Stable carbon isotope data that span part of the last glacial-interglacial transition (ca. 14-9 ka 14 C BP; ca. 15-11 ka cal. BP), and which derive from organ-specific plant macrofossils recovered from two lake sediment profiles in the UK and one in Norway, are compared. The recorded temporal variat
Climate oscillations and tephrochronology in eastern middle Sweden during the last glacial–interglacial transition
✍ Scribed by Jonas Björck; Stefan Wastegård
- Publisher
- John Wiley and Sons
- Year
- 1999
- Tongue
- English
- Weight
- 342 KB
- Volume
- 14
- Category
- Article
- ISSN
- 0267-8179
No coin nor oath required. For personal study only.
✦ Synopsis
Two sequences spanning the last glacial-interglacial transition in southern O ¨stergo ¨tland, eastern middle Sweden have been investigated for high-resolution vegetation change and tephrochronology. Organic carbon and pollen analysis indicates that the Younger Dryas-Preboreal climatic transition was characterised by at least one well-defined oscillation or possibly two shorter climatic oscillations. The Vedde Ash (ca. 12 000 GRIP yr BP or ca. 10 300 14 C yr BP) has been identified at both sites, significantly increasing the known distribution of this marker horizon. In addition, a previously unrecorded rhyolitic tephra of Icelandic origin has been identified at ca. 9000 14 C yr BP. The expansion of Corylus into southern O ¨stergo ¨tland is estimated to be ca. 9400 14 C yr BP.
📜 SIMILAR VOLUMES