The Guaymas Basin Subseafloor Sedimentary Archaeome Reflects Complex Environmental Histories

Abstract

We explore archaeal distribution and environmental niche differentiation in sedimentary subseafloor habitats of Guaymas Basin and the adjacent Sonora Margin, located in the Gulf of California, México. Specifically, we survey diverse subseafloor habitats on the Guaymas Basin flanking regions that are extending from the spreading center, termed here “off-axis” sites. Sampling locations include (i) control sediments without hydrothermal or seep influence, (ii) Sonora Margin sediments underlying oxygen minimum zone water, (iii) compacted, highly reduced sediments from a pressure ridge with numerous seeps at the base of the Sonora Margin, and (iv) sediments impacted by hydrothermal circulation at the off-axis Ringvent site. Generally, archaeal 16S rRNA gene datasets are largely comprised of Bathyarchaeal lineages, members of the Hadesarchaea, MBG-D, TMEG, and ANME-1 groups. The most frequently observed 25 OTUs belong to members of these lineages, and correspond to approx. 40 to 80% of the sequence dataset in each sediment sample. Differential distribution patterns of these archaeal groups in downcore sediments uniquely characterize each major sedimentary environment. Variations in archaeal community composition reflect locally specific environmental challenges throughout the greater Guaymas Basin area. Background sediments are divided into surface and subsurface niches, reflecting increased selection of the archaeal community downcore. In sum, the environmental setting and history of a particular site, not isolated biogeochemical properties out of context, control the subseafloor archaeal communities in Guaymas Basin and Sonora Margin sediments.