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Postglacial evolution of a small lake in the South Baltic coastal zone based on geochemical, pollen and subfossil Cladocera analysis Cover

Postglacial evolution of a small lake in the South Baltic coastal zone based on geochemical, pollen and subfossil Cladocera analysis

Oceanological and Hydrobiological Studies
Volume 47 (2018): Issue 4 (December 2018)
By: Monika Niska,  Joanna Gadziszewska,  Jerzy Jonczak,  Wacław Florek and  Bogusława Kruczkowska  
Open Access
|Dec 2018

Figures & Tables

Figure 1

Location of the site (a, b), morphology of the cliff (c, d), location and morphology of the paleolake profile and its calibrated radiocarbon age (e)
Location of the site (a, b), morphology of the cliff (c, d), location and morphology of the paleolake profile and its calibrated radiocarbon age (e)

Figure 2

Lithology, age (in calibrated years BP) and selected physical and chemical properties of the Debina profile
Lithology, age (in calibrated years BP) and selected physical and chemical properties of the Debina profile

Figure 3

Pollen concentration diagram, of non-pollen palynomorphs (NPPs), aquatic and marsh plants from the Debina profile
Pollen concentration diagram, of non-pollen palynomorphs (NPPs), aquatic and marsh plants from the Debina profile

Figure 4

Relative abundance diagram of subfossil cladoceran taxa, the total number of Cladocera specimens, and the number of species in the Debina profile
Relative abundance diagram of subfossil cladoceran taxa, the total number of Cladocera specimens, and the number of species in the Debina profile

Figure 5

Reconstruction of the hydroclimatic conditions in the Debina paleolake during the Late Glacial and the Early Holocene
Reconstruction of the hydroclimatic conditions in the Debina paleolake during the Late Glacial and the Early Holocene

Results of radiocarbon dating of the Debina profile

Depth (cm)Laboratory numberDated materialResult of dating in 14C yr BPCalibrated ages in 14C cal yr BP (95.4%) probabilityCalibrated ages in 14C cal yr BP (Median)
5–10MKL-2590bark2160 ± 602318–20012165
70–72MKL-2591organic remains8810 ± 9010173–95969870
83–85MKL-2592organic remains9170 ± 11010663–1016010365

Particle size distribution and logarithmic measures of the studied deposits

Depth (cm)% ofLogarithmic measures (ϕ)
gravelsandsiltclayMGσGSkGKG
0–100.090.75.14.32.831.490.221.42
10–560.891.46.12.52.461.290.301.13
56–700.093.84.61.62.241.150.211.16
70–871.490.36.03.72.551.740.221.54
87–1150.093.84.51.73.000.980.141.13
115–1254.693.04.12.82.571.50-0.071.47
125–1350.0100.00.00.01.340.810.001.38
135–1500.091.37.11.62.531.420.231.30
150–1661.293.94.51.62.441.26-0.031.26
166–1860.027.371.41.35.311.670.020.96
186–1900.0100.00.00.02.360.76-0.110.91
190–2000.067.925.76.44.212.180.351.29
200–2500.097.81.50.72.260.880.040.90
DOI: https://doi.org/10.1515/ohs-2018-0036 | Journal eISSN: 1897-3191 | Journal ISSN: 1730-413X
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Language: English
Page range: 384 - 397
Submitted on: Feb 28, 2018
Accepted on: Apr 25, 2018
Published on: Dec 3, 2018
Published by: University of Gdańsk
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year
Keywords:
Late Glacial-Holocene transition,
multi-proxy analysis,
cliff paleolake,
Polish Baltic Coast
Related subjects:
Chemistry,
Chemistry, other,
Geosciences,
Geosciences, other,
Life sciences,
Life sciences, other

© 2018 Monika Niska, Joanna Gadziszewska, Jerzy Jonczak, Wacław Florek, Bogusława Kruczkowska, published by University of Gdańsk
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

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