Marine sediments cover more than two thirds of the Earth’s surface and have been estimated to contain as much as one-third of Earth’s prokaryotic biomass (Whitman et al., 1998). Despite this, relatively little is known about this deep biosphere, and essentially nothing is known about the presence of microbial eukaryotes in sediments deeper than a few centimeters. Through consumption of dissolved organic matter and by selective grazing in subsurface horizons where bacterial and/or archaeal numbers are high, protists and fungi may significantly impact carbon cycling in the marine subsurface.
The first analyses of eukaryotic small subunit ribosomal RNA gene (18S rRNA) sequences obtained from deep marine subsurface sediments, the first metagenome, and a cultivation study based on those samples show that fungi dominate eukaryotic life in the buried marine subsurface. Novel fungi continue to be reported from deep marine environments, and and there is fossil evidence of filamentous structures highly suggestive of fungi within carbonate-filled vesicles within the upper oceanic crust. In collaboration with J. Biddle at U.Del and A. Teske at UNC Chapel Hill, our group is using RNA-based approaches to investigate microbial eukaryote (protist and fungi) communities in deep subsurface samples from around the globe to determine whether fungi dominate the eukaryotic communities in all deep subsurface samples. We also are interested in what types of genes they are expressing in situ.