The full programme book (PDF) - Royal Geographical Society
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T3<br />
Spacial isotopic variations in water isotopes and dissolved inorganic carbon along<br />
the pyrenees during the beginning of spring 2013<br />
M. L. Sanchez Montes 1 *<br />
1 Department of Geography, <strong>The</strong> University of Sheffield, Sheffield<br />
Oxygen (δ 18 O), hydrogen (δ 2 H) and carbon (δ 13 C) stable isotope analyses from 72 rivers<br />
along the Pyrenees have been carried out in order to observe their spatial and temporal<br />
variability. <strong>The</strong> Pyrenees mountain range has been divided into four areas according to<br />
north, south, west and east to compare the stable isotopic values. Spatial isotopic<br />
fractionation differences along the Pyrenees can be explained by different controls. In<br />
order to do that, here we analyse and compare the isotopic data of the four different areas.<br />
Our results show that, despite their complexity, oxygen and hydrogen isotopic values were<br />
subject to spatial differences among the four areas due to differences in moisture sources<br />
of the precipitation and re-evaporation processes. In contrast, the carbon isotopic values<br />
showed a common respiration and erosion controls for the west and the north and<br />
chemical weathering controls for the south and the east. Furthermore, this study contains<br />
an isotopic data record (δ 2 H and δ 18 O and δ 13 C) to help future investigations regarding<br />
temporal changes in these stable isotopic compositions over this place. As far as it could<br />
be found, this study is the first one to characterize these stable isotopes for the entire<br />
Pyrenees range until the present time. Local isotopic data-record for Lannemezan during<br />
spring 2009 (Lambs et al, 2009) was compared with the data collected in this work in<br />
spring 2013. <strong>The</strong> isotopic changes of this area showed to have become lighter during the<br />
last 4 years. It is expected that the evolution trajectory of this mountain could be a good<br />
representation of the evolution of mountain ranges situated at higher latitudes, regarding<br />
the context of future global warming scenario (Lopez-Moreno et al. 2008).<br />
Keywords: oxygen; hydrogen; stable isotopes; dissolved inorganic carbon; rivers;<br />
Pyrenees; climate change.<br />
Lambs, L., Brunet, F. and Probst, J.L., 2009, Isotopic characteristics of the Garonne River and its<br />
tributaries, RCM 2543-2550.<br />
Lopez-Moreno, J. I., Beniston, M. And Garcia-Ruiz, J. M., 2008, Environmental change and water<br />
management in the Pyrenees: Facts and future perspectives for Mediterranean mountains, Global and<br />
Planetary Change 61, 300-312.