KAISER, Sandra I., Tomáš KUMPAN a Michael W. RASSER. High-resolution conodont biostratigraphy in two key sections from the Carnic Alps (Grüne Schneid) and Graz Paleozoic (Trolp) - implications for the biozonation concept at the Devonian-Carboniferous boundary. NEWSLETTERS ON STRATIGRAPHY. STUTTGART: GEBRUDER BORNTRAEGER, 2020, roč. 53, č. 3, s. 249-274. ISSN 0078-0421. Dostupné z: https://dx.doi.org/10.1127/nos/2019/0520.
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Základní údaje
Originální název High-resolution conodont biostratigraphy in two key sections from the Carnic Alps (Grüne Schneid) and Graz Paleozoic (Trolp) - implications for the biozonation concept at the Devonian-Carboniferous boundary
Autoři KAISER, Sandra I., Tomáš KUMPAN (203 Česká republika, garant, domácí) a Michael W. RASSER.
Vydání NEWSLETTERS ON STRATIGRAPHY, STUTTGART, GEBRUDER BORNTRAEGER, 2020, 0078-0421.
Další údaje
Originální jazyk angličtina
Typ výsledku Článek v odborném periodiku
Obor 10505 Geology
Stát vydavatele Německo
Utajení není předmětem státního či obchodního tajemství
WWW URL
Impakt faktor Impact factor: 2.974
Kód RIV RIV/00216224:14310/20:00114272
Organizační jednotka Přírodovědecká fakulta
Doi http://dx.doi.org/10.1127/nos/2019/0520
UT WoS 000535184500001
Klíčová slova anglicky Famennian-Tournaisian boundary; Hangenberg Biocrisis; pelagic limestones; early Protognathodus fauna; sulcata/kuehni Zone
Štítky rivok
Příznaky Mezinárodní význam, Recenzováno
Změnil Změnila: Mgr. Marie Šípková, DiS., učo 437722. Změněno: 17. 8. 2020 13:34.
Anotace
Devonian-Carboniferous boundary successions are globally characterized by conodont-free siliciclastics, stratigraphic gaps, or uncertainties among the first occurrence of biostratigraphically relevant index fossils. This resulted from regionally varying palaeoenvironmental conditions caused by global major environmental changes related to the Hangenberg Crisis. The ongoing search for the ultimate causes of mass extinctions at the end of the Devonian requires a fine biostratigraphic framework, which is developed during the last half of century. This study provides new biostratigraphic implications both from the new and re-evaluated conodont material from two classical continuous pelagic limestone successions of two different geological units in Austria. The Upper Famennian and Lower Tournaisian successions at Trolp (Graz Paleozoic) and Grane Schneid (Camic Alps) have been studied in very high-resolution. This study provides the first record of a joint first occurrence of typical morphotypes of Protognathodus kuehni and Siphonodella sulcata both at Trolp and Grune Schneid in the same biostratigraphic level. This indicates a synchronous first appearance and supports the practicability of the joint sulcata/kuehni Zone previously established. The sampling resulted in a detailed record of the evolution of the biostratigraphically significant Protognathodus fauna, among them Protognathodus kockeli which is currently tested as a potential index for the new Devonian-Carboniferous boundary position. Our analysis revealed taxonomic complexity of Pr. kockeli itself, and in the lineage from its ancestor Protognathodus collinsoni, and to its descendent Protognathodus kuehni. Therefore, using the first occurrence of Protognathodus kockeli as new index fossil for the Devonian-Carboniferous boundary would face the same problem as exists with the current index Siphonodella sulcata which is under revision, and a distinctive conodont-based definition of the system boundary is, under the current taxonomic state of knowledge, difficult to maintain.
Návaznosti
GA16-11563S, projekt VaVNázev: Nejranější karbonské greenhouse-icehouse klimatické oscilace - multidisciplinární přístup
Investor: Grantová agentura ČR, Nejranější karbonské greenhouse-icehouse klimatické oscilace - multidisciplinární přístup
VytisknoutZobrazeno: 4. 10. 2024 16:31