Origin and transformation of organic matter in Pliocene–Pleistocene Mediterranean sapropels: organic geochemical evidence reviewed

Author:

Bouloubassi Ioanna,Rullkötter Jürgen,Meyers Philip A

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference95 articles.

1. Past sedimentary organic matter accumulation and degradation controlled by productivity;Bertrand;Nature,1993

2. Blackburn, J.H., 1980. Seasonal variation in the rate of organic-N mineralization in anoxic marine sediments. In: Daumas, R. (Ed.), Biogéochimie de la Matière Organique à l'Interface Eau–Sédiment Marin. Colloq. Int. CNRS 293, 173–183.

3. Boon, J.J., Hines, H., Burlingame, A.L., Klock, J., Rijpstra, W.I.C., de Leeuw, J.W., Edmunds, K.E., Eglinton, G., 1983. Organic geochemical studies of Solar Lake laminated cyanobacterial mats. In: Bjorøy, M. et al. (Eds.), Advances in Organic Geochemistry 1981. Wiley, Chichester, pp. 239–248.

4. Bouloubassi, I., Guehenneux, G., Rullkötter, J., 1998. Biological marker significance of organic matter in sapropels from the Mediterranean Ridge, Site 969. Proc. ODP, Sci. Results 160 (in press).

5. Distributions of n-paraffins as a clue to recognition of source beds;Bray;Geochim. Cosmochim. Acta,1961

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