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首页> 外文期刊>Facies >New insights into Lithocodium aggregatum Elliott 1956 and Bacinella irregularis Radoicic 1959 (Late Jurassic-Lower Cretaceous): two ulvophycean green algae (?Order Ulotrichales) with a heteromorphic life cycle (epilithic/euendolithic)
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New insights into Lithocodium aggregatum Elliott 1956 and Bacinella irregularis Radoicic 1959 (Late Jurassic-Lower Cretaceous): two ulvophycean green algae (?Order Ulotrichales) with a heteromorphic life cycle (epilithic/euendolithic)

机译:对聚合石藻的新见解Elliott 1956年和不规则芽孢杆菌Radoicic 1959年(侏罗纪-下白垩统):两种藻类藻类藻(Ulotrichales阶)具有异形的生命周期(上石/真石质)

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摘要

The Late Jurassic-Lower Cretaceous microorganisms incertae sedis Lithocodium aggregatum Elliott and Bacinella irregularis RadoiiA double dagger are taxonomically studied based on material from the Lower Aptian of the western Maestrat Basin (Spain). This study is supplemented with detailed photographs from Elliot's type-material. Given that the original description of Lithocodium aggregatum is ambiguous, a detail from the holotype is chosen as an epitype to serve as an interpretative type (article 9.7 ICBN). Lithocodium is re-interpreted as a filamentous-septate heterotrichale ulvophycean alga (?order Ulotrichales) exhibiting a heteromorphic life cycle consisting of two phases: an epilithic gametophytic and a euendolithic sporophytic (Gomontia stage). Bacinella irregularis is interpreted and redescribed as a purely euendolithic ulvophycean alga which bores into either Lithocodium aggregatum or the substrate below Lithocodium crusts. A small microendolith boring into Lithocodium crusts capable of cryptobiotically stretching within its filamentous network is tentatively assigned to the siphonal chlorophyte Ostreobium Bornet and Flahault. Another associated microfilamentous boring chlorophyte with characteristic long thin hairs (setae) is described as Phaeophila? sp. The euendolithic community comprises a variety of micro- and macroborings that affect the thalli of Lithocodium. Finally, the filaments of the outer zone of the Lithocodium crust are infested by calcimicrobes (cyanobacteria, ?fungi). The description made by Elliott in his original work of the "inner layer" of Lithocodium aggregatum as "confused" is explained here as a complex multitaxon chlorophyte-calcimicrobial assemblage overprinted by multiple bioerosion ichnofabrics.
机译:根据马斯特拉特盆地西部(西班牙)下阿普提安地区的资料,对双锯齿的侏罗纪-下白垩纪晚期微生物(共生石藻)和双孢杆菌进行了分类研究。这项研究辅以Elliot的字体材料的详细照片。鉴于聚合石楠的原始描述含糊不清,因此从整体型中选择一个细节作为表型,以作为解释性类型(第9.7 ICBN条)。锂钴被重新解释为一种丝状的杂藻类藻类(Ulotrichales),表现出由两个阶段组成的异形生命周期:上石配子体和真石孢子体(Gomontia阶段)。不规则芽孢杆菌被解释并重新描述为纯正真石质藻类藻类,可钻入石棉合石或石棉外壳下面的基质中。钻入能够在其丝状网络内进行隐源性拉伸的锂co壳中钻出的一个小微内层,暂时分配给虹吸叶绿体Ostreobium Bornet和Flahault。另一种具有特征性的长而稀疏的毛发(刚毛科)的微丝无聊叶绿体被称为嗜碱菌? sp。真石质群落包括影响微石藻co的各种微孔和大孔。最后,石棉外壳的外部区域的细丝被钙微生物(蓝细菌,真菌)侵染。 Elliott在其原始工作中对聚合石棉的“内层”所作的描述被描述为“混淆”,这是由多种生物侵蚀性鱼鳞织物叠印而成的复杂的多分类群叶绿素-钙微生物组合体。

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