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Holocene paleoclimatic and paleohydrological changes in Lake Balaton as inferred from a complex quantitative environmental historical study of a lacustrine sequence of the Szigliget embayment
Sümegi, Pál (Author), Gulyás, Sándor (Author), Jakab, Gusztáv (Author)

URLURL - Presentation file, Visit http://www.dlib.si/details/URN:NBN:SI:DOC-O0Y5O7MU This link opens in a new window

Abstract
Članek predstavlja rezultate kompleksne kvantitativne pelookoljske raziskave, katere cilj je ugotavljanje pleniglacialnega, poznoglacialnega in postglacialnega razvoja Blatnega jezera v zahodni Madžarski. V zaporedju poznopleistocenskih in holocenskih jezerskih sedimentov in šote je ohranjena celotna zgodovina porečja zaliva Szigliget od njegovega nastanka naprej. Ugotovljene paleohidrološke spremembe skupaj s premenami jezera smo primerjalis spremembami v kopenski vegetaciji. Na podlagi raziskav lahko nastanek zaliva umestimo v prehod med pleniglacialom in začetkom kasnega glaciala. Količina vode in geomorfološki položaj je pogojeval nastanku velikega spektra vodne vegetacije in habitatnih tipov. Skupna kvantitativna analiza sedimentacijskih značilnosti in fosilnih zbirov nam omogoča, da lahko opišemo zaporedje paleohidroloških premen v obalnem delu zaliva.

Language:English
Keywords:arheologija, paleohidrološke spremembe, holocen, archaeology, paleohydrological changes, Holocene
Work type:Not categorized (r6)
Tipology:1.01 - Original Scientific Article
Organization:FF - Faculty of Arts
Year:2008
Publisher:Oddelek za arheologijo Filozofske fakultete Univerze v Ljubljani
Number of pages:str. 33-43
Numbering:[Zv.] 35
UDC:551.583.7:911.52(439)"63":902.67
ISSN on article:1408-967X
COBISS.SI-ID:38141794 Link is opened in a new window
Views:489
Downloads:140
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Record is a part of a journal

Title:Documenta Praehistorica
Shortened title:Doc. Praehistor.
Publisher:Oddelek za arheologijo Filozofske fakultete Univerze v Ljubljani
ISSN:1408-967X
COBISS.SI-ID:98765312 This link opens in a new window

Secondary language

Language:English
Abstract:
The present paper discusses the findings of a complex quantitative paleoecological investigation implemented for capturing the Upper Weichselian, Late Glacial and Postglacial development of Lake Balaton in western Hungary, in the heart of Transdanubia. The studied Late Pleistocene and Holocene lacustrine marl and peat sequence preserved the complete evolutionary history of the catchment basin of the Szigliget Embayment from the time of its birth. The inferred palaeohydrological changes, along with that of the hydroseries, were compared to those observable coevally in the terrestrial vegetation. According to the available data, the birth of the studied embayment can be put to the Late Glacial/Upper Weichselian transition.A wide array of hydrophyte vegetation and habitat types emerged in the embayment depending on the actual water supply and geomorphologic position. Based on a collective quantitative evaluation of the observed sedimentary features and fossil assemblages retrieved from the sequence, a record of paleohydrological transformations in the littoral part of the lake was drawn.


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