Published October 2012 | Version Supplemental Material
Journal Article Open

^2H/^1H ratio of hopanes, tricyclic and tetracyclic terpanes in oils and source rocks from the Potiguar Basin, Brazil

  • 1. ROR icon Federal University of Rio de Janeiro
  • 2. ROR icon Petrobras (Brazil)
  • 3. ROR icon California Institute of Technology
  • 4. ROR icon Indiana University Bloomington

Abstract

We report the hydrogen isotope ratio ^2H/^1H (expressed as δ^2H values) of 8 selected hopanes, tricyclic and tetracyclic terpanes from oils and source rocks in the Potiguar Basin, and of associated formation water. Hopanes ranged in δ^2H value from −79‰ to −142‰, whereas tri- and tetracyclic terpanes (TTTs) ranged from −137‰ to −225‰. Formation water δ^2H values ranged from −23‰ to −32‰. The most significant pattern in the data is the systematic ^2H enrichment of hopanes relative to TTTs, by an average of 45‰ in oils and 78‰ in source rock extracts. The hopanes appear close to hydrogen isotopic equilibrium with coeval formation water, whereas TTTs are significantly more ^2H depleted. Given the similarities in structure between the two compound classes, it is unlikely that hopanes would be exchanged completely while the others would not. More likely, both classes have undergone a limited extent of exchange, but with the hopanes being biosynthesized with δ^2H values closer to equilibrium. Our data suggest that at least some primary environmental and/or biotic information can be retained in the δ^2H values of biomarkers in oils and extracts, and is not completely obscured by hydrogen exchange.

Additional Information

© 2012 Elsevier Ltd. Received 16 February 2012. Received in revised form 21 July 2012. Accepted 22 July 2012. Available online 1 August 2012. Associate Editor—K. Grice. We thank L. Zhang for assistance with compound-specific ^2H measurements, P. Velloso and R. Marins for generation and improvements of the images, and PETROBRAS for permission to publish the results of this investigation. The manuscript greatly benefited from constructive reviews by C. Eiserbeck and D. Dawson. A.L.S. was supported by NSF Grant EAR-0645502 and A.S. was funded by U.S. Department of Energy, Basic Energy Research Grant DEFG02-00ER15032.

Attached Files

Supplemental Material - http___dx.doi.org_10.1016_j.orggeochem.2012.07.007_1-s2.0-S0146638012001519-fx1.jpg.ppt

Supplemental Material - mmc1.doc

Supplemental Material - mmc2.doc

Supplemental Material - mmc3.doc

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Additional details

Identifiers

Eprint ID
35518
Resolver ID
CaltechAUTHORS:20121116-131754394

Funding

NSF
EAR-0645502
Department of Energy (DOE)
DE-FG02-00ER15032

Dates

Created
2012-11-16
Created from EPrint's datestamp field
Updated
2021-11-09
Created from EPrint's last_modified field

Caltech Custom Metadata

Caltech groups
Division of Geological and Planetary Sciences (GPS)