“…Our study has shown that the resting spore concentrations of the marine diatom Chaetoceros are very high during three ages (last century, MCA, and HTM) which correspond to times with high primary production, high sea surface temperatures (HTM, MCA), eutrophication (last century), and result in hypoxia (Zillén et al, 2008; Funkey et al, 2014). Recent studies have shown that increased salinity in the Baltic Proper caused increased hypoxic conditions and higher productivity of diatoms during the warm HTM conditions (van Wirdum et al, 2019) that also prevailed during MCA (E. Andrén et al, 2020). Warm climate creates a stronger stratification in the water mass resulting in hypoxic bottoms, but also enhances phosphorus recycling and sustaining cyanobacterial blooms which contribute to increase overall available nutrient concentrations (Funkey et al, 2014; Karlson et al, 2015).…”