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875 results for “Brachiopod”
Fig. 5 in Drilling predation on Permian brachiopods and bivalves from the Glass Mountains, west Texas
Fig. 5. Temporal distribution of drilling predation using three different metrics. AI, assemblage drilling intensity; HDT, highest drilled taxon; PT, percent of taxa drilled. See Fig. 2 for full formation names.
Fig. 3. Drilled brachiopods from the Cooper collection. A in Drilling predation on Permian brachiopods and bivalves from the Glass Mountains, west Texas
Fig. 3. Drilled brachiopods from the Cooper collection. A. Stenocisma camurum (USNM 520070). B. Kurtoginella umbonata (USNM 520071). C. Martinia miranda (USNM 520072). D. Composita affinis (USNM 520073).
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).
Fig. 7 in Drilling predation on Permian brachiopods and bivalves from the Glass Mountains, west Texas
Fig. 7. Size frequency distributions for drilled prey shells and drill holes for: A. Drilled brachiopod specimens. B. Drilled bivalve mollusk specimens. C. Drill holes in brachiopods. D. Drill holes in bivalve mollusks.
Fig. 5 in Diversity dynamics of Early-Middle Jurassic brachiopods of Caucasus, and the Pliensbachian-Toarcian mass extinction
Fig. 5. Brachiopods diversity changes in Lias of Bakony Mts (after Vörös 1993, 1995) and Swiss Alps and Jura Mts. (after Sulser 1999).
Fig. 1 in Diversity dynamics of Early-Middle Jurassic brachiopods of Caucasus, and the Pliensbachian-Toarcian mass extinction
Fig. 1. Geographic location of studied area (A) and paleogeographic situation of areas discussed in the text (B; studied area indicated by 1). Paleogeographic base map is modified from Owen 1983 and Dommergues et al. 2001.
Fig. 2 in New bizarre micro-spiriferid brachiopod from the Early Carboniferous of China
Fig. 2. Ventral valves of Changshunella yangi gen. et sp. nov. Muhua III section, Muhua, Changshun County, Guizhou, China. A. PKUM02−0023, in posterior (A1), ventral (A2), anterior (A3), and lateral (A4, anterior to left) views, and enlargement of part of ventral interarea showing the pseudodeltdium (A5). B. PKUM02−0024, in ventral (B1), anterior (B2),), inclined anterior (B3), and oblique lateral (B4) views. C. PKUM02−0025, in oblique lateral (C1) and ventral (C2) views. D, PKUM02−0026 in posterior view. E. PKUM02−0027, in anterior (E1), ventral (E2), and lateral (E3) views. F. PKUM02−0028, in internal view. G. PKUM02−0029, in posterior (G1) and internal (G2) views. H. PKUM02−0030, in anterior (H1), ventral (H2), and posterior (H3) views. I. PKUM02−0031, in ventral (I1), inclined anterior (I2), more inclined anterior (I3), and oblique lateral (I4) views, and enlargement of part of the valve in inclined anterior view (I5). J. PKUM02−0032, in internal (J1), posterior (J2), and enlarged internal view (J3). K. PKUM02−0042, in anterior (K1), internal (K2) and posterior (K3) views. B, C, I, and J are SEM images. All × 6 except A5, I5, and J3 × 20.
Fig. 2 in Diversity dynamics of Early-Middle Jurassic brachiopods of Caucasus, and the Pliensbachian-Toarcian mass extinction
Fig. 2. Liassic composite lithological section of NW Caucasus and comparison of regional and global (simplified from Hallam and Wignall 1999) sea−level changes.
Fig. 1 in Soft-tissue preservation in the Lower Cambrian linguloid brachiopod from South China
Fig. 1. The lophophore of Lingulellotreta malongensis from the Yu'anshan Member of the Qiongzhusi (Chiungchussu) Formation, Lower Cambrian, China. A. ELI L−0014A, dorsal view of ventral interior, showing lophophore, with a series of definitive filaments, three−dimensionally preserved in a lamina of sediment between valves. B. ELI L−0033, showing paired imprints of brachia and depression of distinctive visceral cavity. C. ELI L−0052A, a specimen strongly compressed, showing lophophore with filaments. D. ELI L−0056A. D1, parallel specimen with straight pedicle strongly compressed, and with paired spiral brachial imprints; D2, details of the brachial imprints of D1. E. ELI L−0073, a lateral oblique view of strongly compressed specimen, showing detail of a hollow brachial tube. F. ELI L−0101, lateral oblique view of the lophophore three−dimensionally preserved in sediment in valves. G. ELI L−0081, a parallel, possible juvenile specimen strongly compressed; note the relatively small brachia. Scale bars 2 mm. See Fig. 2 for some interpretations.
Fig. 5 in Soft-tissue preservation in the Lower Cambrian linguloid brachiopod from South China
Fig. 5. Lingulellotreta malongensis from the Chengjiang Fauna, reconstruction of the internal morphology based on ELI L−0014 and ELI L−0017, showing disposition of lophophore and digestive tract, and location of measurements indicated in Table. 1. Abbreviations: L, length of the shell; Lb, length of the body; Ll, length of the lophophore; Ls, length of the dorsal valve; Wl, width of the lophophore; Ws, width of the shell. Scale bar 1 mm.
Fig. 4 in Soft-tissue preservation in the Lower Cambrian linguloid brachiopod from South China
Fig. 4. Two linguloid brachiopods, Lingulellotreta malongensis and Lingulella chengjiangensis, from the Yu'anshan Member of the Qiongzhusi (Chiungchussu) Formation, Lower Cambrian, South China. A. Lingulellotreta malongensis, ELL L−0017. A1, photograph of the dorsally and right laterally compressed specimen, showing the interiors, including the digestive system and paired imprints of brachia; A2, explanatory drawing of the same. B. ELI L−0091A, a parallel specimen of Lingulellotreta malongensis, note the faint brachial contour and digestive tract with considerable relief. C. Lingulella chengjiangensis, ELI C−0029. C1, photograph (dorsal view) of dorsal interior, showing the digestive tract with an anterior anus, and with impression of visceral cavity; C2, explanatory drawing of the same. D. Lingulella chengjiangensis, ELI C−0027, anterodorsally compressed specimen, showing the position of the mouth. Scale bars 2 mm.
Data from: Identifying the most surprising victims of mass extinction events: an example using Late Ordovician brachiopods
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Data from: Antitropicality and convergent evolution: a case study of Permian neospiriferine brachiopods
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Data from: Phylogenetic revision of the Strophomenida, a diverse and ecologically important palaeozoic brachiopod order
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Data from: Early Cambrian (stage 4) brachiopods from the Shipai Formation in the Three Gorges area of South China
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Data from: Do brachiopods show substrate-related phenotypic variation? A case study from the Burgess Shale
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Data from: Three-dimensional morphological variability of recent rhynchonellide brachiopod crura
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Data from: Morphological analysis of phylogenetic relationships among extant rhynchonellide brachiopods
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Data from: Post-metamorphic allometry in the earliest acrotretoid brachiopods from the lower Cambrian (Series 2) of South China, and its implications
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Permian–Triassic phylogenetic and morphologic evolution of rhynchonellide brachiopods
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