Accelerated Solvent Extractor Accelerated Solvent Extractor

The ASE extracts solid and semisolid samples with liquid solvents at elevated temperatures and pressures for increased efficiency.

Gas Chromatographs Gas Chromatographs

Gas chromatography is the main technique we use to separate out the individual components of very complex mixtures.

High Resolution Mass Spectrometer High Resolution Mass Spectrometer

The autospec combines the separating power of gas chromatography with the sensitivity of mass spectrometric detection.

Isotope Ratio Mass Spectrometer Isotope Ratio Mass Spectrometer

Stable isotope analysis for many different types of substances—organic matter, carbonates, gases and individual organic compounds.

Agilent 6000 Series HPLC-MS Agilent 6000 Series HPLC-MS

High Pressure Liquid Chromatography separates compounds, a Quadrupole Time-of-Flight mass spectrometer identifies lipids.

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Aliphatic and monocyclic saturated hydrocarbons in the molecular fossil record and their paleobiological interpretation

Biomarker Biological and/or environmental interpretation References
outstanding concentrations of n15, n17 and n19 in early Paleozoic rocks Gloeocapsomorpha prisca, marine phytoplankton of uncertain affinity, probably an alga, identified in Cambrian-Devonian sediments but most prominent in Ordovician. Estonian kukersite is a typical source Blokker et al., 2001, Fowler, 1992
n-C27 with OEP1 waxes derived from higher plants, terrestrial input, post-Silurian age Hedberg, 1968, Tissot and Welte, 1984
n-C40 predominantly degradation products of aliphatic macromolecules such as algaenan (marine, lacustrine), cutan and suberan (terrestrial, plant derived) Allard et al., 2002, Killops et al., 2000
Branched alkanes and acyclic isoprenoids
monomethylalkanes and dimethylalkanes (MMA and DMA) cyanobacteria both cultured and in mat communities from hypersaline and hydrothermal environments Dembitsky et al., 2001, Kenig et al., 1995b, Koster et al., 1999, Shiea et al., 1990
5, 5-diethylalkanes with OEP1 (wrongly reported as 3, 7- or 3,w7-dimethyllkanes) these structures widely and incorrectly assigned. Chemical synthesis of a 5, 5-diethylalkane indicates this is a major series. Often occurs with other alkanes with quaternary carbon centers (BAQCs). Source organisms not known but commonly found in association with benthic microbial mats. Arouri et al., 2000a, Arouri et al., 2000b, Kenig et al., 2002, Logan et al., 1999, Logan et al., 2001, Simons et al., 2002
pristane (Pr) and phytane (Ph) from chlorophylls of cyanobacteria, algae and plants, bacteriochlorophylls a and b of phototrophic bacteria, tocopherols, Ph: archaeal membrane lipids Peters and Moldowan, 1993
regular acyclic isoprenoids i-21 to i-30 probable source is halophilic Archaea, abundant in evaporitic environments Grice et al., 1998b
squalane (tail-tail C30 acyclic isoprenoid) all organisms produce some squalene, most sedimentary squalane probably from Archaea. Grice et al., 1998b
crocetane archaea (anaerobic methane oxidizers), associated with sub-sea gas, gas hydrate and mud volcanoes Bian et al., 2001, Thiel et al., 1999
PMI (2,6,10,15,19-pentamethylicosane) methanogenic and methanotrophic archaea Elvert et al., 1999, Schouten et al., 1997, Thiel et al., 1999
TMI (2,6,15,19-tetramethylicosane) only reported from a mid-Cretaceous oceanic anoxic event, nonhyperthermophilic marine Crenarchaeota? Kuypers et al., 2001
C20, C25, C30 and C35 highly branched isoprenoids unsaturated and polyunsaturated isoprenoid hydrocarbons are prominent biochemicals in some diatom taxa such as Rhizoselenia and Haslea Sinninghe Damste et al., 1999a, Volkman et al., 1994, Belt et al., 2000, Rowland et al., 2001
botryococcenes and botryococcanes, cyclobotryococcenes, polymethylsqualenes the unsaturated, sometimes cyclic, biogenic hydrocarbons and their saturated fossil counterparts are diagnostic markers of the chlorophyte B. braunii and their preferred habitat of fresh to brackish water. Huang et al., 1988, Metzger and Largeau, 1999, Summons et al., 2002
Monocyclic saturated hydrocarbons
C42 – C46 cyclopentylalkanes with OEP1 oils from marine environments, unknown biological source Carlson et al., 1993, Hsieh and Philp, 2001
C42 – C46 cyclopentylalkanes with no distinct carbon preference oils from freshwater lacustrine settings, unknown biological source same as above
C42 – C46 cyclopentylalkanes with strong EOP2 oils from saline lacustrine settings, unknown biological source same as above
cyclohexyl alkanes without predominance formed during pyrolysis of biopolymers with long aliphatic carbon chains suggesting an origin from acyclic polymethylenic precursors Gelin et al., 1994
macrocyclic alkanes C15-C34 without preference bitumens extracted from torbanites containing remains of B. braunii, fresh to brackish water Audino et al., 2002

1 Odd-over-even carbon number preference

2 Even-over-odd carbon number preference

Chart adapted from Treatise on Geochemistry Review, Chapter 8, Summons and Brocks