The first high resolution diatom record from Lake Balaton, Hungary in Central Europe

被引:5
|
作者
Buczko, Krisztina [1 ,2 ]
Acs, Eva [1 ]
Baldi, Katalin [3 ]
Pozderka, Virag [4 ]
Braun, Mihaly [5 ]
Kiss, Keve Tiharner [1 ]
Korponai, Janos [6 ,7 ]
机构
[1] MTA Ctr Ecol Res, Danube Res Inst, Karolina St 29, H-1113 Budapest, Hungary
[2] Hungarian Nat Hist Museum, Dept Bot, Baross St 13, H-1088 Budapest, Hungary
[3] Eotvos Lorand Univ, Dept Phys & Appl Geol, Pazmany Peter St 1-C, H-1117 Budapest, Hungary
[4] Eotvos Lorand Univ, Doctoral Sch Environm Sci, Pazmany Peter St 1-C, H-1117 Budapest, Hungary
[5] Hungarian Acad Sci, Inst Nucl Res, Isotope Climatol & Environm Res Ctr ICER, Bem Sq 18-C, H-4026 Debrecen, Hungary
[6] Sapientia Hungarian Univ Transylvania, Dept Environm Sci, Calea Turzii Str 4, Cluj Napoca 400193, Romania
[7] MTA PE Limnoecol Res Grp, Wartha Vince St 1, H-8200 Veszprem, Hungary
来源
LIMNETICA | 2019年 / 38卷 / 01期
关键词
diatoms; geochemistry; Lake Balaton; lake level changes; shallow lake sediments; ORGANIC-MATTER; ZALAVARI POND; SHALLOW LAKE; WATER; SEDIMENTS; IGNITION;
D O I
10.23818/limn.38.24
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
A high-resolution diatom record of the last 7500 years of Lake Balaton, a large, shallow calcareous lake in Central Europe is presented here. Diatom analyses were carried out on a 112 cm long core obtained from the Siofok Basin (eastern part of the lake) combined with loss-on-ignition, geochemical measurements and grain-size analysis. Altogether 140 diatom taxa were distinguished in this study; Amphora pediculus, Cocconeis neothumensis, Fragilaria brevistriata and Karayevia clevei were frequent and ubiquitous members of diatom assemblages. Fragilaroid taxa were dominant through the core in the shallow Lake Balaton, but episodes of higher ratios of planktic forms (Lindavia balatonis, Aulacoseira granulata and Pantocsekiella ocellata) before ca. 2000 cal yr BP, indicated high water level in the lake, and stronger fluctuation than exists today. The diatom-based reconstruction of lake level was in accordance with the geochemical and zoological records, proving the usability of siliceous remains in paleolimnological reconstructions in Lake Balaton, in spite of the unfavourable preservation conditions.
引用
收藏
页码:417 / 430
页数:14
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