165
References
waxes. Elsevier, Amsterdam, 459 pp.
Krey, J., 1970. Die Urproduktion des Meeres (in German). In:
Dietrich, G. (ed), Erforschung des Meeres. Umschau,
Frankfurt, pp. 183-195.
Kristensen, E., Ahmed, S.A. and Devol, A.H., 1995. Aerobic
and anaerobic decomposition of organic matter in marine
sediments. Which is faster? Limnol. Oceanogr., 40: 14301437.
Lallier-Vergès, E., Bertrand, P. and Desprairies, P., 1993.
Organic matter composition and sulfate reduction intensity
in Oman margin sediments. Mar. Geol., 112: 57-69.
Largeau. C., Derenne, S., Casadevall, E., Berkaloff, C., Corolleur,
M., Lugardon, B., Raynaud, J.F. and Connan, J., 1990.
Occurrence and origin of “ultralaminar” structures in
“amorphous” kerogens of various source rocks and oil
shales. Org. Geochem., 16: 889-895.
Larter, S.R. and Horsfield, B., 1993. Determination of structural
components of kerogens by the use of analytical pyrolysis
methods. In: Engel, M.H. and Macko, S.A. (eds), Organic
geochemistry. Principles and applications. Plenum Press,
NY, pp. 271-287.
Leonardos, N. and Geider, R.J., 2004. Limnol. Oceanogr., 49:
2105-2114.
Leventhal, J.S., 1983. An interpretation of carbon and sulphur
relationships in Black Sea sediments as indicators of
environments of deposition. Geochim. Cosmochim. Acta,
47: 133-138.
Littke, R., Rullkötter, J. and Schaefer, R.G., 1991a. Organic
and carbonate carbon accumulation on Broken Ridge and
Ninetyeast Ridge, central Indian Ocean. In: Weissel, J.,
Pierce, J. et al. (eds), Proceedings of the Ocean Drilling
Program, Sci. Res., 121, ODP, College Station (TX), pp.
467-487.
Littke, R., Baker, D.R., Leythaeuser, D. and Rullkötter, J.,
1991b. Keys to the depositional history of the Posidonia
Shale (Toarcian) in the Hils syncline, northern Germany.
In: Tyson, R.V. and Pearson, T.H. (eds), Modern and ancient
continental shelf anoxia. Geol. Soc. Spec. Publ., 58, The
Geological Society, London, pp. 311-334.
Littke, R., Baker, D.R. and Rullkötter, J., 1997a. Deposition of
petroleum source rocks. In: Welte, D.H., Horsfield, B. and
Baker, D.R. (eds), Petroleum and basin evolution. SpringerVerlag, Heidelberg, pp. 271-333.
Littke, R., Lückge, A. and Welte, D.H., 1997b. Quantification
of organic matter degradation by microbial sulphate
reduction for Quaternary sediments from the northern
Arabian Sea. Naturwissenschaften, 84: 312-315.
Lückge, A., Boussafir, M., Lallier-Vergès, E. and Littke, R.,
1996. Comparative study of organic matter preservation
in immature sediments along the continental margins of
Peru and Oman. Part I: Results of petrographical and bulk
geochemical data. Org. Geochem., 24: 437-451.
Mangelsdorf, K., Güntner, U. and Rullkötter, J., 2000. Climatic
and oceanographic variations on the California continental
margin during the last 160 kyr. Org. Geochem., 31: 829846.
Mariotti, A., Gadel, F., Giresse, P. and Kinga-Mouzeo, 1991.
Carbon isotope composition and geochemistry of
particulate organic matter in the Congo River (Central
Africa): Application to the study of Quaternary sediments
off the mouth of the river. Chem. Geol., 86: 345-357.
Martens, C.S. and Klump, J.V., 1984. Biogeochemical cycling in
an organic-rich coastal marine basin - 4. An organic carbon
budget for sediments dominated by sulfate reduction and
methanogenesis. Geochim. Cosmochim. Acta, 48: 1987-2004.
Martens, C.S., Haddad, R.I. and Chanton, J.P., 1992. Organic
matter accumulation, remineralization, and burial in an
anoxic coastal sediment. In: Whelan, J.K. and Farrington,
J.W. (eds), Organic matter: Productivity, accumulation and
preservation in recent and ancient sediments, Columbia
University Press, NY, pp 82-98.
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore,
T.C.J. and Shackleton, N.J., 1987. Age dating and the orbital
theory of the ice ages: Development of a high-resolution 0
to 300,000-year chronostratigraphy. Quat. Res., 27: 1-29.
Mayer, L.M., 1994. Surface area control of organic carbon
accumulation in continental shelf sediments. Geochim.
Cosmochim. Acta, 58: 1271-1284.
Mayer, L.M., 1999. Extent of coverage of mineral surfaces by
organic matter in marine sediments. Geochim. Cosmochim.
Acta, 63: 207-215.
Mayer, L.M., 2005. Erratum to L. M. Mayer (1999) “Extent
of coverage of mineral surfaces by organic matter in marine
sediments” Geochimica et Cosmochimica Acta 63, 207215. Geochim. Cosmochim. Acta, 69: 1375.
McIver, R., 1975. Hydrocarbon occurrences from JOIDES Deep
Sea Drilling Project. Proceedings of the 9
th World Petroleum
Congress (Tokyo), 2, Applied Science Publishers, Barking,
pp. 269-280.
McLafferty, F.W. and Turecek, F., 1993. Interpretation of mass
spectra. University Science Books, Mill Valley (CA), 371
pp.
Meybeck, M., 1982. Carbon, nitrogen, and phosphorus
transport by world rivers. Am. J. Sci., 282: 401-450.
Meyers, P.A., 1994. Preservation of elemental and isotopic
source identification of sedimentary organic matter. Chem.
Geol., 144: 289-302.
Meyers, P.A., 1997. Organic geochemical proxies of
paleoceanographic, paleolimnologic, and paleoclimatic
processes. Org. Geochem., 27: 213-250.
Mitterer, R.M., 1993. The diagenesis of proteins and amino
acids in fossil shells. In: Engel, M.H. and Macko, S.A. (eds),
Organic geochemistry. Principles and applications. Plenum
Press, NY, pp 739-753.
Moers, M.E.C., Jones, D.M., Eakin, P.A., Fallick, A.E., Griffiths,
H. and Larter, S.R., 1993. Carbohydrate diagenesis in
hypersaline environments: Application of GC-IRMS to the
stable isotope analysis of derivatives of saccharides from
surficial and buried sediments. Org. Geochem., 20: 927933.
Mollenhauer, G., Eglinton, T.I., Ohkouchi, N., Schneider, R.R.,
Müller, P.J., Grootes, P.M. and Rullkötter, J., 2003.
Asynchronous alkenone and foraminifera records from the
Benguela Upwelling System. Geochim. Cosmochim. Acta,
67: 2157-2171.
Müller, P.J., 1977. C/N ratios in Pacific deep-sea sediments:
Effect of inorganic ammonium and organic nitrogen
compounds sorbed by clays. Geochim. Cosmochim. Acta,
41: 765-776.
Müller, P.J. and Suess, E., 1979. Productivity, sedimentation
rate and sedimentary organic matter in the oceans - organic
carbon preservation. Deep-Sea Res., 27A: 1347-1362.
References
waxes. Elsevier, Amsterdam, 459 pp.
Krey, J., 1970. Die Urproduktion des Meeres (in German). In:
Dietrich, G. (ed), Erforschung des Meeres. Umschau,
Frankfurt, pp. 183-195.
Kristensen, E., Ahmed, S.A. and Devol, A.H., 1995. Aerobic
and anaerobic decomposition of organic matter in marine
sediments. Which is faster? Limnol. Oceanogr., 40: 14301437.
Lallier-Vergès, E., Bertrand, P. and Desprairies, P., 1993.
Organic matter composition and sulfate reduction intensity
in Oman margin sediments. Mar. Geol., 112: 57-69.
Largeau. C., Derenne, S., Casadevall, E., Berkaloff, C., Corolleur,
M., Lugardon, B., Raynaud, J.F. and Connan, J., 1990.
Occurrence and origin of “ultralaminar” structures in
“amorphous” kerogens of various source rocks and oil
shales. Org. Geochem., 16: 889-895.
Larter, S.R. and Horsfield, B., 1993. Determination of structural
components of kerogens by the use of analytical pyrolysis
methods. In: Engel, M.H. and Macko, S.A. (eds), Organic
geochemistry. Principles and applications. Plenum Press,
NY, pp. 271-287.
Leonardos, N. and Geider, R.J., 2004. Limnol. Oceanogr., 49:
2105-2114.
Leventhal, J.S., 1983. An interpretation of carbon and sulphur
relationships in Black Sea sediments as indicators of
environments of deposition. Geochim. Cosmochim. Acta,
47: 133-138.
Littke, R., Rullkötter, J. and Schaefer, R.G., 1991a. Organic
and carbonate carbon accumulation on Broken Ridge and
Ninetyeast Ridge, central Indian Ocean. In: Weissel, J.,
Pierce, J. et al. (eds), Proceedings of the Ocean Drilling
Program, Sci. Res., 121, ODP, College Station (TX), pp.
467-487.
Littke, R., Baker, D.R., Leythaeuser, D. and Rullkötter, J.,
1991b. Keys to the depositional history of the Posidonia
Shale (Toarcian) in the Hils syncline, northern Germany.
In: Tyson, R.V. and Pearson, T.H. (eds), Modern and ancient
continental shelf anoxia. Geol. Soc. Spec. Publ., 58, The
Geological Society, London, pp. 311-334.
Littke, R., Baker, D.R. and Rullkötter, J., 1997a. Deposition of
petroleum source rocks. In: Welte, D.H., Horsfield, B. and
Baker, D.R. (eds), Petroleum and basin evolution. SpringerVerlag, Heidelberg, pp. 271-333.
Littke, R., Lückge, A. and Welte, D.H., 1997b. Quantification
of organic matter degradation by microbial sulphate
reduction for Quaternary sediments from the northern
Arabian Sea. Naturwissenschaften, 84: 312-315.
Lückge, A., Boussafir, M., Lallier-Vergès, E. and Littke, R.,
1996. Comparative study of organic matter preservation
in immature sediments along the continental margins of
Peru and Oman. Part I: Results of petrographical and bulk
geochemical data. Org. Geochem., 24: 437-451.
Mangelsdorf, K., Güntner, U. and Rullkötter, J., 2000. Climatic
and oceanographic variations on the California continental
margin during the last 160 kyr. Org. Geochem., 31: 829846.
Mariotti, A., Gadel, F., Giresse, P. and Kinga-Mouzeo, 1991.
Carbon isotope composition and geochemistry of
particulate organic matter in the Congo River (Central
Africa): Application to the study of Quaternary sediments
off the mouth of the river. Chem. Geol., 86: 345-357.
Martens, C.S. and Klump, J.V., 1984. Biogeochemical cycling in
an organic-rich coastal marine basin - 4. An organic carbon
budget for sediments dominated by sulfate reduction and
methanogenesis. Geochim. Cosmochim. Acta, 48: 1987-2004.
Martens, C.S., Haddad, R.I. and Chanton, J.P., 1992. Organic
matter accumulation, remineralization, and burial in an
anoxic coastal sediment. In: Whelan, J.K. and Farrington,
J.W. (eds), Organic matter: Productivity, accumulation and
preservation in recent and ancient sediments, Columbia
University Press, NY, pp 82-98.
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore,
T.C.J. and Shackleton, N.J., 1987. Age dating and the orbital
theory of the ice ages: Development of a high-resolution 0
to 300,000-year chronostratigraphy. Quat. Res., 27: 1-29.
Mayer, L.M., 1994. Surface area control of organic carbon
accumulation in continental shelf sediments. Geochim.
Cosmochim. Acta, 58: 1271-1284.
Mayer, L.M., 1999. Extent of coverage of mineral surfaces by
organic matter in marine sediments. Geochim. Cosmochim.
Acta, 63: 207-215.
Mayer, L.M., 2005. Erratum to L. M. Mayer (1999) “Extent
of coverage of mineral surfaces by organic matter in marine
sediments” Geochimica et Cosmochimica Acta 63, 207215. Geochim. Cosmochim. Acta, 69: 1375.
McIver, R., 1975. Hydrocarbon occurrences from JOIDES Deep
Sea Drilling Project. Proceedings of the 9
th World Petroleum
Congress (Tokyo), 2, Applied Science Publishers, Barking,
pp. 269-280.
McLafferty, F.W. and Turecek, F., 1993. Interpretation of mass
spectra. University Science Books, Mill Valley (CA), 371
pp.
Meybeck, M., 1982. Carbon, nitrogen, and phosphorus
transport by world rivers. Am. J. Sci., 282: 401-450.
Meyers, P.A., 1994. Preservation of elemental and isotopic
source identification of sedimentary organic matter. Chem.
Geol., 144: 289-302.
Meyers, P.A., 1997. Organic geochemical proxies of
paleoceanographic, paleolimnologic, and paleoclimatic
processes. Org. Geochem., 27: 213-250.
Mitterer, R.M., 1993. The diagenesis of proteins and amino
acids in fossil shells. In: Engel, M.H. and Macko, S.A. (eds),
Organic geochemistry. Principles and applications. Plenum
Press, NY, pp 739-753.
Moers, M.E.C., Jones, D.M., Eakin, P.A., Fallick, A.E., Griffiths,
H. and Larter, S.R., 1993. Carbohydrate diagenesis in
hypersaline environments: Application of GC-IRMS to the
stable isotope analysis of derivatives of saccharides from
surficial and buried sediments. Org. Geochem., 20: 927933.
Mollenhauer, G., Eglinton, T.I., Ohkouchi, N., Schneider, R.R.,
Müller, P.J., Grootes, P.M. and Rullkötter, J., 2003.
Asynchronous alkenone and foraminifera records from the
Benguela Upwelling System. Geochim. Cosmochim. Acta,
67: 2157-2171.
Müller, P.J., 1977. C/N ratios in Pacific deep-sea sediments:
Effect of inorganic ammonium and organic nitrogen
compounds sorbed by clays. Geochim. Cosmochim. Acta,
41: 765-776.
Müller, P.J. and Suess, E., 1979. Productivity, sedimentation
rate and sedimentary organic matter in the oceans - organic
carbon preservation. Deep-Sea Res., 27A: 1347-1362.