Timing of Langhian bioevents in the Carpathian Foredeep and
north ern Pannonian Basin in relation to oceanographic,
tectonic and climatic processes

J 2018

Timing of Langhian bioevents in the Carpathian Foredeep and north ern Pannonian Basin in relation to oceanographic, tectonic and climatic processes

HOLCOVÁ, Katarina, Nela DOLÁKOVÁ, Slavomír NEHYBA a František VACEK

Základní údaje

Originální název

Timing of Langhian bioevents in the Carpathian Foredeep and north ern Pannonian Basin in relation to oceanographic, tectonic and climatic processes

Autoři

HOLCOVÁ, Katarina (203 Česká republika), Nela DOLÁKOVÁ (203 Česká republika, domácí), Slavomír NEHYBA (203 Česká republika, domácí) a František VACEK (203 Česká republika)

Vydání

Geological Quarterly, Warszawa, Polish Geological Institute, 2018, 1641-7291

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Polsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 0.759

Kód RIV

RIV/00216224:14310/18:00102712

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.7306/gq.1399

UT WoS

000426042600001

Klíčová slova anglicky

Miocene-Central Paratethys-biostratigraphy-calcareous nannoplankton- foraminifera-palynology

Změněno: 23. 4. 2024 11:18, Mgr. Michal Petr

Anotace

V originále

The succession of bioevents in planktonic foraminifer and calcareous nannoplankton communities is reviewed and summarized for the Carpathian Foredeep and northern Pannonian Basin in the time interval between ~16 and 13.5 Ma. This succession can be subdivided into three principal intervals: (1) an interval with rare Praeorbulina sicana and P. glomerosa. It was characterized by a limited immigration of index taxa linked to the lack of a warm surface water layer in the Central Paratethys. This interval can be correlated with the first Badenian transgression near the Burdigalian/Langhian boundary. The rare occurrence of biostratigraphical markers does not allow its precise dating and interregional correlation; (2) a brief interval of the first occurrences of Praeorbulina circularis, Orbulina suturalis and Helicosphaera waltrans. This can be related to the formation of a warm surface water layer suitable for the survival of orbulinas and praeorbulinas and a change from estuarine to anti-estuarine circulation. This interval can be correlated with the second Badenian transgression, which, how ever, was not isochronous over the area as inferred from different successions of these first occurrences; (3) a limited appearance of new index taxa in the Central Paratethys prior to the Wielician Salinity Crisis. This time interval was characterized by increased seasonality and salinity oscillations followed by climate cooling. A “reverse” migration of the stress-tolerant species Helicosphaera walbersdorfensis from the Central Paratethys to the Mediterranean is suggested. Several local bioevents with limited stratigraphic correlation potential have been recognized in this interval.

Návaznosti

2B08036, projekt VaV

Název: Nové molekulárně biologické a biochemické metody pro monitoring estrogenů a dalších chemických endokrinních disruptorů (Akronym: ENVISCREEN)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Nové molekulárně biologické a biochemické metody pro monitoring estrogenů a dalších chemických endokrinních disruptorů

Citovat

HOLCOVÁ, Katarina, Nela DOLÁKOVÁ, Slavomír NEHYBA a František VACEK. Timing of Langhian bioevents in the Carpathian Foredeep and north ern Pannonian Basin in relation to oceanographic, tectonic and climatic processes. Geological Quarterly. Warszawa: Polish Geological Institute, 2018, roč. 62, č. 1, s. 3-17. ISSN 1641-7291. Dostupné z: https://dx.doi.org/10.7306/gq.1399.

@article{1417123,
   author = {Holcová, Katarina and Doláková, Nela and Nehyba, Slavomír and Vacek, František},
   article_location = {Warszawa},
   article_number = {1},
   doi = {http://dx.doi.org/10.7306/gq.1399},
   keywords = {Miocene-Central Paratethys-biostratigraphy-calcareous nannoplankton- foraminifera-palynology},
   language = {eng},
   issn = {1641-7291},
   journal = {Geological Quarterly},
   title = {Timing of Langhian bioevents in the Carpathian Foredeep and north ern Pannonian Basin in relation to oceanographic, tectonic and climatic processes},
   url = {http://dx.doi.org/10.7306/gq.1399},
   volume = {62},
   year = {2018}
}

TY  - JOUR
ID  - 1417123
AU  - Holcová, Katarina - Doláková, Nela - Nehyba, Slavomír - Vacek, František
PY  - 2018
TI  - Timing of Langhian bioevents in the Carpathian Foredeep and north ern Pannonian Basin in relation to oceanographic, tectonic and climatic processes
JF  - Geological Quarterly
VL  - 62
IS  - 1
SP  - 3-17
EP  - 3-17
PB  - Polish Geological Institute
SN  - 16417291
KW  - Miocene-Central Paratethys-biostratigraphy-calcareous nannoplankton- foraminifera-palynology
UR  - http://dx.doi.org/10.7306/gq.1399
N2  - The succession of bioevents in planktonic foraminifer and calcareous nannoplankton communities is reviewed and summarized for the Carpathian Foredeep and northern Pannonian Basin in the time interval between ~16 and 13.5 Ma. This succession can be subdivided into three principal intervals: (1) an interval with rare Praeorbulina sicana and P. glomerosa. It was characterized by a limited immigration of index taxa linked to the lack of a warm surface water layer in the Central Paratethys. This interval can be correlated with the first Badenian transgression near the Burdigalian/Langhian boundary. The rare occurrence of biostratigraphical markers does not allow its precise dating and interregional correlation; (2) a brief interval of the first occurrences of Praeorbulina circularis, Orbulina suturalis and Helicosphaera waltrans. This can be related to the formation of a warm surface water layer suitable for the survival of orbulinas and praeorbulinas and a change from estuarine to anti-estuarine circulation. This interval can be correlated with the second Badenian transgression, which, how ever, was not isochronous over the area as inferred from different successions of these first occurrences; (3) a limited appearance of new index taxa in the Central Paratethys prior to the Wielician Salinity Crisis. This time interval was characterized by increased seasonality and salinity oscillations followed by climate cooling. A “reverse” migration of the stress-tolerant species Helicosphaera walbersdorfensis from the Central Paratethys to the Mediterranean is suggested. Several local bioevents with limited stratigraphic correlation potential have been recognized in this interval.
ER  -

HOLCOVÁ, Katarina, Nela DOLÁKOVÁ, Slavomír NEHYBA a František VACEK. Timing of Langhian bioevents in the Carpathian Foredeep and north ern Pannonian Basin in relation to oceanographic, tectonic and climatic processes. \textit{Geological Quarterly}. Warszawa: Polish Geological Institute, 2018, roč.~62, č.~1, s.~3-17. ISSN~1641-7291. Dostupné z: https://dx.doi.org/10.7306/gq.1399.

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