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Arthropod interactions with bennettitalean roots in a Triassic permineralized peat from Hopen, Svalbard Archipelago (Arctic)

机译:节肢动物与来自Hopen,svalbard archipelago(北极)的三叠纪矿化泥炭中的bennettitalean根的相互作用

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摘要

Multiple thin-sections of a Late Triassic (Carnian) siliceous permineralized peat block likely derived from the De Geerdalen Formation on Hopen Island, Svalbard Archipelago, show a dense mass of roots preserving fine anatomical details of various stages of primary and secondary vascular tissue development. The presence of moderately defined rings with few latewood cells in the secondary xylem attests to growth in a seasonal environment. The presence of mucilage bodies and nests of sclerotic cells in the cortical tissues of the roots and pith of subaerial stem fragments, together with scalariform pitting on radial tracheid walls and 2–12 simple pits per cross-field favor bennettitalean affinities for the roots. Evidence of a rich fauna of detritivores inhabiting the peat profile is represented in the form of extensive damage to cortical tissues of dead roots and abundant coprolites preserved both within chambers excavated in the plant tissues and in the peat matrix. Less common gall-like structures within the roots indicate the presence of parasitic organisms in the palaeo-peat ecosystem.
机译:可能来自斯瓦尔巴特群岛霍本岛上的De Geerdalen组的晚期三叠纪(Carnian)硅质矿化泥炭块的多个薄片显示出密集的根系,保留了原发和继发血管组织发育各个阶段的精细解剖学细节。次生木质部中几乎没有乳木细胞的中度定义的环的存在证明了在季节性环境中的生长。根皮层组织中存在粘液体和硬化细胞巢,而茎基干碎片在径向气管壁上有鳞状点蚀,每个横切面有2–12个简单的凹坑,有利于根的贝内特勒亲和力。居住在泥炭剖面上的丰富的有害动物群的证据以对死根的皮层组织的广泛破坏和在植物组织和泥炭基质中挖掘出的腔室中保存的丰富共腐殖质的广泛破坏的形式表示。根部内不太常见的胆样结构表明寄生生物存在于古豌豆生态系统中。

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