Biomarkers in Cretaceous sedimentary rocks from the Codó Formation - Parnaíba Basin: Paleoenvironmental assessment

Earlier geological works showed that Codó Formation - CF (Parnaíba Basin, Brazil) has been deposited in the Aptian, and suffered the influence of various transgressive-regressive marine cycles, thus suggesting various depositional environment possibilities from saline lacustrine deltaic to shallow m...

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Published in:Journal of South American earth sciences Vol. 92; pp. 265 - 281
Main Authors: da S. Sousa, Edymilaís, Júnior, Gustavo R.Sousa, Silva, Andrenilton F., de A. M. Reis, Francisco, de Sousa, Alek A.C., Cioccari, Giovani M., Capilla, Ramsés, de Souza, Igor V.A.F., Imamura, Paulo M., Rodrigues, Rene, Lopes, José A.D., de Lima, Sidney G.
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Language:English
Published: Elsevier Ltd 01-06-2019
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Abstract Earlier geological works showed that Codó Formation - CF (Parnaíba Basin, Brazil) has been deposited in the Aptian, and suffered the influence of various transgressive-regressive marine cycles, thus suggesting various depositional environment possibilities from saline lacustrine deltaic to shallow marine during sedimentation. Cretaceous potential source rock samples from the CF were investigated to identify diagnostic biomarkers in order to ascertain paleoenvironmental conditions of deposition and thermal evolution of organic matter. The TOC results showed low organic matter (OM) contents and Rock-Eval analysis implying low thermal evolution of organic matter. GC-MS analysis showed a great diversity of biomarkers within the five studied samples. The main features of organic matter composition were: low content of n-alkanes, Ph » Pr, presence of i-25, i-30 (squalane) and gammacerane thus suggesting saline to hypersaline depositional environment. The biomarkers fingerprint showed a full series of ββ hopanes and Δ13(18) hopenes, αααR and βααR steranes, and Δ5 and Δ8(14) sterenes, pointing out immature OM. Several C30 steranes have been detected, among them 4α(methyl)- and 4β(methyl)-24-ethylcholestane, 24-n-propylcholestane and 24-isopropylcholestane (all identified by co-injection) and dinosteranes, which some of them are indicative of a marine depositional system. •Cretaceous potential source rock samples from the Codó Formation (Parnaíba Basin, Brazil).•C30 sterane biomarker: 24-n-propylcholestane and 24-isopropylcholestane.•Indicators of maturity and depositional paleoenvironment.•Evidences of anoxia during the deposition of sediments in Parnaíba Basin.
AbstractList Earlier geological works showed that Codó Formation - CF (Parnaíba Basin, Brazil) has been deposited in the Aptian, and suffered the influence of various transgressive-regressive marine cycles, thus suggesting various depositional environment possibilities from saline lacustrine deltaic to shallow marine during sedimentation. Cretaceous potential source rock samples from the CF were investigated to identify diagnostic biomarkers in order to ascertain paleoenvironmental conditions of deposition and thermal evolution of organic matter. The TOC results showed low organic matter (OM) contents and Rock-Eval analysis implying low thermal evolution of organic matter. GC-MS analysis showed a great diversity of biomarkers within the five studied samples. The main features of organic matter composition were: low content of n-alkanes, Ph » Pr, presence of i-25, i-30 (squalane) and gammacerane thus suggesting saline to hypersaline depositional environment. The biomarkers fingerprint showed a full series of ββ hopanes and Δ13(18) hopenes, αααR and βααR steranes, and Δ5 and Δ8(14) sterenes, pointing out immature OM. Several C30 steranes have been detected, among them 4α(methyl)- and 4β(methyl)-24-ethylcholestane, 24-n-propylcholestane and 24-isopropylcholestane (all identified by co-injection) and dinosteranes, which some of them are indicative of a marine depositional system. •Cretaceous potential source rock samples from the Codó Formation (Parnaíba Basin, Brazil).•C30 sterane biomarker: 24-n-propylcholestane and 24-isopropylcholestane.•Indicators of maturity and depositional paleoenvironment.•Evidences of anoxia during the deposition of sediments in Parnaíba Basin.
Author Cioccari, Giovani M.
Capilla, Ramsés
Júnior, Gustavo R.Sousa
Imamura, Paulo M.
de A. M. Reis, Francisco
Rodrigues, Rene
Lopes, José A.D.
de Lima, Sidney G.
da S. Sousa, Edymilaís
de Sousa, Alek A.C.
de Souza, Igor V.A.F.
Silva, Andrenilton F.
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  givenname: Gustavo R.Sousa
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  givenname: Andrenilton F.
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  givenname: Francisco
  surname: de A. M. Reis
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  givenname: Ramsés
  surname: Capilla
  fullname: Capilla, Ramsés
  organization: Petrobras/CENPES/PDEP/GEOQ, Av. Horácio Macedo 950, Universitária-Ilha do Fundã City, 21941-915, Rio de Janeiro, RJ, Brazil
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  givenname: Igor V.A.F.
  surname: de Souza
  fullname: de Souza, Igor V.A.F.
  organization: Petrobras/CENPES/PDEP/GEOQ, Av. Horácio Macedo 950, Universitária-Ilha do Fundã City, 21941-915, Rio de Janeiro, RJ, Brazil
– sequence: 9
  givenname: Paulo M.
  surname: Imamura
  fullname: Imamura, Paulo M.
  organization: Chemistry Institute, University of Campinas, Box 6154, 13083-970, Campinas, SP, Brazil
– sequence: 10
  givenname: Rene
  surname: Rodrigues
  fullname: Rodrigues, Rene
  organization: Rio de Janeiro State University, Faculty of Geology, Department of Stratigraphy and Paleontology, 20559-900, Rio de Janeiro, RJ, Brazil
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  givenname: José A.D.
  surname: Lopes
  fullname: Lopes, José A.D.
  organization: Laboratory of Organic Geochemistry, Center of Natural Sciences, Federal University of Piaui, Campus Ministro Petrônio Portela, 64049-550, Teresina, PI, Brazil
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  givenname: Sidney G.
  surname: de Lima
  fullname: de Lima, Sidney G.
  email: sidney@ufpi.edu.br
  organization: Laboratory of Organic Geochemistry, Center of Natural Sciences, Federal University of Piaui, Campus Ministro Petrônio Portela, 64049-550, Teresina, PI, Brazil
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Keywords Depositional environment
Dinosterane
Hopenes
4-Methylstigmastane
Sterenes
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Snippet Earlier geological works showed that Codó Formation - CF (Parnaíba Basin, Brazil) has been deposited in the Aptian, and suffered the influence of various...
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SubjectTerms 4-Methylstigmastane
Depositional environment
Dinosterane
Hopenes
Sterenes
Title Biomarkers in Cretaceous sedimentary rocks from the Codó Formation - Parnaíba Basin: Paleoenvironmental assessment
URI https://dx.doi.org/10.1016/j.jsames.2019.03.025
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