Miocene palaeoclimate reconstructions from the North Alpine Foreland Basin in Germany
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
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PANGAEA
2007
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| _version_ | 1867172220580659200 |
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| author | Böhme, Madelaine Bruch, Angela A Selmeier, Alfred |
| author_facet | Böhme, Madelaine Bruch, Angela A Selmeier, Alfred |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Early- and Middle-Miocene sediments of the North Alpine Foreland Basin (NAFB) in Southern Germany contain one of the world richest regional records of silicified wood. Here we analyze over 1,000 identifiable samples, belonging to 80 wood anatomical taxa from 61 stratigraphically well-dated localities using principally the Coexistence Approach. The samples investigated originate from fluvial sediments representing periods of intensified surface runoff in the NAFB and therefore represent and provide information pertaining to the wet end-member of the fluctuating climate system. The dry end of the climate system is represented in the profiles either by hiatuses or palaeosoils. The dataset is split into four xylofloras: (I) the Ortenburg xyloflora (Late Ottnangian; ~17.5 to 17.3 Ma) originating from a paratropical evergreen Carapoxylon (Xylocarpus) forest; (II) the Southern Franconian Alb xyloflora (Late Karpatian; 17.0 to ~16.3 Ma) originating from a subtropical semideciduous limestone forest; (III) the upper Older Series xyloflora (Early Badenian; ~16.3 to ~15.3 Ma) originating from a subtropical oak-laurel forest; and (IV) the upper Middle Series xyloflora (Middle Badenian; 14.3 to ~13.8 Ma) originating from a subtropical dry deciduous forest. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_587447 |
| institution | PANGAEA |
| language | en |
| publishDate | 2007 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Miocene palaeoclimate reconstructions from the North Alpine Foreland Basin in Germany Böhme, Madelaine Bruch, Angela A Selmeier, Alfred Early Badenian; Germany, Bavaria; Late Karpatian; Late Ottnangian; Middle Badenian; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; North_Alpine_Foreland_1; North_Alpine_Foreland_2; North_Alpine_Foreland_3; North_Alpine_Foreland_4 Early- and Middle-Miocene sediments of the North Alpine Foreland Basin (NAFB) in Southern Germany contain one of the world richest regional records of silicified wood. Here we analyze over 1,000 identifiable samples, belonging to 80 wood anatomical taxa from 61 stratigraphically well-dated localities using principally the Coexistence Approach. The samples investigated originate from fluvial sediments representing periods of intensified surface runoff in the NAFB and therefore represent and provide information pertaining to the wet end-member of the fluctuating climate system. The dry end of the climate system is represented in the profiles either by hiatuses or palaeosoils. The dataset is split into four xylofloras: (I) the Ortenburg xyloflora (Late Ottnangian; ~17.5 to 17.3 Ma) originating from a paratropical evergreen Carapoxylon (Xylocarpus) forest; (II) the Southern Franconian Alb xyloflora (Late Karpatian; 17.0 to ~16.3 Ma) originating from a subtropical semideciduous limestone forest; (III) the upper Older Series xyloflora (Early Badenian; ~16.3 to ~15.3 Ma) originating from a subtropical oak-laurel forest; and (IV) the upper Middle Series xyloflora (Middle Badenian; 14.3 to ~13.8 Ma) originating from a subtropical dry deciduous forest. |
| title | Miocene palaeoclimate reconstructions from the North Alpine Foreland Basin in Germany |
| topic | Early Badenian; Germany, Bavaria; Late Karpatian; Late Ottnangian; Middle Badenian; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; North_Alpine_Foreland_1; North_Alpine_Foreland_2; North_Alpine_Foreland_3; North_Alpine_Foreland_4 |
| url | https://doi.org/10.1594/PANGAEA.587447 |