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  3. Response of subfossil Cladocera in Gerzensee (Swiss Plateau) to early Late Glacial environmental change

Response of subfossil Cladocera in Gerzensee (Swiss Plateau) to early Late Glacial environmental change

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DOI
10.7892/boris.52520
Publisher DOI
10.1016/j.palaeo.2012.10.021
Abstract
Sub-fossil Cladocera were studied in a core from Gerzensee (Swiss Plateau) for the late-glacial periods of Oldest Dryas, Bølling, and Allerød. Cladocera assemblages were dominated by cold-tolerant littoral taxa Chydorus sphaericus, Acroperus harpae, Alonella nana, Alona affinis, and Alonella excisa. The rapid warming at the beginning of the Bølling (GI-1e) ca. 14,650 yr before present (BP: before AD 1950) was indicated by an abrupt 2‰ shift in carbonate δ18O and a clear change in pollen assemblages. Cladocera assemblages, in contrast, changed more gradually. C. sphaericus and A. harpae are the most cold-tolerant, and their abundance was highest in the earliest part of the record. Only 150–200 years after the beginning of the Bølling warming we observed an increase in less cold-tolerant A. excisa and A. affinis. The establishment of Alona guttata, A. guttata var. tuberculata, and Pleuroxus unicatus was delayed by ca. 350, 770, and 800 years respectively after the onset of the Bølling. The development of the Cladocera assemblages suggests increasing water temperatures during the Bølling/Allerød, which agrees with the interpretation by von Grafenstein et al. (2013-this issue) that decreasing δ18O values in carbonates in this period reflect increasing summer water temperatures at the sediment–water interface. Other processes also affected the Cladocera community, including the development and diversification of aquatic vegetation favourable for Cladocera. The record is clearly dominated by Chydoridae, as expected for a littoral core. Yet, the planktonic Eubosmina-group occurred throughout the core, with the exception of a period at ca. 13,760–13,420 yr BP. Lake levels reconstructed for this period are relatively low, indicating that the littoral location might have become too shallow for Eubosmina in that period.
Date Issued
2013-12
Publication Type
Article
Subject(s)
500 Science > 580 Plants (Botany)
Subjects
Palaeolimnology
•
Cladocera
•
Late-glacial
•
Bølling
•
Climatic change
•
Biotic response
•
Switzerland
Language(s)
en
Author(s)
Nováková, Katařina
van Hardenbroek, Maarten Reinier  
Institut für Pflanzenwissenschaften (IPS)  
van der Knaap, Willem Oscar  
Institut für Pflanzenwissenschaften (IPS)  
Additional Credits
Institut für Pflanzenwissenschaften (IPS)  
Journal
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier
ISSN
0031-0182
Access(Rights)
restricted
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