Evolution of palaeoclimate, palaeoenvironment and vegetation in
Central Europe during the Miocene Climate Optimum

J 2023

Evolution of palaeoclimate, palaeoenvironment and vegetation in Central Europe during the Miocene Climate Optimum

SCHEINER, Filip; Martina HAVELCOVÁ; Katarina HOLCOVÁ; Nela DOLÁKOVÁ; Slavomír NEHYBA et al.

Základní údaje

Originální název

Evolution of palaeoclimate, palaeoenvironment and vegetation in Central Europe during the Miocene Climate Optimum

Autoři

SCHEINER, Filip; Martina HAVELCOVÁ; Katarina HOLCOVÁ; Nela DOLÁKOVÁ; Slavomír NEHYBA; Lukáš ACKERMAN; Jakub TRUBAČ; Šárka HLADILOVÁ; Jan REJŠEK a Torsten UTESCHER

Vydání

Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2023, 0031-0182

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10511 Environmental sciences

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 2.600

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/23:00132588

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

Biomarker study; Miocene Climate Optimum; N-alkanes; Plant Functional Type; Palaeoclimate; Sr-87; Sr-86

Štítky

14315010, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 20. 12. 2023 11:39, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

The Miocene Climate Optimum was an interval of global climatic warmth characterized by significant global palaeoceanographic changes. In this paper, we describe the parastratotype section of the regional Karpatian stage (late Burdigalian) at Hevlin quarry in the Czech Republic, to improve knowledge of evolving palaeoenvironment and palaeoclimate during the Miocene Climate Optimum. Strontium isotope stratigraphy (87Sr/86Sr) and biostratigraphy allows precise identification of Burdigalian/Langhian boundary, and the studied section is inferred to represent the late Burdigalian time interval (17.2-16 Ma). Analysis of palynological assemblages using the Coexistence Approach and the Plant Functional Type method supported by biomarker study indicates an existence of a warm temperate to subtropical palaeoclimate pattern with a mean annual temperature range of 17-19.5 degrees C and a high degree of seasonality. The mean annual precipitation range was 1050-1600 mm. The zonal vegetation cover was characterized as transitional between subtropical broad-leaved evergreen forest and warm-temperate to subtropical mixed mesophytic forest. Our palaeoclimatic findings in Central Europe agree with global trends (high temperatures and a high sea level) and indicates the occurrence of rather widespread humid conditions. The proximity to our study site of the Mediterranean-Paratethys sea probably played a critical role in moderating regional palaeoclimate.

Citovat

SCHEINER, Filip; Martina HAVELCOVÁ; Katarina HOLCOVÁ; Nela DOLÁKOVÁ; Slavomír NEHYBA; Lukáš ACKERMAN; Jakub TRUBAČ; Šárka HLADILOVÁ; Jan REJŠEK a Torsten UTESCHER. Evolution of palaeoclimate, palaeoenvironment and vegetation in Central Europe during the Miocene Climate Optimum. Palaeogeography, Palaeoclimatology, Palaeoecology. Elsevier, 2023, roč. 611, February, s. 1-19. ISSN 0031-0182. Dostupné z: https://doi.org/10.1016/j.palaeo.2022.111364.

@article{2351662,
   author = {Scheiner, Filip and Havelcová, Martina and Holcová, Katarina and Doláková, Nela and Nehyba, Slavomír and Ackerman, Lukáš and Trubač, Jakub and Hladilová, Šárka and Rejšek, Jan and Utescher, Torsten},
   article_number = {February},
   doi = {https://doi.org/10.1016/j.palaeo.2022.111364},
   keywords = {Biomarker study; Miocene Climate Optimum; N-alkanes; Plant Functional Type; Palaeoclimate; Sr-87; Sr-86},
   language = {eng},
   issn = {0031-0182},
   journal = {Palaeogeography, Palaeoclimatology, Palaeoecology},
   title = {Evolution of palaeoclimate, palaeoenvironment and vegetation in Central Europe during the Miocene Climate Optimum},
   url = {https://doi.org/10.1016/j.palaeo.2022.111364},
   volume = {611},
   year = {2023}
}

TY  - JOUR
ID  - 2351662
AU  - Scheiner, Filip - Havelcová, Martina - Holcová, Katarina - Doláková, Nela - Nehyba, Slavomír - Ackerman, Lukáš - Trubač, Jakub - Hladilová, Šárka - Rejšek, Jan - Utescher, Torsten
PY  - 2023
TI  - Evolution of palaeoclimate, palaeoenvironment and vegetation in Central Europe during the Miocene Climate Optimum
JF  - Palaeogeography, Palaeoclimatology, Palaeoecology
VL  - 611
IS  - February
SP  - 1-19
EP  - 1-19
PB  - Elsevier
SN  - 00310182
KW  - Biomarker study
KW  - Miocene Climate Optimum
KW  - N-alkanes
KW  - Plant Functional Type
KW  - Palaeoclimate
KW  - Sr-87
KW  - Sr-86
UR  - https://doi.org/10.1016/j.palaeo.2022.111364
N2  - The Miocene Climate Optimum was an interval of global climatic warmth characterized by significant global palaeoceanographic changes. In this paper, we describe the parastratotype section of the regional Karpatian stage (late Burdigalian) at Hevlin quarry in the Czech Republic, to improve knowledge of evolving palaeoenvironment and palaeoclimate during the Miocene Climate Optimum. Strontium isotope stratigraphy (87Sr/86Sr) and biostratigraphy allows precise identification of Burdigalian/Langhian boundary, and the studied section is inferred to represent the late Burdigalian time interval (17.2-16 Ma). Analysis of palynological assemblages using the Coexistence Approach and the Plant Functional Type method supported by biomarker study indicates an existence of a warm temperate to subtropical palaeoclimate pattern with a mean annual temperature range of 17-19.5 degrees C and a high degree of seasonality. The mean annual precipitation range was 1050-1600 mm. The zonal vegetation cover was characterized as transitional between subtropical broad-leaved evergreen forest and warm-temperate to subtropical mixed mesophytic forest. Our palaeoclimatic findings in Central Europe agree with global trends (high temperatures and a high sea level) and indicates the occurrence of rather widespread humid conditions. The proximity to our study site of the Mediterranean-Paratethys sea probably played a critical role in moderating regional palaeoclimate.
ER  -

SCHEINER, Filip; Martina HAVELCOVÁ; Katarina HOLCOVÁ; Nela DOLÁKOVÁ; Slavomír NEHYBA; Lukáš ACKERMAN; Jakub TRUBAČ; Šárka HLADILOVÁ; Jan REJŠEK a Torsten UTESCHER. Evolution of palaeoclimate, palaeoenvironment and vegetation in Central Europe during the Miocene Climate Optimum. \textit{Palaeogeography, Palaeoclimatology, Palaeoecology}. Elsevier, 2023, roč.~611, February, s.~1-19. ISSN~0031-0182. Dostupné z: https://doi.org/10.1016/j.palaeo.2022.111364.

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