J 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
Název: Gradienty prostředí, vegetační dynamika a krajinné změny v Západních Karpatech od pozdního glaciálu po současnost (Akronym: PALAEO-CARPATHIANS)
Investor: Grantová agentura ČR, Environmental gradients, vegetation dynamics and landscape changes in the West Carpathians from the Late Glacial up to the present time