Contribution of aerobic photoheterotrophic bacteria to the carbon cycle in the ocean.

The vertical distribution of bacteriochlorophyll a, the numbers of infrared fluorescent cells, and the variable fluorescence signal at 880 nanometers wavelength, all indicate that photosynthetically competent anoxygenic phototrophic bacteria are abundant in the upper open ocean and comprise at least 11% of the total microbial community. These organisms are facultative photoheterotrophs, metabolizing organic carbon when available, but are capable of photosynthetic light utilization when organic carbon is scarce. They are globally distributed in the euphotic zone and represent a hitherto unrecognized component of the marine microbial community that appears to be critical to the cycling of both organic and inorganic carbon in the ocean.

Bacterial photosynthesis in surface waters of the open ocean.

The oxidation of the global ocean by cyanobacterial oxygenic photosynthesis, about 2,100 Myr ago, is presumed to have limited anoxygenic bacterial photosynthesis to oceanic regions that are both anoxic and illuminated. The discovery of oxygen-requiring photosynthetic bacteria about 20 years ago changed this notion, indicating that anoxygenic bacterial photosynthesis could persist under oxidizing conditions. However, the distribution of aerobic photosynthetic bacteria in the world oceans, their photosynthetic competence and their relationship to oxygenic photoautotrophs on global scales are unknown. Here we report the first biophysical evidence demonstrating that aerobic bacterial photosynthesis is widespread in tropical surface waters of the eastern Pacific Ocean and in temperate coastal waters of the northwestern Atlantic. Our results indicate that these organisms account for 2-5% of the photosynthetic electron transport in the upper ocean.

Comparison of approaches to the instrumental response function in fluorescence decay measurements.

Deconvolution of pulse fluorometry data requires knowledge of the instrumental response, which is not directly observable in some circumstances. Various procedures for approaching the instrumental response function were evaluated for nanosecond fluorescence decay data analyzed by nonlinear least squares, including the commonly used time shift correction and several reference fluorophore methods. A new reference fluorophore technique using a Monte Carlo convolution is introduced and tested. The correction for scattered light in several reference techniques is also presented. The random convolution and one other reference fluorophore method consistently gave superior results over a wide range of experimental conditions.