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Items: 6

1.

1.1-billion-year-old porphyrins establish a marine ecosystem dominated by bacterial primary producers.

Gueneli N, McKenna AM, Ohkouchi N, Boreham CJ, Beghin J, Javaux EJ, Brocks JJ.

Proc Natl Acad Sci U S A. 2018 Jul 24;115(30):E6978-E6986. doi: 10.1073/pnas.1803866115. Epub 2018 Jul 9.

PMID:
29987033
2.

Microstructural evolution of source rocks during hydrocarbon generation: A small-angle-scattering study.

Radlinski AP, Boreham CJ, Wignall GD, Lin J.

Phys Rev B Condens Matter. 1996 Jun 1;53(21):14152-14160. No abstract available.

PMID:
9983210
3.

The effect of aromatization on the isotopic compositions of hydrocarbons during early diagenesis.

Freeman KH, Boreham CJ, Summons RE, Hayes JM.

Org Geochem. 1994;21(10-11):1037-49.

PMID:
11539437
4.

Microscale determination of the spectral characteristics and carbon-isotopic compositions of porphyrins.

Popp BN, Hayes JM, Boreham CJ.

Energy Fuels. 1993 Mar-Apr;7(2):185-90.

PMID:
11543593
5.

Origin of petroporphyrins. 2. Evidence from stable carbon isotopes.

Boreham CJ, Fookes CJ, Popp BN, Hayes JM.

Energy Fuels. 1990;4(6):658-61.

PMID:
11538479
6.

Origins of etioporphyrins in sediments: evidence from stable carbon isotopes.

Boreham CJ, Fookes CJ, Popp BN, Hayes JM.

Geochim Cosmochim Acta. 1989;53:2451-5.

PMID:
11539780

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