Late Chadian–early Arundian high-resolution biostratigraphy in
the Ogmore-by- Sea section (South Wales–Mendip shelf) and the
mid-Avonian unconformity

J 2014

Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity

KALVODA, Jiří; John NUDDS; Ondřej BÁBEK a Cindy HOWELLS

Základní údaje

Originální název

Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity

Autoři

KALVODA, Jiří; John NUDDS; Ondřej BÁBEK a Cindy HOWELLS

Vydání

Journal of the Geological Society, London, Geological society, 2014, 0016-7649

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 2.639

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/14:00075360

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

Carboniferous;Foraminifers;Sequence stratigraphy;Correlations

Štítky

AKR, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 13. 3. 2018 15:34, prof. RNDr. Jiří Kalvoda, CSc.

Anotace

V originále

The study of the foraminiferal fauna in the Ogmore section in south Wales produced a detailed late Chadian–early Arundian biostratigraphy and sequence stratigraphy with a higher resolution than in the Arundian stratotype in Hobbyhorse Bay. The earliest Visean (late Chadian) pedogenic horizon close to the Gully Oolite and Caswell Bay Mudstone boundary (MFZ9) corresponds to the mid-Avonian unconformity. The entry of primitive archaediscids of MFZ10 within the Caswell Bay Mudstone is followed by more advanced archaediscids of MFZ11 at the base of the High Tor Limestone. The mid-Avonian unconformity at the Chadian–Arundian boundary is not confined to the London–Brabant Massif, but is also present in central Europe, the East European Platform, the Urals, west Siberia and probably also in Kuzbass and North America. The global extent of the the mid-Avonian unconformity suggests that it is a consequence of early to mid-Visean glacioeustacy

Citovat

KALVODA, Jiří; John NUDDS; Ondřej BÁBEK a Cindy HOWELLS. Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity. Journal of the Geological Society. London: Geological society, 2014, roč. 171, č. 1, s. 41-47. ISSN 0016-7649. Dostupné z: https://doi.org/10.1144/jgs2013-023.

@article{1180913,
   author = {Kalvoda, Jiří and Nudds, John and Bábek, Ondřej and Howells, Cindy},
   article_location = {London},
   article_number = {1},
   doi = {https://doi.org/10.1144/jgs2013-023},
   keywords = {Carboniferous;Foraminifers;Sequence stratigraphy;Correlations},
   language = {eng},
   issn = {0016-7649},
   journal = {Journal of the Geological Society},
   title = {Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity},
   volume = {171},
   year = {2014}
}

TY  - JOUR
ID  - 1180913
AU  - Kalvoda, Jiří - Nudds, John - Bábek, Ondřej - Howells, Cindy
PY  - 2014
TI  - Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity
JF  - Journal of the Geological Society
VL  - 171
IS  - 1
SP  - 41-47
EP  - 41-47
PB  - Geological society
SN  - 00167649
KW  - Carboniferous;Foraminifers;Sequence stratigraphy;Correlations
N2  - The study of the foraminiferal fauna in the Ogmore section in south Wales produced a detailed late Chadian–early Arundian biostratigraphy and sequence stratigraphy with a higher resolution than in the Arundian stratotype in Hobbyhorse Bay. The earliest Visean (late Chadian) pedogenic horizon close to the Gully Oolite and Caswell Bay Mudstone boundary (MFZ9) corresponds to the mid-Avonian unconformity. The entry of primitive archaediscids of MFZ10 within the Caswell Bay Mudstone is followed by more advanced archaediscids of MFZ11 at the base of the High Tor Limestone. The mid-Avonian unconformity at the Chadian–Arundian boundary is not confined to the London–Brabant Massif, but is also present in central Europe, the East European Platform, the Urals, west Siberia and probably also in Kuzbass and North America. The global extent of the the mid-Avonian unconformity suggests that it is a consequence of early to mid-Visean glacioeustacy
ER  -

KALVODA, Jiří; John NUDDS; Ondřej BÁBEK a Cindy HOWELLS. Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity. \textit{Journal of the Geological Society}. London: Geological society, 2014, roč.~171, č.~1, s.~41-47. ISSN~0016-7649. Dostupné z: https://doi.org/10.1144/jgs2013-023.

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