21. BIOLOGICAL MARKER SIGNIFICANCE OF ORGANIC MATTER ORIGIN IN SAPROPELS
FROM THE MEDITERRANEAN RIDGE, SITE 9691

Ioanna Bouloubassi,2 Guillaume Guehenneux,2 and Jürgen Rullkötter3

ABSTRACT

The major extractable lipid components in a series of Pleistocene–Pliocene sapropels from Ocean Drilling Program Leg 160 Site 969 were investigated. The organic-carbon contents in sapropels of Pleistocene age have a typical range of values, up to 7.4%, whereas the Pliocene sapropels were extraordinarily organic-carbon rich with values reaching 32.2%. The molecular composition of extractable lipids was dominated by alkandiols and alkanolones, alkenones, and sterols, with lower amounts of n-alkanes and n-alcohols. The molecular compositions indicate that organic matter in sapropels is predominantly derived from marine algal sources. Nevertheless, the distribution of terrestrial lipids indicates a significant land-derived influx during sapropel formation.

1Robertson, A.H.F., Emeis, K.-C., Richter, C., and Camerlenghi, A. (Eds.), 1998. Proc. ODP, Sci. Results, 160: College Station, TX (Ocean Drilling Program).
2Département de Géologie et Océanographie, Université Bordeaux I, URA CNRS 197, avenue des Facultés, 33405 Talence cedex, France.
bouloubassi@geocean.u-bordeaux.fr
3Institut für Chemie und Biologie des Meeres (ICBM), Carl von Ossietzky Universität Oldenburg, Postfach 2503, 26111 Oldenburg, Federal Republic of Germany.