Holocene changes in vegetation and climate at the Khatanga region, northern Siberia - derived from a lacustrine pollen record -
The northern Siberian treeline is supposed to migrate further north, due to climatic changes in the Tundra-taiga ecosystem. But inhibiting or strengthening factors are still not adequately known, thus the changes of the treeline ecosystem are still not totally predictable.
| Main Authors: | , , |
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| Format: | Conference Object |
| Language: | unknown |
| Published: |
2013
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| Subjects: | |
| Online Access: | https://epic.awi.de/id/eprint/37657/ https://epic.awi.de/id/eprint/37657/1/AK_Permafrost.pdf https://hdl.handle.net/10013/epic.45281 https://hdl.handle.net/10013/epic.45281.d001 |
| Summary: | The northern Siberian treeline is supposed to migrate further north, due to climatic changes in the Tundra-taiga ecosystem. But inhibiting or strengthening factors are still not adequately known, thus the changes of the treeline ecosystem are still not totally predictable. |
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