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Oxygen dynamics and plant-sediment interactions in isoetid ...

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Thesis summaryFig. 4. Chlorophyll content (a) <strong>and</strong> maximum netphotosynthesis (b) of Lobelia leaves after <strong>in</strong>creas<strong>in</strong>gaddition of labile organic matter (% of <strong>sediment</strong> DW).S<strong>in</strong>gle measurements were made after 18 d (○) <strong>and</strong> 59 d(●) <strong>and</strong> triplicate measurements (± SD) after 194 d (□) ofexperiments <strong>in</strong> the laboratory.The long anoxic periods <strong>in</strong> <strong>plant</strong>s dur<strong>in</strong>gthe night is the most plausible reason for theobserved <strong>plant</strong> stress s<strong>in</strong>ce low yield<strong>in</strong>ganaerobic respiration can deplete Lobelia ofcarbon result<strong>in</strong>g <strong>in</strong> <strong>in</strong>sufficient carbon supply toroots. This will cause root malfunction <strong>and</strong>osmotic stress constra<strong>in</strong><strong>in</strong>g transfer of nutrientsto leaves. However, Lobelia can cope withanoxia which is a recurr<strong>in</strong>g phenomenon <strong>in</strong>natural populations dur<strong>in</strong>g the summer.Paper 3 addresses differences <strong>in</strong> <strong>plant</strong>morphology <strong>and</strong> response to organic addition ofLobelia <strong>and</strong> Littorella. Measurements from turfexperiments <strong>in</strong> the laboratory <strong>and</strong> <strong>in</strong>-situexperiments with mixed populations were usedto evaluate effects of enrichment. O 2 loss fromleaf surfaces of both species to hypoxic waterwas used to <strong>in</strong>vestigate leaf gas permeability.Addition of organic matter dramaticallydecreased photosynthetic rates of Lobelia whileLittorella was able to cope with additions <strong>in</strong>laboratory experiments. This is partly expla<strong>in</strong>edby higher <strong>plant</strong> density <strong>in</strong> Littorella turfs, butmarked differences were observed between O 2<strong>dynamics</strong> <strong>in</strong> Lobelia <strong>and</strong> Littorella where O 2concentration <strong>in</strong> leaves was unaffected <strong>in</strong>Littorella regardless of O 2 availability <strong>in</strong><strong>sediment</strong>s while Lobelia faced long anoxicperiods dur<strong>in</strong>g nighttime. Littorella was able toma<strong>in</strong>ta<strong>in</strong> nutrient levels <strong>and</strong> chlorophyll content<strong>in</strong> leaves at higher organic additions thanLobelia. The observed difference <strong>in</strong> O 2<strong>dynamics</strong> is the result of 13-16 times higher gaspermeability of Littorella leaves compared toLobelia (Table 1).In-situ measurements confirmed thatLobelia was more subjected to stress thanLittorella when mixed populations weresubjected to organic enrichments, hence,experienc<strong>in</strong>g exactly the same conditions s<strong>in</strong>cethe higher oxygenation capacity of Littorellaalso benefits Lobelia <strong>in</strong> mixed populations. Inthis experiment Littorella was more stressedthan <strong>in</strong> the laboratory experiments. The higherresponse of both species over the much shorterexperiment (90 days) could be due to highertemperatures (Mean 20.6 o C, maximum 35 o C) <strong>in</strong>the <strong>in</strong>-situ experiment, then the laboratoryTable 1. O 2 flux across leaf surface to hypoxic water withbasal leaf lacunae <strong>in</strong> air contact <strong>and</strong> evaporation to drystill air of Lobelia dortmanna <strong>and</strong> Littorella uniflora.SpeciesTemperature( o C)Flux(n mol O 2 m -2 s -1 )Lobelia 5 30 ± 7 a15 48 ± 3 aLittorella 5 482 ± 199 b15 608 ± 144 bValues are means ± SD of 3 (O 2 flux) or 10 (Evaporation)replicates. Different letters show significant differences(2-way or 1-way ANOVA).21

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