Retallack G J, Landing Ed
Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403
Department of Paleontology, New York State Museum, 222 Madison Avenue, Albany, New York 12230, and Department of Earth and Environmental Sciences, Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964.
Mycologia. 2014 Nov-Dec;106(6):1143-58. doi: 10.3852/13-390. Epub 2014 Jul 2.
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 Schunnemunk 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 (δ(13)CPDB) of -25.03 ± 0.13‰ and -26.17 ± 0.69‰, 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.
泥盆纪时期的洛根原杉化石原木曾被认为是类似海带的水生藻类、卷起来的地钱地毯、巨大的腐生真菌子实体或巨型地衣。藻类和卷起来的地钱模型无法解释这里所描述的来自纽约州东部舒内芒克山泥盆纪中期(3.86亿年前)贝尔韦尔砂岩的完整洛根原杉化石的比例和分支情况。这棵“舒内芒克树”长8.83米,有六个分支,每个分支长约1米,直径9厘米,位于主轴上部1.2米处。舒内芒克树干和分支的煤化最外层的同位素组成(δ(13)CPDB)分别为-25.03±0.13‰和-26.17±0.69‰。树干最外层在被多分支管状细胞包围的球状细胞皮层巢上方有保存不佳的内陷。这种组织学特征不同于藻类、地钱或维管植物,最像带有球状绿藻共生体的地衣。原杉已被归入担子菌门,但缺乏明显的双核特征。原杉及其已灭绝的线虫植物目可能属于毛霉亚门或球囊菌门。