Stable sulfur isotopic distributions and sulfate reduction in lake sediments of the Adirondack Mountains, New York

Author:

Fry Brian

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Water Science and Technology,Environmental Chemistry

Reference42 articles.

1. Aller RC 1980. Diagenetic processes near the sediment-water interface of Long Island Sound. I. Decomposition and nutrient element geochemistry (S,N,P). Advances in Geophysics 22:237–350.

2. Chambers LA and PA Trudinger 1979. Microbiological fractionation of stable sulfur isotopes. Geomicrobiology Journal 1:249–293.

3. Charles DF 1982. Studies of Adirondack Mountain (N.Y.) lakes: Limnological characteristics and sediment diatom-water chemistry relationships. Ph.D. dissertation, Indiana Univ., Bloomington, Indiana. 428 pp.

4. Charles DF 1984. Recent pH history of Big Moose Lake (Adirondack Mountains, New York, U.S.A.) inferred from sediment diatom assemblages. Internationale Vereinigung fuer theoretische and angewandte Limnologie, Verhandlungen 22:559–566.

5. Charles DF, DR Whitehead, DR Engstrom, B Fry, RA Hites, SA Norton, J Owen, L Roll, S Schindler, JP Smol, A Uutala, J White and RJ Wise. In press. Paleolimnological evidence for recent acidification of Big Moose L., Adirondack Mountains, N.Y. (U.S.A.). Biogeochemistry.

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