Differential proxy responses to late Allerød and early Younger Dryas climatic change recorded in varved sediments of the Trzechowskie palaeolake in Northern Poland
High-resolution biological proxies (pollen, macrofossils, Cladocera and diatoms), geochemical data (μ-XRF element scans, TOC, C/N ratios, δ18Ocarb and δ13Corg values) and a robust chronology based on varve counting, AMS 14C dating and tephrochronology were applied to reconstruct lake system response...
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| Main Authors: | , |
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| Format: | Article (Journal) |
| Language: | English |
| Published: |
7 January 2017
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| In: |
Quaternary science reviews
Year: 2017, Volume: 158, Pages: 94-106 |
| ISSN: | 0277-3791 |
| DOI: | 10.1016/j.quascirev.2017.01.005 |
| Online Access: | Verlag, Volltext: http://dx.doi.org/10.1016/j.quascirev.2017.01.005 Verlag, Volltext: http://www.sciencedirect.com/science/article/pii/S0277379117300161 
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| Author Notes: | Michał Słowiński, Izabela Zawiska, Florian Ott, Agnieszka M. Noryśkiewicz, Birgit Plessen, Karina Apolinarska, Monika Rzodkiewicz, Danuta J. Michczyńska, Sabine Wulf, Piotr Skubała, Jarosław Kordowski, Mirosław Błaszkiewicz, Achim Brauer |
| Summary: | High-resolution biological proxies (pollen, macrofossils, Cladocera and diatoms), geochemical data (μ-XRF element scans, TOC, C/N ratios, δ18Ocarb and δ13Corg values) and a robust chronology based on varve counting, AMS 14C dating and tephrochronology were applied to reconstruct lake system responses to rapid climatic and environmental changes of the Trzechowskie palaeolake (TRZ; Northern Poland) during the late Allerød - Younger Dryas (YD) transition. Palaeoecological and geochemical data at 5-15 years temporal resolution allowed tracing the dynamics of short-term shifts of the ecosystem triggered by abrupt climate change. The robust age control together with the high-resolution sampling allowed the detection of leads and lags between different proxies to the climate shift at the Allerød-Younger Dryas transition. Our results indicate (1) a water level decrease and an increase in wind activities during the late Allerød and the Allerød-YD transition, which caused intensified erosion in the catchment, (2) a two-decades delayed vegetation response in comparison to the lake depositional system. Comparison with the Lake Meerfelder Maar record revealed slightly different vegetation responses of the Trzechowskie palaeolake at the YD onset. |
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| Item Description: | Gesehen am 25.09.2018 |
| Physical Description: | Online Resource |
| ISSN: | 0277-3791 |
| DOI: | 10.1016/j.quascirev.2017.01.005 |