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  • 1
    Publication Date: 2021-07-21
    Description: We revise the conceptual model of calcite varves and present, for the first time, a dual lake monitoring study in two alkaline lakes providing new insights into the seasonal sedimentation processes forming these varves. The study lakes, Tiefer See in NE Germany and Czechowskie in N Poland, have distinct morphology and bathymetry, and therefore, they are ideal to decipher local effects on seasonal deposition. The monitoring setup in both lakes is largely identical and includes instrumental observation of (i) meteorological parameters, (ii) chemical profiling of the lake water column including water sampling, and (iii) sediment trapping at both bi‐weekly and monthly intervals. We then compare our monitoring data with varve micro‐facies in the sediment record. One main finding is that calcite varves form complex laminae triplets rather than simple couplets as commonly thought. Sedimentation of varve sub‐layers in both lakes is largely dependent on the lake mixing dynamics and results from the same seasonality, commencing with diatom blooms in spring turning into a pulse of calcite precipitation in summer and terminating with a re‐suspension layer in autumn and winter, composed of calcite patches, plant fragments and benthic diatoms. Despite the common seasonal cycle, the share of each of these depositional phases in the total annual sediment yield is different between the lakes. In Lake Tiefer See calcite sedimentation has the highest yields, whereas in Lake Czechowskie, the so far underestimated re‐suspension sub‐layer dominates the sediment accumulation. Even in undisturbed varved sediments, re‐suspended material becomes integrated in the sediment fabric and makes up an important share of calcite varves. Thus, while the biogeochemical lake cycle defines the varves’ autochthonous components and micro‐facies, the physical setting plays an important role in determining the varve sub‐layers’ proportion.
    Description: Leibniz‐Gemeinschaft http://dx.doi.org/10.13039/501100001664
    Description: Narodowe Centrum Nauki http://dx.doi.org/10.13039/501100004281
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: ICLEA
    Keywords: 552.58 ; 554.3 ; Baltic lowlands ; Tiefer See ; Czechowskie ; calcite varves ; seasonal sedimentation
    Type: article
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  • 2
    Publication Date: 2022-08-05
    Description: Lake‐level reconstructions are a key tool in hydro‐climate reconstructions, based on the assumption that lake‐level changes primarily reflect climatic changes. Although it is known that land cover changes can affect evapotranspiration and groundwater formation, this factor commonly receives little attention in the interpretation of past lake‐level changes. To address this issue in more detail, we explore the effects of land cover change on Holocene lake‐level fluctuations in Lake Tiefer See in the lowlands of northeastern Germany. We reconstruct lake‐level changes based on the analysis of 28 sediment records from different water depths and from the shore. We compare the results with land cover changes inferred from pollen data. We also apply hydrological modelling to quantify effects of land cover change on evapotranspiration and the lake level. Our reconstruction shows an overall lake‐level amplitude of about 10 m during the Holocene, with the highest fluctuations during the Early and Late Holocene. Only smaller fluctuations during the Middle Holocene can unambiguously be attributed to climatic fluctuations because the land cover was stable during that period. Fluctuations during the Early and Late Holocene are at least partly related to changes in natural and anthropogenic land cover. For several intervals the reconstructed lake‐level changes agree well with variations in modelled groundwater recharge inferred from land cover changes. In general, the observed amplitudes of lake‐level fluctuations are larger than expected from climatic changes alone and thus underline that land cover changes in lake catchments must be considered in climatic interpretations of past lake‐level fluctuations.
    Description: Helmholtz Association http://dx.doi.org/10.13039/501100001656
    Description: Leibniz‐Gemeinschaft http://dx.doi.org/10.13039/501100001664
    Keywords: ddc:551.793 ; ddc:551.6
    Language: English
    Type: doc-type:article
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  • 3
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    PANGAEA
    In:  Supplement to: Dräger, Nadine; Theuerkauf, Martin; Szeroczynska, Krystyna; Wulf, Sabine; Tjallingii, Rik; Plessen, Birgit; Kienel, Ulrike; Brauer, Achim (2016): Varve microfacies and varve preservation record of climate change and human impact for the last 6000 years at Lake Tiefer See (NE Germany). The Holocene, https://doi.org/10.1177/0959683616660173
    Publication Date: 2023-01-13
    Description: The Holocene sediment record of Lake Tiefer See exhibits striking alternations between well-varved and non-varved intervals. Here we present a high resolution multi-proxy record for the past ~6000 years and discuss possible causes for the observed sediment variability. This approach comprises of microfacies, geochemical and microfossil analyses as well as of a multiple dating concept including varve counting, tephrochronology and radiocarbon dating. Four periods of predominantly well-varved sediment were identified at 6000-3950 cal. a BP, 3100-2850 cal. a BP, 2100-750 cal. a BP and AD 1924-present. Except of sub-recent varve formation, these periods are considered to reflect reduced lake circulation and consequently, stronger anoxic bottom water conditions. In contrast, intercalated intervals of poor varve preservation or even extensively mixed non-varved sediments indicate strengthened lake circulation. Sub-recent varve formation since AD 1924 is, in addition to natural forcing, influenced by enhanced lake productivity due to modern anthropogenic eutrophication. The general increase in periods of intensified lake circulation in Lake Tiefer See since ~4000 cal. a BP presumably is caused by gradual changes in Northern Hemisphere orbital forcing, leading to cooler and windier conditions in Central Europe. Superimposed decadal to centennial scale variability of the lake circulation regime likely is the result of additional human-induced changes of the catchment vegetation. The coincidence of major non-varved periods at Lake Tiefer See and intervals of bioturbated sediments in the Baltic Sea implies a broader regional significance of our findings.
    Keywords: COMPCORE; Composite Core; Mecklenburg-West Pomerania, Germany; Tiefer-See
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 4
    Publication Date: 2023-01-13
    Keywords: AGE; COMPCORE; Composite Core; Mecklenburg-West Pomerania, Germany; Reconstructed; Sample code/label; Tiefer-See; Vegetation openness
    Type: Dataset
    Format: text/tab-separated-values, 490 data points
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  • 5
    Publication Date: 2023-02-08
    Keywords: AGE; COMPCORE; Composite Core; DEPTH, sediment/rock; ln-Calcium/Manganese ratio; ln-Titanium/Silicon ratio; Mecklenburg-West Pomerania, Germany; Tiefer-See
    Type: Dataset
    Format: text/tab-separated-values, 75714 data points
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  • 6
    Publication Date: 2023-02-08
    Keywords: AGE; Age, maximum/old; Age, minimum/young; Carbon, inorganic, total; Carbon, organic, total; Carbon/Nitrogen ratio; COMPCORE; Composite Core; Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Mecklenburg-West Pomerania, Germany; Sample code/label; Tiefer-See
    Type: Dataset
    Format: text/tab-separated-values, 6579 data points
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  • 7
    Publication Date: 2023-02-08
    Keywords: AGE; COMPCORE; Composite Core; DEPTH, sediment/rock; Mecklenburg-West Pomerania, Germany; Sedimentation rate per year; Tiefer-See; Varve quality index; Varve type
    Type: Dataset
    Format: text/tab-separated-values, 21050 data points
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  • 8
    Publication Date: 2023-02-08
    Keywords: Age, comment; Age, uncertainty; Age model; COMPCORE; Composite Core; Core; DEPTH, sediment/rock; Mecklenburg-West Pomerania, Germany; Tiefer-See
    Type: Dataset
    Format: text/tab-separated-values, 18277 data points
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  • 9
    Publication Date: 2023-07-10
    Keywords: AGE; Bosmina (Eubosmina) coregoni; Bosmina (Eubosmina) longispina; Bosmina longirostris; Cladocera; Cladocera, benthic; COMPCORE; Composite Core; Mecklenburg-West Pomerania, Germany; Sample code/label; Tiefer-See
    Type: Dataset
    Format: text/tab-separated-values, 1092 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Neugebauer, Ina; Brauer, Achim; Dräger, Nadine; Dulski, Peter; Wulf, Sabine; Plessen, Birgit; Mingram, Jens; Herzschuh, Ulrike; Brande, Arthur (2011): A Younger Dryas varve chronology from the Rehwiese palaeolake record in NE-Germany. Quaternary Science Reviews, 36, 91-102, https://doi.org/10.1016/j.quascirev.2011.12.010
    Publication Date: 2024-01-03
    Description: The first 1400-year floating varve chronology for north-eastern Germany covering the late Allerød to the early Holocene has been established by microscopic varve counts from the Rehwiese palaeolake sediment record. The Laacher See Tephra (LST), at the base of the studied interval, forms the tephrochronological anchor point. The fine laminations were examined using a combination of micro-facies and ?-XRF analyses and are typical of calcite varves, which in this case provide mainly a warm season signal. Two varve types with different sub-layer structures have been distinguished: (I) complex varves consisting of up to four seasonal sub-layers formed during the Allerød and early Holocene periods, and, (II) simple two sub-layer type varves only occurring during the Younger Dryas. The precision of the chronology has been improved by varve-to-varve comparison of two independently analyzed sediment profiles based on well-defined micro-marker layers. This has enabled both (1) the precise location of single missing varves in one of the sediment profiles, and, (2) the verification of varve interpolation in disturbed varve intervals in the parallel core. Inter-annual and decadal-scale variability in sediment deposition processes were traced by multi-proxy data series including seasonal layer thickness, high-resolution element scans and total organic and inorganic carbon data at a five-varve resolution. These data support the idea of a two-phase Younger Dryas, with the first interval (12,675 - 12,275 varve years BP) characterised by a still significant but gradually decreasing warm-season calcite precipitation and a second phase (12,275 - 11,640 varve years BP) with only weak calcite precipitation. Detailed correlation of these two phases with the Meerfelder Maar record based on the LST isochrone and independent varve counts provides clues about regional differences and seasonal aspects of YD climate change along a transect from a location proximal to the North Atlantic in the west to a more continental site in the east.
    Keywords: Berlin, Germany; Geological profile sampling; GEOPRO; Palaeolake; Rehwiese
    Type: Dataset
    Format: application/zip, 4 datasets
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