Programa de Pós-Graduação em Ecologia e Recursos Naturais, Universidade Federal de São Carlos, Washington Luiz, 325 km, São Carlos (SP) 13565-905, Brazil.
Unité Mixte de Recherche (UMR), Centre National de la Recherche Scientifique (CNRS), IC2MP 7285, University of Poitiers, 86073 Poitiers, France.
Proc Biol Sci. 2021 Jan 13;288(1942):20202618. doi: 10.1098/rspb.2020.2618. Epub 2021 Jan 6.
Precambrian filamentous microfossils are common and diverse. Nevertheless, their taxonomic assignment can be difficult owing to their overall simple shapes typically lacking in diagnostic features. Here, we report communities of well-preserved, large filamentous impressions from the Ediacaran Itajaí Basin ( 563 Ma) of Brazil. The filaments are uniserial (unbranched) and can reach up to 200 µm in width and up to 44 mm in length. They occur as both densely packed or sparsely populated surfaces, and typically show a consistent orientation. Although simple in shape, their preferred orientation suggests they were tethered to the seafloor, and their overall flexibility (e.g. bent, folded and twisted) supports a biological (rather than sedimentary) affinity. Biometric comparisons with modern filamentous groups further support their biological affinity, suggesting links with either large sulfide-oxidizing bacteria (SOB) or eukaryotes. Other morphological and palaeoecological characteristics further corroborates their similarities with modern large filamentous SOB. Their widespread occurrence and association with complex Ediacaran macrobiota (e.g. frondose organisms, ) suggest that they probably played an important role in the ecological dynamics of these early benthic communities by providing firm substrates for metazoans to inhabit. It is further hypothesized that the dynamic redox condition in the latest Ediacaran, with the non-continuous rise in oxygen concentration and periods of hypoxia, may have created ideal conditions for SOB to thrive.
前寒武纪丝状微生物化石普遍存在且种类繁多。然而,由于它们的整体形状简单,通常缺乏诊断特征,因此其分类归属可能具有一定难度。本文报道了巴西伊塔雅伊盆地埃迪卡拉纪(563 Ma)保存完好的大型丝状印痕群落。这些丝状微生物为单列式(无分支),宽度可达 200 µm,长度可达 44 mm。它们可以呈密集或稀疏分布的表面存在,且通常具有一致的定向。尽管形状简单,但它们的定向排列表明它们被固定在海底,并且其整体柔韧性(如弯曲、折叠和扭曲)支持其具有生物起源(而非沉积起源)。与现代丝状生物群的生物计量学比较进一步支持了它们的生物亲缘关系,表明它们与大型硫氧化细菌(SOB)或真核生物有关。其他形态和古生态学特征进一步证实了它们与现代大型丝状 SOB 的相似性。它们广泛存在并与复杂的埃迪卡拉纪大型生物群(如叶状生物)相关联,这表明它们可能通过为后生动物提供栖息的坚实基质,在前寒武纪晚期的生态动态中发挥了重要作用。进一步假设,在最新的埃迪卡拉纪时期,由于氧气浓度的非连续上升和缺氧期,动态氧化还原条件可能为 SOB 的繁荣创造了理想的条件。