Changes in carbon cycling under lowered sulfate conditions in hypersaline microbial mats as ascertained by stable carbon isotopes

Cheryl A. Kelley; Brad M. Bebout; Leslie E. Prufert-Bebout; Jason M. Smith

doi:10.1117/12.682000

14 September 2006 Changes in carbon cycling under lowered sulfate conditions in hypersaline microbial mats as ascertained by stable carbon isotopes

Cheryl A. Kelley, Brad M. Bebout, Leslie E. Prufert-Bebout, Jason M. Smith

Author Affiliations +

Proceedings Volume 6309, Instruments, Methods, and Missions for Astrobiology IX; 63090N (2006) https://doi.org/10.1117/12.682000
Event: SPIE Optics + Photonics, 2006, San Diego, California, United States

Abstract

The salinity and sulfate concentrations of microbial mats collected from hypersaline salterns were mainipulated to examine the effects of low sulfate concentrations and lowered salinity on carbon metabolism. As sulfate was slowly removed from the mats, methane production and flux increased, with highest fluxes and concentration in mats at lowered salinity (35 ppt) and low sulfate concentrations. The δ¹³C values of bulk particulate organic carbon (POC) ranged from about -10 to -12 &perthou;, similar to what had been observed previously for these cyanobacterial mats. In mats with higher sulfate concentrations, pore water profiles of dissolved inorganic carbon (DIC) δ¹³C values decreased with depth. However, in the mats with lowered sulfate, the DIC δ¹³C values increased substantially, from about -1 &perthou; in the overlying water to +12 &perthou; by 20 mm depth. Although the increase in DIC δ¹³C values is consistent with biogenic methanogenesis, the measured methane concentrations in these mats were not great enough to be the sole cause of the increase. These positive isotopic values, as well as the higher acetate concentrations observed in the low-sulfate mats, are also consistent with the occurrence of acetogenesis.

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Cheryl A. Kelley, Brad M. Bebout, Leslie E. Prufert-Bebout, and Jason M. Smith "Changes in carbon cycling under lowered sulfate conditions in hypersaline microbial mats as ascertained by stable carbon isotopes", Proc. SPIE 6309, Instruments, Methods, and Missions for Astrobiology IX, 63090N (14 September 2006); https://doi.org/10.1117/12.682000

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KEYWORDS

Digital image correlation

Methane

Carbon

Oxygen

Water

Photosynthesis

Oceanography

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