Luo Cui, Reitner Joachim
Department of Geobiology, Centre of Geosciences, University of Göttingen, Goldschmidtstraße 3, 37077, Göttingen, Germany,
Naturwissenschaften. 2014 Jun;101(6):467-77. doi: 10.1007/s00114-014-1176-0. Epub 2014 Apr 25.
Fossil record of Phanerozoic non-spicular sponges, beside of being important with respect to the lineage evolution per se, could provide valuable references for the investigation of Precambrian ancestral animal fossils. However, although modern phylogenomic studies resolve non-spicular demosponges as the sister group of the remaining spiculate demosponges, the fossil record of the former is extremely sparse or unexplored compared to that of the latter; the Middle Cambrian Vauxiidae Walcott 1920, is the only confirmed fossil taxon of non-spicular demosponges. Here, we describe carbonate materials from Devonian (Upper Givetian to Lower Frasnian) bioherms of northern France and Triassic (Anisian) microbialites of Poland that most likely represent fossil remnants of keratose demosponges. These putative fossils of keratose demosponges are preserved as automicritic clumps. They are morphologically distinguishable from microbial fabrics but similar to other spiculate sponge fossils, except that the skeletal elements consist of fibrous networks instead of assembled spicules. Consistent with the immunological behavior of sponges, these fibrous skeletons often form a rim at the edge of the automicritic aggregate, separating the inner part of the aggregate from foreign objects. To confirm the architecture of these fibrous networks, two fossil specimens and a modern thorectid sponge for comparison were processed for three-dimensional (3-D) reconstruction using serial grinding tomography. The resulting fossil reconstructions are three-dimensionally anastomosing, like modern keratose demosponges, but their irregular and nonhierarchical meshes indicate a likely verongid affinity, although a precise taxonomic conclusion cannot be made based on the skeletal architecture alone. This study is a preliminary effort, but an important start to identify fossil non-spicular demosponges in carbonates and to re-evaluate their fossilization potential.
显生宙非骨针海绵的化石记录,除了本身对于谱系演化很重要之外,还能为前寒武纪动物祖先化石的研究提供有价值的参考。然而,尽管现代系统发育基因组学研究将非骨针海绵纲解析为其余有骨针海绵纲的姐妹群,但与后者相比,前者的化石记录极其稀少或未被探索;寒武纪中期的沃氏海绵科(Walcott,1920)是唯一已确认的非骨针海绵纲化石分类单元。在这里,我们描述了来自法国北部泥盆纪(上吉维特阶至下弗拉斯阶)生物礁和波兰三叠纪(安尼西阶)微生物岩中的碳酸盐物质,它们很可能代表了角质海绵纲的化石残余。这些推测的角质海绵纲化石以自微晶团块的形式保存下来。它们在形态上与微生物结构不同,但与其他有骨针海绵化石相似,只是其骨骼元素由纤维网络组成,而非聚集的骨针。与海绵的免疫行为一致,这些纤维状骨骼通常在自微晶聚集体的边缘形成一个边缘,将聚集体的内部与外来物体分隔开。为了确认这些纤维网络的结构,对两个化石标本和一个用于比较的现代胸海绵进行了处理,使用连续研磨断层扫描进行三维(3-D)重建。所得的化石重建结果是三维相互连接的,类似于现代角质海绵纲,但它们不规则且无层次的网眼表明可能具有矾海绵的亲缘关系,尽管仅根据骨骼结构无法得出精确的分类结论。这项研究是一项初步努力,但却是识别碳酸盐中化石非骨针海绵纲并重新评估其石化潜力的重要开端。