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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Molecular composition and chemosystematic aspects of Cretaceous amber from the Amazonas, Araripe and Reconcavo basins, Brazil
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Molecular composition and chemosystematic aspects of Cretaceous amber from the Amazonas, Araripe and Reconcavo basins, Brazil

机译:巴西亚马逊河,阿拉里普和雷康卡沃盆地白垩纪琥珀的分子组成和化学系统方面

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摘要

Amber occurrences in Brazil are rare. In this regard, the molecular composition of three Such fossil resin samples from Brazilian Cretaceous sedimentary basins has been analyzed to determine the botanical origin of the resins. The samples were collected from the Amazonas (Alter do Chao Formation), Araripe (Santana Formation, Crato Member) and Reconcavo (Maracangalha Formation, Caruacu Member) basins. The mono-, sesqui- and diterpenoids in the extracts were used as chemosystematic markers when compared with terpenoids in extant conifers. The compounds were mainly diterpenoids and their degradation products from the labdane, podocarpane, pimarane and isopimarane classes, in addition to paraffins, methoxyphenols and carboxylic acids. Tetracyclic diterpenoids such as phyllocladane, kaurenol and kauranol were also present. The biomarker compositions are certainly typical for conifers and, given the absence of triterpenoids and diterpenoids Such as ozic acid, angiosperms can be excluded as a botanical source. The absence of phenolic diterpenoids (ferruginol, totarol) and their derivatives excludes podocarpaceous affinities for the ambers from the Amazonas and Araripe basins. The fossil records of the embedding sediments (e.g. Araucariaceae pollen and leaves) Support the proposal of an Araucariacae origin for these ambers, but Cupressaceae and Cheirolepidiaceae cannot be excluded. On the other hand, the presence of phyllocladane and kaurane derivatives is evidence for Araucariaceae or Podocarpaceae origins for the amber from the Reconcavo basin, but Cupressaceae cannot be excluded.
机译:在巴西,琥珀很少出现。在这方面,已经分析了来自巴西白垩纪沉积盆地的三种此类化石树脂样品的分子组成,以确定了这些树脂的植物来源。样品采集自亚马孙河流域(Alter do Chao组),Araripe(Santana组,Crato成员)和Reconcavo(Maracangalha组,Caruacu成员)盆地。与现存针叶树中的萜类化合物相比,提取物中的单,倍半萜和二萜类化合物被用作化学系统标记。除石蜡,甲氧基苯酚和羧酸外,这些化合物主要是二萜类化合物及其降解产物,来自拉丹烷,罗汉松,pimarane和isopimarane类。还存在四环二萜类化合物,例如叶绿丹烷,天牛酚和月桂醇。生物标记物组合物对于针叶树无疑是典型的,并且由于不存在三萜类和二萜类化合物(如恶唑酸),被子植物可以作为植物来源被排除。不含酚类二萜类化合物(ferruginol,totarol)及其衍生物排除了亚马逊河盆地和Araripe盆地对琥珀的荚果亲和力。埋藏沉积物的化石记录(例如南洋杉科的花粉和树叶)支持提出将这些琥珀制成南洋杉科的建议,但不能排除柏科和虎皮科。另一方面,茶树素和月桂烷衍生物的存在证明了雷科卡沃盆地琥珀的南洋杉科或罗汉松科起源于琥珀,但不能排除柏科。

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