2017
Palaeodistribution modelling of European vegetation types at the Last Glacial Maximum using modern analogues from Siberia: Prospects and limitations
JANSKÁ, Veronika, Francisco De Borja JIMÉNEZ ALFARO GONZÁLEZ, Milan CHYTRÝ, Jan DIVÍŠEK, Oleg ANENKHONOV et. al.Základní údaje
Originální název
Palaeodistribution modelling of European vegetation types at the Last Glacial Maximum using modern analogues from Siberia: Prospects and limitations
Autoři
JANSKÁ, Veronika (203 Česká republika, domácí), Francisco De Borja JIMÉNEZ ALFARO GONZÁLEZ (724 Španělsko, garant, domácí), Milan CHYTRÝ (203 Česká republika, domácí), Jan DIVÍŠEK (203 Česká republika, domácí), Oleg ANENKHONOV (643 Rusko), Andrey KOROLYUK (643 Rusko), Nikolai LASHCHINSKYI (643 Rusko) a Martin CULEK (203 Česká republika, domácí)
Vydání
Quaternary Science Reviews, Oxford, PERGAMON-ELSEVIER SCIENCE LTD, 2017, 0277-3791
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10611 Plant sciences, botany
Stát vydavatele
Velká Británie a Severní Irsko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 4.334
Kód RIV
RIV/00216224:14310/17:00094647
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000395609300008
Klíčová slova anglicky
Europe; Last Glacial Maximum; Modern analogues; Palaeoecological reconstructions; Siberia; Species distribution modelling
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 10. 4. 2018 13:13, Ing. Nicole Zrilić
Anotace
V originále
We modelled the European distribution of vegetation types at the Last Glacial Maximum (LGM) using present-day data from Siberia, a region hypothesized to be a modern analogue of European glacial climate. Distribution models were calibrated with current climate using 6274 vegetation-plot records surveyed in Siberia. Out of 22 initially used vegetation types, good or moderately good models in terms of statistical validation and expert-based evaluation were computed for 18 types, which were then projected to European climate at the LGM. The resulting distributions were generally consistent with reconstructions based on pollen records and dynamic vegetation models. Spatial predictions were most reliable for steppe, forest-steppe, taiga, tundra, fens and bogs in eastern and central Europe, which had LGM climate more similar to present-day Siberia. The models for western and southern Europe, regions with a lower degree of climatic analogy, were only reliable for mires and steppe vegetation, respectively. Modelling LGM vegetation types for the wetter and warmer regions of Europe would therefore require gathering calibration data from outside Siberia. Our approach adds value to the reconstruction of vegetation at the LGM, which is limited by scarcity of pollen and macrofossil data, suggesting where specific habitats could have occurred. Despite the uncertainties of climatic extrapolations and the difficulty of validating the projections for vegetation types, the integration of palaeodistribution modelling with other approaches has a great potential for improving our understanding of biodiversity patterns during the LGM.
Návaznosti
CZ.1.07/2.3.00/30.0037, interní kód MU (Kód CEP: EE2.3.30.0037) |
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GAP504/11/0454, projekt VaV |
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