—GuajiraPeninsulaofColombiaandVenezuelaStoCaquetaandCaucadepartmentsinWColombia,andelsewhereinVenezuelaNofMéridaState,includingMargaritaI. R. m. cautiva Soriano, Naranjo & Farinas, 2004 — isolated population in xeric intermontane basin of rivers Chama and Nuestra Senora, Mérida State, NW Venezuela. in Vespertilionidae
Subspecies and Distribution. R.m.minutillaG.S.Miller,1897—GuajiraPeninsulaofColombiaandVenezuelaStoCaquetaandCaucadepartmentsinWColombia,andelsewhereinVenezuelaNofMéridaState,includingMargaritaI. R. m. cautiva Soriano, Naranjo & Farinas, 2004 — isolated population in xeric intermontane basin of rivers Chama and Nuestra Senora, Mérida State, NW Venezuela.
Distribution. Central America from Honduras to Panama and along coasts of W Colombia and NW Ecuador. In the literature, there have been two isolated records in the Amazonian Basin, including one in SE Peru, and one in Brazil that probably are misidentifications. in Phyllostomidae
Distribution. Central America from Honduras to Panama and along coasts of W Colombia and NW Ecuador. In the literature, there have been two isolated records in the Amazonian Basin, including one in SE Peru, and one in Brazil that probably are misidentifications.
Distribution. Discontinuous and limited to wetland environments in the Congo Basin N and W of the range of the Zambezi Sitatunga in S Benin (Porto Novo), S Nigeria, Cameroon, Central African Republic, Equatorial Guinea, Gabon, Republic of the Congo, N DR Congo; also several isolated populations in W Africa (Senegal, Gambia & Guinea-Bissau), NE Nigeria and W Chad, and perhaps extreme S Ghana. Maps and distributional information here are provisional pending future research. in Bovidae
Distribution. Discontinuous and limited to wetland environments in the Congo Basin N and W of the range of the Zambezi Sitatunga in S Benin (Porto Novo), S Nigeria, Cameroon, Central African Republic, Equatorial Guinea, Gabon, Republic of the Congo, N DR Congo; also several isolated populations in W Africa (Senegal, Gambia & Guinea-Bissau), NE Nigeria and W Chad, and perhaps extreme S Ghana. Maps and distributional information here are provisional pending future research.
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