TY - JOUR
T1 - Sedimentary balance through geological time.
AU - Lerman, A.
PY - 1982/1/1
Y1 - 1982/1/1
N2 - 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
AB - 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
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U2 - 10.1007/978-3-642-68463-0_13
DO - 10.1007/978-3-642-68463-0_13
M3 - Article
AN - SCOPUS:0019925668
SP - 237
EP - 256
JO - Free Radical Biology and Medicine
JF - Free Radical Biology and Medicine
SN - 0891-5849
ER -