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Journal Article

Middle Ordovician (middle Darriwilian) Archaeospicularia and Entactinaria (radiolarians) from the Table Cove Formation, Piccadilly Quarry, Newfoundland, Canada Open Access

Sarah Kachovich, Jonathan C. Aitchison
Published: 01 September 2021
Journal of Paleontology (2021) 95 (5): 913–943.
DOI: https://doi.org/10.1017/jpa.2021.18
...Sarah Kachovich; Jonathan C. Aitchison Abstract New, distinctive, well-preserved and previously undescribed constituents of a Middle Ordovician (middle Darriwilian, Dw2) radiolarian assemblage from the Table Cove Formation in Newfoundland are described. Three-dimensional X-ray micro-computed...
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View PDF for article title, Middle Ordovician (middle Darriwilian) Archaeospicularia and Entactinaria (radiolarians) from the <span class="search-highlight">Table</span> <span class="search-highlight">Cove</span> <span class="search-highlight">Formation</span>, Piccadilly Quarry, Newfoundland, Canada
Add to Citation Manager for Middle Ordovician (middle Darriwilian) Archaeospicularia and Entactinaria (radiolarians) from the <span class="search-highlight">Table</span> <span class="search-highlight">Cove</span> <span class="search-highlight">Formation</span>, Piccadilly Quarry, Newfoundland, Canada
Journal Article

Ordovician graptolites from the Middle Table Head Formation at Black Cove, near Port Au Port, Newfoundland Free

R. W. Morris, Marshall Kay
Published: 01 September 1966
Journal of Paleontology (1966) 40 (5): 1223–1229.
Add to Citation Manager for Ordovician graptolites from the Middle <span class="search-highlight">Table</span> Head <span class="search-highlight">Formation</span> at Black <span class="search-highlight">Cove</span>, near Port Au Port, Newfoundland
Image
Stratigraphic column of Table Cove Formation at Section TCM, near Marechal Island, Hare Bay, Great Northern Peninsula, western Newfoundland. Horizons from which material is illustrated are shown. Light colored lithologies are limestones; dark interbeds are calcareous shales. Wavy symbols next to the column indicate beds that are debris flows.

Stratigraphic column of Table Cove Formation at Section TCM, near Marechal ... Open Access

Published: 01 September 2022
Figure 1. Stratigraphic column of Table Cove Formation at Section TCM, near Marechal Island, Hare Bay, Great Northern Peninsula, western Newfoundland. Horizons from which material is illustrated are shown. Light colored lithologies are limestones; dark interbeds are calcareous shales. Wavy
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Forteyaspis idoli sp. nov. from Section TCM 18, Table Cove Formation (Darriwilian), near Marechal Island, Hare Bay, northeastern Great Northern Peninsula, western Newfoundland, Canada. (a, e, i) Cranidium, GSC 140019, dorsal, right lateral, and anterior views, ×17. (b, f, j) Cranidium, GSC 140020, dorsal, left lateral, and anterior views, ×20. (c, g, k) Cranidium, GSC 140021, dorsal, left lateral, and anterior views, ×20. (d, h, l) Cranidium, GSC 140022, dorsal, left lateral, and anterior views, ×25. (m–o) Cranidium, GSC 140023, dorsal, anterior, and right lateral views, ×30. (p) Cranidium, GSC 140024, dorsal view, ×30. (q) Cranidium, GSC 140025, dorsal view, ×40. (r) Cranidium, GSC 140026, dorsal view, ×40. (s, v) Right librigena, GSC 140027, ventrolateral and external views, ×12. (t, u) Right librigena, GSC 140028, internal and external views, ×15. (w, z, aa) Left librigena, GSC 140029, ventrolateral, external, and internal views, ×15. (x) Right librigena, GSC 140030, external view, ×15. (y) Cranidium, GSC 140031, dorsal view, ×40. (bb) Right librigena, GSC 140032, external view, ×17. (cc) Right librigena, GSC 140033, external view, ×17. (dd) Left librigena, GSC 140034, external view, ×15. (ee) Right librigena, GSC 140035, external view, ×15. (ff) Left librigena, GSC 140036, external view, ×15. (gg) Right librigena, GSC 140037, external view, ×15.

Forteyaspis idoli sp. nov. from Section TCM 18, Table Cove Formation (Darr... Available to Purchase

Published: 04 February 2022
Fig. 4. Forteyaspis idoli sp. nov. from Section TCM 18, Table Cove Formation (Darriwilian), near Marechal Island, Hare Bay, northeastern Great Northern Peninsula, western Newfoundland, Canada. ( a, e, i ) Cranidium, GSC 140019, dorsal, right lateral, and anterior views, ×17. ( b , f , j
Image
Forteyaspis idoli sp. nov. from Section TCM 18, Table Cove Formation (Darriwilian), near Marechal Island, Hare Bay, northeastern Great Northern Peninsula, western Newfoundland, Canada. (a, e, i, q, u) Pygidium, GSC 140038, dorsal, posterior, ventral, anterior, and left lateral views, ×15. (b, c, f) Pygidium, GSC 140039, dorsal, left lateral, and posterior views, ×15. (d, g, h) Pygidium, GSC 140040, dorsal, left lateral, and posterior views, ×15. (j, m, n) Pygidium, GSC 140041, dorsal, right lateral, and posterior views, ×15. (k, l, o) Pygidium, GSC 140042, dorsal, posterior, and left lateral views, ×15. (p, s, t, x, dd) Pygidium, GSC 140043, dorsal, left lateral, posterior, anterior, and ventral views, ×15. (r, w, bb) Pygidium, GSC 140044, dorsal, right lateral, and posterior views, ×15. (v, y, z) Pygidium, GSC 140045, dorsal, right lateral, and posterior views, ×15. (aa, ee, ff) Pygidium, GSC 140046, left lateral, dorsal, and posterior views, ×17. (cc, gg, hh) Pygidium, GSC 140047, right lateral, dorsal, and posterior views, ×14.

Forteyaspis idoli sp. nov. from Section TCM 18, Table Cove Formation (Darr... Available to Purchase

Published: 04 February 2022
Fig. 5. Forteyaspis idoli sp. nov. from Section TCM 18, Table Cove Formation (Darriwilian), near Marechal Island, Hare Bay, northeastern Great Northern Peninsula, western Newfoundland, Canada. ( a , e , i , q , u ) Pygidium, GSC 140038, dorsal, posterior, ventral, anterior, and left lateral
Image
Stratigraphic context of the Table Cove Formation at the Piccadilly Quarry. (1) Lithostratigraphic log (after Maletz and Egenhoff, 2011; Kachovich and Aitchison, 2020) showing the sampled levels (PD01, -03, -05, -07, -09, -11, -12, and -13). Generalized stratigraphy after Knight (1991) and James et al. (1987); (2) field photo, facing southwest, of the exposure of gently dipping beds of rhythmically bedded limestone. Reprinted with permission from Kachovich and Aitchison (2020, fig. 3).

Stratigraphic context of the Table Cove Formation at the Piccadilly Quarry.... Open Access

Published: 01 September 2021
Figure 2. Stratigraphic context of the Table Cove Formation at the Piccadilly Quarry. ( 1 ) Lithostratigraphic log (after Maletz and Egenhoff, 2011 ; Kachovich and Aitchison, 2020 ) showing the sampled levels (PD01, -03, -05, -07, -09, -11, -12, and -13). Generalized stratigraphy after Knight
Image
Stratigraphic context of the Table Cove Formation at the Piccadilly Quarry: (1) lithostratigraphic log after Maletz and Egenhoff (2011) showing the sampled levels (PD01, -03, -05, -07, -09, -11, -12, and -13). Generalized stratigraphy after Knight (1991) and James et al. (1987); (2) field photo, facing southwest, of the exposure of gently dipping beds of rhythmically bedded limestone.

Stratigraphic context of the Table Cove Formation at the Piccadilly Quarry:... Open Access

Published: 01 May 2020
Figure 3. Stratigraphic context of the Table Cove Formation at the Piccadilly Quarry: ( 1 ) lithostratigraphic log after Maletz and Egenhoff ( 2011 ) showing the sampled levels (PD01, -03, -05, -07, -09, -11, -12, and -13). Generalized stratigraphy after Knight ( 1991 ) and James et al. ( 1987
Image
Figure3—Microfossils from Middle Ordovician Table Cove Formation in western Newfoundland. 1, Conodont Protopanderodus aff. rectus (Lindström, 1955), X120, ROM 46924. 2, Conodont Cordylodus horridus Barnes and Poplawski, 1973, X80, ROM 46925. 3, 4, Scolecodont X120, ROM 46926, ROM 46927. 5, Graptolite Archiclimacograptus sp. X40, ROM 46928. 6, 7, Problematicum Konyrium varium Nazarov and Popov, 1976, arrow indicates a surviving central column, X120, ROM 46929, ROM 46930. 8–10, Radiolarian Inanibigutta sp. X120, X160, X160, ROM 46931, ROM 46932, ROM 46933

Figure 3 —Microfossils from Middle Ordovician Table Cove Formation in west... Available to Purchase

Published: 01 May 2000
Figure 3 —Microfossils from Middle Ordovician Table Cove Formation in western Newfoundland. 1, Conodont Protopanderodus aff. rectus (Lindström, 1955), X120, ROM 46924. 2, Conodont Cordylodus horridus Barnes and Poplawski, 1973, X80, ROM 46925. 3, 4, Scolecodont X120, ROM 46926, ROM
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Figure4—Sponge spicules from Middle Ordovician Table Cove Formation in western Newfoundland. 1–4, Slightly curved oxeas, X40, ROM 46881, ROM 46882, ROM 46883, ROM 46884. 5, Cluster of oxeas, X80, ROM 46885. 6, Clavule with long thin rhabdome and rays, X65, ROM 46886. 7, Anchorate root tuft, X80, ROM 46887. 8, Anchorate root tuft with another set of shorter rays on thin rhabdome, X80, ROM 46888. 9, 10, Bent spicules, X80, ROM 46889, ROM 46890. 11, Modified pentactine with long curved rays, X80, ROM 46891. 12, Modified pentactine with three straight lateral rays, X40, ROM 46892. 13, 14, Hexactines, X80, X40, ROM 46893, ROM 46894. 15, Tetract with flattened rays, X80, ROM 46895. 16, 17, Pinnular pentactines, X80, ROM 46896, ROM 46897. 18, Modified tetract with one stunted ray, X80, ROM 46898. 19, Modified pentactine with one stunted ray, X80, ROM 46899. 20, Modified hexactine with short rhabdome and one pair long and one pair short lateral rays, X80, ROM 46900. 21–25, Hexactines with one short and spinose ray; 21, with long lateral rays, X65, ROM 46901; 22, 24, with short lateral rays, X80, ROM 46902, ROM 46904; 23, with slightly curved lateral rays, X160, ROM 46903; 25, detail of 24, showing axial canal and spines on the short stubby ray, X320

Figure 4 —Sponge spicules from Middle Ordovician Table Cove Formation in w... Available to Purchase

Published: 01 May 2000
Figure 4 —Sponge spicules from Middle Ordovician Table Cove Formation in western Newfoundland. 1 – 4, Slightly curved oxeas, X40, ROM 46881, ROM 46882, ROM 46883, ROM 46884. 5, Cluster of oxeas, X80, ROM 46885. 6, Clavule with long thin rhabdome and rays, X65, ROM 46886. 7, Anchorate root
Image
Figure5—Sponge spicules from Middle Ordovician Table Cove Formation in western Newfoundland. 1, Spinose uncinate, X65, ROM 46905. 2–8, Acanthohexactines; 2, with one curved ray, X80, ROM 46906; 3, 6, with short spines only on rhabdome, X40, ROM 46907, ROM 46908; 4, with two long rays, short spines only on rhabdomes and bases of rays, X40, ROM 46909; 5, broken acanthohexactine fully spinose, showing axial canal, X65, ROM 46910; 7, 8, strongly modified acanthohexactines; 7, with spines only on bases of rays, X150, ROM 46911; 8, with spines only on one side of rays, X150, ROM 46912. 9, Spinose tetraene, X135, ROM 46913. 10–13, Acanthopentactines; 10, spines only on bases of rhabdome and rays, X40, ROM 46914; 11, short spines on rays, X80, ROM 46915; 12, spines on bases of rhabdome and rays, X160, ROM 46916; 13, spines only on the bases of rays, X80, ROM 46917. 14–16, Partially fused dendroclones; 14, arrow indicates zygome articulation, X80, ROM 46918; 15, same specimen as 14 viewed from different direction; 16, X80, ROM 46919. 17, Possible rhizoclone X80, ROM 46920. 18–20, Isolated dendroclones, X80, ROM 46921, ROM 46922, ROM 46923

Figure 5 —Sponge spicules from Middle Ordovician Table Cove Formation in w... Available to Purchase

Published: 01 May 2000
Figure 5 —Sponge spicules from Middle Ordovician Table Cove Formation in western Newfoundland. 1, Spinose uncinate, X65, ROM 46905. 2 – 8, Acanthohexactines; 2, with one curved ray, X80, ROM 46906; 3, 6, with short spines only on rhabdome, X40, ROM 46907, ROM 46908; 4, with two long rays
Journal Article

Middle Ordovician Table Head Group of western Newfoundland: a revised stratigraphy Free

Colin F. Klappa, Paul R. Opalinski, Noel P. James
Published: 01 August 1980
Canadian Journal of Earth Sciences (1980) 17 (8): 1007–1019.
DOI: https://doi.org/10.1139/e80-101
... calcarenites and shales with lime megabreccias. Four new formation names are proposed: Table Point Formation (previously lower Table Head); Table Cove Formation (previously middle Table Head); Black Cove Formation (previously upper Table Head); and Cape Cormorant Formation (previously Caribou Brook formation...
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Journal Article

Carbonate platform to foreland basin: revised stratigraphy of the Table Head Group (Middle Ordovician), western Newfoundland Free

Sheila R. Stenzel, Ian Knight, Noel P. James
Published: 01 January 1990
Canadian Journal of Earth Sciences (1990) 27 (1): 14–26.
DOI: https://doi.org/10.1139/e90-002
.... The stratigraphy of Klappa, Opalinski, and James is here revised to reflect better understanding of lithologic units within this complex tectono-stratigraphic assemblage. The Table Head Group now contains only three formations: the Table Point and Table Cove formations, as originally defined, and the Cape...
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Journal Article

In situ lingulids from deep-water carbonates of the Middle Ordovician Table Head Group of Newfoundland and the Trenton Group of Quebec Free

R. K. Pickerill, T. L. Harland, D. Fillion
Published: 01 February 1984
Canadian Journal of Earth Sciences (1984) 21 (2): 194–199.
DOI: https://doi.org/10.1139/e84-021
... regarding Palaeozoic lingulid ecology. First, they represent one of the few recordings of in situ lingulids in carbonate substrates of Palaeozoic age and, second, they occur mainly in outer shelf and upper slope sediments (Grondines Member of Neuville Formation, Trenton Group, and Table Cove Formation...
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Journal Article

The Ordovician trilobite Oenonella and the new family Oenonellidae, with new species from western Newfoundland, Canada Open Access

Jonathan M. Adrain, Richard A. Fortey
Published: 01 September 2022
Journal of Paleontology (2022) 96 (5): 1061–1077.
DOI: https://doi.org/10.1017/jpa.2022.22
...Figure 1. Stratigraphic column of Table Cove Formation at Section TCM, near Marechal Island, Hare Bay, Great Northern Peninsula, western Newfoundland. Horizons from which material is illustrated are shown. Light colored lithologies are limestones; dark interbeds are calcareous shales. Wavy...
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Journal Article

Micro-CT study of Middle Ordovician Spumellaria (radiolarians) from western Newfoundland, Canada Open Access

Sarah Kachovich, Jonathan C. Aitchison
Published: 01 May 2020
Journal of Paleontology (2020) 94 (3): 417–435.
DOI: https://doi.org/10.1017/jpa.2019.88
...Figure 3. Stratigraphic context of the Table Cove Formation at the Piccadilly Quarry: ( 1 ) lithostratigraphic log after Maletz and Egenhoff ( 2011 ) showing the sampled levels (PD01, -03, -05, -07, -09, -11, -12, and -13). Generalized stratigraphy after Knight ( 1991 ) and James et al. ( 1987...
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Journal Article

A VARIED MIDDLE ORDOVICIAN SPONGE SPICULE ASSEMBLAGE FROM WESTERN NEWFOUNDLAND Available to Purchase

XI-GUANG ZHANG, BRIAN R. PRATT
Published: 01 May 2000
Journal of Paleontology (2000) 74 (3): 386–393.
DOI: https://doi.org/10.1666/0022-3360(2000)074<0386:AVMOSS>2.0.CO;2
...Figure 3 —Microfossils from Middle Ordovician Table Cove Formation in western Newfoundland. 1, Conodont Protopanderodus aff. rectus (Lindström, 1955), X120, ROM 46924. 2, Conodont Cordylodus horridus Barnes and Poplawski, 1973, X80, ROM 46925. 3, 4, Scolecodont X120, ROM 46926, ROM...
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Figure2—Schematic stratigraphic section of the Middle Ordovician Table Cove Formation as exposed in Piccadilly Quarry, Port au Port Peninsula, western Newfoundland. Sponge spicules occur in the shale-argillaceous limestone sequence. Arrow indicates the approximate position of the two productive horizons

Figure 2 —Schematic stratigraphic section of the Middle Ordovician Table C... Available to Purchase

Published: 01 May 2000
Figure 2 —Schematic stratigraphic section of the Middle Ordovician Table Cove Formation as exposed in Piccadilly Quarry, Port au Port Peninsula, western Newfoundland. Sponge spicules occur in the shale-argillaceous limestone sequence. Arrow indicates the approximate position of the two productive
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List of archaeospicularians, entactinarians, and other radiolarians of unce... Open Access

Published: 01 September 2021
Table 1. List of archaeospicularians, entactinarians, and other radiolarians of uncertain affinity from the Table Cove Formation, Piccadilly Quarry, Newfoundland, Canada, with numbers of specimens recovered indicating the relative abundance of different taxa and faunal diversity
Journal Article

Middle Ordovician Table Head Formation, Western Newfoundland Available to Purchase

H. B WHITTINGTON, C. H KINDLE
Journal: GSA Bulletin
Published: 01 June 1963
GSA Bulletin (1963) 74 (6): 745–758.
DOI: https://doi.org/10.1130/0016-7606(1963)74[745:MOTHFW]2.0.CO;2
...H. B WHITTINGTON; C. H KINDLE Abstract At the type section the Table Head Formation is about 1110 feet thick, resting disconformably on the Lower Ordovician St. George Formation, overlain apparently conformably by unnamed gray siltstones and green sandstones. An informal subdivision of the Table...
View PDF for article title, Middle Ordovician <span class="search-highlight">Table</span> Head <span class="search-highlight">Formation</span>, Western Newfoundland
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A new assemblage of juvenile Ediacaran fronds from the Drook Formation, Newfoundland Available to Purchase

Alexander G. Liu, Duncan McIlroy, Jack J. Matthews, Martin D. Brasier
Published: 01 July 2012
Journal of the Geological Society (2012) 169 (4): 395–403.
DOI: https://doi.org/10.1144/0016-76492011-094
...Alexander G. Liu; Duncan McIlroy; Jack J. Matthews; Martin D. Brasier Abstract A new assemblage of frondose and filamentous Ediacaran macrofossils is reported from the upper Drook Formation of Pigeon Cove, Newfoundland. The frondose forms, all less than 3 cm in length, are considered to represent...
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