Development of Kubłowo Palaeolake in Central Poland During Eemian Based on Subfossil Cladocera Analysis – Preliminary Results

Niska, Monika; Roman, Małgorzata

doi:10.2478/squa-2014-0003

Cited by 9 publications

(10 citation statements)

References 2 publications

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“…Similar species composition at the beginning of the early Eemian is observed also in other polish lakes, such as Starowlany paleolake and Kubłowo paleolake (Niska and Roman, 2014;Niska and Kołodziej, 2015), as well as in central and northern european lakes (Szeroczyńska, 1985;Sarmaja-Korjonen and Alhonen, 1999;Gąsiorowski and Szeroczyńska, 2004).…”

Section: Early Eemiansupporting

confidence: 72%

“…Similar Cladocera trends during the Late Eemian is documented in the other paleolakes, e.g., Kuców IIc (Niska, 2008), Kaliska and Kubłowo from central Poland (Mirosław-Grabowska and Niska, 2007a;Niska and Roman, 2014), indicating a comparable regional influence on the Cladocera community by regional climate development. On the other hand, although the Cladocera species diversity and abundance increase in the Herning paleolake as in the other paleolakes, changes in species frequency are not so significant due to the smaller differences in the climate condition and more moist (oceanic) climate .…”

Section: Late Eemiansupporting

confidence: 71%

“…This period are characterize by species preferring warm water temperatures and the replacement of E. coregoni by B. longirostris suggest a reduction in the lake water level and an increase in the lake trophy (Hofman 1987;Szeroczyńska, 1998b;Nevalainen et al, 2013). The high Cadocera abundance and diversity in this period reveal an improvement of the water living conditions, which is also observed in Kubłowo lake (Niska and Roman, 2014). The pollen analysis by Kupryjanowicz (2008) highlight a boreal forest spread, which confirmed the improving of the climate conditions.…”

Section: Early Vistulian Brørupmentioning

confidence: 56%

“…At that time, a significant reduction in the Cladocera abundance is observed in the other Eemian sites in Poland, e.g. Kaliska, Ruszkówek and Kubłowo (Mirosław-Grabowska and Niska, 2007a;Mirosław-Grabowska et al, 2009;Niska and Roman, 2014).…”

Section: Paz S-3 (Quercus-ulmus-fraxinus) -R Paz E3 L Paz S-4 (Cormentioning

confidence: 94%

“…Spruce (Picea) appears and gradually spread, the role of pine and birch also The recorded pollen trees suggest hotter and longer summers than in the zone L PAZ S-4, and still mild winter (Kupryjanowicz, 2008;Niska, 2008 (Kupryjanowicz, 2008), but the palynological analysis indicates a later winter tightening and a climate drying (Kupryjanowicz et al, 2004). At that time, a significant reduction in the abundance of Cladocera is observed in the other Eemian sites in Poland, e.g., Kaliska, Ruszkówek and Kubłowo (Mirosław-Grabowska and Niska, 2007a;Mirosław-Grabowska et al, 2009;Niska and Roman, 2014). In paleolake Herning, a drop in the abundance of Cladocera is noted at the end of R PAZ E4 and the beginning of R PAZ E5 (Frey, 1962).…”

Section: Paz S-3 (Quercus-ulmus-fraxinus) -R Paz E3 L Paz S-4 (Cormentioning

confidence: 98%

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The Eemian/Early Vistulian development of the Solniki paleolake (north-eastern Poland) as shown by subfossil Cladocera

Niska

2016

Adv Ocean Limnol

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This work presents results of a paleolimnological study focussed on subfossil Cladocera analysis and on different aspects of the evolution of the Solniki paleolake during the Eemian/Early Vistulian period. The study aimed at the reconstruction of the long-term dynamics of this paleoecosystem and at defining the conditions (e.g., water level, trophic status and water temperature) of the ancient lake. Paleolacustrine deposits of ca. 10 m thickness were discovered at Solniki during cartographic works for the Trześcianka sheet of the Detailed Geological Map of Poland. This archives recorded one full-interglacial sequence (Eemian Interglacial), one interstadial warming (Brørup) and two stadial coolings (Herning and Rederstall) stages, which were confirmed by palynological analyses. The subfossil Cladocera fauna from the Solniki paleolake consisted in 17 species belonging to the families Bosminidae, Chydoridae, Sididae and Daphniidae. Littoral species were dominant (52%), the most frequent of which were Alona affinis and Camptocercus rectirostris. The most abundance pelagic species were Eubosmina coregoni and Bosmina longirostris. The sediment species composition was quite similar to that of contemporary Central European lakes. The early and the late stages of Eemian Interglacial were likely the most favourable periods for the Cladocera development in the paleolake, in relation to higher water level, moderate water temperature and the mesotrophic state of water. A further ecologically favourable period was the Brørup Interstadial. The highest species richness, abundance, and diversity during the whole paleolake existence were recorded during these three periods. Surprisingly, the middle of the Middle Eemian Interglacial climate optimum appeared as an unfavourable period for the Cladocera growth as it was associated with decreasing water level and pronounced climate fluctuations. This sequence was also recorded by other studies of Eemian lakes in Central Europe.

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Section: Early Eemiansupporting

confidence: 72%

Section: Late Eemiansupporting

confidence: 71%

Section: Early Vistulian Brørupmentioning

confidence: 56%

Section: Paz S-3 (Quercus-ulmus-fraxinus) -R Paz E3 L Paz S-4 (Cormentioning

confidence: 94%

Section: Paz S-3 (Quercus-ulmus-fraxinus) -R Paz E3 L Paz S-4 (Cormentioning

confidence: 98%

See 3 more Smart Citations

The Eemian/Early Vistulian development of the Solniki paleolake (north-eastern Poland) as shown by subfossil Cladocera

Niska

2016

Adv Ocean Limnol

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Reaction of lake environment on the climatic cooling – Transition from the Eemian Interglacial to Early Vistulian on the basis of Solniki palaeolake sediments (NE Poland)

Mirosław‐Grabowska

Niska

Kupryjanowicz

2015

Quaternary International

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Long (MIS 5e – 3) environmental history of a paleolake in central Poland recorded in the succession from Kubłowo

Mirosław‐Grabowska

Niska²,

Roman

2018

Quaternary International

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Development of Kubłowo Palaeolake in Central Poland During Eemian Based on Subfossil Cladocera Analysis – Preliminary Results

Cited by 9 publications

References 2 publications

The Eemian/Early Vistulian development of the Solniki paleolake (north-eastern Poland) as shown by subfossil Cladocera

The Eemian/Early Vistulian development of the Solniki paleolake (north-eastern Poland) as shown by subfossil Cladocera

Reaction of lake environment on the climatic cooling – Transition from the Eemian Interglacial to Early Vistulian on the basis of Solniki palaeolake sediments (NE Poland)

Long (MIS 5e – 3) environmental history of a paleolake in central Poland recorded in the succession from Kubłowo

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