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Goniatites lazarus

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Figure  8 — <b>Goniatites</b> <b>lazarus</b>  n. sp. and  Entogonites saharensis  n. sp. ...
Published: 01 February 2005
Figure 8 — Goniatites lazarus n. sp. and Entogonites saharensis n. sp. from the eastern Anti–Atlas of Morocco. 1, 2 , Goniatites lazarus n. sp., lateral and dorsal views of the holotype, GPIT 1851–97, ×1.5. 3 , Prolecanites sp. and a paratype of Entogonites saharensis n. sp., MB.C.5303
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Table  1 —Conch dimensions (mm) and proportions of  <b>Goniatites</b> <b>lazarus</b>  n. ...
Published: 01 February 2005
Table 1 —Conch dimensions (mm) and proportions of Goniatites lazarus n. sp. from Dar Kaoua
Journal Article
Published: 01 February 2005
Journal of Paleontology (2005) 79 (2): 356–365.
...Figure 8 — Goniatites lazarus n. sp. and Entogonites saharensis n. sp. from the eastern Anti–Atlas of Morocco. 1, 2 , Goniatites lazarus n. sp., lateral and dorsal views of the holotype, GPIT 1851–97, ×1.5. 3 , Prolecanites sp. and a paratype of Entogonites saharensis n. sp., MB.C.5303...
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Figure  3 —External suture lines of species of  <b>Goniatites</b>  de Haan, 1825 ....
Published: 01 February 2005
GPIT 1875–78 from Taouz, ×6, D = 15 mm, from Korn et al., 2003 . 6 , Goniatites lazarus n. sp., holotype GPIT 1851–97 from Erfoud, ×2, D = 36 mm, W = 27 mm. 7 , Goniatites lazarus n. sp., paratype MB.C.5307 from Erfoud, ×2, D = 42 mm, W = 32 mm
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Figure  9 —Diagrams showing the growth-line course of species of  <b>Goniatite</b>...
Published: 01 February 2005
Figure 9 —Diagrams showing the growth-line course of species of Goniatites , ×2. 1 , Goniatites crenistria , specimen WMN 10080 from Herdringen (from Korn, 1988 ), D = 39.6 mm, W = 25.4 mm. 2, G. crenistria , holotype BM NH c282 from Bolland, D = 36.8 mm, W = 24.2 mm. 3 , G. lazarus n. sp
Journal Article
Journal: Paleobiology
Published: 01 January 2003
Paleobiology (2003) 29 (3): 329–348.
... of successive ammonoid faunas across the Devonian/Carboniferous boundary were documented by Korn (2000) . Detailed inquiries into the whorl expansion rate and umbilical width refuted the common assumption, proposed by Nikolaeva and Barskov (1994) , that the earliest Carboniferous goniatites rapidly occupied...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP423.14
EISBN: 9781862399556
... , 1992 b ). Reitenberg road section and Schaumberg, both between Iserlohn-Östrich and -Grürmannsheide, with two Annulata Black Shales, dark-grey to olive-green weathering ( Schmidt 1924 ; Becker 1992 b ), followed by a green shale with abundant platyclymeniids, goniatites, brachiopods and trilobites...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP423.6
EISBN: 9781862399556
... Valisettes, Barvaux, Aisemont (middle member) and Lambermont formations (Fig. 2 ). They can be black, as is sometimes the case for those of the Matagne Formation, but are more generally dark-grey, greenish, brownish or purple. Besides nektonic organisms such as goniatites and cricoconarids ( Matern 1931...
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Journal Article
Journal: Geology
Published: 01 August 2000
Geology (2000) 28 (8): 675–678.
... their ecological position in the Famennian with the evolution of totally new families of goniatites ( Becker and House, 1994 ). More than half of the species of placoderm fish did not survive, and one-third of the surviving placoderm families lost all of their marine members and became exclusively fresh water...
FIGURES
Journal Article
Published: 01 January 2020
Journal of Paleontology (2020) 94 (1): 99–114.
... for one or more of these taxa (i.e., extensive Lazarus species). We have a limited knowledge of the ontogeny of Cyphaspides (see the following). At present, we lack information on such features as the form of the hypostome (aulacopleurid hypostomes are usually rather simple and not particularly...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP423.9
EISBN: 9781862399556
... Exshaw Formation of the type region (e.g. Jura Creek, Crowsnest Pass), between pre-crisis Black Shale Member and lower Tournaisian Siltstone Member, including the goniatite bed ( Macqueen & Sandberg 1970 ; Richards & Higgins 1988 ; Johnston et al. 2010 ); below typical Banff Formation...
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Journal Article
Published: 01 July 2001
Journal of Paleontology (2001) 75 (4): 783–807.
... to reappear as Lazarus taxa in the latest Devonian and Early Mississippian more than 15 to 20 m.y. later. While Baumiller's (1992) data shows an exceptionally high rate of crinoid extinction at the Givetian-Frasnian boundary, the reappearance of Lazarus crinoid taxa in the latest Devonian and Tournaisian...
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Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2002
DOI: 10.2110/pec.02.72.0181
EISBN: 9781565761940
... ). Though some of the stromatoporoids survived as rare Lazarus taxa in the Famennian, especially the domed or laminar labechiids and some stick-like amphiporids, these weregreatly reduced in diversity, with few stromatoporoid reef localities known, and thelaststromatoporoidsdiedoutinthe late Famennian...
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Journal Article
Published: 21 November 2016
Geological Magazine (2018) 155 (3): 586–629.
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