2018
Spatiotemporal heterogeneity of the palaeoecological record in a large temperate palaeolake, Šúr, southwest Slovakia: Comparison of pollen, macrofossil and geochemical data
POTŮČKOVÁ, Anna, Petra HÁJKOVÁ, Pavla ŽÁČKOVÁ, Libor PETR, Grygar Tomáš MATYS et. al.Základní údaje
Originální název
Spatiotemporal heterogeneity of the palaeoecological record in a large temperate palaeolake, Šúr, southwest Slovakia: Comparison of pollen, macrofossil and geochemical data
Autoři
POTŮČKOVÁ, Anna (203 Česká republika), Petra HÁJKOVÁ (203 Česká republika, garant, domácí), Pavla ŽÁČKOVÁ (203 Česká republika), Libor PETR (203 Česká republika, domácí), Grygar Tomáš MATYS (203 Česká republika) a Weiser MARTIN (703 Slovensko)
Vydání
Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2018, 0031-0182
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10600 1.6 Biological sciences
Stát vydavatele
Nizozemské království
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.616
Kód RIV
RIV/00216224:14310/18:00100746
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000416501000005
Klíčová slova anglicky
Palaeorecord heterogeneity Multi-proxy Palaeohydrology Lake ecosystem Lake ontogeny Pannonian Basin
Štítky
Příznaky
Recenzováno
Změněno: 23. 4. 2024 10:47, Mgr. Michal Petr
Anotace
V originále
Aquatic macrophytes living within shallow lakes are particularly sensitive to climate change and fluctuations in water depth. In the Dabubian Lowland of southwestern Slovakia, sediments from the large, shallow palaeolake, named Šúr, provide a unique opportunity to reconstruct changes in water depth to analyse succession within local aquatic and terrestrial vegetation. Here, we used a multi-core, multi-proxy approach (macrofossils, pollen, and geochemistry) in order to reconstruct water depth changes and its influence on aquatic and terrestrial vegetation succession during the Holocene. Additionally, we also consider how heterogeneity in proxy data varied across time and space. Using particular macrophyte taxa found in the macrofossil assemblage, which have specific water depth requirements, our results demonstrate changes in water depth created a long-term mosaic of vegetation succession. In the Early Holocene, aquatic macrophytes suggest the water column was high. During the Middle Holocene, water depths decreased creating mosaics of aquatic succession. By ca 4200 cal yr B.P., terrestrialization had occurred in the former lake area. Regional vegetation succession was likely more influenced by the presence of fluvial sands and/or by low precipitation and high evaporation rates, which delayed the expansion of temperate trees and favoured Pinus until 8850 cal yr B.P. Macrofossils exhibit the lowest temporal variation among all proxies, which suggests a rather stable macrophyte community when water depth was high. Pollen data show very low spatial variation given by the size of the accumulation basin, which reflects regional pollen rain. Higher spatial variation was observed in the geochemistry and macrofossil data compared to the pollen data, which could be the result of different mosaics of aquatic plants, local dispersion of propagules, or changes in sediment types. We conclude that changes in water depth were not homogenous.
Návaznosti
GAP504/11/0429, projekt VaV |
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