Reconstructing the palaeoecology of a middle Permian alkaline lake using molecular fossils, case study of the Lucaogou Formation in the Junggar Basin, NW China

•Palaeoecology during deposition of the Lucaogou Formation was reconstructed.•Type Ⅰ aerobic methanotrophs are indicated by abundant 3β-methylhopanes.•2α-Methylhopanes, 7- and 8-methylheptadecanes indicative of cyanobacteria.•Green algae Chlorophyta were the most likely dominant microalgae.•Some aro...

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Published inOrganic geochemistry Vol. 193; p. 104791
Main Authors Ding, Wenjing, Hou, Dujie, Li, Li, Jiang, Lian, Zhang, Ziming, Jiang, Yuhan, George, Simon C.
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.07.2024
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Abstract •Palaeoecology during deposition of the Lucaogou Formation was reconstructed.•Type Ⅰ aerobic methanotrophs are indicated by abundant 3β-methylhopanes.•2α-Methylhopanes, 7- and 8-methylheptadecanes indicative of cyanobacteria.•Green algae Chlorophyta were the most likely dominant microalgae.•Some aromatic C40 carotenoids diagnostic for green/purple sulfur bacteria. The lacustrine Lucaogou Formation was deposited during the middle Permian in the Junggar Basin, northwestern China. The depositional environment was an alkaline, brackish to saline lake. The biological diversity of the Lucaogou Formation was reconstructed using biologically informative molecules such as n-alkanes, steranes, and hopanes, and the δ13C composition of organic matter. C30 4α-methyl-24-ethylsterane, C31 lanostane, and abundant C30 − C31 3β-methylhopanes were detected in the organic matter, suggesting the presence of type Ⅰ aerobic methanotrophs including the Methylococcaceae. C30 − C31 2α-methylhopanes and 7- and 8-methylheptadecanes are suggestive of the presence of cyanobacteria. Cyanobacteria and green algae are proposed to have made the dominant contribution to the organic matter. The presence of more 13C-enriched hopanoids in the lower unit compared to the upper unit of the Lucaogou Formation suggest a greater contribution of cyanobacteria to the organic matter in the lower unit. The high abundances of C28 and C29 steranes relative to C27 steranes are likely due to green algae from the Chlorophyta, including the class Chlorophyceae. Dinosteranes that are diagnostic for dinoflagellates were not detected. The low concentrations of C40 isorenieratane, renieratane, β-isorenieratane, renierapurpurane, and β-renierapurpurane that are indicative of photosynthetic green and purple sulfur bacteria indicate a minor contribution from Chlorobiaceae and Chromatiaceae to the organic matter. It is inferred that low to moderate amounts of ciliates grew at or below the relatively unstable chemocline in the lake. The presence of C19-norisopimarane, 8β(H)-labdane, and 4β(H)-19-norisopimarane suggests the presence of coniferous plants growing around the lake, probably including Pinaceae, Araucariaceae, Cupressaceae.
AbstractList The lacustrine Lucaogou Formation was deposited during the middle Permian in the Junggar Basin, northwestern China. The depositional environment was an alkaline, brackish to saline lake. The biological diversity of the Lucaogou Formation was reconstructed using biologically informative molecules such as n-alkanes, steranes, and hopanes, and the δ¹³C composition of organic matter. C₃₀ 4α-methyl-24-ethylsterane, C₃₁ lanostane, and abundant C₃₀ − C₃₁ 3β-methylhopanes were detected in the organic matter, suggesting the presence of type Ⅰ aerobic methanotrophs including the Methylococcaceae. C₃₀ − C₃₁ 2α-methylhopanes and 7- and 8-methylheptadecanes are suggestive of the presence of cyanobacteria. Cyanobacteria and green algae are proposed to have made the dominant contribution to the organic matter. The presence of more ¹³C-enriched hopanoids in the lower unit compared to the upper unit of the Lucaogou Formation suggest a greater contribution of cyanobacteria to the organic matter in the lower unit. The high abundances of C₂₈ and C₂₉ steranes relative to C₂₇ steranes are likely due to green algae from the Chlorophyta, including the class Chlorophyceae. Dinosteranes that are diagnostic for dinoflagellates were not detected. The low concentrations of C₄₀ isorenieratane, renieratane, β-isorenieratane, renierapurpurane, and β-renierapurpurane that are indicative of photosynthetic green and purple sulfur bacteria indicate a minor contribution from Chlorobiaceae and Chromatiaceae to the organic matter. It is inferred that low to moderate amounts of ciliates grew at or below the relatively unstable chemocline in the lake. The presence of C₁₉-norisopimarane, 8β(H)-labdane, and 4β(H)-19-norisopimarane suggests the presence of coniferous plants growing around the lake, probably including Pinaceae, Araucariaceae, Cupressaceae.
•Palaeoecology during deposition of the Lucaogou Formation was reconstructed.•Type Ⅰ aerobic methanotrophs are indicated by abundant 3β-methylhopanes.•2α-Methylhopanes, 7- and 8-methylheptadecanes indicative of cyanobacteria.•Green algae Chlorophyta were the most likely dominant microalgae.•Some aromatic C40 carotenoids diagnostic for green/purple sulfur bacteria. The lacustrine Lucaogou Formation was deposited during the middle Permian in the Junggar Basin, northwestern China. The depositional environment was an alkaline, brackish to saline lake. The biological diversity of the Lucaogou Formation was reconstructed using biologically informative molecules such as n-alkanes, steranes, and hopanes, and the δ13C composition of organic matter. C30 4α-methyl-24-ethylsterane, C31 lanostane, and abundant C30 − C31 3β-methylhopanes were detected in the organic matter, suggesting the presence of type Ⅰ aerobic methanotrophs including the Methylococcaceae. C30 − C31 2α-methylhopanes and 7- and 8-methylheptadecanes are suggestive of the presence of cyanobacteria. Cyanobacteria and green algae are proposed to have made the dominant contribution to the organic matter. The presence of more 13C-enriched hopanoids in the lower unit compared to the upper unit of the Lucaogou Formation suggest a greater contribution of cyanobacteria to the organic matter in the lower unit. The high abundances of C28 and C29 steranes relative to C27 steranes are likely due to green algae from the Chlorophyta, including the class Chlorophyceae. Dinosteranes that are diagnostic for dinoflagellates were not detected. The low concentrations of C40 isorenieratane, renieratane, β-isorenieratane, renierapurpurane, and β-renierapurpurane that are indicative of photosynthetic green and purple sulfur bacteria indicate a minor contribution from Chlorobiaceae and Chromatiaceae to the organic matter. It is inferred that low to moderate amounts of ciliates grew at or below the relatively unstable chemocline in the lake. The presence of C19-norisopimarane, 8β(H)-labdane, and 4β(H)-19-norisopimarane suggests the presence of coniferous plants growing around the lake, probably including Pinaceae, Araucariaceae, Cupressaceae.
ArticleNumber 104791
Author Zhang, Ziming
George, Simon C.
Jiang, Lian
Li, Li
Ding, Wenjing
Hou, Dujie
Jiang, Yuhan
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  surname: Ding
  fullname: Ding, Wenjing
  organization: School of Energy Resources, China University of Geosciences, Beijing 100083, China
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  givenname: Dujie
  surname: Hou
  fullname: Hou, Dujie
  email: hdj@cugb.edu.cn
  organization: School of Energy Resources, China University of Geosciences, Beijing 100083, China
– sequence: 3
  givenname: Li
  surname: Li
  fullname: Li, Li
  organization: CNOOC International Limited, Beijing 100028, China
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  givenname: Lian
  surname: Jiang
  fullname: Jiang, Lian
  organization: School of Natural Sciences, Macquarie University, Sydney, NSW 2109, Australia
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  givenname: Ziming
  surname: Zhang
  fullname: Zhang, Ziming
  organization: School of Energy Resources, China University of Geosciences, Beijing 100083, China
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  givenname: Yuhan
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  organization: Guangzhou Marine Geological Survey, Guangzhou 510075, China
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  givenname: Simon C.
  orcidid: 0000-0001-6534-3846
  surname: George
  fullname: George, Simon C.
  email: simon.geroge@mq.edu.au
  organization: School of Natural Sciences, Macquarie University, Sydney, NSW 2109, Australia
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Chlorophyta
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Cyanobacteria
Biological diversity
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Snippet •Palaeoecology during deposition of the Lucaogou Formation was reconstructed.•Type Ⅰ aerobic methanotrophs are indicated by abundant...
The lacustrine Lucaogou Formation was deposited during the middle Permian in the Junggar Basin, northwestern China. The depositional environment was an...
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SubjectTerms alkanes
Araucariaceae
biodiversity
Biological diversity
case studies
China
Chlorobiaceae
Chlorophyceae
Chlorophyta
Chromatiaceae
Ciliophora
class
Conifers
Cupressaceae
Cyanobacteria
geochemistry
hopanoids
methanotrophs
Methylococcaceae
Miozoa
organic matter
paleoecology
Permian period
photosynthesis
Pinaceae
salt lakes
sulfur
Sulfur bacteria
Type Ⅰ methanotrophs
Title Reconstructing the palaeoecology of a middle Permian alkaline lake using molecular fossils, case study of the Lucaogou Formation in the Junggar Basin, NW China
URI https://dx.doi.org/10.1016/j.orggeochem.2024.104791
https://www.proquest.com/docview/3153631118
Volume 193
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