The Greenland Ice Sheet holds a significant amount of freshwater, equivalent to approximately 7.4 meters of potential global sea level rise. Recent research highlights its sensitivity to climate warming and the resulting impact on sea levels and ocean circulations. However, data limitations hinder our understanding of the ice sheet's response to major climate changes, restricting our ability to predict future sea level rise and climate feedback. To address this, I am participating in Expedition 400 of the International Ocean Discovery Program (IODP) to NW Greenland (Baffin Bay) aboard the JOIDES Resolution from August 13th to October 13th, 2023. Expedition 400 aims to recover sediment archives with high temporal resolution, documenting the climate history and variability of the Greenland Ice Sheet over the past 30 million years. Subsequent post-cruise research on these sediment cores will involve utilizing geochemical proxies to trace temperature and precipitation. Additionally, analysis of microfossils (foraminifera) will uncover connections between the Arctic Ocean, North Atlantic, and the Greenland Ice Sheet. Our findings will shed light on the factors influencing the Greenland Ice Sheet, thus contributing to enhanced predictions of global sea level rise amidst ongoing Arctic and global warming.

The increasing uptake of CO2 by the Arctic Ocean leads to ocean acidification and may cause ecosystem and socio-economic stress within and beyond the Arctic region. Ocean acidification in the Arctic is commonly attributed to the rise in atmospheric CO2. However, Arctic warming is expected to trigger massive release of terrestrial organic carbon from rivers and collapsing permafrost, which may exacerbate ocean acidification by additional supply of CO2 from mineralized terrestrial carbon. In this project, we investigate Arctic Ocean acidification during past climate change, such as the last deglaciation or past glacial-interglacial cycles. We study past changes in ocean pH and CO2 using the boron isotope proxy (δ¹¹B) in foraminifera, as well as through microbial biomarkers. Through this work, we aim to expand our understanding of the natural variability of the Arctic Ocean carbonate system during changing climate, and examine the contribution of terrestrial processes to Arctic Ocean acidification.

Arctic warming leads to destabilization of high-latitude soils and permafrost deposits, yet there are large uncertainties regarding the dynamics and processes of carbon release from these systems. Over the past years, I have been part of an international team of scientists that created a new database of biogeochemical observations in Arctic Ocean sediments, the Circum-Arctic Sediment Carbon DatabasE (CASCADE; incl. a paper in Earth System Science Data; Martens et al., 2021). In this effort, we collected and analyzed data of carbon isotopes (δ13C , Δ14C ) and terrestrial biomarkers (such as plant lipids, e.g. n-alkanes and n-alkanoic acids, as well as lignin phenols) in sediments to enable studies of carbon release and re-mineralization from the perspective of the Arctic Ocean as a receptor system.

Based on the creation of CASCADE and a number of application studies, we have also been studying the spatial patterns and differences of carbon release and re-mineralization in the vast circum-Arctic drainage basin. For this work, we use spatial data analysis tools and statistical dual-isotope (δ13C , Δ14C ) source apportionment to estimate terrestrial carbon accumulation in the circum-Arctic shelf seas and study the lateral carbon mobilization from different Arctic carbon reservoirs (such as permafrost and peatlands). This research was recently published in Nature Communications (Martens et al. 2022).