Clément G. L. Pollier, Alejandro N. Guerrero, Jorge Rabassa, Daniel Ariztegui
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This study explores the environmental and biological factors shaping microbialite macrostructure by analysing the distribution of dominant morphotypes across the basin. Concurrently, it examines the internal mesostructure and microstructure of microbialites in association with prevailing algal–microbial communities. The incremental development of these communities contributes to the distinct crater‐like morphology observed in microbialites from Laguna de Los Cisnes. The mineral encrustation of the green alga <jats:italic>Percursaria percursa</jats:italic> emerges as a primary driver of lithification, evidenced by the preservation of microfossils within the microstructure of the microbialites. Simultaneously, physical environmental factors, including waves, Langmuir cells and accommodation space influence the location of the algal–microbial carbonate factory, determining the spatial distribution and temporal succession of different crater architecture variants. Laguna de Los Cisnes, hosting well‐preserved subfossil outcrops and living microbialites, serves as a remarkable living laboratory for understanding microbialite morphogenesis. This study contributes to a novel model that captures the fundamental role of algal–microbial communities in determining the primary macrostructural architecture of microbialites before environmental factors come into play, merely reshaping this architecture into different morphotypes.","PeriodicalId":2,"journal":{"name":"ACS Applied Bio Materials","volume":null,"pages":null},"PeriodicalIF":4.6000,"publicationDate":"2024-03-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The hidden biotic face of microbialite morphogenesis – a case study from Laguna de Los Cisnes, southernmost Patagonia (Chile)\",\"authors\":\"Clément G. L. Pollier, Alejandro N. 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引用次数: 0
摘要
微生物岩提供了地球早期生态系统的地质证据,记录了共同进化的生命与环境之间长期存在的相互作用。然而,经过 100 多年的研究,关于微生物岩生长所涉及的环境和生物力量之间复杂的相互作用仍存在争议。位于智利巴塔哥尼亚火地岛的洛斯西内斯湖(Laguna de Los Cisnes)为研究这些相互作用提供了一个独特的机会。该湖大约在 1 万年前开始结冰,湖中的碳酸盐微生物岩是由藻类微生物群落形成的。从宏观上看,有机沉积物呈现出一致的原生火山口状结构,并呈现出盘状、半球状、柱状和透镜状等宏观结构变化。本研究通过分析整个盆地的主要形态分布,探讨了形成微生物岩宏观结构的环境和生物因素。同时,研究还将微生物岩的内部中观结构和微观结构与当时的藻类微生物群落联系起来。这些群落的渐进式发展造就了在洛斯西斯内湖微生物岩中观察到的独特的火山口状形态。绿藻 Percursaria percursa 的矿物包壳是岩化的主要驱动力,微生物岩微结构中保存的微化石就是证明。同时,物理环境因素,包括波浪、朗缪尔细胞和容纳空间影响着藻类微生物碳酸盐工厂的位置,决定着不同火山口结构变体的空间分布和时间演替。洛斯西内斯湖(Laguna de Los Cisnes)拥有保存完好的亚化石露头和活的微生物岩,是了解微生物岩形态发生的重要活实验室。这项研究提供了一个新的模型,该模型捕捉到了藻类-微生物群落在决定微生物岩的主要宏观结构构造方面的基本作用,然后环境因素才发挥作用,将这种构造重塑为不同的形态。
The hidden biotic face of microbialite morphogenesis – a case study from Laguna de Los Cisnes, southernmost Patagonia (Chile)
Microbialites provide geological evidence into Earth's early ecosystems, recording long‐standing interactions between co‐evolving life and the environment. Yet, after more than 100 years of research, the complex interplay between environmental and biological forces involved in microbialite growth is still debated. Laguna de Los Cisnes, located in Chilean Tierra del Fuego, Patagonia, provides a unique opportunity to study these interactions. This lake, which became ice‐free around 10 000 years ago, features carbonate microbialites developed by algal–microbial communities. Macroscopically, the organo‐sedimentary deposits exhibit a consistent primary crater‐like architecture, showcasing macrostructural variations such as dish‐shaped, hemispherical, columnar and lenticular morphologies. This study explores the environmental and biological factors shaping microbialite macrostructure by analysing the distribution of dominant morphotypes across the basin. Concurrently, it examines the internal mesostructure and microstructure of microbialites in association with prevailing algal–microbial communities. The incremental development of these communities contributes to the distinct crater‐like morphology observed in microbialites from Laguna de Los Cisnes. The mineral encrustation of the green alga Percursaria percursa emerges as a primary driver of lithification, evidenced by the preservation of microfossils within the microstructure of the microbialites. Simultaneously, physical environmental factors, including waves, Langmuir cells and accommodation space influence the location of the algal–microbial carbonate factory, determining the spatial distribution and temporal succession of different crater architecture variants. Laguna de Los Cisnes, hosting well‐preserved subfossil outcrops and living microbialites, serves as a remarkable living laboratory for understanding microbialite morphogenesis. This study contributes to a novel model that captures the fundamental role of algal–microbial communities in determining the primary macrostructural architecture of microbialites before environmental factors come into play, merely reshaping this architecture into different morphotypes.