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Applied Biosystems - Cells to CT

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Science 6 July 2001:
Vol. 293. no. 5527, pp. 92 - 95
DOI: 10.1126/science.1058424


Abstract
Full Text
Massive Expansion of Marine Archaea During a Mid-Cretaceous Oceanic Anoxic Event
Marcel M. M. Kuypers, Peter Blokker, Jochen Erbacher, Hanno Kinkel, Richard D. Pancost, Stefan Schouten, and Jaap S. Sinninghe Damsté

Supplementary Material

Supplemental Table 1. Source organisms, inferred biochemical precursor, isotopic composition and mode of occurrence of C skeletons encountered in the sediment. Carbon skeletons are shown in Fig. 1. Carbon skeletons occur in the following modes: free hydrocarbons (free), macromolecularly S-bound moiety (S-bd), alcohols (Alc.) and ether-bound moiety (E-bd). The range of measured stable carbon isotopic values for individual components is indicated. Abbreviations are isopr., isoprenoid alkanes; 1cycl., mono cyclic; Funct., functionalised; unsat., unsaturated; Heterotr., heterotrophic bacteria; cyanobact., cyanobacteria.
Source organismBiochemical
Precursor
C skeletonModedelta13C
(‰)
Higher plantsn-C27n-C27Free-27.7 to -28.9
n-C31n-C31Free-27.7 to -28.0
Algae/higher plants24-ethyl-cholesterolsC29 sterane (VIII)Alc.-25.1 to -30.2
Algae24-methyl-cholesterolsC28 sterane Alc.-27.0 to -29.2
Algae/zooplanktonSterolsC27 sterane (VII)Alc.-23.9 to -28.5
Algae/cyanobact.Chlorophyll Phytane (IX)Alc.-27.2 to -29.5
Heterotr./cyanobact.BacteriohopanepolyolsC29hopane Free-23.7 to -24.9
BacteriohopanepolyolsC31hopane Free-26.1 to -27.0
Archaea/bacteriaSqualane/squaleneSqualane Free-17.6 to -23.4
ArchaeaGDGTs (III, IV)C40: 1 cycl.(b)E-bd/alc.-17.6 to -20.0
GDGTs (V)C40: 2 cycl.(c)E-bd/alc.-17.1 to -18.4
GDGTs (VI)C40: 3 cycl.(d)E-bd/alc.-17.3 to -18.3
Archaeol Phytane (IX)E-bd.-17.7
PMI (II)/unsat. PMIPMI (II)Free-16.5 to -21.2
UnknownTMI (I)Free-16.2 to -16.7
Funct. TMI/PMI TMI/PMIE-bd-13.1 to -15.0





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