Sediment Organic Matter

Author:

Meyers Philip A.,Teranes Jane L.

Publisher

Kluwer Academic Publishers

Reference102 articles.

1. Altabet, M. A. & R. François, 1993. The use of nitrogen isotopic ratio for reconstruction of past changes in surface ocean nutrient utilization. In Zahn, R., T. R. Pederson, M. Kaminshi & L. Labeyrie (eds.) NATO ASI Series, Series I: Global Environmental Change Vol. 17. Carbon Cycling in the Glacial Ocean; Constraints on the Ocean’s Role in Global Change; Quantitative Approaches in Paleoceanography. Springer Verlag: 281–306.

2. Altabet, M. A. & R. François, 1994. Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilization. Global Biogeochem. Cycles 8: 103–116.

3. Ariztegui, D., P. Farrimond & J. A. McKenzie, 1996a. Compositional variations in sedimentary lacustrine organic matter and their implications for high Alpine Holocene environmental changes; Lake St. Moritz, Switzerland. Org. Geochem. 24: 453–461.

4. Ariztegui, D., D. J. Hollander & J. A. McKenzie, 1996b. Algal dominated lacustrine organic matter can be either Type I or Type II: Evidence for biological, chemical and physical controls on organic matter quality. In Mello, M. R., L. A. F. Trindade & M. H. R. Hessel (eds.) ALAGO Special Publication: Selected Papers from 4th Latin American Congress on Organic Geochemistry. Bucaramanga, Columbia: 12–16.

5. Aucour, A.-M., C. Hillaire-Marcel & R. Bonnefille, 1993. A 30,000 year record of 13C and 18O changes in organic matter from an equatorial peatbog. In Swart, P. K., K.C. Lohmann, J. McKenzie & S. Savin (eds.) Climate Change in Continental Isotopic Records. Am. Geophys. Un. Geophys. Monogr. 78, Washington (DC): 343–351.

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