geosciences Article A Dual Stable Isotope Approach Unravels Common Climate Signals and Species-Specific Responses to Environmental Change Stored in Multi-Century Tree-Ring Series from the Tibetan Plateau Jussi Grießinger 1,*, Achim Bräuning 1, Gerhard Helle 2, Gerhard Hans Schleser 3, Philipp Hochreuther 1 , Wolfgang Jens-Henrik Meier 1 and Haifeng Zhu 4 1 Institute of Geography, Friedrich-Alexander-University Erlangen-Nürnberg, 91058 Erlangen, Germany;
[email protected] (A.B.);
[email protected] (P.H.);
[email protected] (W.J.-H.M.) 2 GFZ German Research Centre for Geoscience, Section 5.2 Climate Dynamics and Landscape Evolution, 14473 Potsdam, Germany;
[email protected] 3 FZJ Research Centre Jülich, Institute of Bio- and Geosciences IBG-3, 52428 Jülich, Germany;
[email protected] 4 Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100864, China;
[email protected] * Correspondence:
[email protected]; Tel.: +49-9131-85-22009 Received: 13 February 2019; Accepted: 23 March 2019; Published: 29 March 2019 Abstract: Tree-rings are recorders of environmental signals and are therefore often used to reconstruct past environmental conditions. In this paper, we present four annually resolved, multi-centennial tree-ring isotope series from the southeastern Tibetan plateau. The investigation site, where juniper and spruce trees jointly occur, is one of the highest known tree-stands in the world. Tree ring cellulose oxygen (δ18O) and carbon (δ13C) isotopes were analyzed for a common period of 1685–2007 AD to investigate climate–isotope relationships. Therefore, various climate parameters from a local meteorological station and from the CRU 4.02 dataset were used.