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FIGURE 4 in Late Miocene molluscs of the Morskaya 2 site (Azov Sea region, Russia)

FIGURE 4. Assemblage of the Middle Sarmatian (Bessarabian) marine gastropods (layers 1 and 2). 1, Acteocina lajonkaireana (Basterot, 1825). 2, Acteocina okeni (Eichwald, 1850). 3, Retusa melitopolitana (Sokolov, 1899). 4, Hydrobia elongata Eichwald, 1830. 5, Pseudamnicola nympha (Eichwald, 1850). 6, Dorsanum duplicata opinabile (Kolesnikov, 1932). 7, Dorsanum corbiana (d'Orbigny, 1844). 8, Dorsanum ignobile (Kolesnikov, 1932). 9, Gibbula (Gibbula) pseudoangulata (Sinzov, 1875). 10, Gibbula (Sarmatigibbula) podolica (Du Bois de Montpéreux, 1831).

opencc-by-4.0Dec 2018View details →
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Figure 2. Physeteroidea indet., MNUL.Pal.100.755a in An unfamiliar physeteroid periotic (Cetacea: Odontoceti) from the German middle-late Miocene North Sea basin at Gross Pampau

Figure 2. Physeteroidea indet., MNUL.Pal.100.755a, fragment of the right tympanic bulla from the upper Langenfeldian (Serravallian– Tortonian boundary) of Gross Pampau. (a) Lateral, (b) medial, (c) dorsal, and (d) ventral view.

opencc-by-4.0Aug 2020View details →
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Figure 4. Physeteroidea indet., MNUL.Pal.100.755a in An unfamiliar physeteroid periotic (Cetacea: Odontoceti) from the German middle-late Miocene North Sea basin at Gross Pampau

Figure 4. Physeteroidea indet., MNUL.Pal.100.755a, measurements of the periotic bone applied in this paper (see Table 1). (a, b) Ventral, (c) medial, (d, e) dorsal, (f) lateral, and (g) posterior view.

opencc-by-4.0Aug 2020View details →
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Figure 1 in An unfamiliar physeteroid periotic (Cetacea: Odontoceti) from the German middle-late Miocene North Sea basin at Gross Pampau

Figure 1. Map of the Kieswerke Ohle & Lau company gravel pit. The dots represent significant marine mammal findings that are already published, currently being studied or were mentioned in local media after discovery. (1) Mysticete, found 1984, partial skeleton. (2) Kentriodon hoepfneri KazAEr and Hampe, 2014, found in two parts in 1984 and 1989, partial skeleton with nearly complete vertebral column. (3) Praemegaptera pampauensis Behrmann, 1995, found 1989, nearly complete specimen. (4) Praemegaptera pampauensis, found 1993, partial skeleton. (5) Hoplocetus ritzi Hampe, 2006; found 1997; teeth, vertebrae, and bone fragments from a single dislocated skeleton. (6) Kentriodon hoepfneri, found 2000, partial skeleton. (7) Mysticete, found 2012, partial skeleton. (8) Physeteroidea indet., this paper, found 2014, right periotic accompanied by diverse isolated bone fragments. (9) Mysticete, found 2016, partial skeleton. (10) Otariid pinniped; found 2016; ± complete hind limb, bone fragments, teeth. (11) Ziphiidae indet., found 2017, skull. (12) Mysticete, found 2019, partial skeleton. Extract of the "DigitalerAtlasNord" (ETRS89/UTM zone 32N), State Office for Surveying and Geoinformation of SchleswigHolstein (LVermGeo SH).

opencc-by-4.0Aug 2020View details →
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Figure 3. Physeteroidea indet., MNUL.Pal.100.755a in An unfamiliar physeteroid periotic (Cetacea: Odontoceti) from the German middle-late Miocene North Sea basin at Gross Pampau

Figure 3. Physeteroidea indet., MNUL.Pal.100.755a, right periotic from the upper Langenfeldian (Serravallian–Tortonian boundary) of Gross Pampau. (a, b) Dorsal, (c) medial, (d) lateral, (e, f) ventral, (g) anterior, and (h) posterior view.

opencc-by-4.0Aug 2020View details →
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Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011). in Feather Palm Foliage From The Messinian Of Italy (Capo Di Fiume, Palena And Pollenzo Near Alba) Within The Framework Of Northern Mediterranean Late Miocene Flora

Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011).

opencc-by-4.0Dec 2015View details →
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Text-fig. 11. Geological map south of the Nel'ma Bay. 1 - granodiorite (Early Palaeogene); 2 – Eocene andesitic and dacitic tuff with plant-bearing argillitic lenses; 3 – Late Eocene to Early Miocene andesite-basalt (Kizi Volcanic Group); 4 – tuffogenous sedimentary plant-bearing lenses with plant fossils; 5 – Dacite neck (Early Oligocene) 1 km south of the Dembi Bay; 6 – Pliocene pebbles and conglomerates; 7 – Plateaubasalts (Sovgavan' Formation, Late Neogene–Quaternary); 8 – Quaternary alluvial deposits; 9 – localities with fossil plants: a – Sonje, b – Bui, c – Dembi. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)

Text-fig. 11. Geological map south of the Nel'ma Bay. 1 - granodiorite (Early Palaeogene); 2 – Eocene andesitic and dacitic tuff with plant-bearing argillitic lenses; 3 – Late Eocene to Early Miocene andesite-basalt (Kizi Volcanic Group); 4 – tuffogenous sedimentary plant-bearing lenses with plant fossils; 5 – Dacite neck (Early Oligocene) 1 km south of the Dembi Bay; 6 – Pliocene pebbles and conglomerates; 7 – Plateaubasalts (Sovgavan' Formation, Late Neogene–Quaternary); 8 – Quaternary alluvial deposits; 9 – localities with fossil plants: a – Sonje, b – Bui, c – Dembi.

opencc-by-4.0Nov 2009View details →
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Text-fig. 2. Main geological structures of the eastern slope of the Sikhote-Alin' ridge and main plant-bearing localities of the Cenozoic floras. I – Mesozoic folded basement; II – East Sikhote-Alin' Volcanic Belt (Late Cretaceous–Early Palaeocene); III – Near-Shore Basaltic Volcanic Belt (Eocene–Early Miocene); IV – Udyl Basin (Cenozoic); V – Late Neogene to Quaternary plateaubasalts; Va – Sovgavan plateau; Vb – Samarga plateau; Vc – Bikin plateau. 1 – Malo-Mikhaylovka; 2 – Siziman; 3 – Sjurkum; 4 – Botchi; 5 – Dembi; 6 – Bui; 7 – Sonje; 8 – Takhobe; 9 – Amgu; 10 – Velikaya Kema; 11 – Zerkal'naya (former Tadushi). in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)

Text-fig. 2. Main geological structures of the eastern slope of the Sikhote-Alin' ridge and main plant-bearing localities of the Cenozoic floras. I – Mesozoic folded basement; II – East Sikhote-Alin' Volcanic Belt (Late Cretaceous–Early Palaeocene); III – Near-Shore Basaltic Volcanic Belt (Eocene–Early Miocene); IV – Udyl Basin (Cenozoic); V – Late Neogene to Quaternary plateaubasalts; Va – Sovgavan plateau; Vb – Samarga plateau; Vc – Bikin plateau. 1 – Malo-Mikhaylovka; 2 – Siziman; 3 – Sjurkum; 4 – Botchi; 5 – Dembi; 6 – Bui; 7 – Sonje; 8 – Takhobe; 9 – Amgu; 10 – Velikaya Kema; 11 – Zerkal'naya (former Tadushi).

opencc-by-4.0Nov 2009View details →
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Figure 10 in Carnivores from the Late Miocene locality of Hayranlı (Hayranlı, Sivas, Turkey)

Figure 10. Machairodus giganteus (Wagner, 1848). Metatarsal III 58-HAY-91/5, 4a; Metatarsal II 58-HAY-91/8, 4b; Astragalus 58 HAY-91/7, 4c; Ictitherium sp., canine 58-HAY-2/132, 5a; canine 58-HAY-2/138, 5b; canine 58-HAY-2/53, 5c; Carnivora, canine 58-HAY-91/33, 5d; canine 58-HAY-2/130, 5e; and part of isolated m1 58- HAY-2/252, 5f.

opencc-by-4.0Mar 2015View details →
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Figure 6 in Carnivores from the Late Miocene locality of Hayranlı (Hayranlı, Sivas, Turkey)

Figure 6. Comparison of the mandibular dimensions of Hyaenictitherium wongii from Hayranlı-Sivas and various localities. 25 Mand bula (r ght); c, p1-p3

opencc-by-4.0Mar 2015View details →
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Figure 5 in Carnivores from the Late Miocene locality of Hayranlı (Hayranlı, Sivas, Turkey)

Figure 5. Comparison of the upper tooth measurements of Hyaenictitherium wongii from Hayranlı-Sivas and various localities.

opencc-by-4.0Mar 2015View details →
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Figure 2 in Carnivores from the Late Miocene locality of Hayranlı (Hayranlı, Sivas, Turkey)

Figure 2. Hyaenictitherium wongii from Hayranlı-Sivas (Zdansky, 1924). Skull 58-HAY- 1996 Sivas Yüzey, 1a. dorsal, 1b. occlusal; maxilla 58-HAY-2/187, 2. occlusal, mandible; 58-HAY-2/51, 3. lateral, mandible; 58-HAY-2/243, 4. buccal, mandible; 58-HAY-2/223, 5. buccal, mandible; and 58-HAY-2/102, 6. lingual.

opencc-by-4.0Mar 2015View details →
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Figure 9 in Carnivores from the Late Miocene locality of Hayranlı (Hayranlı, Sivas, Turkey)

Figure 9. Comparison of the upper tooth measurements of H. intuberculatum from Hayranlı-Sivas and various localities.

opencc-by-4.0Mar 2015View details →
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Figure 8. Hyaenictitherium intuberculatum Ozansoy, 1965 in Carnivores from the Late Miocene locality of Hayranlı (Hayranlı, Sivas, Turkey)

Figure 8. Hyaenictitherium intuberculatum Ozansoy, 1965, from Hayranlı-Sivas, maxilla 58-HAY-2/222, 2a. lateral, 2b. occlusal; maxilla 58-HAY-2/75, 2c. lateral; maxilla 58-HAY-2/168, 2d. occlusal; maxilla 58-HAY- 2/101, 2e. occlusal; maxilla 58-HAY-2/57: 2f. lateral; Lycyaena dubia Zdansky, 1924, from Hayranlı-Sivas, maxilla 58-HAY-2/151, 3a. lateral, 3b. occlusal; and maxilla 58-HAY-2/152, 3c. lateral.

opencc-by-4.0Mar 2015View details →
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Figure 11. Carnivora Bowditch, 1821 in Carnivores from the Late Miocene locality of Hayranlı (Hayranlı, Sivas, Turkey)

Figure 11. Carnivora Bowditch, 1821. Distal part of the humerus 58-HAY-2/55, 6; distal phalanx 58-HAY-2/244, 7; and medial phalanx 58-HAY-2/54, 8.

opencc-by-4.0Mar 2015View details →
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Fig. 10 in Hipparion macedonicum revisited: New data on evolution of hipparionine horses from the Late Miocene of Greece

Fig. 10. Body mass of Hipparion macedonicum from the various Greek localities calculated by various methods and its change in relation to the time. The body mass is estimated using the metapodials (Eisenmann and Sondaar 1998); W1. ln(body mass) = -5,768+3.011 x (lnMc10); W2. ln(body mass) = 3.151+2.665 x (lnMc13); W3. ln(body mass) = -4.525+1.434 x (ln(Mc10 x Mc13)); W4. ln(body mass) = -4.362+2.634 x (lnMt10); W5. ln(body mass) = -4.552+3.100 x (lnMt13); W6. ln(body mass) = -4.585+1.443 x (ln(Mt10 x Mt13)).

opencc-by-4.0Jun 2015View details →
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Fig. 8 in Hipparion macedonicum revisited: New data on evolution of hipparionine horses from the Late Miocene of Greece

Fig. 8. Logarithmic ratio diagram comparing the RPl skull (A) and third metatarsal (B) with the Vallesian hipparions from Sinap, Turkey. Hipparion mediterraneum from Pikermi (Koufos 1987a) is used as standard of comparison. The metrical data for the Sinap material were provided to me by Raymond L. Bernor (unpublished material, personal communication, 2007).

opencc-by-4.0Jun 2015View details →
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Fig.12 in Hipparion macedonicum revisited: New data on evolution of hipparionine horses from the Late Miocene of Greece

Fig.12. Plication number of the upper cheek teeth of Hipparion macedonicum from the various Greek localities.

opencc-by-4.0Jun 2015View details →
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Fig. 9 in Hipparion macedonicum revisited: New data on evolution of hipparionine horses from the Late Miocene of Greece

Fig. 9. Stratigraphic table indicating the distribution of Hipparion macedonicum in Europe. The geomagnetic time scale is from Cande and Kent (1995). The shaded area in the MN zones express the different opinions for the MN 12/13 boundary; according to Sen (1997) it is at ~7.0 Ma while according to Steininger et al. (1999) it is at ~6.6 Ma.

opencc-by-4.0Jun 2015View details →
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Fig. 7 in Hipparion macedonicum revisited: New data on evolution of hipparionine horses from the Late Miocene of Greece

Fig. 7. Logarithmic ratio diagram comparing the RPl third metatarsal with Hipparion macedonicum and other small-sized hipparions from various localities. Hipparion mediterraneum from Pikermi (Koufos 1987a) is used as standard of comparison. The metrical data for the hipparions from Greek localities and AKK are from my own archive; those for Hipparion moldavicum from TAR and Hipparion elegans from PAV are taken from http://www. vera-eisenmann.com.

opencc-by-4.0Jun 2015View details →

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Last verified 2026-04-29Open record