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25th International Meeting on Organic Geochemistry IMOG 2011

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P-249<br />

Habitat adaptati<strong>on</strong> by compositi<strong>on</strong>al changes of cuticular needle<br />

waxes for the Norway Spruce (Observati<strong>on</strong> Platform Eifel<br />

Nati<strong>on</strong>al Parc)<br />

Gina Kuippers 1 , Ulrich Mann 2 , Jan Schwarzbauer 1<br />

1 RWTH Aachen University, Lehrstuhl für Geologie, Geochemie und Lagerstätten des Erdöls und der Kohle,<br />

Aachen, Germany,<br />

2 Forschungszentrum Jülich, Institut für Bio- und Geowissenschaften, Jülich, Germany,<br />

(corresp<strong>on</strong>ding author: ginakuippers@web.de)<br />

The organic-geochemical compositi<strong>on</strong> of cuticular<br />

needle waxes of the Norway spruce from the Eifel<br />

Nati<strong>on</strong>al Parc was investigated by semi-quantitative<br />

GC/MS analyses. Needles of different ages (recent<br />

vs. older generati<strong>on</strong>s) and from different altitude (364<br />

m vs. 603 m) were compared to each other.<br />

Aliquot samples were subjected to a combined<br />

polarity/affinity gas chromatographic separati<strong>on</strong> into<br />

functi<strong>on</strong>alized m<strong>on</strong>oaromatics, fatty acids, fatty acid<br />

methyl esters, n-alkanes as well as terpenoids.<br />

Relative c<strong>on</strong>centrati<strong>on</strong>s of the dominant compound<br />

groups of the needle waxes were represented by<br />

m<strong>on</strong>oterpenes, sesquiterpenes and fatty acids (Fig.<br />

1). According to the age of the cuticular waxes, a<br />

decrease of sesquiterpenes besides an increase of<br />

m<strong>on</strong>oterpenes was observed. By far the most<br />

important representatives of the m<strong>on</strong>oterpenes were<br />

β-phellandrene and camphene, whereas the group of<br />

sesquiterpenes was dominated by δ- and γcadinenes.<br />

The c<strong>on</strong>centrati<strong>on</strong> of fatty acids increased<br />

with sea level. Palmitic acid was particularly prevalent<br />

in the cuticulae of the spruces at high sea level, while<br />

dehydroabietic acid and arachidic acid features were<br />

more prominent at the lower sea level.<br />

Although n-alkanes did not represent a dominant<br />

fracti<strong>on</strong> of the spruce cuticulae, their most prominent<br />

chain length increased with sea level (Fig. 2). In total,<br />

the chain length of the carb<strong>on</strong> atoms ranged from n-<br />

C21 to n-C33 alkanes. Whereas at the lower site the n-<br />

C27 alkane predominates, at the higher locati<strong>on</strong> the n-<br />

C29-alkane clearly represents the dominating chain<br />

length.<br />

Based <strong>on</strong> the amount of samples, present results<br />

can be regarded as a random inspecti<strong>on</strong> <strong>on</strong>ly.<br />

Nevertheless, especially the compositi<strong>on</strong>al<br />

differences of the cuticular waxes were surprisingly<br />

high related to a relative low sea level difference of<br />

239 m between the two sample sets. On the other<br />

side, these results may indicate the high potential of<br />

the Norway spruce for habitat adaptati<strong>on</strong>s during<br />

climate changes.<br />

Acknowledgement<br />

This study was c<strong>on</strong>ducted as part of project TERENO.<br />

Fig. 1: Relative amounts of compound groups for site<br />

Wüstebach (samples 1a-c, 603 m) and site<br />

Wilderness Trail (samples 2a-b, 364 m).<br />

Fig. 2: Relative c<strong>on</strong>tents of n-alkanes. Numbers<br />

marking the peak of each distributi<strong>on</strong>.<br />

385

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