Cara Magnabosco, Fatima Husain, Madeline M. Paoletti, Chris Parsons, Jack G. Payette, Sarah L. Schwartz, Erik Tamre, Gregory P. Fournier
{"title":"迈向微生物生命的自然史","authors":"Cara Magnabosco, Fatima Husain, Madeline M. Paoletti, Chris Parsons, Jack G. Payette, Sarah L. Schwartz, Erik Tamre, Gregory P. Fournier","doi":"10.1146/annurev-earth-031621-070542","DOIUrl":null,"url":null,"abstract":"For most of Earth's history life was microbial, with archaeal and bacterial cells mediating biogeochemical cycles through their metabolisms and ecologies. This diversity was sufficient to maintain a habitable planet across dramatic environmental transitions during the Archean and Proterozoic Eons. However, our knowledge of the first 3 billion years of the biosphere pales in comparison to the rich narrative of complex life documented through the Phanerozoic geological record. In this review, we attempt to lay out a microbial natural history framework that highlights recent and ongoing research unifying microbiology, geochemistry, and traditional organismal evolutionary biology, and we propose six broadly applicable principles to aid in these endeavors. In this way, the evolutionary history of microbial life—once considered only a prelude to the much more storied history of complex metazoan life in the Phanerozoic—is finally coming into its own. ▪The outlines of microbial natural history are now starting to appear through the integration of genomic and geological records.▪Microorganisms drive Earth's biogeochemical cycles, and their natural history reflects a coevolution with the planet.▪Past environmental changes have induced microbial biotic transitions, marked by extinction, taxonomic shifts, and new metabolisms and ecologies.▪Microbial evolution can benefit from a historical perspective of processes and successions as established by macropaleontology.","PeriodicalId":8034,"journal":{"name":"Annual Review of Earth and Planetary Sciences","volume":"102 1","pages":""},"PeriodicalIF":11.3000,"publicationDate":"2024-07-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Toward a Natural History of Microbial Life\",\"authors\":\"Cara Magnabosco, Fatima Husain, Madeline M. Paoletti, Chris Parsons, Jack G. Payette, Sarah L. Schwartz, Erik Tamre, Gregory P. Fournier\",\"doi\":\"10.1146/annurev-earth-031621-070542\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"For most of Earth's history life was microbial, with archaeal and bacterial cells mediating biogeochemical cycles through their metabolisms and ecologies. This diversity was sufficient to maintain a habitable planet across dramatic environmental transitions during the Archean and Proterozoic Eons. However, our knowledge of the first 3 billion years of the biosphere pales in comparison to the rich narrative of complex life documented through the Phanerozoic geological record. In this review, we attempt to lay out a microbial natural history framework that highlights recent and ongoing research unifying microbiology, geochemistry, and traditional organismal evolutionary biology, and we propose six broadly applicable principles to aid in these endeavors. In this way, the evolutionary history of microbial life—once considered only a prelude to the much more storied history of complex metazoan life in the Phanerozoic—is finally coming into its own. ▪The outlines of microbial natural history are now starting to appear through the integration of genomic and geological records.▪Microorganisms drive Earth's biogeochemical cycles, and their natural history reflects a coevolution with the planet.▪Past environmental changes have induced microbial biotic transitions, marked by extinction, taxonomic shifts, and new metabolisms and ecologies.▪Microbial evolution can benefit from a historical perspective of processes and successions as established by macropaleontology.\",\"PeriodicalId\":8034,\"journal\":{\"name\":\"Annual Review of Earth and Planetary Sciences\",\"volume\":\"102 1\",\"pages\":\"\"},\"PeriodicalIF\":11.3000,\"publicationDate\":\"2024-07-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Annual Review of Earth and Planetary Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1146/annurev-earth-031621-070542\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ASTRONOMY & ASTROPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Annual Review of Earth and Planetary Sciences","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1146/annurev-earth-031621-070542","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
For most of Earth's history life was microbial, with archaeal and bacterial cells mediating biogeochemical cycles through their metabolisms and ecologies. This diversity was sufficient to maintain a habitable planet across dramatic environmental transitions during the Archean and Proterozoic Eons. However, our knowledge of the first 3 billion years of the biosphere pales in comparison to the rich narrative of complex life documented through the Phanerozoic geological record. In this review, we attempt to lay out a microbial natural history framework that highlights recent and ongoing research unifying microbiology, geochemistry, and traditional organismal evolutionary biology, and we propose six broadly applicable principles to aid in these endeavors. In this way, the evolutionary history of microbial life—once considered only a prelude to the much more storied history of complex metazoan life in the Phanerozoic—is finally coming into its own. ▪The outlines of microbial natural history are now starting to appear through the integration of genomic and geological records.▪Microorganisms drive Earth's biogeochemical cycles, and their natural history reflects a coevolution with the planet.▪Past environmental changes have induced microbial biotic transitions, marked by extinction, taxonomic shifts, and new metabolisms and ecologies.▪Microbial evolution can benefit from a historical perspective of processes and successions as established by macropaleontology.
期刊介绍:
Since its establishment in 1973, the Annual Review of Earth and Planetary Sciences has been dedicated to providing comprehensive coverage of advancements in the field. This esteemed publication examines various aspects of earth and planetary sciences, encompassing climate, environment, geological hazards, planet formation, and the evolution of life. To ensure wider accessibility, the latest volume of the journal has transitioned from a gated model to open access through the Subscribe to Open program by Annual Reviews. Consequently, all articles published in this volume are now available under the Creative Commons Attribution (CC BY) license.