Sedimentary balance through geological time.

A. Lerman

doi:10.1007/978-3-642-68463-0_13

Sedimentary balance through geological time.

A. Lerman

Earth and Planetary Sciences

Research output: Contribution to journal › Article

2 Scopus citations

Abstract

Balance in the sedimentary cycle is maintained by the sum total of weathering, transport, deposition of sediments, and their eventual reincorporation in the continental crust. Biological activity and primarily photosynthesis strongly affect the fluxes and deposition of carbon, sulfur, iron, and phosphorus containing sediments. Changes in the net deposition rate of organic carbon produce changes in all the other fluxes within the cycle. -from Author

Original language	English (US)
Pages (from-to)	237-256
Number of pages	20
Journal	Unknown Journal
DOIs	https://doi.org/10.1007/978-3-642-68463-0_13
State	Published - Jan 1 1982

ASJC Scopus subject areas

Environmental Science(all)
Earth and Planetary Sciences(all)

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Lerman, A. (1982). Sedimentary balance through geological time. Unknown Journal, 237-256. https://doi.org/10.1007/978-3-642-68463-0_13

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