Climate evolution across the earth's history
সংরক্ষণ করুন:
| লেখক: | , , , |
|---|---|
| বিন্যাস: | artículo original |
| বর্তমান অবস্থা: | Versión publicada |
| প্রকাশনার তারিখ: | 2014 |
| বিবরন: | In a natural way, the atmosphere –and therefore the climate- evolved together with the continent, the ocean, the interior Earth an all the other planetary components. This co-evolution was often via catastrophes, certainly very fruitful, especially for the biological evolution and diversification. In several stages, the volcanism contributed ingredients to the atmosphere, as much more arrived with the comets and meteorites; the ocean brought water vapor to it with its successive state changes; the continental drift increased the oceanity and decreased the continentality of climates. The ocean gave also thermal inertia and so stability to the climate. The oxygen appearance favored the life, and its subsequent photochemical dissociation and recombination yielded the stratospheric ozone layer. The spontaneous fires put upper limit to the atmospheric concentration of the oxygen generated by the vegetation, making up the present atmosphere. |
| দেশ: | Portal de Revistas UCR |
| প্রতিষ্ঠান: | Universidad de Costa Rica |
| Repositorio: | Portal de Revistas UCR |
| ভাষা: | Español |
| OAI Identifier: | oai:archivo.portal.ucr.ac.cr:article/13748 |
| অনলাইন ব্যবহার করুন: | https://archivo.revistas.ucr.ac.cr/index.php/reflexiones/article/view/13748 |
| মুখ্য শব্দ: | climate biology evolution history earth clima biología evolución historia tierra |