Droevendaalsesteeg 10
6708 PB Wageningen
The Netherlands
As part of the CLIMET project, I am working on microbial interactions in Greenlandic lakes, and their influence on methane emissions.
I’m a microbiologist with a special interest in Arctic microbes and the surprising things they can do. During my PhD, I worked on the Greenland Ice Sheet, where I studied the diversity of these cold-adapted communities and the molecules they produce—both what they mean for microbial ecology and how they might be useful in biotechnology.
At NIOO, I’m a postdoc in the CLIMET project, where I look at the microbes that consume methane in Arctic lakes. My work is a mix of lab experiments and fieldwork, and I really value being able to see the system that we study in real life. Being out in Greenland again, sampling lakes and getting a feel for the landscape, gives me ideas and helps me understand the ecology of these microbes in a much more intuitive way.
I really enjoy being part of a big multidisciplinary team, and I’m motivated by simple curiosity about how these unique Arctic microbes live, interact with, and shape their environment.
Cryoconite holes host diverse microbiomes on glaciers and ice sheets and are important habitats for supraglacial biogeochemical cycling. Despite reports of relative stability of cryoconite hole community composition on the Greenland Ice Sheet, it is not known how microbial function in cryoconite holes evolves under varying environmental conditions. Here, we address this knowledge gap by quantifying the active community members in five cryoconite holes on the Greenland Ice Sheet over a 3-week period during the 2022 melt season using TotalRNA. Active microbiomes were enriched in cyanobacterial sequences (25%–50%). Spatial variation between cryoconite holes had a greater impact than temporal variation on community composition quantified by rRNA SSUs, suggesting location-distinct and highly stable active microbiomes. In contrast, minor temporal variations in gene expression were identified in the mRNA data (∼1% of quantified transcripts), mostly due to cellular stress responses from washed-in glacier ice algae. Photosynthesis was the dominant active function across all surveyed cryoconite holes and time points, associated with both cyanobacterial taxa and washed-in chlorophyte snow algae. Overall, our data indicate that core cryoconite hole communities stably ensure their ecological roles, such as carbon fixation, regardless of variations in weather, highlighting their resilience and self-sufficiency.