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Spatial variability in photosynthetic and heterotrophic activity drives localized δ 13 C org fluctuations and carbonate precipitation in hypersaline microbial mats
Author(s) -
Houghton J.,
Fike D.,
Druschel G.,
Orphan V.,
Hoehler T. M.,
Des Marais D. J.
Publication year - 2014
Publication title -
geobiology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.859
H-Index - 72
eISSN - 1472-4669
pISSN - 1472-4677
DOI - 10.1111/gbi.12113
Subject(s) - microbial mat , anoxygenic photosynthesis , carbonate , phototroph , photic zone , environmental chemistry , cyanobacteria , photosynthesis , carbon cycle , chemocline , carbon fixation , sulfate , geology , chemistry , botany , anoxic waters , ecology , biology , bacteria , nutrient , phytoplankton , ecosystem , paleontology , organic chemistry
Modern laminated photosynthetic microbial mats are ideal environments to study how microbial activity creates and modifies carbon and sulfur isotopic signatures prior to lithification. Laminated microbial mats from a hypersaline lagoon (Guerrero Negro, Baja California, Mexico) maintained in a flume in a greenhouse at NASA Ames Research Center were sampled for δ 13 C of organic material and carbonate to assess the impact of carbon fixation (e.g., photosynthesis) and decomposition (e.g., bacterial respiration) on δ 13 C signatures. In the photic zone, the δ 13 C org signature records a complex relationship between the activities of cyanobacteria under variable conditions of CO 2 limitation with a significant contribution from green sulfur bacteria using the reductive TCA cycle for carbon fixation. Carbonate is present in some layers of the mat, associated with high concentrations of bacteriochlorophyll e (characteristic of green sulfur bacteria) and exhibits δ 13 C signatures similar to DIC in the overlying water column (−2.0‰), with small but variable decreases consistent with localized heterotrophic activity from sulfate‐reducing bacteria (SRB). Model results indicate respiration rates in the upper 12 mm of the mat alter in situ pH and HCO 3 − concentrations to create both phototrophic CO 2 limitation and carbonate supersaturation, leading to local precipitation of carbonate minerals. The measured activity of SRB with depth suggests they variably contribute to decomposition in the mat dependent on organic substrate concentrations. Millimeter‐scale variability in the δ 13 C org signature beneath the photic zone in the mat is a result of shifting dominance between cyanobacteria and green sulfur bacteria with the aggregate signature overprinted by heterotrophic reworking by SRB and methanogens. These observations highlight the impact of sedimentary microbial processes on δ 13 C org signatures; these processes need to be considered when attempting to relate observed isotopic signatures in ancient sedimentary strata to conditions in the overlying water column at the time of deposition and associated inferences about carbon cycling.