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Arctic plant ecology: From tundra to polar desert in Svalbard - Unis

Arctic plant ecology: From tundra to polar desert in Svalbard - Unis

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The percentage area of different substrate types of <strong>Svalbard</strong> was estimated by means<br />

of the prelim<strong>in</strong>ary substrate map of <strong>Svalbard</strong> (Arnesen, personal communication)<br />

us<strong>in</strong>g GIPM Version 2.2.1.1. The pixels of each substrate category were counted and<br />

expressed as percentage area <strong>in</strong> relation <strong>to</strong> the pixel sum of entire <strong>Svalbard</strong>. The<br />

dom<strong>in</strong>ant substrate type is weakly acidic and covers 14.1% of entire <strong>Svalbard</strong>. Acidic<br />

substrates cover 6.1%, followed by the alkal<strong>in</strong>e circumneutral type with 5.4%. The<br />

rema<strong>in</strong><strong>in</strong>g substrate consists of sediments (3.6%), sal<strong>in</strong>e steppe substrate (0.1%) and<br />

undef<strong>in</strong>ed substrate (0.2%). <strong>Svalbard</strong> is dom<strong>in</strong>ated by glaciers occupy<strong>in</strong>g 67.5% of<br />

the surface area.<br />

Meteorological data<br />

Data from the meteorological station at <strong>Svalbard</strong> Airport (MET 2007) were used <strong>to</strong><br />

calculate the <strong>in</strong>crease <strong>in</strong> mean summer temperatures for the last ten years (1997­<br />

2007). Figure 2 shows a simplified model of the temperature data us<strong>in</strong>g a l<strong>in</strong>ear<br />

regression. In the period 1997­2007 mean summer temperatures <strong>in</strong>creased with a rate<br />

of 0.16 K per year. As a comparison the mean summer temperature of the last normal<br />

period (1961­1990) is <strong>in</strong>cluded <strong>in</strong> the diagram.<br />

Degrees Celsius<br />

7<br />

6<br />

5<br />

4<br />

3<br />

2<br />

1<br />

0<br />

1997<br />

1998<br />

Mean summer temperature at <strong>Svalbard</strong> Airport<br />

1999<br />

2000<br />

2001<br />

2002<br />

2003<br />

2004<br />

37<br />

2005<br />

2006<br />

2007<br />

Mean temperatures<br />

Regression model<br />

Mean summer temperature<br />

1961­1990<br />

Figure 2. Mean summer (June, July and august) temperature at <strong>Svalbard</strong> airport (R 2 = 0.52).<br />

Study species<br />

The annual thermophilic Euphrasia wettste<strong>in</strong>ii G.Gusarova belongs <strong>to</strong> the family<br />

Scrophulariaceae. The species was earlier treated as E. frigida Pugsley (PAF 2007).<br />

Euphrasia wettste<strong>in</strong>ii is a root hemiparasite, but it is still unclear which hosts the<br />

<strong>Svalbard</strong>­populations are parasitis<strong>in</strong>g (Alsos et al. 2004). Some hemiparasites are<br />

reported with only one host. However, E. wettste<strong>in</strong>ii is found physically connected <strong>to</strong><br />

a variety of hosts or it may grow unconnected <strong>to</strong> a host (Seel & Press 1993).<br />

Euphrasia wettste<strong>in</strong>ii is ma<strong>in</strong>ly self­poll<strong>in</strong>at<strong>in</strong>g. The <strong>plant</strong>s are found <strong>in</strong> closed <strong>plant</strong><br />

communites, therefore open<strong>in</strong>gs <strong>in</strong> the cover are needed <strong>to</strong> expose the soil and provide<br />

a seed bed. Some disturbance which causes small open patches <strong>in</strong> the growth sites is<br />

needed for establishment of the seeds (Molau 1993, Seel & Press 1993). Reproduc<strong>in</strong>g<br />

by seeds may be of advantage <strong>to</strong> survive unfavourable w<strong>in</strong>ter times, but a long series

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