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212 results for “Fossil localities”
Fig. 1 in Description of the Earliest Fossil Penguin from South America and First Paleogene Vertebrate Locality of Tierra Del Fuego, Argentina
Fig. 1. Simplified geologic map of central and eastern Isla Grande, Tierra del Fuego, showing outcrops of Upper Cretaceous to Miocene synorogenic clastic wedges. The area of the penguin locality, at Cabo Campo del Medio–Punta Torcida, is bounded by a rectangle and detailed in the map provided in figure 2.
Fig. 8 in Description of the Earliest Fossil Penguin from South America and First Paleogene Vertebrate Locality of Tierra Del Fuego, Argentina
Fig. 8. The distal tibiotarsus of CADIC P 21 in anterior view. Anatomical abreviation: ot, ossified tendon.
Fig. 3 in Description of the Earliest Fossil Penguin from South America and First Paleogene Vertebrate Locality of Tierra Del Fuego, Argentina
Fig. 3. Correlation of sections and sedimentary facies of the lower and upper middle Eocene strata across the Cabo Campo del Medio–Punta Torcida anticline showing the complex geometry and variable thickness of the three main stratigraphic intervals of the Leticia Formation (adapted from Olivero and LópezCabrera, 2001). The penguin remains (CADIC P 21; indicated by a star) were recovered near the top of the midshelf sandstone interval of the Leticia Formation near Punta Torcida.
Text-fig. 1. Map of the Carboniferous-Permian non-marine basins of the Czech Republic; the star indicates roughly the position of the locality Ploužnice in the north-western part of the Krkonoše Piedmont Basin (according to Opluštil et al. 2016b). 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. 1. Map of the Carboniferous-Permian non-marine basins of the Czech Republic; the star indicates roughly the position of the locality Ploužnice in the north-western part of the Krkonoše Piedmont Basin (according to Opluštil et al. 2016b).
Text-fig. 2. Field photograph of the sampling locality, together with a schematic profile. Stratigraphic horizon from which the fossil wood fragment was extracted (white arrow) (Modified from Pires and Da Rosa 2000). in A New Fossil Fabaceae Wood From The Pleistocene Touro Passo Formation Of Rio Grande Do Sul, Brazil
Text-fig. 2. Field photograph of the sampling locality, together with a schematic profile. Stratigraphic horizon from which the fossil wood fragment was extracted (white arrow) (Modified from Pires and Da Rosa 2000).
Text-fig. 1. Map of westernmost part of Rio Grande do Sul showing the position of the sampling locality (star). Adapted from Oliveira and Kerber (2009). in A New Fossil Fabaceae Wood From The Pleistocene Touro Passo Formation Of Rio Grande Do Sul, Brazil
Text-fig. 1. Map of westernmost part of Rio Grande do Sul showing the position of the sampling locality (star). Adapted from Oliveira and Kerber (2009).
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. 7. Fossil urodelans from studied localities. a, b – Mioproteus caucasicus, trunk vertebra, dorsal (a) and lateral (b) views; c, d – Chelotriton paradoxus, trunk vertebra, dorsal (c) and lateral (d) view. Scale bar 1 mm. in Late Miocene (Early Turolian) Vertebrate Faunas And Associated Biotic Record Of The Northern Caucasus: Geology, Taxonomy, Palaeoenvironment, Biochronology
Text-fig. 7. Fossil urodelans from studied localities. a, b – Mioproteus caucasicus, trunk vertebra, dorsal (a) and lateral (b) views; c, d – Chelotriton paradoxus, trunk vertebra, dorsal (c) and lateral (d) view. Scale bar 1 mm.
Text-fig. 21. Palaeogene fossil mammal localities of Africa and the Arabian Peninsula, highlighting the distribution of Omanitherium and other numidotheres and barytheres. in Large Mammals From The Rupelian Of Oman - Recent Finds
Text-fig. 21. Palaeogene fossil mammal localities of Africa and the Arabian Peninsula, highlighting the distribution of Omanitherium and other numidotheres and barytheres.
Text-fig. 8. Plant fossils from Primorye, Partizansk coal basin, Frentsevka Formation, Bolshoy Kuvshin locality, early – middle Albian. a – undetermined species, spec. IBSS 320-137; b, c – Asiatifolium elegans G.SUN, S.X.GUO et SHAO L.ZHENG: b – spec. IBSS 320-86, c – spec. IBSS 320-8. Scale bar 0.5 cm. in An Angiosperm Dominated Herbaceous Community From The Early - Middle Albian Of Primorye, Far East Of Russia
Text-fig. 8. Plant fossils from Primorye, Partizansk coal basin, Frentsevka Formation, Bolshoy Kuvshin locality, early – middle Albian. a – undetermined species, spec. IBSS 320-137; b, c – Asiatifolium elegans G.SUN, S.X.GUO et SHAO L.ZHENG: b – spec. IBSS 320-86, c – spec. IBSS 320-8. Scale bar 0.5 cm.
Text-fig. 9. Plant fossils from Primorye, Partizansk coal basin, Frentsevka Formation, Bolshoy Kuvshin locality, early – middle Albian. a, b – Ternaricarpites floribundus KRASSILOV et VOLYNETS: a – spec. IBSS 320-10, b – spec. IBSS 320-31; c – Jixia pinnatipartita S.X.GUO et G.SUN, spec. IBSS 320-57. Scale bar 0.5 cm. in An Angiosperm Dominated Herbaceous Community From The Early - Middle Albian Of Primorye, Far East Of Russia
Text-fig. 9. Plant fossils from Primorye, Partizansk coal basin, Frentsevka Formation, Bolshoy Kuvshin locality, early – middle Albian. a, b – Ternaricarpites floribundus KRASSILOV et VOLYNETS: a – spec. IBSS 320-10, b – spec. IBSS 320-31; c – Jixia pinnatipartita S.X.GUO et G.SUN, spec. IBSS 320-57. Scale bar 0.5 cm.
Text-fig. 7. Plant fossils from Primorye, Partizansk coal basin, Frentsevka Formation, Bolshoy Kuvshin locality, early – middle Albian. a, c, e – Achaenocarpites capitellatus KRASSILOV et VOLYNETS: a – spec. IBSS 320-132, c – spec. IBSS 320-132, e – spec. IBSS 320-120; b – Onychiopsis psilotoides (STOKES et WEBB) WARD, spec. – IBSS 320-165; d, g – branching infructescence with several follicular fruits: d – spec. IBSS 320-145, g – IBSS 320-145; f – Asiatifolium elegans G.SUN, S.X.GUO et SHAO L.ZHENG, spec. IBSS 320-75. Scale bar 0.5 cm. in An Angiosperm Dominated Herbaceous Community From The Early - Middle Albian Of Primorye, Far East Of Russia
Text-fig. 7. Plant fossils from Primorye, Partizansk coal basin, Frentsevka Formation, Bolshoy Kuvshin locality, early – middle Albian. a, c, e – Achaenocarpites capitellatus KRASSILOV et VOLYNETS: a – spec. IBSS 320-132, c – spec. IBSS 320-132, e – spec. IBSS 320-120; b – Onychiopsis psilotoides (STOKES et WEBB) WARD, spec. – IBSS 320-165; d, g – branching infructescence with several follicular fruits: d – spec. IBSS 320-145, g – IBSS 320-145; f – Asiatifolium elegans G.SUN, S.X.GUO et SHAO L.ZHENG, spec. IBSS 320-75. Scale bar 0.5 cm.
Text-fig. 7. Molars referred to Karnimata fejfari sp. nov. from type locality Y 311. Right M2, a) YGSP 34588 and b) 54187, buccal upward. Lower teeth c) YGSP 34528 and d) 36166 both left m1, and e) 36170 and f) 54176, left and right m2; c–f figured lingual side upward. All teeth same scale. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 7. Molars referred to Karnimata fejfari sp. nov. from type locality Y 311. Right M2, a) YGSP 34588 and b) 54187, buccal upward. Lower teeth c) YGSP 34528 and d) 36166 both left m1, and e) 36170 and f) 54176, left and right m2; c–f figured lingual side upward. All teeth same scale.
Text-fig. 2. First upper molar variation in Progonomys husssaini from three localities in the upper part of the Nagri Formation, Potwar Plateau, Pakistan. The 12 molars are oriented with buccal side upward, each at the same 1 mm scale, making size variation apparent. a) YGSP 33187 from locality Y 450; b) 34556, c) 54131, d) 54143, e) 54151, f) 54152, all from Y 311; g) 33937, h) 33947, i) 33957, j) 33959, k) 33963, l) 33976 all from Y 259. Figures a, c, e, f, h, k are all right M1; the others are left M1. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 2. First upper molar variation in Progonomys husssaini from three localities in the upper part of the Nagri Formation, Potwar Plateau, Pakistan. The 12 molars are oriented with buccal side upward, each at the same 1 mm scale, making size variation apparent. a) YGSP 33187 from locality Y 450; b) 34556, c) 54131, d) 54143, e) 54151, f) 54152, all from Y 311; g) 33937, h) 33947, i) 33957, j) 33959, k) 33963, l) 33976 all from Y 259. Figures a, c, e, f, h, k are all right M1; the others are left M1.
Text-fig. 10. List of Siwalik murine rodents. a) Stratigraphic occurrence of fossil localities of the Potwar Plateau, Pakistan. b) Murine species recovered from the Siwaliks, updated from Kimura et al. (2015). All localities but DP 13 have Y as prefix. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 10. List of Siwalik murine rodents. a) Stratigraphic occurrence of fossil localities of the Potwar Plateau, Pakistan. b) Murine species recovered from the Siwaliks, updated from Kimura et al. (2015). All localities but DP 13 have Y as prefix.
Text-fig. 9. First upper molars of Parapodemus badgleyae sp. nov. (a–d) and Muridae, gen. et sp. indet. (e). a) YGSP 33936, holotype, locality Y 259, b) 33939 from Y 259, c) 34542 from Y 311, d) 34543 from Y 311, e) 34559 from Y 311. All molars but c are left molars, all figured with buccal side upward and at the same scale. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 9. First upper molars of Parapodemus badgleyae sp. nov. (a–d) and Muridae, gen. et sp. indet. (e). a) YGSP 33936, holotype, locality Y 259, b) 33939 from Y 259, c) 34542 from Y 311, d) 34543 from Y 311, e) 34559 from Y 311. All molars but c are left molars, all figured with buccal side upward and at the same scale.
Text-fig. 4. First upper molars of Karnimata fejfari sp. nov. from type locality Y 311, all figured with buccal side upward. a) YGSP 34551, b) 34544, c) 34546 holotype, d) 34548, e) 34540, f) 34547, g) 34554, h) 36162, i) 54126, j) 54127, k) 54147, l) 54153. All at same 1 mm scale, all left M1 except for right h and l. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 4. First upper molars of Karnimata fejfari sp. nov. from type locality Y 311, all figured with buccal side upward. a) YGSP 34551, b) 34544, c) 34546 holotype, d) 34548, e) 34540, f) 34547, g) 34554, h) 36162, i) 54126, j) 54127, k) 54147, l) 54153. All at same 1 mm scale, all left M1 except for right h and l.
Text-fig. 5. First upper molars of Karnimata fejfari sp. nov. from localities Y 450 (a–d) and Y 259 (e–l). a) YGSP 33181, b) 33182, c) 33185, d) 33186, e) 33945, f) 33940, g) 33948, h) 33958, i) 33960, j) 33946, k) 33967, l) 33973. Figured at same scale, buccal upward, all right M1 except for left f, g, j, l. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 5. First upper molars of Karnimata fejfari sp. nov. from localities Y 450 (a–d) and Y 259 (e–l). a) YGSP 33181, b) 33182, c) 33185, d) 33186, e) 33945, f) 33940, g) 33948, h) 33958, i) 33960, j) 33946, k) 33967, l) 33973. Figured at same scale, buccal upward, all right M1 except for left f, g, j, l.
Text-fig. 6. Scatter diagram of length and width of M1 specimens in Progonomys hussaini and Karnimata fejfari from localities Y 259, 450, 311. The solid line ellipse is a 55% concentration ellipse for P. hussaini, and the dashed ellipse is a 55% concentration ellipse for Karnimata fejfari, all specimens combined. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 6. Scatter diagram of length and width of M1 specimens in Progonomys hussaini and Karnimata fejfari from localities Y 259, 450, 311. The solid line ellipse is a 55% concentration ellipse for P. hussaini, and the dashed ellipse is a 55% concentration ellipse for Karnimata fejfari, all specimens combined.
Text-fig. 3. Scatter diagram of mean L/W values of selected Spermophilinus upper first molars (M1 and M2) from Switzerland and south Germany. The crosses correspond to the minimum and maximum values of the length and width. The intersection gives the value of the mean. Comparative data are after Ziegler and Fahlbusch (1986), Bolliger (1992), Kälin (1993), Ziegler (1995, 2005), Kälin and Engesser (2001), Prieto (2007), Prieto et al. (2009, 2017), Seehuber (2009). Blue: localities younger than ~14 Ma (S. bredai); Green: localities ranging from ~14 Ma to ~15Ma (S. bredai); Red: localities ranging from ~15 Ma to ~16 Ma (S. besana); Yellow: older localities (most S. besana). in Dental Anomaly In A Middle Miocene Fossil Of The Genus Spermophilinus (Rodentia, Sciuridae) From Southern Germany
Text-fig. 3. Scatter diagram of mean L/W values of selected Spermophilinus upper first molars (M1 and M2) from Switzerland and south Germany. The crosses correspond to the minimum and maximum values of the length and width. The intersection gives the value of the mean. Comparative data are after Ziegler and Fahlbusch (1986), Bolliger (1992), Kälin (1993), Ziegler (1995, 2005), Kälin and Engesser (2001), Prieto (2007), Prieto et al. (2009, 2017), Seehuber (2009). Blue: localities younger than ~14 Ma (S. bredai); Green: localities ranging from ~14 Ma to ~15Ma (S. bredai); Red: localities ranging from ~15 Ma to ~16 Ma (S. besana); Yellow: older localities (most S. besana).
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