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144 results for “Piedmont”
FIGURE 2 in Riparian and valley-margin hardwood species of pre-colonial Piedmont forests: A preliminary study of subfossil leaves from White Clay Creek, southeastern Pennsylvania, USA
FIGURE 2. White Clay Creek leaf mat site, illustrating the contact (at trowel) between the darker hydric soil layer containing subfossil leaves and the overlying, lighter-colored legacy sediments. Stadia rod for scale.
FIG. 2 in A Messinian (latest Miocene) occurrence for Albanerpeton Estes & Hoffstetter, 1976 (Lissamphibia: Albanerpetontidae) at Moncucco Torinese, Piedmont Basin, northwestern Italy, and a review of the European Cenozoic record for albanerpetontids
FIG. 2. — Stratigraphic section for the Miocene through Pliocene succession at Moncucco Torinese, Piedmont Basin, northwestern Italy. Arrows indicate the main biostratigraphic events and the Messinian-Zanclean (Miocene-Pliocene) boundary, all of which help constrain the age of the fossil-bearing interval within the Cassano Spinola Conglomerates. Numbered layers yielding isolated Albanerpeton Estes & Hoffstetter, 1976 bones are indicated by Albanerpeton silhouettes to the right of the stratigraphic log. Modified from Colombero et al. (2017: fig. 2); for details see Dela Pierre et al. (2007, 2011). Abbreviations for rock units exposed within the section (left side of stratigraphic logs) (from top-to-bottom): AAF, Argille Azzurre Formation; CSC, Cassano Spinola Conglomerates; VVC, Valle Versa chaotic complex; PLG, Primary Lower Gypsum; SAF, Sant'Agata Fossili Marls.
FIG. 1 in A Messinian (latest Miocene) occurrence for Albanerpeton Estes & Hoffstetter, 1976 (Lissamphibia: Albanerpetontidae) at Moncucco Torinese, Piedmont Basin, northwestern Italy, and a review of the European Cenozoic record for albanerpetontids
FIG. 1. — Location and setting of the uppermost Miocene Moncucco Torinese fossil locality: detail map (A) of northwestern Italy showing geographic setting and regional geology of the Tertiary age Piedmont Basin and regional map (B) showing locations of the three known albanerpetontid localities within Italy. Maps modified from Lozar et al. (2015: fig. 4) and Colombero et al. (2015: fig. 1).
FIG. 4 in A Messinian (latest Miocene) occurrence for Albanerpeton Estes & Hoffstetter, 1976 (Lissamphibia: Albanerpetontidae) at Moncucco Torinese, Piedmont Basin, northwestern Italy, and a review of the European Cenozoic record for albanerpetontids
FIG. 4. — Isolated dentaries (A-M) and vertebrae (N-U) of Albanerpeton pannonicum Venczel & Gardner, 2005 from the uppermost Miocene (Messinian) locality of Moncucco Torinese, Piedmont Basin, northwestern Italy: A-C, MGPT-PU 132003, right dentary preserving about anterior four-fifths of bone, including entire tooth-bearing region, in labial (A), lingual (B), and dorsal (C) views, from layer M5; D-F, MGPT-PU 132643, left dentary preserving about anterior one-half of bone, in labial (D), lingual (E), and dorsal (F) views, from layer M3/4; G-I, MGPT-PU 132010, right dentary preserving about anterior one-third of bone and exhibiting anomalous, plate-like bony growth (arrow) on ventral surface of symphyseal region, in labial (G), lingual (H), and dorsal (I) views, surface collected; J, K, MGPT-PU 132631, left dentary preserving posterior portion of tooth-bearing region and adjacent part of area for attachment of post-dentary bones, in labial (J) and lingual (K) views, from layer M3; L, M, MGPT-PU 132638, left dentary preserving posterior portion of tooth-bearing region and adjacent part of area for attachment of post-dentary bones, in labial (L) and lingual (M) views, from layer M4/5; N-P, MGPT-PU 132015, trunk vertebra missing much of neural arch, in right lateral (N) view, in ventral (O) view with anterior end to right, and in anterior (P) view, from layer M4/5; Q-U, MGPT-PU 132017, sacral vertebra missing much of neural arch, in right lateral (Q) view, in dorsal (R) and ventral (S) views, both with anterior end towards top of figure, and in anterior (T) and posterior (U) views, from layer M4. Abbreviations: aapd, area for attachment of post-dentary bones; ab, anterior basapophysis; ac, anterior cotyle; c, centrum; dp, dental parapet; enfo, external nutritive foramina; naw, broken base of neural arch wall; ncp, notochordal pit; oMc, opening for Meckelian canal; rcc, rim of calcified cartilage; sd, subdental shelf; sp, symphyseal prongs; t, functional teeth; tp, transverse process; ts, tooth slot. All images are photographs of undusted specimens. Dentaries (upper scale bar) are depicted at same magnification and vertebrae (lower scale bar) are depicted at same magnification. Scale bars: 1 mm.
FIG. 3 in A Messinian (latest Miocene) occurrence for Albanerpeton Estes & Hoffstetter, 1976 (Lissamphibia: Albanerpetontidae) at Moncucco Torinese, Piedmont Basin, northwestern Italy, and a review of the European Cenozoic record for albanerpetontids
FIG. 3. — Isolated premaxillae (A-L) and maxillae (M-S) of Albanerpeton pannonicum Venczel & Gardner, 2005 from the uppermost Miocene (Messinian) locality of Moncucco Torinese, Piedmont Basin, northwestern Italy: A-C, MGPT-PU 132112, complete left premaxilla, in labial (A), ventral (B), and lingual (C) views, from layer M3; D-F, MGPT-PU 132001, nearly complete left premaxilla, in labial (D), ventral (E), and lingual (F) views, from layer M4/5; G, H, MGPT-PU 132165, nearly complete left premaxilla, in labial (G) and lingual (H) views, from unrecorded layer; I, J, MGPT-PU 132232, nearly complete left premaxilla, in labial (I) and lingual (J) views, from layer M4/5; K, L, MGPT-PU 132648, nearly complete right premaxilla, in labial (K) and lingual (L) views, from layer M7+25; M-O, MGPT- PU 132307, nearly complete right maxilla, in labial (M), lingual, (N), and dorsal (O) views, from unrecorded layer; P, Q, MGPT-PU 132012, left maxilla missing anterior and posterior ends, in labial (P) and lingual (Q) views, from layer M4/5; R, S, MGPT-PU 132014, left maxilla preserving about anterior one-half of bone, in labial (R) and lingual (S) views, surface collected. Abbreviations: b, boss; fjl, flattened area for contact with jugal and lacrimal; inm, internal narial margin; ldn, lateral dorsal notch; mp, maxillary process; mt, misshaped functional tooth; mrt, misshaped replacement tooth; np, nasal process; pden, pars dentalis; pdor, pars dorsalis; pdp, premaxillary dorsal process; pfo, palatal foramen; plp, premaxillary lateral process; ppal, pars palatinum; rt, replacement tooth; spp, suprapalatal pit; t, functional teeth; ts, tooth slot; vp, vomerine process. All images are photographs of undusted specimens. All specimens are depicted at same magnification. Scale bar: 1 mm.
Figure 17 in Five new species of Anillinus Casey from the Southern Appalachian Mountains and the Piedmont Plateau of eastern U.S.A. (Coleoptera: Carabidae: Trechinae: Bembidiini)
Figure 17. Locality records for the valentinei-group and cornelli-group species. Anillinus valentinei – red triangle; A. smokiensis – red quadrangle; A. chandleri – red star; A. cornelli – red circles.
Figure 16 in Five new species of Anillinus Casey from the Southern Appalachian Mountains and the Piedmont Plateau of eastern U.S.A. (Coleoptera: Carabidae: Trechinae: Bembidiini)
Figure 16. Locality records for the moseleyae-group (red color) and loweae-group species from Chilhowee and Starr Mountains (yellow color). Anillinus moseleyae – red quadrangles; A. carltoni, new species – red circle; A. unicoi – red star; A. juliae – yellow circle; A. chilhowee – yellow star.
Figure 11-15 in Five new species of Anillinus Casey from the Southern Appalachian Mountains and the Piedmont Plateau of eastern U.S.A. (Coleoptera: Carabidae: Trechinae: Bembidiini)
Figure 11-15. Illustrations of male aedeagus. 11) Anillinus unicoi (NC, Graham Co., Unicoi Mtns.). 12) A. carltoni (TN, Blount Co., GSMNP, Thunderhead Mtn.). 13) A. chilhowee (TN, Polk Co., Chilhowee Mtn.). 14) A. smokiensis (TN, Blount Co., GSMNP). 15) A. chandleri (SC, Edgefield Co., Sumter National Forest). a-Median lobe, right lateral aspect; b-Left paramere, left lateral aspect; c-Right paramere, right lateral aspect. Scale = 100 µm.
Figure 1-5. Habitus images. 1 in Five new species of Anillinus Casey from the Southern Appalachian Mountains and the Piedmont Plateau of eastern U.S.A. (Coleoptera: Carabidae: Trechinae: Bembidiini)
Figure 1-5. Habitus images. 1) Anillinus unicoi (NC, Graham Co., Unicoi Mtns.), holotype. 2) A. carltoni (TN, Blount Co., GSMNP, Thunderhead Mtn.), paratype. 3) A. chilhowee (TN, Polk Co., Chilhowee Mtn.), holotype. 4) A. smokiensis (TN, Blount Co., GSMNP), paratype. 5) A. chandleri (SC, Edgefield Co., Sumter National Forest), holotype.
Figure 6-10. Pronotum images. 6 in Five new species of Anillinus Casey from the Southern Appalachian Mountains and the Piedmont Plateau of eastern U.S.A. (Coleoptera: Carabidae: Trechinae: Bembidiini)
Figure 6-10. Pronotum images. 6) Anillinus unicoi (NC, Graham Co., Unicoi Mtns.). 7) A. carltoni (TN, Blount Co., GSMNP, Thunderhead Mtn.). 8) A. chilhowee (TN, Polk Co., Chilhowee Mtn.). 9) A. smokiensis (TN, Blount Co., GSMNP). 10) A. chandleri (SC, Edgefield Co., Sumter National Forest).
FIG. 8. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins
FIG. 8. — Igornichthys bohemicus n. sp., holotype MHK 30866: A, scales with one spine sharply pointing in posterior direction and slightly downwards on each scale; B, scale with two sharply pointed tubercles. Scale bars: 1 mm.
FIG. 7. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins
FIG. 7. — Igornichthys bohemicus n. sp., holotype MHK 30866, scales on the left lateral side of the body: A, scales from rows 23-27 with conspicuous spines; B, detail of the scales from rows 25-27 with single spine; C, scales with two spines; D, detail of the scale with single spine in medial view; E, detail of the scale from row 27 with microsculpture of spines, whereas the surrounding scale surface is rough, which indicates bony surface; F, detail of the microsculpture on the spine of the previous scale. Scale bars: A, B, C, 500 µm; D, E, F, 100 µm.
FIG. 6. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins
FIG. 6. — Igornichthys bohemicus n. sp., holotype MHK 30866: A, general view of the teeth of upper and lower jaws; B, detail of the teeth of the upper and lower jaws, which interlock, when the jaws are closed; C, detail of the teeth of the anterior region of the lower jaw; D, detail of the teeth of the lower jaw. Scale bars: A, B, 500 µm; C, D, 100 µm.
FIG. 5. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins
FIG. 5. — Igornichthys bohemicus n. sp., reconstruction of the body in left lateral view. Posterior part of the body which is not preserved is grey. Scale bar: 5 mm.
FIG. 4. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins
FIG. 4. — Igornichthys bohemicus n. sp., reconstruction of the skull in left lateral view. The outlines of the bones, which are ill-defined, are marked with dashed lines. Abbreviations: see Methods. Scale bar: 5 mm.
FIG. 10 in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins
FIG. 10. — Reconstructions of the skull in dorsal view of some Aeduellidae and Igornichthyidae. The outlines of the bones, which are ill-defined, are marked with dashed lines: A, Aeduella blainvillei (Agassiz, 1833), after Heyler (1969); B, Neslovicella rzehaki Štamberg, 2007, after Štamberg (2007); C, Setlikia bohemica Štamberg & Zajíc, 1994, after Štamberg & Zajíc (1994); D, Igornichthys bohemicus n. sp. Abbreviations: see Methods. Scale bars: 1 cm.
FIG. 3. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins
FIG. 3. — Igornichthys bohemicus n. sp., holotype MHK 30866: A, left view of the whole specimen; B, detail of the skull in left lateral view. Scale bars: 5 mm.
FIG. 2. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins
FIG. 2. — Igornichthys bohemicus n. sp., outprint of the skull in left lateral view, holotype MHK 30866. The outlines of the bones, which are ill-defined, are marked with dashed lines. Abbreviations: see Methods. Scale bar: 5 mm.
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. 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.
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