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Appl Environ Microbiol. 1980 October; 40(4): 735-740

Mineralization of Detrital Lignocelluloses by Salt Marsh Sediment Microflora

Department of Microbiology, University of Georgia, Athens, Georgia 30602

ABSTRACT

Specifically radiolabeled ¹⁴C-(cellulose)-lignocellulose and ¹⁴C-(lignin)-lignocellulose were isolated from labeled cuttings of Spartina alterniflora (cordgrass) and Pinus elliottii (slash pine). These were used to estimate the rates of mineralization to CO₂ of lignocelluloses of estuarine and terrestrial origin in salt marsh estuarine sediments. The lignin moiety of pine lignocellulose was mineralized 10 to 14 times more slowly than that of Spartina lignocellulose, depending on the source of inoculum. Average values for percent mineralization after 835 h of incubation were 1.4 and 13.9%, respectively. For Spartina lignocellulose, mineralization of the cellulose moiety was three times faster than that of the lignin moiety. Average values for percent mineralization after 720 h of incubation were 32.1 and 10.6%, respectively. Lignocellulose and lignin contents of live pine and Spartina plants were analyzed and found to be 60.7 and 20.9%, respectively, for pine and 75.6 and 15.1%, respectively, for Spartina.

Contribution no. 420 of the Marine Institute, University of Georgia, Sapelo Island, GA 31327.

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