Oligocene to Pliocene palaeoclimate reconstructions from 18 sites in Hungary
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2007
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| _version_ | 1867171355796963328 |
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| author | Erdei, Boglarka Hably, Lilla Kazmer, Miklos Utescher, Torsten Bruch, Angela A |
| author_facet | Erdei, Boglarka Hably, Lilla Kazmer, Miklos Utescher, Torsten Bruch, Angela A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | A survey of the Neogene flora and vegetation pattern of the Pannonian domain based on 18 selected fossil plant assemblages is given. Flora and vegetation patterns are based on well-documented and studied fossil plant assemblages (macrofloras, primarily leaves). A general but slow cooling trend is definitely observable after the Early Miocene as reflected by both quantitative climate reconstructions and floristic change, i.e. decrease of diversity, slow disappearance of thermophilous and exotic elements, as well as decrease in the variety of vegetation types. A significant decline of coldest month temperatures (as compared to warmest month temperatures) must have played a defining role in forming flora and vegetation through the Neogene. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_587448 |
| institution | PANGAEA |
| language | en |
| publishDate | 2007 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Oligocene to Pliocene palaeoclimate reconstructions from 18 sites in Hungary Erdei, Boglarka Hably, Lilla Kazmer, Miklos Utescher, Torsten Bruch, Angela A Andornaktalya; Budapest_city; Eger-Kiseged; Eger-Wind; Erdobenye-Barnamaj; Erdobenye-Kovago-oldal; Erdobenye-Ligetmajor; Felsotarkany; Gerce; Hungary; Hungary, Baranya; Hungary, Borsod-Abauj-Zemplen; Hungary, Budapest; Hungary, Fejer; Hungary, Heves; Hungary, Pest; Hungary, Vas; Hungary, Veszprem; Ipolytarnoc; Kesztolc; Magyaregregy; Nagybatony-Ujlak; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Nogradszakal; OUTCROP; Outcrop sample; Pomaz; Pula; QU; Quarry; Tallya; Vertesszolos A survey of the Neogene flora and vegetation pattern of the Pannonian domain based on 18 selected fossil plant assemblages is given. Flora and vegetation patterns are based on well-documented and studied fossil plant assemblages (macrofloras, primarily leaves). A general but slow cooling trend is definitely observable after the Early Miocene as reflected by both quantitative climate reconstructions and floristic change, i.e. decrease of diversity, slow disappearance of thermophilous and exotic elements, as well as decrease in the variety of vegetation types. A significant decline of coldest month temperatures (as compared to warmest month temperatures) must have played a defining role in forming flora and vegetation through the Neogene. |
| title | Oligocene to Pliocene palaeoclimate reconstructions from 18 sites in Hungary |
| topic | Andornaktalya; Budapest_city; Eger-Kiseged; Eger-Wind; Erdobenye-Barnamaj; Erdobenye-Kovago-oldal; Erdobenye-Ligetmajor; Felsotarkany; Gerce; Hungary; Hungary, Baranya; Hungary, Borsod-Abauj-Zemplen; Hungary, Budapest; Hungary, Fejer; Hungary, Heves; Hungary, Pest; Hungary, Vas; Hungary, Veszprem; Ipolytarnoc; Kesztolc; Magyaregregy; Nagybatony-Ujlak; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Nogradszakal; OUTCROP; Outcrop sample; Pomaz; Pula; QU; Quarry; Tallya; Vertesszolos |
| url | https://doi.org/10.1594/PANGAEA.587448 |