Nemiah Ladd, Daniel Nelson, Blake Matthews, Shannon Dyer, Romana Limberger, Antonia Klatt, Anita Narwani, Nathalie Dubois, Carsten Schubert

Phytoplankton play a key role in biogeochemical cycles, impacting atmospheric and aquatic chemistry, food webs, and water quality. However, it remains challenging to reconstruct changes in algal community composition throughout the geologic past, as existing proxies are suitable only for a subset of taxa and/or influenced by degradation. Here, we investigate if compound-specific hydrogen isotope ratios (d2H values) of common algal lipids can serve as (paleo)ecological indicators. First, we grew 20 species of algae – representing cyanobacteria, diatoms, dinoflagellates, green algae, and cryptomonads – in batch cultures under identical conditions and measured d2H values of their lipids. Despite identical source water d2H values, lipid d2H values ranged from -455 ‰ to -52 ‰, and clustered according to taxonomic groups and chemical compound classes. In particular, green algae synthesized fatty acids with higher d2H values than other taxa, cyanobacteria synthesized phytol with relatively low d2H values, and diatoms synthesized sterols with higher d2H values than other eukaryotes. Second, we assessed how changes in algal community composition can affect net d2H values of common algal lipids in 20 experimental outdoor ponds, which were manipulated via nutrient loading, and the addition of macrophytes and mussels. High algal biomass in the ponds, which was mainly caused by cyanobacterial and green algal blooms, was associated with higher d2H values for generic fatty acids, relatively stable d2H values for phytol and the dinoflagellate biomarker dinostanol, and lower d2H values for the more cosmopolitan sterol stigmasterol. These results are consistent with expectations from our culture-based analyses, suggesting that measuring d2H values of multiple lipids from sediment and calculating 2H-offsets between them can resolve changes in algal community composition from changes in source water isotopes. With an appropriate availability of sedimentary lipids, this approach could permit the reconstruction of both taxonomic variability and hydroclimate from diverse sedimentary systems.