The usefulness of n-propyl-, iso-propyl-, and cyclopropylamines for the location of double bonds positions in C 37 -C 40 alkenones after formation of imino derivatives has been evaluated. Cyclopropylamine is the best reagent for its high reaction yields, GC retention time difference between derivatives and precursor compounds, and absence of generation of byproducts. The use of this C 3 amine involves higher sensitivity and ease of application than previously reported C 5 amines. Examination of a large group of alkenones from cultures of Emiliania huxleyi, water particles, and recent and ancient sediments with cyclopropylamine derivatization shows that, in all cases, the double bonds were located at the same carbon atom distance from the carbonyl group, and spaced in intervals of five methylene groups either from the carbonyl or between them, e.g., at sites 7, 14, 21, and 28. This result represents a correction from previous assumptions in which double-bond positions were situated by reference to the methyl end. 4,4-Dimethyloxazoline derivatization of hexatriacontenoates showed that these compounds have also their unsaturations with seven carbon atom spacing and counting by reference to the carboxyl group. The concurrence of both series of isomers in compounds of different oxygen functionalities indicates that the precursor haptophycean algal species have a major biosynthetic pathway leading to the formation of these lipids. The data presented in this work unify the structures of the known alkenones in the present and the recent past under a common metabolic pathway. These compounds currently encompass mixtures of straight chain methyl and ethyl ketones with one to four unsaturations and all trans-configuration. They constitute one of the groups of marine lipids most intensively studied because of the clear relationship between composition of the C 37 di-and triunsaturated homologues and sea surface temperature (SST) [2,3] being widely used for the estimation of past ocean temperatures [4 -7].Structural characterization of these low volatile compounds is needed for a full understanding of their biosynthetic origin and geochemical meaning. However, attempts to locate the positions of the double bonds based on GC-MS studies of vicinal bistrimethylsilyl ethers [8] or dimethanethiols [9] had limited success because they generated derivatives with much longer retention times than the original compounds [10]. Recently, the application of a novel technique based on the mass spectra of phenyl and cyclopentylimines has been used to characterize distributions of alkenones found in hypersaline sediments and coastal tidal ponds [1].However, the study of alkenone structures in samples from old sediments, e.g., those covering the last 250 k years of the history of the Mediterranean SST [6], showed that in some cases the sensitivity of the methods available [1] was not sufficient for the unambiguous determination of the position of the unsaturations because of the low concentrations of these compounds. Keeping in mind the prev...