Compound specific hydrogen isotope ratios (2 H/ 1 H) of lipid biomarkers 36! preserved in sediments are used as a paleohydrologic proxies. However, several 37! variables, including contributions from different source organisms and their growth 38! rates, can influence 2 H/ 1 H fractionation between lipids and source water. Significant 39! uncertainties remain about how these factors combine to produce the net 2 H/ 1 H signal 40! exported to sediments. 41! To assess the influence of phosphorus availability on 2 H/ 1 H ratios of lipids 42! accumulating in lake sediments, we analyzed surface sediments and sediment traps 43! from ten central Swiss lakes, representing a wide range of trophic states. In agreement 44! with results from laboratory cultures, 2 H/ 1 H fractionation for the diatom biomarker 45! brassicasterol (24-methyl cholest-5,22-dien-3β-ol) increased in more productive lakes 46! (0.6 ± 0.1 ‰ per µg/L total P in sediment traps and surface sediments). In contrast, 47! 2 H/ 1 H fractionation for phytol, the isoprenoid side-chain moiety of chlorophyll, 48! decreased with increasing total P (-0.4 ± 0.1 ‰ per µg/L total P in sediment traps), 49! suggesting that different biochemical mechanisms are responsible for changes in 2 H/ 1 H 50! fractionation for each class of isoprenoidal lipids. Opposing changes in 2 H-51! fractionation for sterols and phytol cause their 2 H/ 1 H ratios to converge as total P 52! increases. This response may be a new tracer for phytoplankton growth conditions and 53! is not influenced by the source water isotope value. 54! Interpreting the 2 H/ 1 H ratios of short to long chain (C 14-C 30) n-alkanoic acids 55! and n-alkanols is complicated by likely contributions from heterotrophs and/or 56! vascular plants. These values generally did not correlate with lake water isotopes, nor 57! did their fractionation factors correlate with total P. For most lipids there was no 58! significant difference between sediment trap and surface sediment 2 H/ 1 H ratios. 59! However, n-C 14n-C 18 fatty acids were 2 H-enriched in the surface sediments, most 60! likely due to degradation in the water column. Our results indicate that interpretations 61! of short-chain fatty acids as a water isotope signal likely require supporting 62! information about ecological conditions and community structure, but that paired H 63! isotope measurements of phytoplankton-derived sterols and phytol may be developed 64! as a proxy for phytoplankton growth.