Conodonts from the lowermost Ordovician strata of South-Central Sweden

Lindström, Maurits

doi:10.1080/11035895409453581

Cited by 234 publications

(199 citation statements)

References 9 publications

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“…nov. and unidentified lingulides, and the conodonts Baltoniodus aff. B. triangularis (Lindström, 1955) and Drepanoistodus sp. (sample MG10002/1).…”

Section: Seyahou Formationmentioning

confidence: 99%

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Dapingian-lower Darriwilian (Ordovician) stratigraphic gap in the Faraghan Mountains, Zagros Ranges, south-eastern Iran

Ghavidel‐Syooki¹,

Popov²,

Álvaro³

et al. 2014

Bull. Geosci.

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The Lower-Middle Ordovician sediments exposed in the Faraghan Mountains, south-eastern Zagros Ranges, represent a condensed succession of siliciclastic-dominated rocks rich in palynomorph assemblages (acritarchs and subsidiary chitinozoans) and sparse shelly concentrations bearing biostratigraphically significant brachiopods and conodonts. The Lower Ordovician Zard-Kuh Formation comprises coarse-grained siliciclastic deposits rich in Cruziana ichnofossils. The lower 80 m of the overlying Seyahou Formation, late Floian to Katian in age, form a heterolithic succession composed of black and green shales, subarkoses and silty limestones. Its lower part is punctuated by a centimetric phosphoarenite that contains lingulate brachiopods (Atansoria yaseri sp. nov.) and conodonts (Baltoniodus aff. B. triangularis Lindström and Drepanoistodus sp.) that suggest a latest Floian age. The top of the condensed phosphoarenite is marked by a considerable hiatus that ranges the Dapingian and early Darriwilian interval. Overlying the hiatus, the Seyahou Formation comprises two fossiliferous levels, the oldest dated as mid-Darriwilian with chitinozoans characteristic of the Siphonochitina formosa Zone, and the youngest of the Katian Acanthochitina barbata Zone. Mid Ordovician phosphogenesis associated with starvation, reworking, resedimentation, and the onset of distinct stratigraphic gaps was a complex process recorded throughout the Arabian margin of Gondwana. In the Zagros Ranges, maximum flooding and phosphate precipitation are suggested as the counterpart of the Helskjer Drowning Event of Baltoscandia and the third-order maximum flooding surface that punctuates the Siphonochitina formosa Zone in North Africa.•

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“…nov. and unidentified lingulides, and the conodonts Baltoniodus aff. B. triangularis (Lindström, 1955) and Drepanoistodus sp. (sample MG10002/1).…”

Section: Seyahou Formationmentioning

confidence: 99%

“…-Prioniodus navis Lindström, 1955; Middle Ordovician, Dapingian, Baltoscandia. Figure 10A-J 2011 Baltoniodus sp.…”

Section: Genus Baltoniodus Lindström 1971mentioning

confidence: 99%

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Dapingian-lower Darriwilian (Ordovician) stratigraphic gap in the Faraghan Mountains, Zagros Ranges, south-eastern Iran

Ghavidel‐Syooki¹,

Popov²,

Álvaro³

et al. 2014

Bull. Geosci.

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“…The latter consists of dominantly hyaline elements. Moreover, some specimens ascribed to Oelandodus elongatus (Lindstro¨m, 1955) and Oelandodus? costatus van Wamel, 1974 by Bagnoli et al (1988, pl.…”

Section: Protoprioniodus Mctavish 1973mentioning

confidence: 99%

Conodont fauna and biostratigraphy of the Honghuayuan Formation (Early Ordovician) of Guizhou, South China

Zhen

Percival

Liu

et al. 2009

Alcheringa: An Australasian Journal of Palaeontology

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“…Extensive recent work on Early Ordovician conodonts in th e Balto-Scandic area has made it possible to establish a detailed conodont zonation (Lindstrom , 1955(Lindstrom , , 1957(Lindstrom , , 1971Serge eva , 1962Serge eva , , 1963Serge eva , , 1964Viira, 1967Viira, , 1970Bergstrom , 1968). The id entified species in the coll ec tions from the Hamburg klippe and South Catcher Pond, as well as those of the small Cow Head collection mentioned above, are charac teristic of a very restricted stratigraphic interval in th e lower parl of th e lower Aren igian of Sweden ( fig.…”

Section: Biostratigraphic Significancementioning

confidence: 99%

Geological Survey research 1972

1972

Professional Paper

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Conodonts from the lowermost Ordovician strata of South-Central Sweden

Cited by 234 publications

References 9 publications

Dapingian-lower Darriwilian (Ordovician) stratigraphic gap in the Faraghan Mountains, Zagros Ranges, south-eastern Iran

Dapingian-lower Darriwilian (Ordovician) stratigraphic gap in the Faraghan Mountains, Zagros Ranges, south-eastern Iran

Conodont fauna and biostratigraphy of the Honghuayuan Formation (Early Ordovician) of Guizhou, South China

Geological Survey research 1972

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