The nature and fate of natural resins in the geosphere XIII: a probable pinaceous resin from the early Cretaceous (Barremian), Isle of Wight.

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Title: The nature and fate of natural resins in the geosphere XIII: a probable pinaceous resin from the early Cretaceous (Barremian), Isle of Wight.
Authors: Bray, P. Sargent1 sargentb@siu.edu, Anderson, Ken B.1 kanderson@geo.siu.edu
Source: Geochemical Transactions. 1/29/2008, Vol. 9, p3-5. 5p. 1 Diagram, 1 Graph.
Subjects: Fossil resins, Gums & resins, Conifers, Terpenes, Chromatographic analysis, Cheirolepidiaceae
Geographic Terms: Isle of Wight (England), England
Abstract: Terpenoid resin is produced by all families and most genera of the order Coniferales (the conifers), and the distribution of terpenes present in most conifer resins is characteristic of the originating family. Analyses of early Cretaceous (Barremian) amber (fossil resin) from the English Wealden, Isle of Wight, southern England, by pyrolysis-gas chromatography-mass spectrometry (Py-GC-MS), indicate a terpene distribution dominated by abietane- and labdane-type terpenes. Similar distributions are observed in some species of the extant family Pinaceae. The Pinaceae are well represented within the Wealden deposits of southern England, by only one (known) species, Pityites solmsii (Seward) Seward, whereas the macro-fossil record of these deposits is dominated by the extinct conifer family Cheirolepidiaceae, for which no resin chemistry has been reported. By analogy with modern materials, it is probable that the ambers found in these deposits are derived from an extinct member of the Pinaceae, but given the absence of evidence concerning the chemotaxonomy of the Cheirolepidiaceae, this family cannot be excluded a priori as a possible paleobotanical source. These ambers may therefore be assigned to either the Pinaceae or to the Cheirolepidiaceae. These samples are the oldest ambers to date to yield useful chemotaxonomic data. [ABSTRACT FROM AUTHOR]
Copyright of Geochemical Transactions is the property of BioMed Central 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: The nature and fate of natural resins in the geosphere XIII: a probable pinaceous resin from the early Cretaceous (Barremian), Isle of Wight.
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  Data: <searchLink fieldCode="JN" term="%22Geochemical+Transactions%22">Geochemical Transactions</searchLink>. 1/29/2008, Vol. 9, p3-5. 5p. 1 Diagram, 1 Graph.
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  Data: <searchLink fieldCode="DE" term="%22Fossil+resins%22">Fossil resins</searchLink><br /><searchLink fieldCode="DE" term="%22Gums+%26+resins%22">Gums & resins</searchLink><br /><searchLink fieldCode="DE" term="%22Conifers%22">Conifers</searchLink><br /><searchLink fieldCode="DE" term="%22Terpenes%22">Terpenes</searchLink><br /><searchLink fieldCode="DE" term="%22Chromatographic+analysis%22">Chromatographic analysis</searchLink><br /><searchLink fieldCode="DE" term="%22Cheirolepidiaceae%22">Cheirolepidiaceae</searchLink>
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  Data: <searchLink fieldCode="DE" term="%22Isle+of+Wight+%28England%29%22">Isle of Wight (England)</searchLink><br /><searchLink fieldCode="DE" term="%22England%22">England</searchLink>
– Name: Abstract
  Label: Abstract
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  Data: Terpenoid resin is produced by all families and most genera of the order Coniferales (the conifers), and the distribution of terpenes present in most conifer resins is characteristic of the originating family. Analyses of early Cretaceous (Barremian) amber (fossil resin) from the English Wealden, Isle of Wight, southern England, by pyrolysis-gas chromatography-mass spectrometry (Py-GC-MS), indicate a terpene distribution dominated by abietane- and labdane-type terpenes. Similar distributions are observed in some species of the extant family Pinaceae. The Pinaceae are well represented within the Wealden deposits of southern England, by only one (known) species, Pityites solmsii (Seward) Seward, whereas the macro-fossil record of these deposits is dominated by the extinct conifer family Cheirolepidiaceae, for which no resin chemistry has been reported. By analogy with modern materials, it is probable that the ambers found in these deposits are derived from an extinct member of the Pinaceae, but given the absence of evidence concerning the chemotaxonomy of the Cheirolepidiaceae, this family cannot be excluded a priori as a possible paleobotanical source. These ambers may therefore be assigned to either the Pinaceae or to the Cheirolepidiaceae. These samples are the oldest ambers to date to yield useful chemotaxonomic data. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
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  Data: <i>Copyright of Geochemical Transactions is the property of BioMed Central 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: 10.1186/1467-4866-9-3
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        Text: English
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      – SubjectFull: Gums & resins
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      – SubjectFull: Conifers
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      – SubjectFull: Terpenes
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      – SubjectFull: Chromatographic analysis
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      – SubjectFull: Cheirolepidiaceae
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      – SubjectFull: Isle of Wight (England)
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      – SubjectFull: England
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      – TitleFull: The nature and fate of natural resins in the geosphere XIII: a probable pinaceous resin from the early Cretaceous (Barremian), Isle of Wight.
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              Text: 1/29/2008
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