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)
The result's identifiers
Result code in 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>
Result on the web
<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>
Alternative languages
Result language
angličtina
Original language name
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)
Original language description
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.
Czech name
—
Czech description
—
Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10505 - Geology
Result continuities
Project
—
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2024
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Newsletters on Stratigraphy
ISSN
0078-0421
e-ISSN
—
Volume of the periodical
57
Issue of the periodical within the volume
1
Country of publishing house
DE - GERMANY
Number of pages
24
Pages from-to
65-88
UT code for WoS article
001013930700001
EID of the result in the Scopus database
2-s2.0-85182852723