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89 results for “Eastern Alps”
Linked collectors and determiners for: geophilidae_of_south_eastern_alps.
Natural history specimen data linked to collectors and determiners held within, "geophilidae_of_south_eastern_alps". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/51b027b6-b6bb-4cac-bb5e-286d3a5a53ee">https://bionomia.net/dataset/51b027b6-b6bb-4cac-bb5e-286d3a5a53ee</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/51b027b6-b6bb-4cac-bb5e-286d3a5a53ee">https://gbif.org/dataset/51b027b6-b6bb-4cac-bb5e-286d3a5a53ee</a>. Formatted as a Frictionless Data package.
Data used in the paper entitled: "Hidden faults: the Late Pleistocene transpression of the Königssee–Lammertal–Traunsee Fault inferred from caves deformation (Eastern Alps)"
<p><strong>Manuscript Abstract: </strong>The Eastern Alps have undergone lateral extrusion since the late Oligocene, with major crustal-scale strike-slip faults still active, as evidenced by earthquakes up to M6, despite scant geological record. Research has focused more on the Salzach-Ennstal-Mariazell-Puchberg (SEMP) and Mur-Mürz faults, leaving the central part of the Northern Calcareous Alps cut by the 110 km long Königssee–Lammertal–Traunsee (KLT) fault system under-studied. We took advantage of a cave environment isolated from erosion, providing unparalleled structural indicators exposure to fill the Pleistocene deformation history gap of the KLT. We reconstruct paleostress for 26 reverse, strike-slip, and oblique reactivated faults that offset passages in seven caves close to sinistral KLT and dextral Lammertal faults. <sup>230</sup>Th/U dating of faulted and broken speleothems revealed two reactivation events since the Middle Pleistocene. The older event dates can be constrained to 331 (+89/-54) to 287 ± 6 ka, or 297-281 ka if the KLT and Lammertal faults were reactivated simultaneously. The younger event occurred between 130 and 90 ka, aligning with fault reactivations in the eastern Alps.</p> <p>Cave observations allowed us to analyze reverse faults in the positive flower structure of the KLT and mode I fracture with minor antithetic dextral slip, suggesting a sinistral component of regional rejuvenation. Our findings indicate that the KLT was reactivated due to simple shear with NNE compression. Along the Lammertal fault, we recorded a strike-slip regime driven by NNW compression. The KLT and Lammertal faults form a system of conjugated shears that efficiently accommodate N-S shortening compared to the SEMP fault, which is perpendicular to the compression. Combining our neotectonic data with current seismicity shows that the KLT plays a key role in the Quaternary extrusion process in the studied Alpine sector, surpassing the more prominent SEMP fault.</p> <p><strong>In this dataset, we make available:</strong></p> <p>iPhone13Pro LiDAR scan of the two cave passage offsets: one in the Dependance cave and Gamssteig cave</p> <p>PDF file with dated sample location and description</p> <p> </p> <p>Published in:</p> <p><strong>Szczygieł, J., Plan, L., Hellstrom, J., & Grasemann, B. (2024). Hidden Faults : The Late Pleistocene Transpression of the Königs- see – Lammertal – Traunsee Fault Inferred from Caves Deformation ( Eastern Alps ). Lithosphere, (Number Special 15), lithosphere_2024_177, 14. https://doi.org/10.2113/2024/lithosphere</strong></p> <p><strong>This research was founded by the NCN Polish National Science Center [grant No 2020/39/D/ST10/00615]</strong></p>
FIGURES 47-54 in Comparative larval ultramorphology of three endemic Lathrobium (Glyptomerus) species (Coleoptera, Staphylinidae, Paederinae) from the Eastern Alps in Italy
FIGURES 47-54. Mature larva of L. alzonai (47, 47A, 48, 51, 52), L. freyi (49, 53) and L. pacei (50, 54). 47-54, right maxilla with stipes (48), microstructure near trichobothrium (51) and region of mala (52-54) in ventral aspect. Abbreviations: Cd— cardo, Pf—palpifer, Ma—mala, I-III—antennal and maxillary palp articles, St—stipes, Trb—trichobothrium, 1, 2—setae of maxillary palp.
Figure 5 in Shedding light on species boundaries in small endogeic animals through an integrative approach: species delimitation in the centipede Clinopodes carinthiacus (Chilopoda: Geophilidae) in the south-eastern Alps
Figure 5. Contribution of the bioclimatic variables on the first two principal components of climatic variation in the study area, and density of occurrence of Clinopodes carinthiacus s.s. and Clinopodes strasseri on the two principal components estimated with ecospat, based on 106 sites (former species) and 16 sites (latter). Continuous and dashed contour lines indicate 100% and 50% of the available climatic space, respectively.
Fig. 4 Zospeum spelaeum. a lectotype SMF 158543 in An integrative taxonomic study reveals carychiid microsnails of the troglobitic genus Zospeum in the Eastern and Dinaric Alps (Gastropoda, Ellobioidea, Carychiinae)
Fig. 4 Zospeum spelaeum. a lectotype SMF 158543, Postojnska jama, sh: 1.634 mm. — b1–6 NMBE 553308, Betalov Spodmol, sh: 1.8 mm; c ditto, sh: 1.495 mm. — d NMBE 553306, Betalov Spodmol, sh: 1.8 mm. — e NMBE 553310, Mačkovica jama, sh: 2.39 mm. — f1–2 NMBE 553312, Velika Pasica, sh: 2.055 mm. —(g) NMBE 553311, sh: 1.957 mm; h ditto, sh: 2.07 mm. — i NMBE 553304, Čampari jama,
Fig. 2 in An integrative taxonomic study reveals carychiid microsnails of the troglobitic genus Zospeum in the Eastern and Dinaric Alps (Gastropoda, Ellobioidea, Carychiinae)
Fig. 2 Top: The nine measurements as illustrated on the frontal (left) and apical (right) view of a Zospeum manitaense shell (NMBE 549731). Bottom right: Position of the 14 landmarks on the shell. Bottom left: Nomenclature to dentition indicated on shell of Zospeum lamellatum (MCSMNH 35995)
Fig. 6 in An integrative taxonomic study reveals carychiid microsnails of the troglobitic genus Zospeum in the Eastern and Dinaric Alps (Gastropoda, Ellobioidea, Carychiinae)
Fig. 6 (a–e) Zospeum alpestre, (a1–2) NHMW 75000 (E 12483), Dovja griča, sh: 1.485 mm; (b) ditto, sh: 1.369 mm; (c1–2) ditto, sh: 1.432 mm. — (d1–2) NMBE 553373, Jama pod Mokrico, sh: 1.652 mm. — (e) SMNH 2216, Jama pod Mokrico, sh: 1.53 mm. —(f–i) Zospeum kupitzense, (f) Holotype, SMF 256354, Kupitzklamm, sh: 1.67 mm. — (g1–2) Paratype, NMBE 549730, sh: 1.551 mm; (h) ditto, sh: 1.536 mm. — (i1–2) NMBE 553393, Ložekarjeva jama, sh: 1.657 mm. —(j–k) Zospeum isselianum, (j1–2) Neotype, MCSMNH 37013, Turjeva jama,
Fig. 1 a in An integrative taxonomic study reveals carychiid microsnails of the troglobitic genus Zospeum in the Eastern and Dinaric Alps (Gastropoda, Ellobioidea, Carychiinae)
Fig. 1 a Currently known distribution of the genus Zospeum in the southwestern Alps and the Dinarids; b Distribution of recovered clades
Fig. 5 a–f in An integrative taxonomic study reveals carychiid microsnails of the troglobitic genus Zospeum in the Eastern and Dinaric Alps (Gastropoda, Ellobioidea, Carychiinae)
Fig. 5 a–f Zospeum costatum, (a) NHMW 71848, Babja luknja, Goričane, sh: 2.214 mm; (b) ditto, sh: 2.043 mm. — (c1–3) NHMW 71847, Babja luknja, Goričane, sh: 2.08 mm. — (d) NMBE 553383, Jama 2 pri Jabljah, sh: 1.86 mm; (e) ditto, sh: 1.92 mm; (f) ditto, sh: 2.03 mm. —(g–k) Zospeum lamellatum, (g1–3) Lectotype, MCSMNH 35995, Krasnica, sh: 2.059 mm. — (h) MCSMNH 7057, Ukovnik pri sp. Idriji, sh: 1.751 mm; (i) ditto, sh: 1.739 mm; (j) ditto, sh: 1.733 mm; (k) ditto, sh: 1.766 mm. —(l–m) Zospeum lautum, (l1–2) NHMW 71828,
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