Umeå universitets logga

• Elevated atmospheric input of nitrogen (N) is currently affecting plant biodiversity and ecosystem functioning. The growth and survival of numerous plant species is known to respond strongly to N fertilisation. Yet, few studies have assessed the effects of N deposition on seed quality and reproductive performance, which is an important life-history stage of plants.
• Here we address this knowledge gap by assessing the effects of atmospheric N deposition on seed quality of the ancient forest herb Anemone nemorosa using two complementary approaches.
• By taking advantage of the wide spatiotemporal variation in N deposition rates in pan-European temperate and boreal forests over 2years, we detected positive effects of N deposition on the N concentration (percentage N per unit seed mass, increased from 2.8% to 4.1%) and N content (total N mass per seed more than doubled) of A.nemorosa seeds. In a complementary experiment, we applied ammonium nitrate to aboveground plant tissues and the soil surface to determine whether dissolved N sources in precipitation could be incorporated into seeds. Although the addition of N to leaves and the soil surface had no effect, a concentrated N solution applied to petals during anthesis resulted in increased seed mass, seed N concentration and N content.
• Our results demonstrate that N deposition on the petals enhances bioaccumulation of N in the seeds of A.nemorosa. Enhanced atmospheric inputs of N can thus not only affect growth and population dynamics via root or canopy uptake, but can also influence seed quality and reproduction via intake through the inflorescences.

• Metacaspases are a subgroup of caspase homologues represented in bacteria, algae and plants. Although type I and type II metacaspases are present in plants, recently discovered and uncharacterized type III metacaspases can only be found in algae which have undergone secondary endosymbiosis.
• We analysed the expression levels of all 13 caspase homologues in the cryptophyte Guillardia theta invivo and biochemically characterized its only type III metacaspase, GtMC2, invitro.
• Type III metacaspase GtMC2 was shown to be an endopeptidase with a preference for basic amino acids in the P1 position, which exhibited specific N-terminal proteolytic cleavage for full catalytic efficiency. Autolytic processing, as well as the activity of the mature enzyme, required the presence of calcium ions in low millimolar concentrations. In GtMC2, two calcium-binding sites were identified, one with a dissociation constant at low and the other at high micromolar concentrations.
• We show high functional relatedness of type III metacaspases to type I metacaspases. Moreover, our data suggest that the low-affinity calcium-binding site is located in the p10 domain, which contains a well-conserved N-terminal region. This region can only be found in type I/II/III metacaspases, but is absent in calcium-independent caspase homologues.

Root phenology is important in controlling carbon and nutrient fluxes in terrestrial ecosystems, yet, remains largely unexplored, especially in the Arctic. We compared below- and aboveground phenology and ending of the growing season in two contrasting vegetation types of subarctic tundra: heath and meadow, and their response to experimental warming in autumn. 

Root phenology was measured in-situ with minirhizotrons and compared with aboveground phenology assessed with repeat digital photography. 

The end of the growing season, both below- and aboveground, was similar in meadow and heath and the belowground growing season ended later than aboveground in the two vegetation types. Root growth was higher and less equally distributed over time in meadow compared to heath. The warming treatment increased air and soil temperature by 0.5 A degrees C and slightly increased aboveground greenness, but did not affect root growth or prolong the below- and aboveground growing season in either of the vegetation types. 

These results imply that vegetation types differ in root dynamics and suggest that other factors than temperature control autumnal root growth in these ecosystems. Further investigations of root phenology will help to identify those drivers, in which including responses of functionally contrasting vegetation types will help to estimate how climate change affects belowground processes and their roles in ecosystem function.