Biological Origins
299
Stedmon C.A, Markager, S., Søndergaard, M., Vang, T., Laubel, A., Borch, N.H., and
Windelin, A. (2006). Dissolved organic matter (DOM) export to a temperate estuary:
Seasonal variations and implications of land use. Estuaries Coasts, 29, 388–400.
Stevensen, F.J. (1982). Biochemistry of the Formation of Humic Substances. In F.J.
Stevensen (Ed.), Humus Chemistry (pp. 195–220). New York: John Wiley & Sons.
Strom, S.L., Benner, R., Ziegler, S., and Dagg, M.J. (1997). Planktonic grazers are a potentially important source of marine dissolved organic carbon. Limnol. Oceanogr., 42,
1364–1374.
Tipping, E., Woof, C., Rigg, E., Harrison, A.F., Ineson, P., Taylor, K., Benham, D., Poskitt,
J., Rowland, A.P., Bol, R., and Harkness, D.D. (1999). Climatic influences on the
leaching of dissolved organic matter from upland UK moorland soils, investigated by
a field manipulation experiment. Environ. Int., 25, 83–95.
Tranvik, L. and Kokalj, S. (1998). Decreased biodegradability of algal DOC due to interactive effects of UV radiation and humic matter. Aquat. Microb. Ecol., 14, 301–307.
Tranvik, L.J. and Bertilsson, S. (2001). Contrasting effects of solar UV radiation on dissolved organic sources for bacterial growth. Ecol. Lett., 4, 458–463.
Tranvik, L.J., Downing, J., and Cotner, J. (2009). Lakes and reservoirs as regulators of
carbon cycling and climate. Limnol. Oceanogr., 54(1), 2298–2314.
Urban-Rich, J., McCarty, J.T., and Shailer, M. (2004). Effects of food concentration and
diet on chromophoric dissolved organic matter accumulation and fluorescent composition during grazing experiments with the copepod, Calanus finmarchicus. ICES J.
Mar. Sci., 61, 542–551.
Vähätalo, A.V. and Wetzel, R.G.. (2004). Photochemical and microbial decomposition of
chromophoric dissolved organic matter during long (months-years) exposures. Mar.
Chem., 89, 313–326.
Vähätalo, A.V. and Wetzel, R.G. (2008). Long-term photochemical and microbial decomposition of wetland-derived dissolved organic matter with alteration of C-13: C-12
mass ratio. Limnol. Oceanogr., 53, 1387–1392.
Yamamoto, S. and Ishiwatari, R. (1989). A study of the formation mechanism of sedimentary humic substances-II. Protein-based melanoidin model. Org. Geochem., 14,
479–489.
Yamashita, Y. and Tanoue, E. (2003). Chemical characterization of protein-like fluorophores in DOM in relation to aromatic amino acids. Mar. Chem., 82, 255–271.
Yamashita, Y. and Tanoue, E. (2004). In situ production of chromophoric dissolved organic
matter in coastal environments. Geophys. Res. Lett., doi: 10.1029/2004GL019734.
Yamashita, Y. and Tanoue, E. (2008). Production of bio-refractory fluorescent dissolved
organic matter in the ocean interior. Nature Geosci., 1, 579–582, doi:10.1038/
ngeo279.
Zsolnay, A. (2003). Dissolved organic matter: Artefacts, definitions, and functions.
Geoderma, 113, 187–209.
Zsolnay, A., Baigar, E., Jimenez, M., Steinweg, B., and Saccomandi, F. (1999).
Differentiating with fluorescence spectroscopy the sources of dissolved organic matter in soils subjected to drying. Chemosphere, 38, 45–50.
299
Stedmon C.A, Markager, S., Søndergaard, M., Vang, T., Laubel, A., Borch, N.H., and
Windelin, A. (2006). Dissolved organic matter (DOM) export to a temperate estuary:
Seasonal variations and implications of land use. Estuaries Coasts, 29, 388–400.
Stevensen, F.J. (1982). Biochemistry of the Formation of Humic Substances. In F.J.
Stevensen (Ed.), Humus Chemistry (pp. 195–220). New York: John Wiley & Sons.
Strom, S.L., Benner, R., Ziegler, S., and Dagg, M.J. (1997). Planktonic grazers are a potentially important source of marine dissolved organic carbon. Limnol. Oceanogr., 42,
1364–1374.
Tipping, E., Woof, C., Rigg, E., Harrison, A.F., Ineson, P., Taylor, K., Benham, D., Poskitt,
J., Rowland, A.P., Bol, R., and Harkness, D.D. (1999). Climatic influences on the
leaching of dissolved organic matter from upland UK moorland soils, investigated by
a field manipulation experiment. Environ. Int., 25, 83–95.
Tranvik, L. and Kokalj, S. (1998). Decreased biodegradability of algal DOC due to interactive effects of UV radiation and humic matter. Aquat. Microb. Ecol., 14, 301–307.
Tranvik, L.J. and Bertilsson, S. (2001). Contrasting effects of solar UV radiation on dissolved organic sources for bacterial growth. Ecol. Lett., 4, 458–463.
Tranvik, L.J., Downing, J., and Cotner, J. (2009). Lakes and reservoirs as regulators of
carbon cycling and climate. Limnol. Oceanogr., 54(1), 2298–2314.
Urban-Rich, J., McCarty, J.T., and Shailer, M. (2004). Effects of food concentration and
diet on chromophoric dissolved organic matter accumulation and fluorescent composition during grazing experiments with the copepod, Calanus finmarchicus. ICES J.
Mar. Sci., 61, 542–551.
Vähätalo, A.V. and Wetzel, R.G.. (2004). Photochemical and microbial decomposition of
chromophoric dissolved organic matter during long (months-years) exposures. Mar.
Chem., 89, 313–326.
Vähätalo, A.V. and Wetzel, R.G. (2008). Long-term photochemical and microbial decomposition of wetland-derived dissolved organic matter with alteration of C-13: C-12
mass ratio. Limnol. Oceanogr., 53, 1387–1392.
Yamamoto, S. and Ishiwatari, R. (1989). A study of the formation mechanism of sedimentary humic substances-II. Protein-based melanoidin model. Org. Geochem., 14,
479–489.
Yamashita, Y. and Tanoue, E. (2003). Chemical characterization of protein-like fluorophores in DOM in relation to aromatic amino acids. Mar. Chem., 82, 255–271.
Yamashita, Y. and Tanoue, E. (2004). In situ production of chromophoric dissolved organic
matter in coastal environments. Geophys. Res. Lett., doi: 10.1029/2004GL019734.
Yamashita, Y. and Tanoue, E. (2008). Production of bio-refractory fluorescent dissolved
organic matter in the ocean interior. Nature Geosci., 1, 579–582, doi:10.1038/
ngeo279.
Zsolnay, A. (2003). Dissolved organic matter: Artefacts, definitions, and functions.
Geoderma, 113, 187–209.
Zsolnay, A., Baigar, E., Jimenez, M., Steinweg, B., and Saccomandi, F. (1999).
Differentiating with fluorescence spectroscopy the sources of dissolved organic matter in soils subjected to drying. Chemosphere, 38, 45–50.