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492 results for “Silurian”
Figure 1. A in The histology and affinities of sinacanthid fishes: primitive gnathostomes from the Silurian of China
Figure 1. A, morphological terms used to describe sinacanthid spines; B, diagrammatic illustration of tissue distribution in a transverse section through a sinacanthid spine.
Fig. 10 in Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes
Fig. 10. Morinorhynchus rubeli sp. nov. A. VU B20499, ventral exterior (A1), and interior (A2), Nova Beds of Dubysa Formation (Gorstian–Ludfordian), Šiupyliai−69, 879.4 m, × 6. B. VU B20498, holotype, ventral exterior (B1), and interior (B2), Mituva Formation (Ludfordian), Virbalis−5, 881.5 m, × 4. C. VU B20501, dorsal interior, Ventspils Formation (Ludfordian), Kurtuvėnai−162, 1097.2 m, × 2. D. VU B20500, dorsal interior, Vievis Formation (Pridoli), Grauţai−105, 580.9 m, × 5. E. VU B10146, dorsal exterior (E1), and interior (E2), Mituva Formation (Ludfordian), Virbalis−5, 887.45 m, × 5.
Fig. 2 in Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes
Fig. 2. Correlation of the Silurian of west, central and east Lithuania with the international Silurian stages, the East Baltic regional stages and the graptolite and conodont zones.
Fig. 3 in Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes
Fig. 3. Ranges of Silurian plectambonitoidean, strophomenoidean, and orthotetoidean brachiopods within the Lithuanian boreholes (see Appendix, Table 1 for details).
Data from: Comparing taxonomic and geographic scales in the morphologic disparity of Ordovician through Early Silurian Laurentian Crinoids
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Telychian Bryozoa, Matrix (Bryozoans from the lower Silurian (Telychian) Hanchiatien Formation from southern Chongqing, South China)
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Fig. 1 in Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes
Fig. 1. Map of Lithuania showing the positions of the boreholes mentioned in the text.
FIGURE 19 in Evolutionary significance of the retiolitine Gothograptus (Graptolithina) with four new species from the Silurian of the East European Platform (Baltica), Poland and Lithuania
FIGURE 19. Mature tubarium with appendix of Gothograptus obtectus Kozłowska-Dawidziuk, 1990 from the Bartoszyce IG- 1 core, depth 1677.5 m, lundgreni Biozone, Poland, ZPAL G.55/48. A. enlargement of distal part of specimen. B. enlargement of proximal end. C. whole specimen, reverse view. Abbreviations: lat. ap.—lateral apertural.
FIGURE 16 in Evolutionary significance of the retiolitine Gothograptus (Graptolithina) with four new species from the Silurian of the East European Platform (Baltica), Poland and Lithuania
FIGURE 16. Tubaria of mature colonies of Gothograptus domeyki n. sp., Šiupyliai-69 core, upper part of lundgreni Biozone, Lithuania. A–B. finite tubarium with seven pairs of thecae and appendix, holotype, depth 1009,1 m, VU RET-13; A. ventrolateral view of specimen; B. enlargement of thick ancora and broken outer ancora, oblique view. C, H. finite tubarium, depth 1010.0 m, VU RET-14; C. enlargement of two thecae; H. enlargement of proximal end. D–E. fragment of finite tubarium, paratype, depth 1010.0 m, VU RET-15; D. whole specimen, ventro-lateral view; E. proximal thecae with spines. F–G. proximal end of young tubarium, depth 1010.0 m, VU RET-16; F. enlargement of proximal theca; G. enlargement of ancora
FIGURE 18 in Evolutionary significance of the retiolitine Gothograptus (Graptolithina) with four new species from the Silurian of the East European Platform (Baltica), Poland and Lithuania
FIGURE 18. Details of mature tubarium of Gothograptus kozlowskii Kozłowska-Dawidziuk, 1990 holotype, ZPAL G.XIII/43, Baltic erratic boulder 147 from Jarosławiec, Poland. A. ventral view; B. lateral view, reverse side of tubarium; C. proximal end, outside view; D. orifice of th51; E. opening of appendix.
Silurian coral Acervularia sp. BIRUG 15411
Fossil coral of the genus *Acervularia* (specimen number: BIRUG 15411). This specimen of a rugose coral was collected from Wren's Nest, in the Much Wenlock Limestone Formation of the English West Midlands by W. Woodall. Rugose corals were abundant from the mid Ordovician to the end of the Permian (~470–252 million years ago), but became extinct in the Permian–Triassic mass extinction. This specimen was donated to the Lapworth Museum by Sir George Holcroft (1916). Model created by Andrew Jones with photogrammetry in Agisoft Photoscan. Source: Objaverse 1.0 / Sketchfab
Cambrian–Silurian sedimentary processes and provenance with basin shift in southeastern Qilian Orogenic Belt: implications for crustal and tectonic evolution in northern Proto-Tethyan realm
<p>This datatset contains detrital zircon U-Pb-Hf isotope, whole-rock major and trace elemental, and Nd isotopic data of the Cambrian to Silurian sedimentary rocks in the southeastern Qilian Orogenic Belt.</p>
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