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Climate reconstruction from pollen and δ 13C records using inverse vegetation modeling – Implication for past and future climates

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Academic year: 2021

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Figure

Fig. 1. Climatic and isotopic niches for nine temperate and boreal biomes.
Fig. 2. Relationship between potential δ 13 C and precipitation or temperature for nine temperate and boreal biomes, with an enlargement for CoMxFo and TeGrl in Fig
Fig. 3. Measured δ 13 C bracketed by the potential isotopic niches of targeted biomes.
Fig. 6. Atlantic and Grande Pile Eemian paleoclimatic records. The left panel shows N

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