Research



Ongoing projects....

Wildfire 

... and peatland resilience

With the prospect of increasing temperatures at higher latitudes, wildfire frequency and severity in forested boreal ecosystems are expected to increase. In combination with other perturbations such as drainage, the boreal ecosystems may experience more regime shifts; that is, when ecosystems are pushed into alternative states which can have important implications for both boreal ecosystem structure and function (e.g. water balance, biodiversity and carbon balance).  

... ecosystem development
The boreal landscape changes fundamentaly when a fire occurs, but what determines the development post-fire? I am investigating how carbon and nitrogen accumualtion varies spatially and temporally post-fire and the interplay between abiotic and biotic factors. Here I want to link processes involved in plant community composition and link this to ecosystem processes at multiple scales. The goal is to develop models that predict post-fire development of ecosystem processes, including the aggregation of biodiversity in space and time.

In addition, I want to explore how today's management of pre-scribed burning affect processes and biodiversity in the landscape. We still know relatively little how this practice should be performed to achieve the set goal.  
 

Global Sphagnum Production

We know, surprisingly, rather little about global patterns of Sphagnum production and the influence of environmental variables. There have been two major attempts to model Sphagnum production on a global scale (Gunnarsson 2005, Loisel et al. 2012). These publications, however, are based on data collected from the literature, based on different methods, with limited spatial cover, over a long time period and with no estimation of variability.

The idea with this project is to measure Sphagnum production along major gradients of climate and N deposition, by engaging peatland reserachers around the world. We focus on two species, S. fuscum and S. magellanicum. These species have a wide distribution and are of large ecological importance.


Eutrophication of forests and peatlands
Deposition of reactive nitrogen (N) has increased rapidly since the industrial revolution and consists of wet deposition (mainly NH4+,NO3-) and dry deposition (mainly NH3). In addition, fertilizers (mainly N) is sometimes used to enhance forest production Sweden. Because terrestrial ecosystems are mainly N limited, increased N input generally increases biomass production. However, in nutrient poor ecosystems, high N input can have severe negative effects on species diversity (e.g. competitive exclusion of slow growing plants) and ecosystem functions (e.g. microbial composition and C accumulation).

... effects of N application on boreal forests
Here we take advantage of a country wide fertilization and thinning experiments that has been running for over 40 years. We are looking at the impact of these treatments on biodiversity, berry production and carbon storage.

... effects of N deposition on peatlands
Peatlands are partparticularly poor habitats and therefore expected to be vulnerable to increased N input. In my work, I have investigated the underlying mechanisms causing changes in Sphagnum production under high N input. In addition, I have with Juul Limpens summarized the experimental work on N effects on Sphagnum growth in three meta-analyses. However, the picture is still incomplete and additional work is needed.