Record of archaeal activity at the serpentinite-hosted Lost City Hydrothermal Field.

Samples of young, outer surfaces of brucite-carbonate deposits from the ultramafic-hosted Lost City hydrothermal field were analyzed for DNA and lipid biomarker distributions and for carbon and hydrogen stable isotope compositions of the lipids. Methane-cycling archaeal communities, notably the Lost City Methanosarcinales (LCMS) phylotype, are specifically addressed. Lost City is unlike all other hydrothermal systems known to date and is characterized by metal- and CO2 -poor, high pH fluids with high H2 and CH4 contents resulting from serpentinization processes at depth. The archaeal fraction of the microbial community varies widely within the Lost City chimneys, from 1-81% and covaries with concentrations of hydrogen within the fluids. Archaeal lipids include isoprenoid glycerol di- and tetraethers and C25 and C30 isoprenoid hydrocarbons (pentamethylicosane derivatives - PMIs - and squalenoids). In particular, unsaturated PMIs and squalenoids, attributed to the LCMS archaea, were identified for the first time in the carbonate deposits at Lost City and probably record processes exclusively occurring at the surface of the chimneys. The carbon isotope compositions of PMIs and squalenoids are remarkably heterogeneous across samples and show highly (13) C-enriched signatures reaching δ(13) C values of up to +24.6‰. Unlike other environments in which similar structural and isotopic lipid heterogeneity has been observed and attributed to diversity in the archaeal assemblage, the lipids here appear to be synthesized solely by the LCMS. Some of the variations in lipid isotope signatures may, in part, be due to unusual isotopic fractionation during biosynthesis under extreme conditions. However, we argue that the diversity in archaeal abundances, lipid structure and carbon isotope composition rather reflects the ability of the LCMS archaeal biofilms to adapt to chemical gradients in the hydrothermal chimneys and possibly to perform either methanotrophy or methanogenesis using dissolved inorganic carbon, methane or formate as a function of the prevailing environmental conditions.

Did life originate from a global chemical reactor?

Many decades of experimental and theoretical research on the origin of life have yielded important discoveries regarding the chemical and physical conditions under which organic compounds can be synthesized and polymerized. However, such conditions often seem mutually exclusive, because they are rarely encountered in a single environmental setting. As such, no convincing models explain how living cells formed from abiotic constituents. Here, we propose a new approach that considers the origin of life within the global context of the Hadean Earth. We review previous ideas and synthesize them in four central hypotheses: (i) Multiple microenvironments contributed to the building blocks of life, and these niches were not necessarily inhabitable by the first organisms; (ii) Mineral catalysts were the backbone of prebiotic reaction networks that led to modern metabolism; (iii) Multiple local and global transport processes were essential for linking reactions occurring in separate locations; (iv) Global diversity and local selection of reactants and products provided mechanisms for the generation of most of the diverse building blocks necessary for life. We conclude that no single environmental setting can offer enough chemical and physical diversity for life to originate. Instead, any plausible model for the origin of life must acknowledge the geological complexity and diversity of the Hadean Earth. Future research may therefore benefit from identifying further linkages between organic precursors, minerals, and fluids in various environmental contexts.

The bld1 mutation identifies the Chlamydomonas osm-6 homolog as a gene required for flagellar assembly.

Insertional mutagenesis procedures in Chlamydomonas have facilitated the identification and characterization of dozens of genes required for the assembly and motility of flagella in Chlamydomonas. Many of these genes have been found to have homologs in animal systems. Here we describe a new gene required for flagellar assembly. Null mutants at the BLD1 locus assemble no flagella, and the flagellar membrane abuts the end of the transition zone distal to the basal body. Unlike mutants with basal body ultrastructural defects, such as bld2, bld1 mutants have normal basal bodies and cytoplasmic microtubule rootlets. The wild-type BLD1 gene was cloned by using DNA flanking the site of insertion of plasmid DNA in an insertional mutant; the cloned gene rescues the bld1 mutant phenotype upon transformation. The predicted BLD1 gene product is a 50.4 kDa protein with extensive regions of sequence similarity to the osm-6 gene of Caenorhabditis elegans whose product is necessary for the assembly of a set of sensory cilia. The protein product of the BLD1 gene corresponds to IFT52, a protein component of "raft" particles shown to undergo rapid transport up and down Chlamydomonas flagella between the flagellar membrane and the axoneme in a process known as intraflagellar transport (IFT). The BLD1 RNA transcript is upregulated upon flagellar amputation, as observed for many other genes encoding flagellar proteins. These results demonstrate that the function of the IFT52 protein in Chlamydomonas is essential for the assembly and/or maintenance of the flagella.