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
{"title":"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","authors":"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","doi":"10.1016/j.precamres.2025.107823","DOIUrl":null,"url":null,"abstract":"<div><div>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 <em>Arctacellularia</em> 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 <em>Arctacellularia</em> 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 <em>Arctacellularia tetragonala</em>, with one trichome showing evidence of a possible nodal cell indicative of branching, and <em>Arctacellularia ellipsoidea</em>, distinguished by the presence/absence of barrel-like to long cylindrical cells (with a length/width ratio ≥ 1.5). <em>Arctacellularia</em> 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 <em>Arctacellularia</em> is achieved by a combination of common membrane, terminal folds, and siphonous construction. Furthermore, the dichotomous branching of <em>Arctacellularia</em> appears morphologically more primitive than those observed in other Pre-Cryogenian fossils, including <em>Cheilofilum</em>, <em>Jacutianema</em>, and <em>Proterocladus</em>. Given that <em>Arctacellularia</em> has been phylogenetically placed in the total group of Archaeplastida and the oldest <em>Arctacellularia</em> 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.</div></div>","PeriodicalId":49674,"journal":{"name":"Precambrian Research","volume":"425 ","pages":"Article 107823"},"PeriodicalIF":3.2000,"publicationDate":"2025-05-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"One-billion-year-old eukaryotic algal fossil Arctacellularia from North China and its implications for the evolution of pre-Cryogenian filamentous multicellularity\",\"authors\":\"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\",\"doi\":\"10.1016/j.precamres.2025.107823\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>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 <em>Arctacellularia</em> 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 <em>Arctacellularia</em> 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 <em>Arctacellularia tetragonala</em>, with one trichome showing evidence of a possible nodal cell indicative of branching, and <em>Arctacellularia ellipsoidea</em>, distinguished by the presence/absence of barrel-like to long cylindrical cells (with a length/width ratio ≥ 1.5). <em>Arctacellularia</em> 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 <em>Arctacellularia</em> is achieved by a combination of common membrane, terminal folds, and siphonous construction. Furthermore, the dichotomous branching of <em>Arctacellularia</em> appears morphologically more primitive than those observed in other Pre-Cryogenian fossils, including <em>Cheilofilum</em>, <em>Jacutianema</em>, and <em>Proterocladus</em>. Given that <em>Arctacellularia</em> has been phylogenetically placed in the total group of Archaeplastida and the oldest <em>Arctacellularia</em> 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.</div></div>\",\"PeriodicalId\":49674,\"journal\":{\"name\":\"Precambrian Research\",\"volume\":\"425 \",\"pages\":\"Article 107823\"},\"PeriodicalIF\":3.2000,\"publicationDate\":\"2025-05-27\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Precambrian Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0301926825001494\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Precambrian Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0301926825001494","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
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.
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.