Regional climate change from peat stratigraphy for the mid- to late Holocene in central Ireland
At the millennial scale bog surface wetness (BSW) records show a clear Holocene climate event stratigraphy, with major phases comparable with other regional climate proxies such as chironomid inferred temperature records. Moving towards the centennial scale, however, and towards the limits of chrono...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
2012-08.
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| Subjects: | |
| Online Access: | Get fulltext |