IntroductionIn <strong>sediment</strong>s of high O 2 dem<strong>and</strong> <strong>isoetid</strong>sroots are restricted to the uppermost <strong>sediment</strong>layer where O 2 supply to root tips is possible(S<strong>and</strong>-Jensen et al. 2005; Raun et al. 2010).Short roots offer low anchorage <strong>and</strong> is furtherweakened <strong>in</strong> organic <strong>sediment</strong>s by low density<strong>in</strong>creas<strong>in</strong>g the risk of uproot<strong>in</strong>g <strong>and</strong> loss ofpopulations (Pulido et al. 2010). Furthermore,anoxia <strong>in</strong> roots of <strong>isoetid</strong>s leads to reducedtranslocation of nutrients with decreasedphotosynthesis <strong>and</strong> low tissue content ofnutrients as a result (Sorrell 2004; Møller &S<strong>and</strong>-Jensen 2011). To promote the return of<strong>isoetid</strong>s to their former growth sites improvedunderst<strong>and</strong><strong>in</strong>g of how <strong>isoetid</strong>s respond <strong>and</strong> copewith changes <strong>in</strong> <strong>sediment</strong> biogeochemistry isneeded. This was the ma<strong>in</strong> aim of this thesis.ReferencesArmstrong W. 1979. Aeration <strong>in</strong> higher <strong>plant</strong>s. Advances<strong>in</strong> Botanical Research 7: 225–332.Arts GHP. 2002. Deterioration of Atlantic soft watermacrophyte communities by acidification, eutrophication<strong>and</strong> alkal<strong>in</strong>isation. Aquatic Botany 73: 373-393.Beck-Nielsen D, Madsen TV. 2001. Occurrence ofViscicular-arbuscular mycorrhiza <strong>in</strong> <strong>plant</strong>s from lakes <strong>and</strong>streams. Aquatic Botany 71: 141-148Christensen PB, Sørensen J. 1986. 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