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  • 2015-2019  (1,648)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Stuttgart : J.B. Metzler Verlag
    Call number: IASS 17.91075
    Type of Medium: Monograph available for loan
    Pages: VIII, 367 Seiten , Diagramme , 25 cm
    ISBN: 9783476023896 , 9783476051936 (electronic)
    Language: German
    Branch Library: RIFS Library
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  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Dietze, Elisabeth; Brykała, Dariusz; Schreuder, Laura T; Jażdżewski, Krzysztof; Blarquez, Olivier; Brauer, Achim; Dietze, Michael; Obremska, Milena; Ott, Florian; Pieńczewska, Anna; Schouten, Stefan; Hopmans, Ellen C; Słowiński, Michał (2019): Human-induced fire regime shifts during 19th century industrialization: A robust fire regime reconstruction using northern Polish lake sediments. PLoS ONE, 14(9), e0222011, https://doi.org/10.1371/journal.pone.0222011
    Publication Date: 2023-11-03
    Description: Here we provide the data set of fire proxies from the 77 ha, 32 m deep Lake Czechowskie (53°52′27″N 18°14′12″E, 109 m a.s.l.), northern Poland. The sediment core JC11-K5 was recovered in 2011 in 30 m water depth using an UWITEC gravity corer. JC11-K5 was dated by correlating ten macroscopically visible layers with counted annual layer sequences of adjacent cores and tephra shards related to the Askja eruption in 1875 CE. As a conservative estimate, we assigned a 2σ error of 10 years to the marker layers that we used for calculating the age-depth model in OxCal v. 4.2, a Bayesian age-depth modelling approach that provides posterior age uncertainties. For sedimentary macroscopic charcoal analysis, 1 cm3 of wet sediment was dissolved in water, sieved through a 150-µm mesh. Under a stereomicroscope, macroscopic charcoal of three size classes (150-300, 300-500, and ≥500 µm) was counted continuously throughout the core. To estimate a proxy error that combines sampling, preparation and macrocharcoal counting uncertainties, we continuously sampled short core JC11-K2 between 35-55 cm core depth (n = 20), i.e., interval 1840-1875 CE, that could be linked to core JC11-K5 by four marker layers as determined from varve counting. Samples were processed in the same way as for JC11-K5. The numbers of absolute particles cm-³ were compared with the JC11-K5 samples of the same time interval (n = 31) to determine an overall mean relative standard deviation of 0.8 % of each sample. The topmost 75 samples (1780-2010 CE) were also analyzed for monosaccharide anhydrides (MAs) (n = 75, 1780-2011 CE): 125-250 mg dry sediment were extracted with a DIONEX Accelerated Solvent Extractor (ASE 200, 100 °C, 7.6×106 Pa) using a 9:1 solvent mixture of dichloromethane (DCM):methanol (MeOH). As an internal standard, 2.5-5 ng deuterated levoglucosan (dLVG) was added. The total lipid extracts were separated on an unactivated SiO2 gel column (Merck Si60, grade 7754) using sequential elution with DCM:MeOH (9:1) and DCM:MeOH (1:1). The 1:1 fractions were re-dissolved in 95:5 acetonitrile:H2O and filtered using a 0.45 µm polytetrafluoroethylene filter before analysis. The MAs were analyzed by ultra-high pressure liquid chromatography-high resolution mass spectrometry. Authentic standards for LVG, GAL and MAN were obtained from Sigma Aldrich, and that for dLVG (C6H3D7O5) from Cambridge Isotope Laboratories, Inc. Integrations were performed on mass chromatograms within 3 ppm mass accuracy. Concentrations were corrected for relative response factors to dLVG of 0.997, 0.822, and 2.137 for LVG, MAN, and GAL, respectively. Instrumental (standard) errors for LVG, MAN, and GAL were 4 ± 3, 14 ± 15, and 28 ± 38% (1σ), respectively.
    Keywords: AWI_Envi; GeoForschungszentrum Potsdam; GFZ; lake sediment proxies; levoglucosan; macroscopic charcoal; paleofire; Polar Terrestrial Environmental Systems @ AWI
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 3
    Publication Date: 2023-11-03
    Description: Processed monosaccharide anhydrides records based on the raw data of sediment core JC11-K5 of Lake Czechowskie, N Poland using a robust Monte Carlo based approach that includes age and proxy measurement uncertainties in equally spaced time windows. For details and code see Dietze et al. (2019).
    Keywords: Age; AGE; AWI_Envi; Galactosan, flux; GCUWI; GeoForschungszentrum Potsdam; GFZ; Gravity corer, UWITEC; JC11-K5; Lake Czechowskie; lake sediment proxies; levoglucosan; Levoglucosan, flux; macroscopic charcoal; Mannosan, flux; Monte Carlo based quartile ranges; paleofire; Polar Terrestrial Environmental Systems @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 836 data points
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  • 4
    Publication Date: 2023-11-03
    Description: Processed charcoal records based on the raw data of sediment core JC11-K5 of Lake Czechowskie, N Poland using a robust Monte Carlo based approach that includes age and proxy measurement uncertainties in equally spaced time windows. For details and code see Dietze et al. (2019).
    Keywords: Age; AGE; AWI_Envi; Charcoal, flux; GCUWI; GeoForschungszentrum Potsdam; GFZ; Gravity corer, UWITEC; JC11-K5; Lake Czechowskie; lake sediment proxies; levoglucosan; macroscopic charcoal; Monte Carlo based quartile ranges; paleofire; Polar Terrestrial Environmental Systems @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 1176 data points
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  • 5
    Publication Date: 2023-11-03
    Description: JC11-K5 was dated by correlating ten macroscopically visible layers with counted annual layer sequences of adjacent cores and tephra shards related to the Askja eruption in 1875 CE. As a conservative estimate, we assigned a 2σ error of 10 years to the marker layers that we used for calculating the age-depth model in OxCal v. 4.2, a Bayesian age-depth modelling approach that provides posterior age uncertainties.
    Keywords: Age; AGE; Age, error; AWI_Envi; correlation method; DEPTH, sediment/rock; GCUWI; GeoForschungszentrum Potsdam; GFZ; Gravity corer, UWITEC; JC11-K5; Lake Czechowskie; Polar Terrestrial Environmental Systems @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 243 data points
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  • 6
    Publication Date: 2023-11-03
    Description: For sedimentary macroscopic charcoal analysis, 1 cm3 of wet sediment was dissolved in water, sieved through a 150-µm mesh. Under a stereomicroscope, macroscopic charcoal of three size classes (150-300, 300-500, and ≥500 µm) was counted continuously throughout the core. To estimate a proxy error that combines sampling, preparation and macrocharcoal counting uncertainties, we continuously sampled short core JC11-K2 between 35-55 cm core depth (n = 20), i.e., interval 1840-1875 CE, that could be linked to core JC11-K5 by four marker layers as determined from varve counting. Samples were processed in the same way as for JC11-K5. The numbers of absolute particles cm-³ were compared with the JC11-K5 samples of the same time interval (n = 31) to determine an overall mean relative standard deviation of 0.8 % of each sample. The topmost 75 samples (1780-2010 CE) were also analyzed for monosaccharide anhydrides (MAs) (n = 75, 1780-2011 CE): 125-250 mg dry sediment were extracted with a DIONEX Accelerated Solvent Extractor (ASE 200, 100 °C, 7.6×106 Pa) using a 9:1 solvent mixture of dichloromethane (DCM):methanol (MeOH). As an internal standard, 2.5-5 ng deuterated levoglucosan (dLVG) was added. The total lipid extracts were separated on an unactivated SiO2 gel column (Merck Si60, grade 7754) using sequential elution with DCM:MeOH (9:1) and DCM:MeOH (1:1). The 1:1 fractions were re-dissolved in 95:5 acetonitrile:H2O and filtered using a 0.45 µm polytetrafluoroethylene filter before analysis. The MAs were analyzed by ultra-high pressure liquid chromatography-high resolution mass spectrometry using a method adapted from earlier HPLC-ESI/MS2 methods (Hopmans et al., 2013). Authentic standards for LVG, GAL and MAN were obtained from Sigma Aldrich, and that for dLVG (C6H3D7O5) from Cambridge Isotope Laboratories, Inc. Integrations were performed on mass chromatograms within 3 ppm mass accuracy. Concentrations were corrected for relative response factors to dLVG of 0.997, 0.822, and 2.137 for LVG, MAN, and GAL, respectively. Instrumental (standard) errors for LVG, MAN, and GAL were 4 ± 3, 14 ± 15, and 28 ± 38% (1σ), respectively.
    Keywords: AWI_Envi; Charcoal; Counting, charcoal; DEPTH, sediment/rock; Galactosan; Galactosan per unit sediment mass; GCUWI; GeoForschungszentrum Potsdam; GFZ; Gravity corer, UWITEC; High-performance liquid chromatography electrospray ionization-tandemmass spectrometry system (HPLC-ESI-MS/MS); JC11-K5; Lake Czechowskie; lake sediment proxies; levoglucosan; Levoglucosan; Levoglucosan per unit sediment mass; macroscopic charcoal; Mannosan; Mannosan per unit sediment mass; paleofire; Polar Terrestrial Environmental Systems @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 622 data points
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Czymzik, Markus; Muscheler, Raimund; Brauer, Achim; Adolphi, Florian; Ott, Florian; Kienel, Ulrike; Dräger, Nadine; Słowiński, Michał; Aldahan, Ala; Possnert, Göran (2015): Solar cycles and depositional processes in annual 10Be from two varved lake sediment records. Earth and Planetary Science Letters, 428, 44-51, https://doi.org/10.1016/j.epsl.2015.07.037
    Publication Date: 2024-04-05
    Description: Beryllium 10 concentrations (10Becon) were measured at annual resolution from varved sediment cores of Lakes Tiefer See (TSK) and Czechowskie (JC) for the period 1983-2009 (~solar cycles 22 and 23). Calibrating the 10Becon time-series against complementing proxy records from the same archive as well as local precipitation and neutron monitor data, reflecting solar forced changes in atmospheric radionuclide production, allowed (i) identifying the main depositional processes and (ii) evaluating the potential for solar activity reconstruction. 10Becon in TSK and JC sediments are significantly correlated to varying neutron monitor counts (TSK: r=0.5, p=0.05, n=16; JC: r=0.46, p=0.03, n=22). However, the further correlations with changes in organic carbon contents in TSK as well as varying organic carbon and detrital matter contents in JC point to catchment specific biases in the 10Becon time-series. In an attempt to correct for these biases multiple regression analysis was applied to extract an atmospheric 10Be production signal (10Be atmosphere). To increase the signal to noise ratio a 10Be composite record (10Be composite) was calculated from the TSK and JC 10Be atmosphere time-series. 10Becomposite is significantly correlated to variations in the neutron monitor record (r=0.49, p=0.01, n=27) and matches the expected amplitude changes in 10Be production between solar cycle minima and maxima. This calibration study on 10Be from two sites indicates the large potential but also, partly site-specific, limitations of 10Be in varved lake sediments for solar activity reconstruction.
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Czymzik, Markus; Muscheler, Raimund; Adolphi, Florian; Mekhaldi, Florian; Dräger, Nadine; Ott, Florian; Słowiński, Michał; Blaskiewicz, Mirsolaw; Aldahan, Ala; Possnert, Göran; Brauer, Achim (2018): Synchronizing 10Be in two varved lake sediment records to IntCal13 14C during three grand solar minima. Climate of the Past, 14, 687-696, https://doi.org/10.5194/cp-14-687-2018
    Publication Date: 2024-04-05
    Description: Time-scale uncertainties between paleoclimate reconstructions often inhibit studying the exact timing, spatial expression and driving mechanisms of climate variations. Detecting and aligning the globally common cosmogenic radionuclide production signal via a curve fitting method provides a tool for the quasi-continuous synchronization of paleoclimate archives. In this study, we apply this approach to synchronize 10Be records from varved sediments of Lakes Tiefer See and Czechowskie covering the Maunder-, Homeric- and 5500 a BP grand solar minima with 14C production rates inferred from the IntCal13 calibration curve. Our analyses indicate best fits with 14C production rates when the 10Be records from Lake Tiefer See were shifted for 8 (-12/+4) (Maunder Minimum), 31 (-16/+12) (Homeric Minimum) and 86 (-22/+18) years (5500 a BP grand solar minimum) towards the past. The best fit between the Lake Czechowskie 10Be record for the 5500 a BP grand solar minimum and 14C production was obtained when the 10Be time-series was shifted 29 (-8/+7) years towards present. No significant fits were detected between the Lake Czechowskie 10Be records for the Maunder- and Homeric Minima and 14C production, likely due intensified in-lake sediment resuspension since about 2800 a BP, transporting 'old' 10Be to the coring location. Our results provide a proof of concept for facilitating 10Be in varved lake sediments as novel synchronization tool required for investigating leads and lags of proxy responses to climate variability. However, they also point to some limitations of 10Be in these archives mainly connected to in-lake sediment resuspension processes.
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 9
    Publication Date: 2024-04-05
    Keywords: Age; Beryllium-10; Lake_Czechowskie; Poland
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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  • 10
    Publication Date: 2024-04-05
    Keywords: Age; Beryllium-10; COMPCORE; Composite Core; Mecklenburg-West Pomerania, Germany; Tiefer-See
    Type: Dataset
    Format: text/tab-separated-values, 34 data points
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