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首页> 外文期刊>Journal of the Geological Society of India >Generic distinguishing characteristics and stratigraphic ranges of fossil corallines: An update
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Generic distinguishing characteristics and stratigraphic ranges of fossil corallines: An update

机译:化石珊瑚线的一般区别特征和地层范围:更新

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摘要

Corallines or coralline algae are carbonate secreting and strongly calcified red algae of the order Corallinales of division Rhodophyta. Architecturally, the corallines have two groups, the nongeniculate and geniculate coralline forms. Corallines are used as a potential tool for paleoecology, paleoenvironments and paleobathymetry. Coralline algae are builder of porous and permeable carbonate reservoir rocks for hydrocarbon and reefs rich in hydrocarbon. The old approach, ca. prior to 1977, of taxonomy of fossil coralline genera has been replaced by the modern approach that established during the last decade using certain distinguishing features such as arrangement of basal filaments, cell fusions, conceptacle perforations and orientation of filaments around conceptacles of living corallines. The earliest confirmed fossil record of coralline algae is from the Hauterivian (Early Cretaceous) and from the Hauterivian to the Pleistocene 9 nongeniculate coralline genera, namely Distichoplax, Lithophyllum, Lithoporella, Lithothamnion, Mesophyllum, Neogoniolithon, Phymatolithon, Spongites and Sporolithon and 7 geniculate genera, viz. Amphiroa, Arthrocardia, Calliarthron, Corallina, Jania, Metagoniolithon and Subterraniphyllum having different stratigraphic ranges are unequivocally known as fossils. After 1977, we do not have a comprehensive publication giving the generic distinguishing characteristics and stratigraphic ranges of both nongeniculate and geniculate corallines. The present paper gives an update of distinguishing characteristics of fossil coralline algal genera and their stratigraphic ranges.
机译:珊瑚或珊瑚藻是碳酸盐分泌物,是红藻科Corallinales的强钙化红藻。在结构上,珊瑚线有两种类型,非膝形和膝形珊瑚线形式。珊瑚线被用作古生态,古环境和古生物学的潜在工具。珊瑚藻是多孔的和可渗透的碳酸盐储集岩的建造者,用于碳氢化合物和富含碳氢化合物的礁石。旧方法,约。 1977年之前,珊瑚化石属的分类学已被近十年来建立的现代方法所取代,该方法采用了某些显着特征,例如基底细丝的排列,细胞融合,概念性穿孔以及围绕活珊瑚线概念的细丝方向。最早证实的珊瑚藻化石记录是从上特统(早白垩世)和上新世至更新世的9个非生代珊瑚属,即Distichoplax,Lithophyllum,Lithoporella,Lithothamnion,Mesophyllum,Neogoniolithon,Phymatolitholion,Spongitesra和Songites和,即明确地将具有不同地层范围的两栖动物,心律失常,Calliarthron,Corallina,Jania,Metagoniolithon和Subterraniphyllum称为化石。 1977年以后,我们还没有全面的出版物来提供非成岩和成膝珊瑚线的一般区别特征和地层范围。本文给出了珊瑚化石藻类属的特征及其地层范围的更新。

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