Aspects of the biogeochemistry of methane in Mono Lake and the Mono Basin of California

By: , and 
Edited by: R. Oremland



Above-ambient levels of methane and higher hydrocarbons were detected in the atmosphere of the Mono Basin. These gases emanated from several different sources, including natural gas seeps (thermogenic and biogenic), and methanogenic activity in sediments. Seeps were distributed over nearly 33% of the lake bottom and were also present in the exposed former lakebed. They originated from one or more natural gas deposits that underlie the basin. Seeps associated with hot springs had a thermogenic character, whereas the others had the characteristics of bacterially formed gases. The radiocarbon content of methane in all seep gases was low (5-11% modern carbon), indicating an age of greater than about 20,000 years.

Dissolved methane increased with depth in the sediments, ultimately reaching saturation levels (1-3 mM). The outward diffusive flux of methane into the anoxic bottom waters elevated concentrations to 60 µM during the 1984-1988 meromictic interval. The radiocarbon content of hypolimnion methane was equivalent to that of the dissolved inorganic carbon (~80% modern carbon), indicating derivation from current methanogenic activity. Oxidation by anaerobic bacteria was the major sink for this methane. Methane that escaped oxidation transited to the epilimnion where it attained supersaturation (0.1-3.0 µM) relative to the atmosphere. Measured outward fluxes over a 2-year period were highly variable, ranging from 0.01 to 4.82 mmoles CH4 m-2 d-1.

Bacterial activity was detected in the sediments of the hypolimnion High rates of sulfate reduction (~200 µmoles L-1 d-1) were measured in the upper 5-cm interval but decreased > 10-fold with depth. The highest rate of methanogenic activity was ~1 µmole L-1 d-1, as measured by reduction of 14CO2. Bacteria metabolized dimethylsulfide, trimethylamine, acetate, and glucose to primarily CO2 and some CH4. Turnovers of glucose (k = 0.16 d-1) and trimethylamine (k =0.09 d-1) were highest in the upper 2.5-cm interval and decreased as much as 10-fold with depth. These results confirm that a low rate of methanogenic activity occurs in this extreme environment and is the source of methane to the hypolimnion.

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Additional publication details

Publication type Book chapter
Publication Subtype Book Chapter
Title Aspects of the biogeochemistry of methane in Mono Lake and the Mono Basin of California
DOI 10.1007/978-1-4615-2812-8_39
Year Published 1993
Language English
Publisher Chapman and Hall
Publisher location New York
Contributing office(s) National Research Program - Western Branch, Toxic Substances Hydrology Program, National Research Program - Central Branch
Description 38 p.
Larger Work Type Book
Larger Work Title Aspects of the biogeochemistry of methane in Mono Lake and the Mono Basin of California
First page 704
Last page 741
Country United States
State California
Other Geospatial Mono Lake
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