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New Evidence of High Ocean Temperatures, Greatly Increased Hydrological Cycle At/After Permian Triassic Extinction
Source info:
| Author: | Will Baird |
|---|---|
| Date: | 2013-08-21 18:00:00 |
| Blog: | The Dragon’s Tales  |
| URL: | http://thedragonstales.blogspot.com/2013/08/new-evidence-of-high-ocean-temperatures.html |
Summary:
Palaeotethys seawater temperature rise and an intensified hydrological cycle following the end-Permian mass extinction Authors: 1. Martin Schobben (a) 2. Michael M. Joachimski (b) 3. Dieter Korn (a) 4. Lucyna Leda (a) 5. Christoph Korte (c) Affiliations: a. Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstr 43, D-10115 Berlin,Content analysis:
Stratigraphic context:
| Recognized stratigraphic terms [n]: | Triassic [1] Permian [2] |
|---|---|
| Agenames chronostratigraphy [rating]: | Triassic [0.1] Permian [0.33] Mesozoic [0.1] Paleozoic [0.33] Phanerozoic [0.61] |
Geographic context:
| Location | Country | Latitude | Longitude |
|---|---|---|---|
| 10115 | DE | 52.532 | 13.3838 |
Keywords:
Affiliations, At/After, Christoph Korte, D-10115 Berlin, Dieter Korn, end-Permian mass extinction, High Ocean Temperatures Greatly Increased Hydrological, hydrological cycle, intensified hydrological cycle, Leibniz-Institut für Evolutions, Lucyna Leda, Martin Schobben, mass extinction, Michael M. Joachimski, Museum für Naturkunde, New Evidence, Palaeotethys, Permian Triassic Extinction, Permian Triassic Mass Extinction, seawater temperature rise, und Biodiversitätsforschung
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