Case study on Hangenberg Crisis equivalent deposits and associated conodont faunas including Siphonodella progenitors from late Devonian island arc settings (Indert Formation, Shine Jinst region, southern Mongolia)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F24%3A10168884" target="_blank" >RIV/00025798:_____/24:10168884 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.schweizerbart.de/papers/nos/detail/57/102937/Case_study_on_Hangenberg_Crisis_equivalent_deposits_and_associated_conodont_faunas_including_Siphonodella_progenitors_from_late_Devonian_island_arc_settings_Indert_Formation_Shine_Jinst_region_southern_Mongolia" target="_blank" >https://www.schweizerbart.de/papers/nos/detail/57/102937/Case_study_on_Hangenberg_Crisis_equivalent_deposits_and_associated_conodont_faunas_including_Siphonodella_progenitors_from_late_Devonian_island_arc_settings_Indert_Formation_Shine_Jinst_region_southern_Mongolia</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1127/nos/2023/0760" target="_blank" >10.1127/nos/2023/0760</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Case study on Hangenberg Crisis equivalent deposits and associated conodont faunas including Siphonodella progenitors from late Devonian island arc settings (Indert Formation, Shine Jinst region, southern Mongolia)
Popis výsledku v původním jazyce
The Late Devonian-early Carboniferous aged Indert Formation near Shine Jinst (southern Mongolia) is subdivided into the Heermorit and Shombon members. A systematic collection of the few marine carbonaterich levels from the Heermorit Member resulted in a low-diverse conodont assemblage indicating the late Famennian Bispathodus ultimus conodont Biozone at the Tsagaankhaalga-2 section. Supplemental conodont data from the Yamaan Us section support early Tournaisian age for the lowermost limestone beds of the above deposited Shombon Member. In total, twelve species in seven genera are identified and include Apatognathus, Mehlina, Pandorinellina, Polygnathus (including the new taxon Polygnathus communis tomurtogooi n. ssp.), Pseudopolygnathus, transitional forms of Polygnathus-Siphonodella and Siphonodella. The significance and palaeogeographic distribution of the markedly increased occurrence of intergeneric transitional forms before and during the Late Devonian Hangenberg Event and regionally lacking evidence of the end-Famennian Protognathodus kockeli conodont Biozone and associated early protognathodid assemblage below the Devonian/ Carboniferous boundary are discussed.
Název v anglickém jazyce
Case study on Hangenberg Crisis equivalent deposits and associated conodont faunas including Siphonodella progenitors from late Devonian island arc settings (Indert Formation, Shine Jinst region, southern Mongolia)
Popis výsledku anglicky
The Late Devonian-early Carboniferous aged Indert Formation near Shine Jinst (southern Mongolia) is subdivided into the Heermorit and Shombon members. A systematic collection of the few marine carbonaterich levels from the Heermorit Member resulted in a low-diverse conodont assemblage indicating the late Famennian Bispathodus ultimus conodont Biozone at the Tsagaankhaalga-2 section. Supplemental conodont data from the Yamaan Us section support early Tournaisian age for the lowermost limestone beds of the above deposited Shombon Member. In total, twelve species in seven genera are identified and include Apatognathus, Mehlina, Pandorinellina, Polygnathus (including the new taxon Polygnathus communis tomurtogooi n. ssp.), Pseudopolygnathus, transitional forms of Polygnathus-Siphonodella and Siphonodella. The significance and palaeogeographic distribution of the markedly increased occurrence of intergeneric transitional forms before and during the Late Devonian Hangenberg Event and regionally lacking evidence of the end-Famennian Protognathodus kockeli conodont Biozone and associated early protognathodid assemblage below the Devonian/ Carboniferous boundary are discussed.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2024
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Newsletters on Stratigraphy
ISSN
0078-0421
e-ISSN
—
Svazek periodika
57
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
24
Strana od-do
65-88
Kód UT WoS článku
001013930700001
EID výsledku v databázi Scopus
2-s2.0-85182852723