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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F14%3A00075360%21RIV15-MSM-14310___
rdf:type
skos:Concept n17:Vysledek
dcterms:description
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 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
dcterms:title
Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity
skos:prefLabel
Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity Late Chadian–early Arundian high-resolution biostratigraphy in the Ogmore-by- Sea section (South Wales–Mendip shelf) and the mid-Avonian unconformity
skos:notation
RIV/00216224:14310/14:00075360!RIV15-MSM-14310___
n3:aktivita
n11:S n11:I
n3:aktivity
I, S
n3:cisloPeriodika
1
n3:dodaniDat
n12:2015
n3:domaciTvurceVysledku
n4:6213405 n4:1283987
n3:druhVysledku
n7:J
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n18:predkladatel
n3:idSjednocenehoVysledku
25727
n3:idVysledku
RIV/00216224:14310/14:00075360
n3:jazykVysledku
n8:eng
n3:klicovaSlova
Carboniferous; Foraminifers; Sequence stratigraphy; Correlations
n3:klicoveSlovo
n9:Foraminifers n9:Correlations n9:Sequence%20stratigraphy n9:Carboniferous
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[E7C6C5801ABD]
n3:nazevZdroje
Journal of the Geological Society
n3:obor
n13:DB
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
4
n3:rokUplatneniVysledku
n12:2014
n3:svazekPeriodika
171
n3:tvurceVysledku
Kalvoda, Jiří Howells, Cindy Bábek, Ondřej Nudds, John
n3:wos
000329924200006
s:issn
0016-7649
s:numberOfPages
7
n16:doi
10.1144/jgs2013-023
n15:organizacniJednotka
14310