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Goniatites lazarus

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Figure8—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, ×1.25. 4, 5, Goniatites lazarus n. sp., ventral and lateral views of the paratype, MB.C.5307, ×1. 6, Close-up of part of the body chamber of the same specimen with two paratypes of Entogonites saharensis n. sp. (arrows pointing at specimens) and a disarticulated trilobite identified as Archegonus sp., ×2. 7, 8, Entogonites saharensis n. sp., lateral and dorsal views of the holotype, MB.C.5301, ×5. 9, Entogonites saharensis n. sp., lateral and dorsal views of a paratype, MB.C.5304, ×10. 10, Entogonites saharensis n. sp., lateral and dorsal views of a paratype, MB.C.5305, ×10. 11, 12, Entogonites saharensis n. sp., lateral and dorsal views of a paratype, MB.C.5302, ×10
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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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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Figure3—External suture lines of species of Goniatitesde Haan, 1825. 1, Goniatites hudsoniBisat, 1934, specimen WMN 11071 from Rüthen, ×3, D = 30 mm, from Korn, 1990. 2, Goniatites crenistriaPhillips, 1836, specimen WMN 10080 from Herdringen, ×4, W = 22.0 mm, from Korn, 1988. 3, Goniatites fimbriatus (Foord and Crick, 1897), specimen WMN 11063 from Nehden, ×4, D = 23 mm, from Korn, 1990. 4, Goniatites spiriferRoemer, 1850, specimen WMN 11071 from Scharfenberg, ×3.5, D = 27 mm, from Korn, 1990. 5, Progoniatites maghribensisKorn et al., 2003, holotype 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
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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Figure9—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., holotype GPIT 1851–97 from Erfoud, D = 36 mm, W = 27 mm
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.
.../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 the morphospace abandoned by the clymeniid...
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Journal Article
Journal: Geology
Published: 01 August 2000
Geology (2000) 28 (8): 675–678.
.... , 1995 , Entities in the ecological hierarchy and the comparison between neontology and paleontology : Geological Society of America Abstracts with Programs , v. v. 27 pp. A168 . Becker , R.T. , and House , M.R. , 1994 , Kellwasser events and goniatite successions in the Devonian...
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Journal Article
Published: 01 January 2020
Journal of Paleontology (2020) 94 (1): 99–114.
... (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 distinctive or useful for taxonomy...
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Book Chapter

Author(s)
S. V. Nikolaeva
Series: Geological Society, London, Special Publications
Published: 13 April 2022
DOI: 10.1144/SP512-2020-229
EISBN: 9781786205827
... in the Entogonites–Maxigoniatites Zone show the co-occurrence of Entogonites saharense and Goniatites lazarus (in Dar Kaoua) ( Korn et al. 2007 ); the assemblage also contains Bollandoceras , Beyrichoceras , Beyrichoceratoides , Calygirtyoceras and Merocanites ( Delépine 1941 ; Pareyn 1961 ; Korn et...
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Journal Article
Published: 01 July 2001
Journal of Paleontology (2001) 75 (4): 783–807.
... of the Middle Devonian only 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...
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Series: Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP423.14
EISBN: 9781862399556
... eustatic low of the main part of the middle Famennian (see the global sea-level curve of Johnson et al. 1985 , with refinements in Becker 1993 b ). The Upper Annulata Event is often followed by goniatite-rich limestones, the ‘Wagnerbank’ of the Thuringian Bohlen section (e.g. Schindewolf 1952...
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Journal Article
Published: 21 November 2016
Geological Magazine (2018) 155 (3): 586–629.
... Lazarus Taxa are B. stabilis stabilis (= stabilis Morphotype 2) and Pa. gracilis sigmoidalis. Conodont–ammonoid correlation . In the Tafilalt, the base of the B. ultimus ultimus Zone is directly correlated with the onset of the Kallo. subarmata Zone at M'karig (Kaiser, 2005 : Bed 18; see...
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Series: Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP423.6
EISBN: 9781862399556
... in Western Europe is focused on deep-setting sections where the sedimentary record is extremely condensed, but usually well dated by conodonts and goniatites, contrary to their contemporaneous equivalents in ramp and platform settings. However, the historical type area of the Frasnian and Famennian stages...
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Series: Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP423.9
EISBN: 9781862399556
... Morocco (new records). The genus must have survived in unknown refugia regions and became a Lazarus Taxon. Plants/miospores The uppermost Famennian was characterized globally by a surprisingly similar vegetation composed of the widespread Retispora lepidophyta palynomorph assemblages of coastal...
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Series: SEPM Special Publication
Published: 01 January 2002
DOI: 10.2110/pec.02.72.0181
EISBN: 9781565761940
... patch reef or thicket is known, and it is small ( Poty, 1999 ). 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...
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