Introduction: The significance of paleodata in understanding global changes in climate and environment
Chapter 2. The arctic regions
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Table of Contents - Special Paper 382Cenozoic Climatic and Environmental Changes in RussiaEdited by: A. a. Velichko and V.P. Neechaev |
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| Summary | 1 | ||
Introduction: The significance of paleodata in understanding global changes in climate and environment |
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| Introduction | 1 | ||
| Paleobotanical Data | 3 | ||
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Reconstructions for the Cenozoic | 3 | |
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Paleoclimatic Reconstructions Based on Spore-Pollen Spectra | 3 | |
| Paleoclimatic Reconstructions Based on Spore-Pollen Spectra | 3 | ||
| Taxon Indicators | 3 | ||
| Paleoclimatic Reconstructions Based on Fossil Floras | 3 | ||
| Reconstruction for the Postglacial Epoch (Holocene) | 4 | ||
| Zonal-Formation Method of Paleoclimatic Reconstruction for the Holocene | 4 | ||
| Information-Statistical Method of Paleoclimatic Reconstruction of Palynological Data | 4 | ||
| Paleozoological Data | 4 | ||
| Paleoteriological Data | 4 | ||
| Paleomalacological Data | 5 | ||
| Zoogeographical Methods | 5 | ||
| Ecological Methods | 5 | ||
| Geochemical Methods | 6 | ||
| Methods of Magnesium Thermometry | 6 | ||
| Paleopedological Data | 6 | ||
| Lithological Data | 7 | ||
| Laterite (Ferralite) Regolith (Bauxites) | 7 | ||
| Kaolin Regolith | 7 | ||
| Carboniferous Formations | 7 | ||
| Red formations (Continental, Carbonate) | 7 | ||
| Silicic Weathering Crusts | 7 | ||
| Paleocryogenic Data | 7 | ||
| Large Polygonal Structures | 8 | ||
| Small Polygonal-crack Formations | 8 | ||
| Solifluctional Formations | 8 | ||
| Astructural Plastic Deformation | 8 | ||
| Paleoglaciological Data | 8 | ||
| Relief | 9 | ||
| Sediments | 9 | ||
Chapter 2. The arctic regions |
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