RESPONSE OF LATE CARBONIFEROUS AND EARLY PERMIAN PLANT COMMUNITIES TO CLIMATE CHANGE
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | DiMichele W.A. | |
dc.contributor.author | Pfefferkorn H.W. | |
dc.contributor.author | Gastaldo R.A. | |
dc.date.accessioned | 2021-03-03T03:56:30Z | |
dc.date.available | 2021-03-03T03:56:30Z | |
dc.date.issued | 2001 | |
dc.identifier | https://elibrary.ru/item.asp?id=13685703 | |
dc.identifier.citation | Annual Review of Earth and Planetary Sciences, 2001, 29, С. 4, 461-487 | |
dc.identifier.issn | 0084-6597 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/26183 | |
dc.description.abstract | Late Carboniferous and Early Permian strata record the transition from a cold interval in Earth history, characterized by the repeated periods of glaciation and deglaciation of the southern pole, to a warm-climate interval. Consequently, this time period is the best available analogue to the Recent in which to study patterns of vegetational response, both to glacial-interglacial oscillation and to the appearance of warm climate. Carboniferous wetland ecosystems were dominated by spore-producing plants and early gymnospermous seed plants. Global climate changes, largely drying, forced vegetational changes, resulting in a change to a seed plant-dominated world, beginning first at high latitudes during the Carboniferous, reaching the tropics near the Permo-Carboniferous boundary. For most of this time plant assemblages were very conservative in their composition. Change in the dominant vegetation was generally a rapid process, which suggests that environmental thresholds were crossed, and involved little mixing of elements from the wet and dry floras. | |
dc.subject | Permian | |
dc.subject | Carboniferous | |
dc.subject | ecosystem stability | |
dc.subject | glaciation | |
dc.subject | biome | |
dc.subject | coal | |
dc.subject | extinction | |
dc.title | RESPONSE OF LATE CARBONIFEROUS AND EARLY PERMIAN PLANT COMMUNITIES TO CLIMATE CHANGE | |
dc.type | Статья | |
dc.subject.age | Палеозой::Пермская | ru |
dc.subject.age | Paleozoic::Permian | en |
dc.subject.age | Палеозой::Каменноугольная | ru |
dc.subject.age | Paleozoic::Carboniferous | en |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru