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Scaliognathus anchoralis

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Series: GSA Memoirs
Published: 01 January 1970
DOI: 10.1130/MEM127-p353
... zone. The occurrence of Pseudopolygnathus triangulus pinnatus in the Doliognathus latus fauna, accompanied in some places by Scaliognathus anchoralis , correlates with part of the S. anchoralis Zone in the German Sauerland. The upper Valmeyeran (Meramecian) zones are characterized...
Series: GSA Special Papers
Published: 01 January 1984
DOI: 10.1130/SPE196-p195
... are documented including a new discovery of Scaliognathus anchoralis . The absence, or near-absence, of conodonts from a significant portion of the Chadian to Asbian sequence is attributed to extreme water shallowness over very broad areas of the Dinantian shelf. It is suggested that lack of competition...
Image
Distribution of the most significant conodonts at the Tournaisian–Viséan t...
Published: 01 November 2006
. – Scaliognathus anchoralis; M. p. – Mestognathus praebeckmanni Zone; bisch. – Polygnathus bischoffi Zone ; anchoralislatus – S. anchoralis–Doliognathus latus Zone ; fairch. – S. fairchildi Zone.
Image
Correlation of former USSR local horizons (Urals and Russian Platform) and ...
Published: 01 January 2007
. a., Scaliognathus anchoralis; G., Gnathodus . The shaded area in the conodont zones column indicates the “ Gnathodus interzone”.
Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.6
EISBN: 9781862396944
... . The subgroup also spans the Zaphrentites delanouei and Caninophyllum patulum assemblage coral biozones ( Mitchell et al. 1982 ). The upper part of the overlying Cannington Reef Limestone spans the Scaliognathus anchoralis Biozone and contains the deep water index conodont Eotaphrus burlingtonensis O4...
FIGURES
Journal Article
Published: 01 November 2006
Geological Magazine (2006) 143 (6): 829-857.
.... – Scaliognathus anchoralis; M. p. – Mestognathus praebeckmanni Zone; bisch. – Polygnathus bischoffi Zone ; anchoralislatus – S. anchoralis–Doliognathus latus Zone ; fairch. – S. fairchildi Zone. ...
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Journal Article
Published: 01 January 2007
Journal of Foraminiferal Research (2007) 37 (1): 69-89.
.... a., Scaliognathus anchoralis; G., Gnathodus . The shaded area in the conodont zones column indicates the “ Gnathodus interzone”. ...
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Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.5
EISBN: 9781862396944
... such as Eotaphrus bultynki , Dollymae bouckaerti and Scaliognathus anchoralis have been noted. Coral faunas span the Zaphrentis delanouei and Caniniophyllum patulum assemblage biozones 0*8 , but their distribution on the ramp is diachronous (see Riley 1993 a ), the caniniod corals first appearing...
FIGURES
Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.4
EISBN: 9781862396944
... bivalves (e.g. Posidonia becheri), ammonoids (e.g. Neoglyphioceras spirale ), Cyrtosymbolinid and Griffithidinid trilobites, and conodonts of the Scaliognathus anchoralis , Gnathodus texanus and Gnathodus bilineatus zones +O~T2 indicating an early to late Visean age for the formation ( Leveridge...
FIGURES
Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.10
EISBN: 9781862396944
... ). The lower part of the formation in the Caldon Low Borehole (Fig. 32 , Col. 4) contains foraminifers indicative of the Cf4α1 subzone O2 ( Chisholm et al. 1988 ). At outcrop, late Tournaisian conodonts, including Scaliognathus anchoralis, have also been recorded at Brownend Quarry, near Waterhouses [SK...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1974
AAPG Bulletin (1974) 58 (2): 269-282.
... Canyon, and it is assumed that beds equivalent to the Tierra Blanca are missing because of an unconformity at that locality. Form species in faunal unit 4 include Doliognathus latus, Pseudopolygnathus triangulus pinnatus, P. triangulus n. subsp., Scaliognathus anchoralis, Staurognathus cruciformis...
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Book Chapter

Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.21
EISBN: 9781862396944
...). The base of the Waulsortian in the Dublin Basin lies substantially above the base of the Scaliognathus anchoralis conodont Biozone (Sevastopulo & Wyse Jackson 2009). The uppermost Argillaceous Limestones ( Morris et al. 2003 ) represents an informally defined unit, previously referred...
FIGURES
Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.3
EISBN: 9781862396944
... 1994 ). This taxon first appears slightly above the last occurrence of Scaliognathus anchoralis in many sections. The Visean/Serpukhovian (Namurian) boundary is currently defined by the first appearance of Lochriea ziegleri ( Nemyrovska 2005 ). Also, many authors equate the combined Lochriea...
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Journal Article
Published: 19 September 2018
Journal of Paleontology (2019) 93 (1): 126-136.
... Bank limestones with shales (Metcalfe, 1981 ), although specimens from this horizon have not been illustrated. The lowest figured occurrence of V . campbelli is from the late Tournaisian of the Pyrenees together with Scaliognathus anchoralis Branson and Mehl, 1941 (Marks and Wensink, 1970...
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Journal Article
Published: 10 September 2013
Geological Magazine (2014) 151 (2): 229-243.
... communis carina and the Scaliognathus anchoralis Zones and the lower part of the CC4 Zone ( Mestognathus praebeckmanni Subzone) (Groessens in Conil et al . 1991 ; Poty et al . 2006 ). Corals are common and diversified in the relatively shallow-water facies...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2005
AAPG Bulletin (2005) 89 (7): 897-919.
... the base of the Woodhurst-Paine sequence (figure 3 in Petty, 2003 ). A second transgression (event 19 in Sandberg et al., 1982 ) was placed at the boundary between the Gnathodus typicus Zone and the Scaliognathus anchoralis – Doliognathus latus Zone and was described as a major event that flooded...
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Journal Article
Published: 08 October 2013
Geological Magazine (2014) 151 (2): 269-298.
..., Palmatolepis sp., Hindeodella sp., Siphonodella cf. obsoleta Hass, Scaliognathus anchoralis Branson & Mehl. Lime breccia (sample 77/4) is composed of bioclasts and lithoclasts (micritic, algal, etc.) and contained a redeposited specimen of the early Viséan foraminifer...
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Series: Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP376.15
EISBN: 9781862396449
... contains no siphonodellides; B, Siphonodella sulcata–S. duplicata ; C, Siphonodella sandbergi ; D, Lower Siphonodella crenulata ; E, Upper Siphonodella crenulata ; F, Scaliognathus anchoralis ; G, Gnathodus typicus . U, M, L: Upper, Middle, Lower. The Steinberg section presented in this paper...
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Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.22
EISBN: 9781862396944
... ). The Limerick Limestone Formation is of late Courceyan age (Polygnathus bischoffi Subzone of Polygnathus mehli Local Range Biozone and Scaliognathus anchoralis Biozone) at the base; locally Gnathodus homopunctatus Biozone (Chadian) at the top (e.g. as at Buttevant) (Somerville & Jones 1985...
FIGURES
Series: SEPM Special Publication
Published: 01 January 2003
DOI: 10.2110/pec.03.78.0239
EISBN: 9781565763340
... of Waulsortian banks was in the succeeding Scaliognathus anchoralis Zone. This coincides with the Cf3-Cf4α1 Foraminifera zones and subzones of Conil et al. (1991) and Jones and Somerville (1996) . However, diagnostic taxa such as Tetrataxis, Eotextularia diversa , and Valvulinella are rare in the mounds...
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