Identification of Carboniferous (320 Million Years Old) Class Ic Amber.

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Title: Identification of Carboniferous (320 Million Years Old) Class Ic Amber.
Authors: Bray, P. Sargent, Anderson, Ken B.
Source: Science (pre-March 2025). 10/2/2009, Vol. 326 Issue 5949, p132-134. 3p.
Subjects: Amber fossils, Carboniferous stratigraphic geology, Rock analysis, Fossil resins, Plant product synthesis, Fossil conifers, Biological divergence, Plant evolution
Abstract: The presence of amber, the fossil form of the resins produced by many types of higher plants, has been reported from many localities in Mesozoic and Cenozoic rocks. We have found Class I (polylabdanoid) amber in Carboniferous sediments dating to ∼320 million years ago. This result demonstrates that preconifer gymnosperms evolved the biosynthetic mechanisms to produce complex polyterpenoid resins earlier than previously believed and that the biosynthetic pathways leading to the types of polylabdanoid resins that are now typically found in conifers and those now typically found in angiosperms had already diverged by the Carboniferous. [ABSTRACT FROM AUTHOR]
Copyright of Science (pre-March 2025) is the property of American Association for the Advancement of 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.)
Database: Psychology and Behavioral Sciences Collection
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  Data: Identification of Carboniferous (320 Million Years Old) Class Ic Amber.
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  Data: <searchLink fieldCode="AR" term="%22Bray%2C+P%2E+Sargent%22">Bray, P. Sargent</searchLink><br /><searchLink fieldCode="AR" term="%22Anderson%2C+Ken+B%2E%22">Anderson, Ken B.</searchLink>
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  Data: <searchLink fieldCode="JN" term="%22Science+%28pre-March+2025%29%22">Science (pre-March 2025)</searchLink>. 10/2/2009, Vol. 326 Issue 5949, p132-134. 3p.
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  Data: <searchLink fieldCode="DE" term="%22Amber+fossils%22">Amber fossils</searchLink><br /><searchLink fieldCode="DE" term="%22Carboniferous+stratigraphic+geology%22">Carboniferous stratigraphic geology</searchLink><br /><searchLink fieldCode="DE" term="%22Rock+analysis%22">Rock analysis</searchLink><br /><searchLink fieldCode="DE" term="%22Fossil+resins%22">Fossil resins</searchLink><br /><searchLink fieldCode="DE" term="%22Plant+product+synthesis%22">Plant product synthesis</searchLink><br /><searchLink fieldCode="DE" term="%22Fossil+conifers%22">Fossil conifers</searchLink><br /><searchLink fieldCode="DE" term="%22Biological+divergence%22">Biological divergence</searchLink><br /><searchLink fieldCode="DE" term="%22Plant+evolution%22">Plant evolution</searchLink>
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  Data: The presence of amber, the fossil form of the resins produced by many types of higher plants, has been reported from many localities in Mesozoic and Cenozoic rocks. We have found Class I (polylabdanoid) amber in Carboniferous sediments dating to ∼320 million years ago. This result demonstrates that preconifer gymnosperms evolved the biosynthetic mechanisms to produce complex polyterpenoid resins earlier than previously believed and that the biosynthetic pathways leading to the types of polylabdanoid resins that are now typically found in conifers and those now typically found in angiosperms had already diverged by the Carboniferous. [ABSTRACT FROM AUTHOR]
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  Data: <i>Copyright of Science (pre-March 2025) is the property of American Association for the Advancement of 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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        Value: 10.1126/science.1177539
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      – Code: eng
        Text: English
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        PageCount: 3
        StartPage: 132
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      – SubjectFull: Amber fossils
        Type: general
      – SubjectFull: Carboniferous stratigraphic geology
        Type: general
      – SubjectFull: Rock analysis
        Type: general
      – SubjectFull: Fossil resins
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      – SubjectFull: Plant product synthesis
        Type: general
      – SubjectFull: Fossil conifers
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      – SubjectFull: Biological divergence
        Type: general
      – SubjectFull: Plant evolution
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              Text: 10/2/2009
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              Y: 2009
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