Synthesis of 26-methyl cholestane and identification of cryostanes in mid-Neoproterozoic sediments.

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Title: Synthesis of 26-methyl cholestane and identification of cryostanes in mid-Neoproterozoic sediments.
Authors: Adam, Pierre1 padam@unistra.fr, Schaeffer, Philippe1, Brocks, Jochen J.2
Source: Organic Geochemistry. Jan2018, Vol. 115, p246-249. 4p.
Subjects: Cholestanes, Marine sediments, Steranes, Gas chromatography, Mass spectrometry, Molecular clock
Abstract: The biomarker distributions of mid-Neoproterozoic sediments (800–717 million yr, Ma) from various locations are characterized by the occurrence, besides cholestane isomers, of a novel series of C 28 steranes, whereas classical C-24 alkylated steranes are absent. These unusual C 28 steranes, termed cryostanes, seem to be restricted to pre-Snowball Earth sediments. We report their conclusive identification as 26-methyl cholestanes based on comparison of gas chromatographic (GC) behavior and mass spectrum of the last eluting cryostane isomer with those of a 26-methyl 5α(H),14α(H),17α(H),20 R -cholestane standard obtained by way of synthesis. Sterols methylated at C-26 seem to be restricted to some demosponges and, based on molecular clock estimates, demosponges may have emerged in the time interval 800–700 Ma. A sponge origin of cryostanes is thereby conceivable, making cryostanes the oldest molecular markers for animals. However, other biological sources need to be explored, including the wide variety of eukaryotic protists. [ABSTRACT FROM AUTHOR]
Copyright of Organic Geochemistry is the property of Pergamon Press - An Imprint of Elsevier Science and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: Synthesis of 26-methyl cholestane and identification of cryostanes in mid-Neoproterozoic sediments.
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  Data: <searchLink fieldCode="AR" term="%22Adam%2C+Pierre%22">Adam, Pierre</searchLink><relatesTo>1</relatesTo><i> padam@unistra.fr</i><br /><searchLink fieldCode="AR" term="%22Schaeffer%2C+Philippe%22">Schaeffer, Philippe</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Brocks%2C+Jochen+J%2E%22">Brocks, Jochen J.</searchLink><relatesTo>2</relatesTo>
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  Data: <searchLink fieldCode="JN" term="%22Organic+Geochemistry%22">Organic Geochemistry</searchLink>. Jan2018, Vol. 115, p246-249. 4p.
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  Data: <searchLink fieldCode="DE" term="%22Cholestanes%22">Cholestanes</searchLink><br /><searchLink fieldCode="DE" term="%22Marine+sediments%22">Marine sediments</searchLink><br /><searchLink fieldCode="DE" term="%22Steranes%22">Steranes</searchLink><br /><searchLink fieldCode="DE" term="%22Gas+chromatography%22">Gas chromatography</searchLink><br /><searchLink fieldCode="DE" term="%22Mass+spectrometry%22">Mass spectrometry</searchLink><br /><searchLink fieldCode="DE" term="%22Molecular+clock%22">Molecular clock</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: The biomarker distributions of mid-Neoproterozoic sediments (800–717 million yr, Ma) from various locations are characterized by the occurrence, besides cholestane isomers, of a novel series of C 28 steranes, whereas classical C-24 alkylated steranes are absent. These unusual C 28 steranes, termed cryostanes, seem to be restricted to pre-Snowball Earth sediments. We report their conclusive identification as 26-methyl cholestanes based on comparison of gas chromatographic (GC) behavior and mass spectrum of the last eluting cryostane isomer with those of a 26-methyl 5α(H),14α(H),17α(H),20 R -cholestane standard obtained by way of synthesis. Sterols methylated at C-26 seem to be restricted to some demosponges and, based on molecular clock estimates, demosponges may have emerged in the time interval 800–700 Ma. A sponge origin of cryostanes is thereby conceivable, making cryostanes the oldest molecular markers for animals. However, other biological sources need to be explored, including the wide variety of eukaryotic protists. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
  Group: Ab
  Data: <i>Copyright of Organic Geochemistry is the property of Pergamon Press - An Imprint of Elsevier Science and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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      – Type: doi
        Value: 10.1016/j.orggeochem.2017.11.006
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      – Code: eng
        Text: English
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        PageCount: 4
        StartPage: 246
    Subjects:
      – SubjectFull: Cholestanes
        Type: general
      – SubjectFull: Marine sediments
        Type: general
      – SubjectFull: Steranes
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      – SubjectFull: Gas chromatography
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      – SubjectFull: Mass spectrometry
        Type: general
      – SubjectFull: Molecular clock
        Type: general
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      – TitleFull: Synthesis of 26-methyl cholestane and identification of cryostanes in mid-Neoproterozoic sediments.
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            NameFull: Schaeffer, Philippe
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            NameFull: Brocks, Jochen J.
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              M: 01
              Text: Jan2018
              Type: published
              Y: 2018
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