Late Pleniglacial vegetation in eastern-central Europe: are
there modern analogues in Siberia?

J 2014

Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia?

MAGYARI, Enikö Katalin, Petr KUNEŠ, Gusztav JAKAB, Pál SÜMEGI, Barbora PELÁNKOVÁ et. al.

Základní údaje

Originální název

Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia?

Autoři

MAGYARI, Enikö Katalin (348 Maďarsko), Petr KUNEŠ (203 Česká republika), Gusztav JAKAB (348 Maďarsko), Pál SÜMEGI (348 Maďarsko), Barbora PELÁNKOVÁ (703 Slovensko, domácí), Frank SCHÄBITZ (276 Německo), Mihály BRAUN (348 Maďarsko) a Milan CHYTRÝ (203 Česká republika, garant, domácí)

Vydání

Quaternary Science Reviews, 2014, 0277-3791

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10600 1.6 Biological sciences

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 4.572

Kód RIV

RIV/00216224:14310/14:00074251

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.quascirev.2014.04.020

UT WoS

000338604200004

Klíčová slova anglicky

Last Glacial Maximum; Late Pleniglacial vegetation; Modern analogue; Carpathians; Carpathian Basin

Štítky

AKR, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 13. 3. 2018 10:48, Mgr. Lucie Jarošová, DiS.

Anotace

V originále

To characterize Late Pleniglacial (LPG: 26.5-15 lea cal BP) and particularly Last Glacial Maximum (LGM: 21 +/- 2 lea cal BP) vegetation and climate, fossil pollen assemblages are often compared with modern pollen assemblages. Given the non-analogue climate of the LPG, a key question is how glacial pollen assemblages and thereby vegetation compare with modern vegetation. In this paper we present three LPG pollen records from the Carpathian Basin and the adjoining Carpathian Mountains to address this question and provide a concise compositional characterization of the LPG vegetation. Fossil pollen assemblages were compared with surface pollen spectra from the Altai-Sayan Mountains in southern Siberia. This area shows many similarities with the LPG vegetation of eastern-central Europe, and has long been considered as its best modern analogue. Ordination and analogue matching were used to characterize vegetation composition and find the best analogues. Our results show that few LPG pollen assemblages have statistically significant analogues in southern Siberia. When analogue pairings occur they suggest the predominance of wet and mesic grasslands and dry steppe in the studied region. Wooded vegetation types (continental and suboceanic hemiboreal forest, continental taiga) appear as significant analogues only in a few cases during the LGM and more frequently after 16 lea cal BP. These results suggest that the LPG landscape of the Carpathian Basin was dominated by dry steppe that occurred outside the river floodplains, while wet and mesic grasslands occurred in the floodplains and on other sites influenced by ground water. Woody vegetation mainly occurred in river valleys, on wet north-facing hillsides, and scattered trees were likely also present on the loess plateaus. The dominant woody species were Larix, Pious sylvestris, Pinus mugo, Pinus cembra, Picea abies, Betula pendula/pubescens, Betula nano, Juniperus, Hippophae rhamnoides, Populus, Salix and Alnus. The pollen records suggest uninterrupted presence of mesophilous temperate trees (Quercus, Ulmus, Corylus, Fagus and Fraxinus excelsior) in the Eastern Carpathian Mountains throughout the LPG. We demonstrate that the LPG vegetation in this area was characterized by increasing grass cover and high frequency of wildfires. We conclude that pollen spectra over represent trees in the forest-steppe landscape of the LPG, furthermore pollen-based quantitative climate reconstructions for the LPG are challenging in this area due to the scarcity of modern analogues.

Návaznosti

GAP504/11/0454, projekt VaV

Název: Změny biodiverzity na přechodu pleistocénu a holocénu: současné analogie v reliktních ekosystémech Sibiře

Investor: Grantová agentura ČR, Změny biodiverzity na přechodu pleistocénu a holocénu: současné analogie v reliktních ekosystémech Sibiře

Citovat

MAGYARI, Enikö Katalin, Petr KUNEŠ, Gusztav JAKAB, Pál SÜMEGI, Barbora PELÁNKOVÁ, Frank SCHÄBITZ, Mihály BRAUN a Milan CHYTRÝ. Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia? Quaternary Science Reviews. 2014, roč. 95, JULY, s. 60-79. ISSN 0277-3791. Dostupné z: https://dx.doi.org/10.1016/j.quascirev.2014.04.020.

@article{1214695,
   author = {Magyari, Enikö Katalin and Kuneš, Petr and Jakab, Gusztav and Sümegi, Pál and Pelánková, Barbora and Schäbitz, Frank and Braun, Mihály and Chytrý, Milan},
   article_number = {JULY},
   doi = {http://dx.doi.org/10.1016/j.quascirev.2014.04.020},
   keywords = {Last Glacial Maximum; Late Pleniglacial vegetation; Modern analogue; Carpathians; Carpathian Basin},
   language = {eng},
   issn = {0277-3791},
   journal = {Quaternary Science Reviews},
   title = {Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia?},
   url = {http://www.sciencedirect.com/science/article/pii/S0277379114001449},
   volume = {95},
   year = {2014}
}

TY  - JOUR
ID  - 1214695
AU  - Magyari, Enikö Katalin - Kuneš, Petr - Jakab, Gusztav - Sümegi, Pál - Pelánková, Barbora - Schäbitz, Frank - Braun, Mihály - Chytrý, Milan
PY  - 2014
TI  - Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia?
JF  - Quaternary Science Reviews
VL  - 95
IS  - JULY
SP  - 60-79
EP  - 60-79
SN  - 02773791
KW  - Last Glacial Maximum
KW  - Late Pleniglacial vegetation
KW  - Modern analogue
KW  - Carpathians
KW  - Carpathian Basin
UR  - http://www.sciencedirect.com/science/article/pii/S0277379114001449
N2  - To characterize Late Pleniglacial (LPG: 26.5-15 lea cal BP) and particularly Last Glacial Maximum (LGM: 21 +/- 2 lea cal BP) vegetation and climate, fossil pollen assemblages are often compared with modern pollen assemblages. Given the non-analogue climate of the LPG, a key question is how glacial pollen assemblages and thereby vegetation compare with modern vegetation. In this paper we present three LPG pollen records from the Carpathian Basin and the adjoining Carpathian Mountains to address this question and provide a concise compositional characterization of the LPG vegetation. Fossil pollen assemblages were compared with surface pollen spectra from the Altai-Sayan Mountains in southern Siberia. This area shows many similarities with the LPG vegetation of eastern-central Europe, and has long been considered as its best modern analogue. Ordination and analogue matching were used to characterize vegetation composition and find the best analogues. Our results show that few LPG pollen assemblages have statistically significant analogues in southern Siberia. When analogue pairings occur they suggest the predominance of wet and mesic grasslands and dry steppe in the studied region. Wooded vegetation types (continental and suboceanic hemiboreal forest, continental taiga) appear as significant analogues only in a few cases during the LGM and more frequently after 16 lea cal BP. These results suggest that the LPG landscape of the Carpathian Basin was dominated by dry steppe that occurred outside the river floodplains, while wet and mesic grasslands occurred in the floodplains and on other sites influenced by ground water. Woody vegetation mainly occurred in river valleys, on wet north-facing hillsides, and scattered trees were likely also present on the loess plateaus. The dominant woody species were Larix, Pious sylvestris, Pinus mugo, Pinus cembra, Picea abies, Betula pendula/pubescens, Betula nano, Juniperus, Hippophae rhamnoides, Populus, Salix and Alnus. The pollen records suggest uninterrupted presence of mesophilous temperate trees (Quercus, Ulmus, Corylus, Fagus and Fraxinus excelsior) in the Eastern Carpathian Mountains throughout the LPG. We demonstrate that the LPG vegetation in this area was characterized by increasing grass cover and high frequency of wildfires. We conclude that pollen spectra over represent trees in the forest-steppe landscape of the LPG, furthermore pollen-based quantitative climate reconstructions for the LPG are challenging in this area due to the scarcity of modern analogues.
ER  -

MAGYARI, Enikö Katalin, Petr KUNEŠ, Gusztav JAKAB, Pál SÜMEGI, Barbora PELÁNKOVÁ, Frank SCHÄBITZ, Mihály BRAUN a Milan CHYTRÝ. Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia? \textit{Quaternary Science Reviews}. 2014, roč.~95, JULY, s.~60-79. ISSN~0277-3791. Dostupné z: https://dx.doi.org/10.1016/j.quascirev.2014.04.020.

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