Early Tournaisian (Mississippian) unornamented siphonodellid
conodonts: biostratigraphic and paleogeographic remarks

a 2014

Early Tournaisian (Mississippian) unornamented siphonodellid conodonts: biostratigraphic and paleogeographic remarks

KUMPAN, Tomáš a Sandra I. KAISER

Základní údaje

Originální název

Early Tournaisian (Mississippian) unornamented siphonodellid conodonts: biostratigraphic and paleogeographic remarks

Autoři

KUMPAN, Tomáš (203 Česká republika, garant, domácí) a Sandra I. KAISER (276 Německo)

Vydání

15th Czech-Polish-Slovak Paleontological Conference, Banska Bystrica, Slovak Republic, 2014

Další údaje

Jazyk

angličtina

Typ výsledku

Konferenční abstrakt

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Slovensko

Utajení

není předmětem státního či obchodního tajemství

Kód RIV

RIV/00216224:14310/14:00074153

Organizační jednotka

Přírodovědecká fakulta

ISBN

978-80-224-1399-2

Klíčová slova anglicky

conodonts;Siphonodella;biostratigraphy

Změněno: 30. 11. 2014 22:55, Mgr. Tomáš Kumpan, Ph.D.

Anotace

V originále

One of the unornamented species - Siphonodella belkai - described from Poland and further known from Russian Tournaisian is the index taxa of eponymous belkai conodont zone distinguished in these regions. Sudden ventral narrowing of Si. belkai platform elements resemble platform features of Si. sandbergi and, moreover, presence of three or more (up to 7) rostral ridges is common characteristic with Si. quadruplicata. Because Si. belkai has been defined by Dzik in 1997, confusing of Si. belkai with Si. sandbergi and Si. quadruplicata is common in older, but, even in more recent publications. The misleading determination leads to stratigraphic discrepancies and older sediments of the hassi Zone are identified as younger ones (sandbergi and quadruplicata zones). The lower Tournaisian deep-water limestones (upper to lower slope) in the Rhenish Slate Mountains (Oese, Oberrödinghausen) and Moravian Karst (Lesní lom Quarry) recently yielded relatively abundant Si. belkai (Fig. 1ab) with rare unornamented Siphonodella sp. (Fig. 1c), accompanied by conodonts typical for the hassi and sandbergi zones. The first appearance datum (FAD) of Si. belkai matches with FAD of Si. hassi and therefore bases of these zones can be tentatively correlated.

Návaznosti

GAP210/11/1891, projekt VaV

Název: Hranice devonu a karbonu v Evropě - multidisciplinární přístup

Investor: Grantová agentura ČR, Hranice devonu a karbonu v Evropě - multidisciplinární přístup

Citovat

KUMPAN, Tomáš a Sandra I. KAISER. Early Tournaisian (Mississippian) unornamented siphonodellid conodonts: biostratigraphic and paleogeographic remarks. In 15th Czech-Polish-Slovak Paleontological Conference, Banska Bystrica, Slovak Republic. 2014. ISBN 978-80-224-1399-2.

@proceedings{1210916,
   author = {Kumpan, Tomáš and Kaiser, Sandra I.},
   booktitle = {15th Czech-Polish-Slovak Paleontological Conference, Banska Bystrica, Slovak Republic},
   keywords = {conodonts;Siphonodella;biostratigraphy},
   language = {eng},
   isbn = {978-80-224-1399-2},
   title = {Early Tournaisian (Mississippian) unornamented siphonodellid conodonts: biostratigraphic and paleogeographic remarks},
   year = {2014}
}

TY  - CONF
ID  - 1210916
AU  - Kumpan, Tomáš - Kaiser, Sandra I.
PY  - 2014
TI  - Early Tournaisian (Mississippian) unornamented siphonodellid conodonts: biostratigraphic and paleogeographic remarks
SN  - 9788022413992
KW  - conodonts;Siphonodella;biostratigraphy
N2  - One of the unornamented species - Siphonodella belkai - described from Poland and further known from Russian Tournaisian is the index taxa of eponymous belkai conodont zone distinguished in these regions. Sudden ventral narrowing of Si. belkai platform elements resemble platform features of Si. sandbergi and, moreover, presence of three or more (up to 7) rostral ridges is common characteristic with Si. quadruplicata. Because Si. belkai has been defined by Dzik in 1997, confusing of Si. belkai with Si. sandbergi and Si. quadruplicata is common in older, but, even in more recent publications. The misleading determination leads to stratigraphic discrepancies and older sediments of the hassi Zone are identified as younger ones (sandbergi and quadruplicata zones). The lower Tournaisian deep-water limestones (upper to lower slope) in the Rhenish Slate Mountains (Oese, Oberrödinghausen) and Moravian Karst (Lesní lom Quarry) recently yielded relatively abundant Si. belkai (Fig. 1ab) with rare unornamented Siphonodella sp. (Fig. 1c), accompanied by conodonts typical for the hassi and sandbergi zones. The first appearance datum (FAD) of Si. belkai matches with FAD of Si. hassi and therefore bases of these zones can be tentatively correlated.
ER  -

KUMPAN, Tomáš a Sandra I. KAISER. Early Tournaisian (Mississippian) unornamented siphonodellid conodonts: biostratigraphic and paleogeographic remarks. In \textit{15th Czech-Polish-Slovak Paleontological Conference, Banska Bystrica, Slovak Republic}. 2014. ISBN~978-80-224-1399-2.

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