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9 results for “Vosges”
Magnetic data grids of the Northern Vosges, surveys EOST2008 and GPR2015.
<p>Grid computation and details are explained in Gavazzi et al., 2019 [1] and exploited in Bertrand et al., [2].<br> This file contains non-null grid elements.</p> <p>PARAMETERS<br> Format : ASCII<br> Number of elements : 86902<br> Grid cell size : 125 m</p> <p>FIELDS<br> - LON : grid cell WGS84 longitude (°East);<br> - LAT : grid cell WGS84 latitude (°North );<br> - ALT : grid cell altitude amsl (m) - this grid was computed at a constant altitude of 1400 m above mean sea level;<br> - TMI : total magnetic intensity anomaly (nT);<br> - RTP : (double) reduction to the pole of the TMI (nT) - mean regional field direction Inclination=1.60°, Declination=64.14°;<br> - DV : vertical derivative of the RTP at order 0.5 (nT/m);<br> - DH : horizontal derivative of the RTP at order 1 (nT/m);</p> <p>[1] Gavazzi, B., Bertrand, L., Munschy, M., Mercier de Lépinay, J., Diraison, M. & Géraud, Y. (submitted). On the use of aeromagnetism for geological interpretation part I: comparison of 1 scalar and vector magnetometers for aeromagnetic surveys and an equivalent source 2 interpolator for combining, gridding and transform fixed altitude and draping 3 datasets, Journal of Geophysical Research: Solid Earth (2019).</p> <p>[2] Bertrand, L., Gavazzi, B., Mercier de Lépinay, J., Diraison, M., Géraud, Y. & Munschy, M. (submitted). On the use of aeromagnetism for geological interpretation part II: geological interpretation on outcropping basement rocks for geothermal energy prospection, Journal of Geophysical Research: Solid Earth (2019).</p>
Fig. 3 in The oldest aphid insect from the Middle Triassic of the Vosges, France
Fig. 3. Schema of range and relationships of Permian and Triassic Aphidomorpha and their relatives. Asterisks in circle, mean taxa figured in the schema; empty circle, non figured taxon. Insert: supposed cladogram of Permian and Triassic Aphidomorpha, inferred from data and opinions from Shcherbakov (2007) and Heie and Wegierek (2009a, b).
Fig. 1 in The oldest aphid insect from the Middle Triassic of the Vosges, France
Fig. 1. Forewing of the early Middle Triassic (early Anisian) aphid Vosegus triassicus gen. et sp. nov. A. Reconstruction. B. Venation scheme. C. Part (No. 5916). D. Counterpart (No. 5917).
Fig. 2 in The oldest aphid insect from the Middle Triassic of the Vosges, France
Fig. 2. Distribution of Permian and Triassic Aphidomorpha (Middle Triassic, 240 Ma). Vosegus (Aphidomorpha: Triassoaphidoidea: Vosegidae); Middle Triassic, Anisian; "Grès à Voltzia" Formation, France; Creaphis (Aphidomorpha: Triassoaphidoidea: Creaphididae); Upper Triassic, Carnian; DzhailouTcho, Madygen Formation, Kyrgyzstan; Triassoaphis (Aphidomorpha: Triassoaphidoidea: Triassoaphididae); Upper Triassic, Carnian; Belmont, NSW, Australia; Boreoscyta (Pincombeomorpha: Pincombeoidea: Boreoscytidae); Upper Permian, Roadian; Soyana, Russia; Dinoscyta (Pincombeomorpha: Pincombeoidea: Boreoscytidae); Lower Permian, Kungurian; Koshelevka Formation, Chekarda, Russia; Madygenopsyllidium (Pincombeomorpha: Pincombeoidea: Pincombeidae); Upper Triassic, Carnian; Dzhailou−Tcho, Madygen Formation, Kyrgyzstan; Pincombea (Pincombeomorpha: Pincombeoidea: Pincombeidae); Upper Permian, Lopingian (Changhsingian); Newcastle Coal Measures, NSW, Australia; Simulaphis (Aphidomorpha: Naibioidea: Simulaphididae); Upper Permian, Lopingian (Changhsingian); Newcastle Coal Measures, NSW, Australia; Simulaphididae indet. (Aphidomorpha: Naibioidea); Upper Triassic, Carnian; Garazhovka Formation, Ukraine; Coccavus (Aphidomorpha: Naibioidea: Naibiidae); Upper Triassic, Carnian; Dzhailou−Tcho, Madygen Formation, Kyrgyzstan; Dracaphis (Aphidomorpha: Naibioidea: Dracaphididae); Middle Triassic, Ladinian; Tongchuan Formation, Shaanxi, China.
FIG. 3 in Discovery of the mountain glass snail, Hessemilimax kotulae (Westerlund, 1883) (Mollusca, Gastropoda, Vitrinidae), in the High Vosges Mountains (northeast France) and its conservation
FIG. 3. — Reproductive system of two specimens of Hessemilimax kotulae (Westerlund, 1883) from the High Vosges: A, mature stage II (animal figured in Fig. 2F); B, juvenile stage III (animal figured in Fig. 2E). Solid lines indicate the parts cut during dissection. Abbreviations: see Material and methods. Scale bars: A, 1 mm; B, 0.5 mm.
FIG. 2 in Discovery of the mountain glass snail, Hessemilimax kotulae (Westerlund, 1883) (Mollusca, Gastropoda, Vitrinidae), in the High Vosges Mountains (northeast France) and its conservation
FIG. 2. — Sampling sites and specimens of Hessemilimax kotulae (Westerlund, 1883) from the High Vosges: A, locality no. 01: small stream in a mixed forest dominated by fir, Hirschsteinried, altitude 1050 m; B, locality no. 02: scree slope, Schluchtmatt, elevation 880 m; C, locality no. 03: Rothried, foot of avalanche slope, elevation 895 m; D, locality no. 04: Pourri-Faing, scree slope covered by beech, elevation 1145 m; E, live specimen of H. kotulae sampled at locality no. 01 (extended body length: 8.1 mm); F, live specimen of H. kotulae sampled at locality no. 02 (extended body length: 14.7 mm); G, shell of the specimen of H. kotulae illustrated in F (shell length: 4.7 mm, shell width: 3.3 mm); H, live specimen of H. kotulae sampled at locality no. 03 (extended body length: 15.9 mm); I, live specimen of H. kotulae sampled at locality no. 04 (extended body length: 12.1 mm).
FIG. 1 in Discovery of the mountain glass snail, Hessemilimax kotulae (Westerlund, 1883) (Mollusca, Gastropoda, Vitrinidae), in the High Vosges Mountains (northeast France) and its conservation
FIG. 1. — Geographical location of the sampling area: A, global view; B, location of the sampling sites in the high Vosges. Symbols: ⎕, cities; △, main peaks with elevation indicated; ○, sampling sites; ●, new records of Hessemilimax kotulae (Westerlund, 1883) (localities no. 01 to no. 04); ●, past records of Semilimax semilimax (locality no. 05, Geissert 1996a) and H. kotulae (locality no. 06, Brugel 2014). The dotted line on A indicates the boundary between the sandstone Vosges (north Vosges) and the crystalline Vosges (High Vosges). This line passes approximately between Saint-Dié-des-Vosges and Schirmeck on B.
Data from: The effect of reintroductions on the genetic variability in Eurasian lynx populations: the cases of Bohemian-Bavarian and Vosges-Palatinian populations
Open the record for dataset details and reuse information.
FIG. 4 in Discovery of the mountain glass snail, Hessemilimax kotulae (Westerlund, 1883) (Mollusca, Gastropoda, Vitrinidae), in the High Vosges Mountains (northeast France) and its conservation
FIG. 4. — Vitrinid species occurring in syntopy with Hessemilimax kotulae (Westerlund, 1883) in the High Vosges and apex of the shells: A, Eucobresia diaphana (Draparnaud, 1805) (extended body length: 14.6 mm), specimen sampled at locality no. 01; B, Phenacolimax major (A. Férussac, 1807) (extended body length: 9.6 mm), specimen sampled at locality no. 04; C, Vitrina pellucida (O. F. Müller, 1774) (extended body length: 9.3 mm), specimen sampled at locality no. 03; D, apex of the shell of H. kotulae (animal figured in Fig. 2I); E, apex of the shell of E. diaphana with spiral rows of small pits (animal figured in Fig. 4A); F, apex of the shell of P. major with spiral rows of small pits (animal figured in Fig. 4B); G, apex of the shell of V. pellucida with spiral rows of small pits (animal figured in Fig. 4C). Scale bar: 500 µm. In A to C, the white arrows indicate the folding of the mantle onto the shell. In E, F and G the arrows indicate the spirals of small pits.
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