A pseudohomologous series of branched aliphatic alkanes with a quaternary substituted carbon atom (BAQCs, specifically 2,2-dimethylalkanes and 3,3-and 5,5-diethylalkanes) were identified in warm (65°C) deep-sea hydrothermal waters and Late Cretaceous black shales. 5,5-Diethylalkanes were also observed in modern and Holocene marine shelf sediments and in shales spanning the last 800 million years of the geological record. The carbon number distribution of BAQCs indicates a biological origin. These compounds were observed but not identified in previous studies of 2.0 billion-to 2.2 billion-year-old metasediments and were commonly misidentified in other sediment samples, indicating that BAQCs are widespread in the geological record. The source organisms of BAQCs are unknown, but their paleobiogeographic distribution suggests that they have an affinity for sulfides and might be nonphotosynthetic sulfide oxidizers. P rokaryotes in ancient environments usually are detected by microscopy (1, 2) and geochemical evidence (e.g., stable isotope fractionation of carbon and sulfur; ref.3). The fossil record of bacteria and archaea is meager and controversial because of their poor preservation potential (1, 4). However, some lipids have excellent preservation potential and are used to demonstrate the presence of archaea and bacteria in ancient sedimentary environments (2, 5-9). Here we identify branched aliphatic alkanes with quaternary substituted carbon atoms (BAQCs). These compounds, observed in hydrothermal waters at the Ocean Drilling Project (ODP) site 1026B on the flanks of the Juan de Fuca ridge (Northeast Pacific) are natural products and occur in nonhydrothermal sediments ranging in age from modern to at least 2.0 billion to 2.2 billion years (Ga).
MethodsField Sampling. Particulate organic material was retrieved from hydrothermal waters by using a combusted glass-fiber filter (142 mm) affixed to a circulation obviation retrofit kit (10) The Cenomanian and Turonian (Late Cretaceous) samples were collected at outcrops along the Bainbridge river in the Pasquia Hills region of easternmost central Saskatchewan, Canada (12). They are thermally immature based on the dominant 17,21(H) stereochemical configuration of the hopanes. The descriptions of other sediment samples analyzed can be found in the references listed in the Fig. 3 legend. Laboratory Methods. Extraction, separation, and GC-MS were performed as described (13). The filter and sediment samples were Soxhlet-extracted by using dichloromethane and methanol (7.5:1, vol͞vol). The sediment extracts were further separated by column chromatography to obtain a hydrocarbon fraction. Linear alkanes were removed from the hydrocarbon fraction by adduction on US-Y zeolite to obtain a fraction of branched and cyclic hydrocarbons. The total extract and subfractions, as well as authentic standards, were analyzed by GC-MS on a HewlettPackard 6890 gas chromatograph coupled to a Hewlett-Packard 5973 mass selective detector operated in electron ionization mode at 70 eV, scannin...