Comparison of δ¹³C and δ¹⁸O from cellulose, whole wood, and resin-free whole wood from an old high elevation Pinus uncinata in the Spanish central PyreneesFootnote^*
* The topic of this manuscript was presented as part of an oral presentation on the Annual Meeting of the German Association for Stable Isotope Research (GASIR), 28–30 September 2015, Heidelberg, Germany.

Dana F. C. RiechelmannInstitute of Geography, Johannes Gutenberg-University Mainz, Mainz, Germany;Institute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, GermanyCorrespondence[email protected]

Michael MausInstitute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, Germany

Willi DindorfInstitute of Organic Chemistry, Johannes Gutenberg-University Mainz, Mainz, Germany

Oliver KonterInstitute of Geography, Johannes Gutenberg-University Mainz, Mainz, Germany

Bernd R. SchöneInstitute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, Germany

Jan EsperInstitute of Geography, Johannes Gutenberg-University Mainz, Mainz, Germany

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