CALIBRATION OF ALKENONE UNSATURATION RATIOS (U-37(K')) FOR PALEOTEMPERATURE ESTIMATION IN COLD POLAR WATERS

C37-C39 long-chain unsaturated ketones (alkenones) and alkenes were id entified in samples of particulate organic matter obtained from surfac e waters spanning the temperature range -0.7-12.2-degrees-C in the Sou thern Ocean south of Australia. The carbon number distribution indicat es that these compounds are derived from the prymnesiophyte alp Emilia nia huxleyi which is the predominant coccolithophorid in these waters. Values of U37k' were calculated according to the definition U37k' = [ 37:2]/([37:2] +[37:3]), where [37:x] is the concentration of the C37 a lkenone with ''x'' double bonds, and plotted against sea surface tempe rature (SST). Our data form a contiguous set with earlier compilations of data from warmer waters. Over much of the temperature range the re lationship between U37k' and temperature is remarkably linear, and is best fitted by the simple equation U37k' = 0.0414T-0.156 (for temperat ures 4-25-degrees-C). This calibration of U37k' with temperature for f ield samples is significantly different from that established from ana lyses of prymnesiophyte algae in culture, and it diverges especially a t the colder temperatures. Data for temperatures below about 4-6-degre es-C show increased scatter and the calibration at these low temperatu res may be better fitted by a nonlinear exponential function, but this requires further testing. Certainly, the predictive power of the line ar calibration is severely constrained at temperatures less than 5.0-d egrees-C, but at temperatures above this our data establish the useful ness of U37k' as an SST indicator for waters north of the polar front in the Southern Ocean and for several regions of the world ocean.