Viséan Lithostrotionidae (Rugosa) from Zonguldak and Bart&amp;#305;n (NW Turkey)

Denayer, Julien

doi:10.3140/bull.geosci.1496

Cited by 12 publications

(8 citation statements)

References 25 publications

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“…Similar palaeokarsts of common origin were also recorded for example at Argenteau, in the VSA (Fig. 18, Poty & Delculée, 2011), at the top of the Viséan in the French Montagne Noire (Poty et al, 2002b) and in NW Turkey (Denayer, 2014).…”

Section: Warnantianmentioning

confidence: 69%

“…The Belgian Dinantian sequence stratigraphy, supported by robust biostratigraphic dates, was successfully extended to the Boulonnais in northern France (Hance et al, 2001), England (Hance et al, 2002), southern France (Poty et al, 2002b;Aretz, 2016, this volume), Poland , China (Poty et al, 2011b;Hance et al, 2011), NW Turkey (Denayer, 2014) and recently in Germany (Herbig, 2016, this volume). These correlations allowed us to check, to detail, to complete and to globalize the Belgian Dinantian sequence stratigraphy .…”

Section: Sequence Stratigraphymentioning

confidence: 99%

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The Dinantian (Mississippian) succession of southern Belgium and surrounding areas: stratigraphy improvement and inferred climate reconstruction

Poty¹

2016

Geol. Belg.

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ABSTRACT. The interactions between sea-level changes, local and global tectonics, and palaeoclimates have influenced the sedimentary deposition and the stratigraphy of the Belgian Dinantian. This paper emends the Belgian Dinantian sequence stratigraphy pattern and the third-order sequence 4 is divided into two sequences (4A, 4B). We also confirm that the sudden sea-level drop corresponding to the Hangenberg Sandstone at the Devonian -Carboniferous transition does not correspond to a third-order sequence boundary, but to an out-of-sequence event. The stratigraphy of the Tournaisian in the Namur, South Avesnois and Vesdre -Aachen sedimentation areas is clarified and leads to restrict the latter area to the Aachen vicinity only. The shape of the Namur -Dinant basin is revised and shows a migration of the depocenter northward during Dinantian times. During the Tournaisian, precession cycles are well developed and correspond to alternations of monsoon and dryer climates, without marked changes in the sea level. However, superimposed on these alternations, the Tournaisian third-order sequences recorded higher sea-level variations, which are considered to be due to glacioeustatism, indicating long-duration period of ice formation. The very strong fall in the sea-level at the Tournaisian -Viséan boundary is considered to record the development of an ice-cap and to a heralding change to the Carboniferous climate with glaciations. From that time (sequence 5), marked eccentricity parasequences developed during the Viséan, recording alternating shorter interglacial-glacial periods. Thus, the onset of the Carboniferous glaciations is as early as the Early Viséan and not in the Late Viséan as usually considered.

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Section: Warnantianmentioning

confidence: 69%

Section: Sequence Stratigraphymentioning

confidence: 99%

The Dinantian (Mississippian) succession of southern Belgium and surrounding areas: stratigraphy improvement and inferred climate reconstruction

Poty¹

2016

Geol. Belg.

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“…However, it is necessary for the study of additional areas in the eastern Mediterranean region, such as Turkey (Denayer, 2011;Denayer and Aretz, 2011) or Libya, where the knowledge of Upper Devonian stratigraphy and palaeontology is quite good, but the Mississippian is still little known (Fröhlich et al, 2009;Wehrmann et al, 2009). …”

Section: Comparison With Other Areas In North Africamentioning

confidence: 97%

Mississippian coral assemblages from the Khenifra area, Central Morocco: Biostratigraphy, biofacies, palaeoecology and palaeobiogeography

et al. 2013

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“…Lithostrotion termieri has several features in common with L. potii Denayer 2014 from the lower Viséan of NW Turkey, in its similar size and number of septa, and also L. sp. from the upper Viséan of NW Turkey (Denayer 2014;fi g. 16BC). However, it can be distinguished from L. potii by its thicker spindle-shaped columella, longer and thicker spindle-shaped major septa, many of which reach the columella, longer minor septa that extend into the tabularium, and shorter cardinal septum in a cardinal fossula.…”

Section: Systematic Palaeontologymentioning

confidence: 99%

“…The presence of both trends simultaneously in the late Viséan (cf. Denayer, 2014) is also shown by the fasciculate genus Siphonodendron (Poty, 1984;Denayer, 2014).…”

Section: T E R M I E R I P O S E S S O M E Q U E S T I O N S F R mentioning

confidence: 99%

New species of the rugose coral genus Lithostrotion Fleming in the upper Viséan from the Azrou-Khenifra Basin (Morocco)

Rodrı́guez

Somerville

Said³

2020

Spanish J. Palaeontol.

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The new species Lithostrotion termieri Rodríguez & Somerville is described. It shows very large corallites of the rugose genus Lithostrotion Fleming. It has been recorded up to now only in upper Viséan rocks from the type locality, the Akrab ridge, Morocco also called Tizi Ben Zizouit by Termier & Termier (1950), who identifi ed it as Lonsdaleia fl oriformis, and southeast from Tabainout, also from the Azrou-Khenifra Basin.

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Viséan Lithostrotionidae (Rugosa) from Zonguldak and Bartın (NW Turkey)

Cited by 12 publications

References 25 publications

The Dinantian (Mississippian) succession of southern Belgium and surrounding areas: stratigraphy improvement and inferred climate reconstruction

The Dinantian (Mississippian) succession of southern Belgium and surrounding areas: stratigraphy improvement and inferred climate reconstruction

Mississippian coral assemblages from the Khenifra area, Central Morocco: Biostratigraphy, biofacies, palaeoecology and palaeobiogeography

New species of the rugose coral genus Lithostrotion Fleming in the upper Viséan from the Azrou-Khenifra Basin (Morocco)

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