Lake level reconstruction Lake Fürstenseer See, NE Germany, supplement to: Dietze, Elisabeth; Słowiński, Michał; Zawiska, Izabela; Veh, Georg; Brauer, Achim (2016): Multiple drivers of Holocene lake level changes at a lowland lake in northeastern Germany. Boreas, 45(4), 828-845
Many German lakes experienced significant water level declines in recent decades that are not fully understood due to the short observation period. At a typical northeastern German groundwater-fed lake with a complex basin morphology, an acoustic sub-bottom profile was analysed together with a trans...
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ftdatacite:10.1594/pangaea.881812 2023-05-15T16:37:57+02:00 Lake level reconstruction Lake Fürstenseer See, NE Germany, supplement to: Dietze, Elisabeth; Słowiński, Michał; Zawiska, Izabela; Veh, Georg; Brauer, Achim (2016): Multiple drivers of Holocene lake level changes at a lowland lake in northeastern Germany. Boreas, 45(4), 828-845 Dietze, Elisabeth 2017 application/zip https://dx.doi.org/10.1594/pangaea.881812 https://doi.pangaea.de/10.1594/PANGAEA.881812 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://store.pangaea.de/Publications/Dietze_2017/OriginalFiles.zip https://dx.doi.org/10.1111/bor.12190 https://store.pangaea.de/Publications/Dietze_2017/OriginalFiles.zip Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY article Supplementary Collection of Datasets Collection 2017 ftdatacite https://doi.org/10.1594/pangaea.881812 https://doi.org/10.1111/bor.12190 2022-02-09T13:17:41Z Many German lakes experienced significant water level declines in recent decades that are not fully understood due to the short observation period. At a typical northeastern German groundwater-fed lake with a complex basin morphology, an acoustic sub-bottom profile was analysed together with a transect of five sediment cores, which were correlated using multiple proxies (sediment facies, mu-XRF, macrofossils, subfossil Cladocera). Shifts in the boundary between sand and mud deposition were controlled by lake level changes, and hence, allowed the quantification of an absolute lake level amplitude of ~8 m for the Holocene. This clearly exceeded observed modern fluctuations of 1.3 m (AD 1973-2010). Past lake level changes were traced continuously using the calcium-record. During high lake levels, massive organic muds were deposited in the deepest lake basin, whereas lower lake levels isolated the sub-basins and allowed carbonate deposition. During the beginning of the Holocene (>9700 cal. a BP), lake levels were high, probably due to final melting of permafrost and dead-ice remains. The establishment of water-use intensive Pinus forests caused generally low (3-4 m below modern) but fluctuating lake levels (9700-6400 cal. a BP). Afterwards, the lake showed an increasing trend and reached a short-term highstand at c. 5000 cal. a BP (4 m above modern). At the transition towards a cooler and wetter late Holocene, forests dominated by Quercus and Fagus and initial human impact probably contributed more positively to groundwater recharge. Lake levels remained high between 3800 and 800 cal. a BP, but the lake system was not sensitive enough to record short-term fluctuations during this period. Lake level changes were recorded again when humans profoundly affected the drainage system, land cover and lake trophy. Hence, local Holocene water level changes reflect feedbacks between catchment and vegetation characteristics and human impact superimposed by climate change at multiple temporal scales. Article in Journal/Newspaper Ice permafrost DataCite Metadata Store (German National Library of Science and Technology) Boreas ENVELOPE(-3.933,-3.933,-71.300,-71.300) Lower Lake ENVELOPE(-129.290,-129.290,53.428,53.428) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
description |
Many German lakes experienced significant water level declines in recent decades that are not fully understood due to the short observation period. At a typical northeastern German groundwater-fed lake with a complex basin morphology, an acoustic sub-bottom profile was analysed together with a transect of five sediment cores, which were correlated using multiple proxies (sediment facies, mu-XRF, macrofossils, subfossil Cladocera). Shifts in the boundary between sand and mud deposition were controlled by lake level changes, and hence, allowed the quantification of an absolute lake level amplitude of ~8 m for the Holocene. This clearly exceeded observed modern fluctuations of 1.3 m (AD 1973-2010). Past lake level changes were traced continuously using the calcium-record. During high lake levels, massive organic muds were deposited in the deepest lake basin, whereas lower lake levels isolated the sub-basins and allowed carbonate deposition. During the beginning of the Holocene (>9700 cal. a BP), lake levels were high, probably due to final melting of permafrost and dead-ice remains. The establishment of water-use intensive Pinus forests caused generally low (3-4 m below modern) but fluctuating lake levels (9700-6400 cal. a BP). Afterwards, the lake showed an increasing trend and reached a short-term highstand at c. 5000 cal. a BP (4 m above modern). At the transition towards a cooler and wetter late Holocene, forests dominated by Quercus and Fagus and initial human impact probably contributed more positively to groundwater recharge. Lake levels remained high between 3800 and 800 cal. a BP, but the lake system was not sensitive enough to record short-term fluctuations during this period. Lake level changes were recorded again when humans profoundly affected the drainage system, land cover and lake trophy. Hence, local Holocene water level changes reflect feedbacks between catchment and vegetation characteristics and human impact superimposed by climate change at multiple temporal scales. |
format |
Article in Journal/Newspaper |
author |
Dietze, Elisabeth |
spellingShingle |
Dietze, Elisabeth Lake level reconstruction Lake Fürstenseer See, NE Germany, supplement to: Dietze, Elisabeth; Słowiński, Michał; Zawiska, Izabela; Veh, Georg; Brauer, Achim (2016): Multiple drivers of Holocene lake level changes at a lowland lake in northeastern Germany. Boreas, 45(4), 828-845 |
author_facet |
Dietze, Elisabeth |
author_sort |
Dietze, Elisabeth |
title |
Lake level reconstruction Lake Fürstenseer See, NE Germany, supplement to: Dietze, Elisabeth; Słowiński, Michał; Zawiska, Izabela; Veh, Georg; Brauer, Achim (2016): Multiple drivers of Holocene lake level changes at a lowland lake in northeastern Germany. Boreas, 45(4), 828-845 |
title_short |
Lake level reconstruction Lake Fürstenseer See, NE Germany, supplement to: Dietze, Elisabeth; Słowiński, Michał; Zawiska, Izabela; Veh, Georg; Brauer, Achim (2016): Multiple drivers of Holocene lake level changes at a lowland lake in northeastern Germany. Boreas, 45(4), 828-845 |
title_full |
Lake level reconstruction Lake Fürstenseer See, NE Germany, supplement to: Dietze, Elisabeth; Słowiński, Michał; Zawiska, Izabela; Veh, Georg; Brauer, Achim (2016): Multiple drivers of Holocene lake level changes at a lowland lake in northeastern Germany. Boreas, 45(4), 828-845 |
title_fullStr |
Lake level reconstruction Lake Fürstenseer See, NE Germany, supplement to: Dietze, Elisabeth; Słowiński, Michał; Zawiska, Izabela; Veh, Georg; Brauer, Achim (2016): Multiple drivers of Holocene lake level changes at a lowland lake in northeastern Germany. Boreas, 45(4), 828-845 |
title_full_unstemmed |
Lake level reconstruction Lake Fürstenseer See, NE Germany, supplement to: Dietze, Elisabeth; Słowiński, Michał; Zawiska, Izabela; Veh, Georg; Brauer, Achim (2016): Multiple drivers of Holocene lake level changes at a lowland lake in northeastern Germany. Boreas, 45(4), 828-845 |
title_sort |
lake level reconstruction lake fürstenseer see, ne germany, supplement to: dietze, elisabeth; słowiński, michał; zawiska, izabela; veh, georg; brauer, achim (2016): multiple drivers of holocene lake level changes at a lowland lake in northeastern germany. boreas, 45(4), 828-845 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2017 |
url |
https://dx.doi.org/10.1594/pangaea.881812 https://doi.pangaea.de/10.1594/PANGAEA.881812 |
long_lat |
ENVELOPE(-3.933,-3.933,-71.300,-71.300) ENVELOPE(-129.290,-129.290,53.428,53.428) |
geographic |
Boreas Lower Lake |
geographic_facet |
Boreas Lower Lake |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_relation |
https://store.pangaea.de/Publications/Dietze_2017/OriginalFiles.zip https://dx.doi.org/10.1111/bor.12190 https://store.pangaea.de/Publications/Dietze_2017/OriginalFiles.zip |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.881812 https://doi.org/10.1111/bor.12190 |
_version_ |
1766028261259739136 |