Peatlands provide multiple ecosystem services, including extensive carbon sequestration and storage, yet many peatlands have been degraded or destroyed. Peatlands carbon storage capacity is connected to inherently low decomposition rates, causing the build-up of organic matter. Reasons suggested for this include waterlogged conditions that reduce the amount of available oxygen for the decomposer community, a low pH that inhibits bacterial decomposition, and colder temperatures lowering metabolic rates. This study focused on edge effects on decomposition in the transition zone between Sphagnum bogs and surrounding forest, with the expectation that decomposition is lowest in the bog and highest in the forest, but with a mix of factors causing intermediate decomposition rates near the bog edge. Transitional decomposition rates were measured across six bogs in central Sweden during the summer of 2021, using the tea bag index. Three 20 meter transects, each containing seven pairs of tea bags, were buried across the margins of each bog, centred at the edge of the Sphagnum moss. Soil moisture content, pH, and plant composition was also recorded at each burial site, and with 12 temperature loggers placed evenly among four of the bogs. The results confirmed the hypothesis regarding edge effects, and soil moisture was the dominant factor affecting the decomposition rate, having a strong significant negative correlation. The interaction of pH was significant but with an unexpected negative correlation, most likely due to the low pH in the surrounding forest. Temperature displayed no significance, and plants indicative of low decomposition rates included Vaccinium oxycoccos, Drosera rotundifolia, and especially Sphagnum species. The conclusions are that there is an edge effect on decomposition, and maintaining, or restoring, the hydrology of a peatland is the most important factor for continued carbon storage, with a rough estimation of an areas decomposition rate possible to estimate based on its vegetation. / Torvmarker bidrar med flera ekosystemtjänster, däribland utbrett koldioxidupptag och kollagring, trots detta har många torvmarker idag antingen skadats eller förstörts. Torvmarkers förmåga att lagra kol beror på en låg nedbrytningstakt, vilket gör att organiskt material ackumuleras; möjliga förklaringar som föreslagits till detta är vattensjuk mark som minskar syretillgången för nedbrytarsamhället, ett surt pH som missgynnar bakteriell nedbrytning, samt lägre temperaturer vilket sänker metabolismen generellt. Den här studien fokuserade på hur kanteffekter påverkar nedbrytningen i övergångszonen mellan vitmossemyrar och skog, med förväntningen att nedbrytningen är lägst ute i myren och högst i skogen, men att flera olika faktorer orsakar en intermediär nedbrytningshastighet i myrkanten. Nedbrytningshastigheten i 6 myrars övergångszoner, belägna i centrala Sverige, uppskattades under sommaren 2021 med hjälp av tepåseindexet (tea bag index). Tre 20 meters transekter med 7 par tepåsar vardera begravdes vid varje myr, med mitten vid kanten på vitmossan. Mätningar gjordes vid varje tepåsepar gällande markfuktighet, pH, och växtsamhälle, samt vid 4 myrar så placerades totalt 12 temperaturloggrar. Resultaten bekräftar hypotesen om kanteffekter och markfuktighet framträdde som den dominerande faktorn, med en signifikant negativ effekt på nedbrytningshastigheten. Effekten av pH var också signifikant men med en oväntad negativ korrelation, förmodligen på grund av den sura jorden i omgivande tallskog (Pinus sylvestris). Temperatur hade inte någon signifikant effekt, och växter som indikerade låg nedbrytning var Vaccinium oxycoccos, Drosera rotundifolia, samt framförallt Sphagnum spp.. Slutsatsen är att det finns en kanteffekt och att bevara, eller återskapa, hydrologin av en vitmossemyr är den viktigaste faktorn för fortsatt kolinlagring, med en grov skattning av ett områdes nedbrytningshastighet möjlig att basera på markernas växtlighet.

Dry, boreal, forest ecosystems have been shown to alternate due to reindeer presence by changing the field layer. This affects the temperature of the soil, changes the microclimate and the nutrients of soil and field layer. By removal of biomass and trampling stress the ground lichen mats reduce in cover and thickness. In this thesis two dry, boreal pine forests in Northern Finland were studied, to see how the nutrient stocks in the field layer are impacted by reindeer presence. A comparison of the same site, with >20 years in between was studied to see how year-round grazing affect the carbon storage in the field layer compared to winter grazing.    I found that reindeer grazing reduces the vegetation carbon storage, however, the impact on the vegetation nitrogen storage differs with site. Furthermore, the lichens and shrubs had lower C:N ratios because of increased nitrogen content in the plant tissue and unaffected carbon content. These results show that reindeer actively changes the vegetation quantity and quality which will have implications for the soil carbon storage.

The wild boar is known to disturb the forest floor by rooting in the soil as they search for food. Soil is a vital part of the carbon cycle and stores large amounts of carbon. There is limited knowledge on how this feeding behavior may alter the content of organic matter in the soil and consequently the ability of the soil to store carbon. The objective of this study was to examine the effects of rooting on organic matter concentration by (1) comparing soil from rooted and un-rooted plots and (2) investigating whether the density of rooted areas within each plot affects organic matter concentration. Our results showed no effects of rooting on organic matter concentration. The soil in our study area contained very high concentrations of organic matter (83%) which could have been a factor in why no effects were detected. Our overall results indicate that rooting does not, in the short term, affect the ability of the soil to store carbon in a coniferous forest in southern Sweden. However, this does not exclude rooting as a potential factor influencing soil carbon storage, as several other studies have detected significant differences in soil concentration. The complexity of ecosystems and factors influencing their properties leads to contrasting results between studies. It is relevant in a climate change perspective to further investigate the effects rooting may have on carbon storage in the soil.

Koldioxidhalterna stiger i världen, vilket bidrar till global uppvärmning. Skogen har en viktig roll i klimatarbetet då stora mängder kol finns lagrad i skog och mark. Speciellt mycket kol finns i boreal skog, som bland annat finns i norra Sverige. Idag pågår en debatt huruvida det är mer fördelaktigt att behålla gammal skog som kolsänka, eller avverka den för att ge plats åt yngre träd. Syftet med litteraturstudien var att ge en klargörande bild över hur åldern på boreal skog påverkar ekosystemets kolbalans, genom att undersöka skogens kolupptagningshastighet samt möjlighet till kollagring. Studien visade att äldre skog har ett större totalt kollager, att medelåldrig skog har högst tillväxthastighet (nettoekosystemproduktion, NEP och nettoprimärproduktion, NPP) samt att NEP är negativ de första 10 åren. Studien visade på osäkerhet kring kolupptag i gamla skogar. Flera variabler, såsom substitution, störningar och biologisk mångfald är inte undersökta i studien och behövs tas i beaktning vid beslutsfattande. Trots detta, antyder litteraturstudien att det är fördelaktigt att låta gammal skog stå kvar som kolsänka, eftersom koldioxidutsläppen behöver minska snarast. Ytterligare ett syfte med studien var att kartlägga de missuppfattningar elever, i senare delen av skolan, har gällande kolets kretslopp. Studien visade på missuppfattningar gällande fotosyntes och respiration hos växter, nedbrytarnas roll samt sammanblandning av begrepp. För att åtgärda problemet kan uppgifter göras där atomer följs över olika nivåer, för att sätta processerna i sitt sammanhang. Stort fokus gällande missuppfattningarna ligger på fotosyntes och respiration och inga artiklar hittades gällande exempelvis det snabba, respektive långsamma, kretsloppet. Få studier är gjorda på svenska elever och då svensk kursplan lägger fokus på samband mellan olika nivåer kan missuppfattningarna vara i annorlunda i Sverige. Hur missuppfattningarna ser ut i svensk skola är föremål för vidare forskning. / The amount of carbon dioxide is rising in the atmosphere, which contributes, to global warming. Since large amounts of carbon are stored in forests, forests play an important part the efforts to improve the environment. Boreal forests, found in e.g. the northern part of Sweden, store especially large amounts of carbon. Today it is being debated whether it is more beneficial for the environment to keep old forests as a carbon sink, or to cut them down in order to make room for younger trees. The purpose of this literature study was to clarify how the age of the forest affects the carbon balance of the ecosystem, by examining the forest’s rate of carbon sequestration and capability of carbon storage. The literature study concluded that older forests, in total, store larger amounts of carbon, while middle-aged forests have he highest growth rate (net ecosystem production, NEP, and gross primary production, GPP) and that NEP is negative in the first ten years. The study showed some uncertainty concerning carbon uptake in old forests. Several variables, such as the effects of substitution, disturbances and biodiversity were not examined in this study and need to be further considered before making decisions. However, the literature study suggests that it is more beneficial to leave old forests as a carbon sink, since emissions of carbon dioxide urgently need to be reduced. Another purpose of the study was to examine the misconceptions that students, in the later school years, have regarding the carbon cycle. This study found misconceptions concerning photosynthesis and respiration in plants, the role of decomposers, as well as getting concepts mixed up with one another. To solve this problem, assignments could be designed where atoms are traced between different levels, in order to put the processes in context. A large part of the focus regarding these misconceptions has been on photosynthesis and respiration and no articles were found regarding e.g. the fast; and the slow; carbon cycle. Few studies of Swedish students have been made and since the Swedish curriculum focuses on the relationship between different levels, the misconceptions might be different in Sweden; what these misconceptions could be in Swedish schools is yet to be investigated.