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  • 2000-2004  (3)
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  • 1
    Publication Date: 2023-07-10
    Keywords: AGE; Biozone; Bispingen; Core; CORE; Covariance; DEPTH, sediment/rock; Duration; Germany, Lower Saxony; Sample code/label; Sigma; Temperature, coldest month; Temperature, warmest month
    Type: Dataset
    Format: text/tab-separated-values, 960 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-07-10
    Keywords: AGE; Biozone; Covariance; Depth, reference; DEPTH, sediment/rock; Duration; Groebern; Sample code/label; Sigma; Temperature, coldest month; Temperature, warmest month
    Type: Dataset
    Format: text/tab-separated-values, 544 data points
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Litt, Thomas; Stebich, Martina (1999): Bio- and chronostratigraphy of the Lateglacial in the Eifel region, Germany. Quaternary International, 61(1), 5-16, https://doi.org/10.1016/S1040-6182(99)00013-0
    Publication Date: 2023-12-16
    Description: In recent years enormous success has been achieved in varve counting of the Eifel maar lakes, but a detailed correlation with the biostratigraphy has been missing. In this paper, we present new palynological results of the Lateglacial sequences from Holzmaar Lake and Meerfelder Maar Lake based on annually laminated sediments. In particular, the Meerfelder Maar has great potential, because, in contrast to the Holzmaar, the sequence between the Ulmener Maar Tephra (11 000 varve years BP) and the Laacher See Tephra (12 880 varve years BP) including the Younger Dryas is undisturbed and complete. Therefore, we currently use the Meerfelder Maar chronology (Brauer et al., 1999b) as an independent varve calendar for the biostratigraphy of the Lateglacial. The palynological signals of both maar lakes are in good agreement and can easily be correlated with one another and with type sections/type regions in northwestern Germany and Jutland. The sequences of the Eifel maar lakes have the quality of hypostratotypes with regional biozones based on an absolute time scale.
    Keywords: Abies; AGE; Alnus; Armeria maritima; Artemisia; Asteroideae; Betula; Botrychium; Calluna; Campanula; Carpinus; Caryophyllaceae; Centaurea scabiosa; cf. Centaurea cyanus; cf. Parnassia; Changes in the Geo-Biosphere during the last 15000 years; Chenopodiaceae; Cichorioideae; Corylus; Counting, palynology; Cruciferea; Cyperaceae; DEPTH, sediment/rock; Ephedra distachya-type; Epilobium; Equisetum; Fagus; Filicopsida, monolete indeterminata; Filipendula; Galium-type; Gentianaceae; GeoBio15k; Geranium; Germany; Gramineae; Gypsophila-type; Helianthemum; Hippophae rhamnoides; Hypericum-type; Juniperus; Labiatae; Leguminosae; Liliaceae; Linum catharticum; Littorella; Meerfelder Maar; Mentha-type; Menyanthes; MFM6; Myriophyllum spicatum/verticillatum; Pediastrum; Picea; Pinus; Plantago; Plantago lanceolata; Plantago major/media; Polemonium; Pollen and spores; Polygonum amphibium; Polygonum bistorta; Populus; Potamogeton; Potentilla; Primulaceae; Quercus; Ranunculaceae; Ranunculus subgen. Batrachium-type; Rhamnus catharticus; Ribes-type; Rosaceae; Rumex; Salix; Sanguisorba minor; Sanguisorba officinalis; Saxifraga cf. stellaris; Scrophulariaceae; Selaginella selaginoides; Sphagnum; Succisa; Symphytum; Thalictrum; Tilia; Typha angustifolia/Sparganium; Typha latifolia; Ulmus; Umbelliferae; UPC; Urtica dioica-type; Usinger Piston Corer; Vaccinium-type; Valeriana officinalis; Varia
    Type: Dataset
    Format: text/tab-separated-values, 17794 data points
    Location Call Number Limitation Availability
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