Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
Infobox references
Chemical compound
Chlorobactane is the diagenetic product of an aromatic carotenoid produced uniquely by green-pigmented green sulfur bacteria (GSB) in the order Chlorobiales.[1] Observed in organic matter as far back as the Paleoproterozoic, its identity as a diagnostic biomarker has been used to interpret ancient environments.[2][3]
^Summons, R.E.; Powell, T.G. (1987). “Identification of aryl isoprenoids in source rocks and crude oils: Biological markers for the green sulphur bacteria”. Geochimica et Cosmochimica Acta. 51: 557 – 566.
^Brocks, J. J.; Love, G. D.; Summons, R. E.; Knoll, A. H.; Logan, G. A.; Bowden, S. A. (2005). "Biomarker evidence for green and purple sulphur bacteria in a stratified Palaeoproterozoic sea". Nature. 437 (7060): 866–70. Bibcode:2005Natur.437..866B. doi:10.1038/nature04068. PMID 16208367. S2CID 4427285.
^French, K. L.; Rocher, D.; Zumberge, J. E.; Summons, R. E. (2015). "Assessing the distribution of sedimentary C40carotenoids through time". Geobiology. 13 (2): 139–151. Bibcode:2015Gbio...13..139F. doi:10.1111/gbi.12126. PMID 25631735. S2CID 22535663.
Chlorobactane is the diagenetic product of an aromatic carotenoid produced uniquely by green-pigmented green sulfur bacteria (GSB) in the order Chlorobiales...
The molecular formula C40H74 (molar mass: 555.03 g/mol) may refer to: Chlorobactane, a bio-marker for green sulphur bacteria Okenane, a bio-marker for purple...
oxic to anoxic transition as well as confine past ecology. Okenane and chlorobactane discovered in Australian Paleoproterozoic samples allowed conclusions...
pigments used to identify past presence of green sulfur bacteria are chlorobactane and isorenieratene. The pigments used to identify past presence of purple...