华北10亿年真核藻类化石Arctacellularia及其对前低温系丝状多细胞生物进化的意义

IF 3.2 2区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Rui Huang , Guangjin Li , Jiayue Wang , Qing Tang , Mingyang Qiu , Qian Chen , Hanzhi Qu , Chengxi Wu , Wenfei Cui , Xianqin Yan , Chuanming Zhou , Xunlai Yuan , Ke Pang
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引用次数: 0

摘要

具有精细细胞保存的前低温期有机壁微化石可以为多细胞真核生物的起源和早期进化提供关键信息。根据先前报道的证据,真正的二分分支和光合作用,丝状化石Arctacellularia是前低温期明确的多细胞藻类的少数例子之一。然而,该属的分类多样性几十年来一直存在争议,其对真核生物丝状多细胞和分支的出现和维持的进化意义尚未得到充分探讨。本文报道了在皖北淮南地区早第三纪六老北组(~ 0.95 ~ 0.92 Ga)岩心样品中提取的保存完好的Arctacellularia化石。在六老北组中发现了两个种,包括模式种Arctacellularia tetragonala,其中一个毛状体显示可能的节细胞,表明分支,以及Arctacellularia ellipsoidea,以桶状到长圆柱形细胞(长/宽比≥1.5)的存在或不存在为特征。本研究重建了单列多细胞丝状生物,由共同的膜包裹;它由三种可能分化的细胞组成,其特征是末端折叠(或末端延伸),偶尔可以通过节细胞分叉一次。本研究表明,丝状多细胞的维持是通过共同膜、末端褶皱和虹吸结构的结合来实现的。此外,与Cheilofilum、Jacutianema和Proterocladus等前低温纪化石相比,Arctacellularia的二分分支在形态上更为原始。考虑到在系统发育上,Arctacellularia被归为始祖菌的总类群,而最古老的Arctacellularia标本可以追溯到~ 1.7-1.4 Ga,如果证实中元古代早期的材料与早期的Tonian同类生物具有生物学同一性,这表明,至少在14亿年前,Archaeplastida可能已经获得了多细胞、管状结构、细胞分化和分支。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
One-billion-year-old eukaryotic algal fossil Arctacellularia from North China and its implications for the evolution of pre-Cryogenian filamentous multicellularity
Pre-Cryogenian organic-walled microfossils with delicate cellular preservation can provide pivotal information for the origin and early evolution of multicellular eukaryotes. With previously reported evidence for true dichotomous branching and photosynthesis, the filamentous fossil Arctacellularia is among one of the few examples of pre-Cryogenian unambiguous multicellular algae. However, the taxonomic diversity of this genus has remained controversial for decades, and its evolutionary implications for understanding the emergence and maintenance of filamentous multicellularity and branching in eukaryotes have been underexplored. Here, we report well-preserved Arctacellularia fossils extracted from the drill core samples of the early Tonian Liulaobei Formation (∼0.95–0.92 Ga), Huainan region, northern Anhui Province, North China. Two species have been recognized in the Liulaobei Formation, including the type species Arctacellularia tetragonala, with one trichome showing evidence of a possible nodal cell indicative of branching, and Arctacellularia ellipsoidea, distinguished by the presence/absence of barrel-like to long cylindrical cells (with a length/width ratio ≥ 1.5). Arctacellularia is reconstructed as a uniserial multicellular filamentous organism enveloped by common membrane in this study; it consists of three types of possibly differentiated cells that are characterized by terminal folds (or terminal extensions), and can occasionally bifurcate once via a nodal cell. This study suggests that the maintenance of filamentous multicellularity of Arctacellularia is achieved by a combination of common membrane, terminal folds, and siphonous construction. Furthermore, the dichotomous branching of Arctacellularia appears morphologically more primitive than those observed in other Pre-Cryogenian fossils, including Cheilofilum, Jacutianema, and Proterocladus. Given that Arctacellularia has been phylogenetically placed in the total group of Archaeplastida and the oldest Arctacellularia specimens date back to ∼1.7–1.4 Ga, if the early Mesoproterozoic material is confirmed to be biologically congeneric with the early Tonian counterpart, it suggests that Archaeplastida may have acquired multicellularity, siphonous construction, cellular differentiation, and possibly branching at least 1.4 billion years ago.
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来源期刊
Precambrian Research
Precambrian Research 地学-地球科学综合
CiteScore
7.20
自引率
28.90%
发文量
325
审稿时长
12 months
期刊介绍: Precambrian Research publishes studies on all aspects of the early stages of the composition, structure and evolution of the Earth and its planetary neighbours. With a focus on process-oriented and comparative studies, it covers, but is not restricted to, subjects such as: (1) Chemical, biological, biochemical and cosmochemical evolution; the origin of life; the evolution of the oceans and atmosphere; the early fossil record; palaeobiology; (2) Geochronology and isotope and elemental geochemistry; (3) Precambrian mineral deposits; (4) Geophysical aspects of the early Earth and Precambrian terrains; (5) Nature, formation and evolution of the Precambrian lithosphere and mantle including magmatic, depositional, metamorphic and tectonic processes. In addition, the editors particularly welcome integrated process-oriented studies that involve a combination of the above fields and comparative studies that demonstrate the effect of Precambrian evolution on Phanerozoic earth system processes. Regional and localised studies of Precambrian phenomena are considered appropriate only when the detail and quality allow illustration of a wider process, or when significant gaps in basic knowledge of a particular area can be filled.
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