Abrupt vegetation and environmental change since the MIS 2: A
unique paleorecord from Slovakia (Central Europe)

J 2020

Abrupt vegetation and environmental change since the MIS 2: A unique paleorecord from Slovakia (Central Europe)

ŠOLCOVÁ, Anna, Eva JAMRICHOVÁ, Michal HORSÁK, Petr PAŘIL, Libor PETR et. al.

Základní údaje

Originální název

Abrupt vegetation and environmental change since the MIS 2: A unique paleorecord from Slovakia (Central Europe)

Autoři

ŠOLCOVÁ, Anna (203 Česká republika), Eva JAMRICHOVÁ (703 Slovensko, domácí), Michal HORSÁK (203 Česká republika, garant, domácí), Petr PAŘIL (203 Česká republika, domácí), Libor PETR (203 Česká republika, domácí), Oliver HEIRI (756 Švýcarsko), Jiří KVĚTOŇ (203 Česká republika), Marek KŘÍŽEK (203 Česká republika), Filip HARTVICH (203 Česká republika), Michal HÁJEK (203 Česká republika, domácí) a Petra HÁJKOVÁ (203 Česká republika, domácí)

Vydání

Quaternary Science Reviews, Oxford, Pergamon-Elsevier Science Ltd, 2020, 0277-3791

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10618 Ecology

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

Full text

Impakt faktor

Impact factor: 4.112

Kód RIV

RIV/00216224:14310/20:00114070

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.quascirev.2020.106170

UT WoS

000514754000018

Klíčová slova anglicky

MIS 2/MIS 1 transition; Lateglacial; Holocene; Paleolimnology; Paleoclimatology; Central Europe; Travertine; Stable isotopes; Chironomids; Vegetation dynamics;

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 20. 11. 2020 14:00, Mgr. Marie Šípková, DiS.

Anotace

V originále

Research on past abrupt climate change and linked biotic response is essential for understanding of the future development of biota under changing climatic conditions, which, in turn, is necessary for adequate progress in ecosystem management and nature conservation. The present study presents the first comprehensive reconstruction of local and regional environment at the Western Carpathian/Pannonian Basin border, including a first chironomid-based paleoclimate reconstruction and delta18O and delta13C records from travertine, to investigate abrupt biota and climate shifts since the Marine Isotope Stage (MIS) 2. A range of biotic and abiotic proxy data in organic-calcareous sediment sequence were analysed using a multi-proxy approach to produce a detailed reconstruction of past ecosystem conditions. The results illustrate that the most prominent abrupt change in the local environment occurred directly at the MIS 2/MIS 1 transition at 14,560 cal BP as a consequence of increased precipitation and an increase in reconstructed mean July temperature by -2.2 °C. Abrupt changes in local environment during the early Holocene were closely linked to travertine precipitation rate around thermal springs and thus indirectly to the climate until the arrival of the Late Neolithics around 6400 cal BP. Regional vegetation response (derived from pollen data) to the climatic fluctuations lagged, with the most prominent changes around 14,410 cal BP and 10,140 cal BP. Our data suggest the presence of a steppe-tundra ecosystem with evidence for low amounts of temperate broadleaf trees during the MIS 2, indicating close proximity to their northern glacial refugium. We demonstrate the ability of delta18O and delta13C stable isotope record from travertine to reflect abrupt climatic and environmental changes. The study provides evidence about benefits using travertine deposits coupled with high-resolution paleoecological data to investigate past biotic and abiotic responses to abrupt climate change.

Návaznosti

GA17-05696S, projekt VaV

Název: Holocenní vývoj evropské bioty mírného pásu: vlivy klimatu, refugií a lokálních faktorů testované na komplexních datech nezávislých proxy

Investor: Grantová agentura ČR, Holocenní vývoj evropské bioty mírného pásu: vlivy klimatu, refugií a lokálních faktorů testované na komplexních datech nezávislých proxy

LM2015055, projekt VaV

Název: Centrum pro systémovou biologii (Akronym: C4SYS)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, The national infrastructure C4SYS - Centre for Systems Biology

Citovat

ŠOLCOVÁ, Anna, Eva JAMRICHOVÁ, Michal HORSÁK, Petr PAŘIL, Libor PETR, Oliver HEIRI, Jiří KVĚTOŇ, Marek KŘÍŽEK, Filip HARTVICH, Michal HÁJEK a Petra HÁJKOVÁ. Abrupt vegetation and environmental change since the MIS 2: A unique paleorecord from Slovakia (Central Europe). Quaternary Science Reviews. Oxford: Pergamon-Elsevier Science Ltd, 2020, roč. 230, FEB 15 2020, s. 1-16. ISSN 0277-3791. Dostupné z: https://dx.doi.org/10.1016/j.quascirev.2020.106170.

@article{1632339,
   author = {Šolcová, Anna and Jamrichová, Eva and Horsák, Michal and Pařil, Petr and Petr, Libor and Heiri, Oliver and Květoň, Jiří and Křížek, Marek and Hartvich, Filip and Hájek, Michal and Hájková, Petra},
   article_location = {Oxford},
   article_number = {FEB 15 2020},
   doi = {http://dx.doi.org/10.1016/j.quascirev.2020.106170},
   keywords = {MIS 2/MIS 1 transition; Lateglacial; Holocene; Paleolimnology; Paleoclimatology; Central Europe; Travertine; Stable isotopes; Chironomids; Vegetation dynamics;},
   language = {eng},
   issn = {0277-3791},
   journal = {Quaternary Science Reviews},
   title = {Abrupt vegetation and environmental change since the MIS 2: A unique paleorecord from Slovakia (Central Europe)},
   url = {https://www.sciencedirect.com/science/article/pii/S027737911931087X},
   volume = {230},
   year = {2020}
}

TY  - JOUR
ID  - 1632339
AU  - Šolcová, Anna - Jamrichová, Eva - Horsák, Michal - Pařil, Petr - Petr, Libor - Heiri, Oliver - Květoň, Jiří - Křížek, Marek - Hartvich, Filip - Hájek, Michal - Hájková, Petra
PY  - 2020
TI  - Abrupt vegetation and environmental change since the MIS 2: A unique paleorecord from Slovakia (Central Europe)
JF  - Quaternary Science Reviews
VL  - 230
IS  - FEB 15 2020
SP  - 1-16
EP  - 1-16
PB  - Pergamon-Elsevier Science Ltd
SN  - 02773791
KW  - MIS 2/MIS 1 transition
KW  - Lateglacial
KW  - Holocene
KW  - Paleolimnology
KW  - Paleoclimatology
KW  - Central Europe
KW  - Travertine
KW  - Stable isotopes
KW  - Chironomids
KW  - Vegetation dynamics;
UR  - https://www.sciencedirect.com/science/article/pii/S027737911931087X
L2  - https://www.sciencedirect.com/science/article/pii/S027737911931087X
N2  - Research on past abrupt climate change and linked biotic response is essential for understanding of the future development of biota under changing climatic conditions, which, in turn, is necessary for adequate progress in ecosystem management and nature conservation. The present study presents the first comprehensive reconstruction of local and regional environment at the Western Carpathian/Pannonian Basin border, including a first chironomid-based paleoclimate reconstruction and delta18O and delta13C records from travertine, to investigate abrupt biota and climate shifts since the Marine Isotope Stage (MIS) 2. A range of biotic and abiotic proxy data in organic-calcareous sediment sequence were analysed using a multi-proxy approach to produce a detailed reconstruction of past ecosystem conditions. The results illustrate that the most prominent abrupt change in the local environment occurred directly at the MIS 2/MIS 1 transition at 14,560 cal BP as a consequence of increased precipitation and an increase in reconstructed mean July temperature by -2.2 °C. Abrupt changes in local environment during the early Holocene were closely linked to travertine precipitation rate around thermal springs and thus indirectly to the climate until the arrival of the Late Neolithics around 6400 cal BP. Regional vegetation response (derived from pollen data) to the climatic fluctuations lagged, with the most prominent changes around 14,410 cal BP and 10,140 cal BP. Our data suggest the presence of a steppe-tundra ecosystem with evidence for low amounts of temperate broadleaf trees during the MIS 2, indicating close proximity to their northern glacial refugium. We demonstrate the ability of delta18O and delta13C stable isotope record from travertine to reflect abrupt climatic and environmental changes. The study provides evidence about benefits using travertine deposits coupled with high-resolution paleoecological data to investigate past biotic and abiotic responses to abrupt climate change.
ER  -

ŠOLCOVÁ, Anna, Eva JAMRICHOVÁ, Michal HORSÁK, Petr PAŘIL, Libor PETR, Oliver HEIRI, Jiří KVĚTOŇ, Marek KŘÍŽEK, Filip HARTVICH, Michal HÁJEK a Petra HÁJKOVÁ. Abrupt vegetation and environmental change since the MIS 2: A unique paleorecord from Slovakia (Central Europe). \textit{Quaternary Science Reviews}. Oxford: Pergamon-Elsevier Science Ltd, 2020, roč.~230, FEB 15 2020, s.~1-16. ISSN~0277-3791. Dostupné z: https://dx.doi.org/10.1016/j.quascirev.2020.106170.

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