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fenestrae

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Journal Article
Published: 01 January 1994
Journal of Sedimentary Research (1994) 64 (1a): 140–146.
...Roger J. Bain; Pascal Kindler Abstract Fenestrae are primary or penecontemporaneous pores in the sediment framework that are larger than grain-supported interstices. These features have long been used to characterize peritidal environments and as a sea-level indicator in ancient successions. We...
Journal Article
Published: 01 June 1983
Journal of Sedimentary Research (1983) 53 (2): 619–628.
...Eugene A. Shinn Abstract Birdseyes, birdseye limestone, fenestrae, fenestral fabric, shrinkage pores, and loferites are considered similar or synonymous when occurring in lime mudstone or syndepositional dolomite, especially in association with mudcracks and stromatolites. Compaction experiments...
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Oral fenestrae and jaw elements in antiarchs: (1, 2) Yunnanolepidoidei; (3–5) Asterolepidoidei; (6, 7) Bothriolepidoidei. (1) Parayunnanolepis xitunensis Zhang, Wang, and Wang, 2001. (2) Phymolepis cuifenshanensis Zhang, 1978. (3) Pterichthyodes milleri (Miller, 1841). (4) Asterolepis scabra (Woodward, 1891). (5) Asterolepis ornata Eichwald, 1840. (6) Bothriolepis canadensis (Whiteaves, 1880). (7) Bothriolepis sp. from Gogo. All figures are redrawn from the original reconstructions and photographs: (1) from Wang and Zhu (2021); (2) from Young and Zhang (1996); (3) from Hemmings (1978); (4) from Nilsson (1941); (5) from Upeniece (2011); (6) from Stensiø (1948); (7) from Young (1984). In (4), the right suborbital is mirrored from the left one for better comparison with other figures. AVL = anterior ventrolateral; IG = infragnathal; SL = semilunar; SO = suborbital; of = oral fenestra; rm = rostral margin of the skull roof. Not to scale.
Published: 01 November 2022
Figure 2. Oral fenestrae and jaw elements in antiarchs: ( 1, 2 ) Yunnanolepidoidei; ( 3–5 ) Asterolepidoidei; ( 6, 7 ) Bothriolepidoidei. ( 1 ) Parayunnanolepis xitunensis Zhang, Wang, and Wang, 2001 . ( 2 ) Phymolepis cuifenshanensis Zhang, 1978 . ( 3 ) Pterichthyodes milleri (Miller
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Lenticular to consistent stratiform stromatolites with laminoid fenestrae (thinner arrow) and tufted and irregular-shaped microbial clots (thicker arrow) within finely laminated impure carbonates of Krol A Member. Note the presence of crude laminae and imbrications (black arrow) in these clots and their lateral gradation to laminites. Discontinuous flat laminites pass upwards into more continuous wavy to mm size LLH type pseudocolumnar stromatolites with crinckled laminae. Location: Manora village.
Published: 01 September 2021
Fig. 4 Lenticular to consistent stratiform stromatolites with laminoid fenestrae (thinner arrow) and tufted and irregular-shaped microbial clots (thicker arrow) within finely laminated impure carbonates of Krol A Member. Note the presence of crude laminae and imbrications (black arrow
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Mulargia–Escalaplano Basin. (a) Domal algal bindstone with fenestrae. (b) Micrograph detail of the microbialites. (c) Evaporites, plane-polarized light. (d) Evaporites, cross-polarized light. Scale bar = 1 cm.
Published: 31 May 2019
Fig. 17. Mulargia–Escalaplano Basin. (a) Domal algal bindstone with fenestrae. (b) Micrograph detail of the microbialites. (c) Evaporites, plane-polarized light. (d) Evaporites, cross-polarized light. Scale bar = 1 cm.
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(a, b) Overview of fenestrae-filling DYC-1 in thin-section. Arrows and dashed rectangles indicate places which are enlarged in (c–j). (c) The innermost lamina of the thick wall overgrows a fissure in earlier laminae. The arrow indicates where a lamina in the thick wall is separated from other laminae. (d) A part of (b), exhibits well-preserved lamination in the thick wall. A gap between the thick wall and host rock is indicated with a hollow arrow. The solid arrow indicates where a lamina diverges from the thick wall and directly contacts the host rock. (e) The innermost lamina of the thick wall diverges from other laminae to form a thin wall. (f) A thin wall is connected to the innermost laminae of the thick wall with a cuspate tubercle. (g) The innermost lamina of the thick wall overgrows the tubercles formed by earlier laminae. (h–j) The same area under plane-polarized light (h), crossed polarized light (i) and CL (j), where the chamber wall is immediately overgrown with a thin, isopachous cement, which exhibits dull CL. Abbreviations: is – isopachous cements; for others see the caption of Figure 4. All photos are oriented upwards. Sample number: Ls45b.
Published: 29 August 2017
Figure 5. (a, b) Overview of fenestrae-filling DYC-1 in thin-section. Arrows and dashed rectangles indicate places which are enlarged in (c–j). (c) The innermost lamina of the thick wall overgrows a fissure in earlier laminae. The arrow indicates where a lamina in the thick wall is separated from
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Fenestrae in ooidal dolomite, West End Quarry, Boston Spa Riverside Woods [SE 4247 4619]. Scale in mm.
Published: 25 July 2017
Fig. 14. Fenestrae in ooidal dolomite, West End Quarry, Boston Spa Riverside Woods [SE 4247 4619]. Scale in mm.
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Cross-sections through oncoids, highlighting bubble fenestrae and conical growth. Views A and B represent the same oncoid. A) Locations of bubble fenestrae. B–D) Growth patterns based on light-dark laminae couplets and hourglass fenestrae. Laminae with bubble fenestrae present around the entire circumference indicate conical growth into/out of the plane of dissection, represented by bulls-eye structures.
Published: 01 December 2015
Fig. 4.— Cross-sections through oncoids, highlighting bubble fenestrae and conical growth. Views A and B represent the same oncoid. A ) Locations of bubble fenestrae. B – D ) Growth patterns based on light-dark laminae couplets and hourglass fenestrae. Laminae with bubble fenestrae present
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Petrographic details of fenestrae. All images in plain polarized light with white card technique. A–D) Bubble-associated fenestrae, defined by rounded edges and division by thin micritic pillars. E) Girvanella filaments lining bottom of dividing pillar. F) The fenestrae on the right breaks through a dark laminae that apparently bounds similar fenestrae on the left.
Published: 01 December 2015
Fig. 5.— Petrographic details of fenestrae. All images in plain polarized light with white card technique. A – D ) Bubble-associated fenestrae, defined by rounded edges and division by thin micritic pillars. E ) Girvanella filaments lining bottom of dividing pillar. F ) The fenestrae
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1–3, fenestrae microbialite with plumose morphology (Sumner, 1997b) in outcrop, hand sample, and serial-section, respectively. Microbial mats defined by kerogen (K) are black and are surrounded by gray herringbone calcite (HC) and white void-filling calcite (C); hand sample shows the relationship between supports (S) and undulose structures (US).
Published: 01 July 2014
Figure 2 1–3 , fenestrae microbialite with plumose morphology ( Sumner, 1997b ) in outcrop, hand sample, and serial-section, respectively. Microbial mats defined by kerogen (K) are black and are surrounded by gray herringbone calcite (HC) and white void-filling calcite (C); hand sample shows
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Plate II
Published: 01 February 2009
Plate II 1) Wackestones with irregular fenestrae, of bird’s eyes type. Note the geopetal internal filling; 2) Wackestones with microepikarstic cavities, filled with speleotheme-like cement; 3) Mudstone with sparse calcite replacement evaporite pseudomorphs; 4) Replacing calcite/dolomite textures
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Polished slab showing fenestrae-rich microbial matrix (M) separated by a cement-filled cavity. Microbialite is very dense, with few fenestrae adjacent to the cavity walls (DM). White cement generations consist of radiaxial fibrous calcite (RFC), while light gray bands consist of herringbone calcite (HBC). Dark internal sediment patchily overlies the first generation of radiaxial fibrous cement (black arrow), and the bright spot in the center of the cavity is baroque dolomite. Slab in the field of view is 30 cm across.
Published: 01 November 2004
Figure 1 Polished slab showing fenestrae-rich microbial matrix (M) separated by a cement-filled cavity. Microbialite is very dense, with few fenestrae adjacent to the cavity walls (DM). White cement generations consist of radiaxial fibrous calcite (RFC), while light gray bands consist
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Microkarst fenestrae in Opache Formation palustrine limestones. The limestone matrix is a dense mudstone-wackestone with no porosity. Fenestrae develop as a result of desiccation and gas generation and provide high local porosity in thin discontinuous horizons. The coin is 2 cm in diameter.
Published: 01 February 2004
Fig. 7 Microkarst fenestrae in Opache Formation palustrine limestones. The limestone matrix is a dense mudstone-wackestone with no porosity. Fenestrae develop as a result of desiccation and gas generation and provide high local porosity in thin discontinuous horizons. The coin is 2 cm in diameter.
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Photographs and line drawings of the skull of G. brevipes (GIN 100/13) in right lateral view (A, D), right mandible in lateral view (B, E), and left mandible in medial view (C, F). an, angular; aof, antorbital fenestra; ar, articular; d, dentary; ect, ectopterygoid; emf, external mandibular fenestra; eo, exoccipital; f, frontal; fo, foramen; imf, internal mandibular fenestra; j, jugal; l, lacrimal; m, maxilla; m.fen, maxillary fenestra; n, nasal; nlc, nasolacrimal canal; oc, occipital condyle; p, parietal; pal, palatine; pf, prefrontal; pm, premaxilla; pm.fen, promaxillary fenestra; po, postorbital; ps, parasphenoid; q, quadrate; qj, quadratojugal; racq, ridge for accessory condyle of quadrate; sa, surangular; sp, splenial; sq, squamosal; stf, supratemporal fenestra.
Published: 23 November 2005
Fig. 2. Photographs and line drawings of the skull of G. brevipes (GIN 100/13) in right lateral view (A, D), right mandible in lateral view (B, E), and left mandible in medial view (C, F). an, angular; aof, antorbital fenestra; ar, articular; d, dentary; ect, ectopterygoid; emf, external
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Figure 1. A, “Oreinirostral” facial morphology. B, “Platyrostral” facial morphology. C, Oreinirostral Sphenosuchus (after Walker 1990), dorsal view. D, Ventral view. E, Platyrostral Alligator mississippiensis, dorsal view. F, Ventral view. Abbreviations: aof, antorbital fenestra; en, external naris; ltf, lower temporal fenestra; o, orbit; mf, mandibular fenestra; stf, supratemporal fenestra
Published: 01 November 2008
Figure 1. A, “Oreinirostral” facial morphology. B, “Platyrostral” facial morphology. C, Oreinirostral Sphenosuchus (after Walker 1990), dorsal view. D, Ventral view. E, Platyrostral Alligator mississippiensis , dorsal view. F, Ventral view. Abbreviations: aof, antorbital fenestra; en, external
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†Parapsephurus willybemisi n. gen. n. sp., digital reconstruction from tomography data of the skull roof; FAU.DGS.ND.161.4559.T. (1) Dorsal view. (2) Ventral view. Anterior facing left. Scale bar = 2 cm. afl = anterior fenestra longitudinalis; c3 = posterior bone of the c series; dpt = dermopterotic (= intertemporo-supratemporal of Grande and Bemis, 1991; see Grande et al., 2002); dsp = dermosphenotic; mfl = middle fenestra longitudinalis; pa = parietal; pfl = posterior fenestra longitudinalis; pt = posttemporal.
Published: 01 May 2023
Figure 5. † Parapsephurus willybemisi n. gen. n. sp., digital reconstruction from tomography data of the skull roof; FAU.DGS.ND.161.4559.T. ( 1 ) Dorsal view. ( 2 ) Ventral view. Anterior facing left. Scale bar = 2 cm. afl = anterior fenestra longitudinalis; c3 = posterior bone of the c series
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Figure 2
Published: 23 December 2015
fenestra; ec, ectopterygoid; en, external nares; fr, frontal; j, jugal; l, lacrimal; ltf, lower temporal fenestra; mx, maxilla; n, nasal; or, orbit; p, parietal; pa, palatine; pfr, prefrontal; pmx, premaxilla; po, postorbital; pt, pterygoid; q, quadrate
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Published: 01 September 2014
; LSTO=length of supratemporal opening; WSTO=width of supratemporal opening; LSTF=length of supratemporal fenestrae; WSTF=width of supratemporal fenestrae; LO=length of orbit; WO=width of orbit; LITF=length of infratemporal fenestrae; WITF=width of infratemporal fenestrae; LSY=length of symphysis
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Photographs and line drawings of the skull of G. brevipes (GIN 100/13) in left lateral view (A, D), left mandible in lateral view (B, E), and right mandible in medial view (C, F). an, angular; ar, articular; bs, basisphenoid; d, dentary; ect, ectopterygoid; emf, external mandibular fenestra; eo, exoccipital; f, frontal; fm, foramen magnum; fo, foramen; imf, internal mandibular fenestra; l, lacrimal; m, maxilla; m.fen, maxillary fenestra; n, nasal; nlc, nasolacrimal canal; oc, occipital condyle; p, parietal; pa, prearticular; pal, palatine; pf, prefrontal; pm, premaxilla; pm.fen, promaxillary fenestra; po, postorbital; ps, parasphenoid; pt, pterygoid; pt.h, hook of pterygoid; pt.pr, pterygoid process of quadrate; q, quadrate; qj, quadratojugal; sa, surangular; sc, sclerotic plate; so, supraoccipital; sp, splenial; sq, squamosal; stf, supratemporal fenestra.
Published: 23 November 2005
fenestra; eo, exoccipital; f, frontal; fm, foramen magnum; fo, foramen; imf, internal mandibular fenestra; l, lacrimal; m, maxilla; m.fen, maxillary fenestra; n, nasal; nlc, nasolacrimal canal; oc, occipital condyle; p, parietal; pa, prearticular; pal, palatine; pf, prefrontal; pm, premaxilla; pm.fen
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Figure 8. Ratio of fenestra : no fenestra peak Von Mises stress. A, Oreinirostral model. B, Platyrostral model. Key in A applies to both graphs
Published: 01 November 2008
Figure 8. Ratio of fenestra : no fenestra peak Von Mises stress. A, Oreinirostral model. B, Platyrostral model. Key in A applies to both graphs