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Affinities and architecture of Devonian trunks of Prototaxites loganii

机译:轮生原生生物泥盆纪树干的亲和力和结构

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Devonian fossil logs of Prototaxites loganii have been considered kelp-like aquatic algae, rolled up carpets of liverworts, enormous saprophytic fungal fruiting bodies or giant lichens. Algae and rolled liverwort models cannot explain the proportions and branching described here of a complete fossil of Prototaxites loganii from the Middle Devonian (386 Ma) Bellvale Sandstone on Schunn emunk Mountain, eastern New York. The "Schunnemunk tree" was 8.83 m long and had six branches, each about 1 m long and 9 cm diam, on the upper 1.2 m of the main axis. The coalified outermost layer of the Schunnemunk trunk and branches have isotopic compositions (delta C-13(PDB)) of -25.03 +/- 0.13 parts per thousand and -26.17 +/- 0.69 parts per thousand, respectively. The outermost part of the trunk has poorly preserved invaginations above cortical nests of coccoid cells embraced by much-branched tubular cells. This histology is unlike algae, liverworts or vascular plants and most like lichen with coccoid chlorophyte phycobionts. Prototaxites has been placed within Basidiomycota but lacks clear dikaryan features. Prototaxites and its extinct order Nematophytales may belong within Mucoromycotina or Glomeromycota.
机译:原生藻类loganii的泥盆纪化石原木被认为是海带状的水生藻类,卷起了艾蒿,巨大的腐生真菌子实体或巨型地衣。藻类和滚动的艾蒿模型无法解释这里描述的来自纽约东部Schunn Emunk山上的中泥盆世(386 Ma)Bellvale砂岩的完整原生石对虾的化石的比例和分支。 “ Shunnemunk树”长8.83 m,在主轴的上端1.2 m上有六个分支,每个分支约1 m长,直径9 cm。 Schunnemunk干线和分支的碳化最外层的同位素组成(δC-13(PDB))分别为每千分之-25.03 +/- 0.13和每千分之-26.17 +/- 0.69。树干的最外层在球状管状细胞所包围的球状细胞的皮质巢上方的内翻保留得不好。这种组织学不同于藻类,地艾或维管植物,最像带有球状绿藻类藻类生物的地衣。原生生物已被放置在担子菌内,但缺乏明显的双核生物特征。原生生物及其灭绝的线虫目可能属于毛霉菌纲或球菌纲。

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