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| Titel |
Calibration of the stable oxygen and carbon isotope signals of stone pine (Pinus cembra L.) tree rings at the Eastern Carpathian timberline |
| VerfasserIn |
Zoltán Kern, Ionel Popa, Anca Semeniuc, Gabriella Scholl-Barna, Aurel Persoiu |
| Konferenz |
EGU General Assembly 2014
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 16 (2014) |
| Datensatznummer |
250090953
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| Publikation (Nr.) |
 EGU/EGU2014-5214.pdf |
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| Zusammenfassung |
| Swiss stone pine (Pinus cembra L.) presented the greatest dendroclimatological potential in the Eastern Carpathians owing to the i) significant longevity, ii) strictly constrained ecological preference and the related pronounced temperature regulated growth and iii) well-preserved snag and subfossil findings. Dendroisotope signals, however, were not tested for the species. Increment cores were extracted from three individuals at a timberline site located in the Calimani Mts, Romania. Annual rings were cut with a scalpel under a binocular microscope from each core and each year. Annual increments were treated separately (i.e. non-pooled) to monitor between tree variability and estimate real uncertainty. Extracted α-cellulose was homogenized by ultrasound and converted to CO at high-temperature and the stable oxygen (18O/16O) and carbon (13C/12C) ratios were measured and expressed relative to standards in the conventional delta notation.
Both isotopes presented strong intra-tree correlation, therefore the stand average was estimated from the measurements. Carbon isotope record performed the characteristic decline throughout the recent decades; therefore this non-climatic trend was corrected before climate calibration. Mean δ18O yielded significant positive connection (r>0.5) with temperature of the summer months for the last century. Spatial signature obtained from a preliminary correlation field analysis suggests that Stone pine δ18O from the Calimani Mts will give relevant temperature record for the historical times not only for the Eastern Carpathians but also much southward directions as far as the Central Balkan.
Acknowledgement: RO-2013-0014 and LP2012-27/2012. |
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