| _version_ | 1867168587513331712 |
|---|---|
| author | Litt, Thomas Stebich, Martina |
| author_facet | Litt, Thomas Stebich, Martina |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_59877 |
| institution | PANGAEA |
| language | en |
| publishDate | 2001 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Pollen counts of sediment core MFM6 Litt, Thomas Stebich, Martina 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 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. |
| title | Pollen counts of sediment core MFM6 |
| topic | 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 |
| url | https://doi.org/10.1594/PANGAEA.59877 |