{"title":"美国犹他州大盐湖的真菌:空间调查。","authors":"David L Parrott, Bonnie K Baxter","doi":"10.3389/ffunb.2024.1438347","DOIUrl":null,"url":null,"abstract":"<p><p>The natural system at Great Salt Lake, Utah, USA was augmented by the construction of a rock-filled railroad causeway in 1960, creating two lakes at one site. The north arm is sequestered from the mountain snowmelt inputs and thus became saturated with salts (250-340 g/L). The south arm is a flourishing ecosystem with moderate salinity (90-190 g/L) and a significant body of water for ten million birds on the avian flyways of the western US who engorge themselves on the large biomass of brine flies and shrimp. The sediments around the lake shores include calcium carbonate oolitic sand and clay, and further away from the saltwater margins, a zone with less saline soil. Here a small number of plants can thrive, including <i>Salicornia</i> and <i>Sueda</i> species. At the north arm at Rozel Point, halite crystals precipitate in the salt-saturated lake water, calcium sulfate precipitates to form gypsum crystals embedded in the clay, and high molecular weight asphalt seeps from the ground. It is an ecosystem with gradients and extremes, and fungi are up to the challenge. We have collected data on Great Salt Lake fungi from a variety of studies and present them here in a spatial survey. Combining knowledge of cultivation studies as well as environmental DNA work, we discuss the genera prevalent in and around this unique ecosystem. A wide diversity of taxa were found in multiple microniches of the lake, suggesting significant roles for these genera: <i>Acremonium, Alternaria</i>, <i>Aspergillus</i>, <i>Cladosporium</i>, <i>Clydae</i>, <i>Coniochaeta</i>, <i>Cryptococcus</i>, <i>Malassezia</i>, <i>Nectria</i>, <i>Penicillium</i>, <i>Powellomyces</i>, <i>Rhizophlyctis</i>, and <i>Wallemia</i>. Considering the species present and the features of Great Salt Lake as a terminal basin, we discuss of the possible roles of the fungi. These include not only nutrient cycling, toxin mediation, and predation for the ecosystem, but also roles that would enable other life to thrive in the water and on the shore. Many genera that we discovered may help other organisms in alleviating salinity stress, promoting growth, or affording protection from dehydration. The diverse taxa of Great Salt Lake fungi provide important benefits for the ecosystem.</p>","PeriodicalId":73084,"journal":{"name":"Frontiers in fungal biology","volume":"5 ","pages":"1438347"},"PeriodicalIF":2.1000,"publicationDate":"2024-09-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC11427377/pdf/","citationCount":"0","resultStr":"{\"title\":\"Fungi of Great Salt Lake, Utah, USA: a spatial survey.\",\"authors\":\"David L Parrott, Bonnie K Baxter\",\"doi\":\"10.3389/ffunb.2024.1438347\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p><p>The natural system at Great Salt Lake, Utah, USA was augmented by the construction of a rock-filled railroad causeway in 1960, creating two lakes at one site. The north arm is sequestered from the mountain snowmelt inputs and thus became saturated with salts (250-340 g/L). The south arm is a flourishing ecosystem with moderate salinity (90-190 g/L) and a significant body of water for ten million birds on the avian flyways of the western US who engorge themselves on the large biomass of brine flies and shrimp. The sediments around the lake shores include calcium carbonate oolitic sand and clay, and further away from the saltwater margins, a zone with less saline soil. Here a small number of plants can thrive, including <i>Salicornia</i> and <i>Sueda</i> species. At the north arm at Rozel Point, halite crystals precipitate in the salt-saturated lake water, calcium sulfate precipitates to form gypsum crystals embedded in the clay, and high molecular weight asphalt seeps from the ground. It is an ecosystem with gradients and extremes, and fungi are up to the challenge. We have collected data on Great Salt Lake fungi from a variety of studies and present them here in a spatial survey. Combining knowledge of cultivation studies as well as environmental DNA work, we discuss the genera prevalent in and around this unique ecosystem. A wide diversity of taxa were found in multiple microniches of the lake, suggesting significant roles for these genera: <i>Acremonium, Alternaria</i>, <i>Aspergillus</i>, <i>Cladosporium</i>, <i>Clydae</i>, <i>Coniochaeta</i>, <i>Cryptococcus</i>, <i>Malassezia</i>, <i>Nectria</i>, <i>Penicillium</i>, <i>Powellomyces</i>, <i>Rhizophlyctis</i>, and <i>Wallemia</i>. Considering the species present and the features of Great Salt Lake as a terminal basin, we discuss of the possible roles of the fungi. These include not only nutrient cycling, toxin mediation, and predation for the ecosystem, but also roles that would enable other life to thrive in the water and on the shore. Many genera that we discovered may help other organisms in alleviating salinity stress, promoting growth, or affording protection from dehydration. 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引用次数: 0
摘要
美国犹他州大盐湖的自然系统在 1960 年修建了一条填满岩石的铁路堤道,从而在一个地点形成了两个湖泊。北侧的湖泊受到高山融雪的阻隔,因此盐分饱和(250-340 克/升)。南臂是一个繁荣的生态系统,盐度适中(90-190 克/升),是美国西部鸟类迁徙路线上千万只鸟类的重要水域,这些鸟类在这里捕食大量的卤水蝇和虾。湖岸周围的沉积物包括碳酸钙鲕状沙和粘土,离咸水边缘更远的地方则是盐碱较少的土壤区。这里有少量植物可以繁衍生息,包括盐生植物和水田植物。在罗泽尔角的北臂,盐饱和的湖水中会析出海绿石晶体,硫酸钙析出形成石膏晶体嵌在粘土中,高分子量的沥青从地下渗出。这是一个具有梯度和极端性的生态系统,而真菌可以应对这一挑战。我们从各种研究中收集了有关大盐湖真菌的数据,并在这里以空间调查的形式展示出来。结合栽培研究和环境 DNA 工作的知识,我们讨论了这一独特生态系统中及周边地区普遍存在的菌属。我们在湖泊的多个微区发现了多种分类群,这表明这些菌属发挥了重要作用:这些菌属包括:Acremonium、Alternaria、Aspergillus、Cladosporium、Clydae、Coniochaeta、Cryptococcus、Malassezia、Nectria、Penicillium、Powellomyces、Rhizophlyctis 和 Wallemia。考虑到存在的物种和大盐湖作为终端流域的特点,我们讨论了真菌可能发挥的作用。这些作用不仅包括营养循环、毒素调解和生态系统捕食,还包括使其他生物在水中和岸上繁衍生息的作用。我们发现的许多菌属可能有助于其他生物减轻盐度压力、促进生长或提供脱水保护。大盐湖真菌类群的多样性为生态系统提供了重要的益处。
Fungi of Great Salt Lake, Utah, USA: a spatial survey.
The natural system at Great Salt Lake, Utah, USA was augmented by the construction of a rock-filled railroad causeway in 1960, creating two lakes at one site. The north arm is sequestered from the mountain snowmelt inputs and thus became saturated with salts (250-340 g/L). The south arm is a flourishing ecosystem with moderate salinity (90-190 g/L) and a significant body of water for ten million birds on the avian flyways of the western US who engorge themselves on the large biomass of brine flies and shrimp. The sediments around the lake shores include calcium carbonate oolitic sand and clay, and further away from the saltwater margins, a zone with less saline soil. Here a small number of plants can thrive, including Salicornia and Sueda species. At the north arm at Rozel Point, halite crystals precipitate in the salt-saturated lake water, calcium sulfate precipitates to form gypsum crystals embedded in the clay, and high molecular weight asphalt seeps from the ground. It is an ecosystem with gradients and extremes, and fungi are up to the challenge. We have collected data on Great Salt Lake fungi from a variety of studies and present them here in a spatial survey. Combining knowledge of cultivation studies as well as environmental DNA work, we discuss the genera prevalent in and around this unique ecosystem. A wide diversity of taxa were found in multiple microniches of the lake, suggesting significant roles for these genera: Acremonium, Alternaria, Aspergillus, Cladosporium, Clydae, Coniochaeta, Cryptococcus, Malassezia, Nectria, Penicillium, Powellomyces, Rhizophlyctis, and Wallemia. Considering the species present and the features of Great Salt Lake as a terminal basin, we discuss of the possible roles of the fungi. These include not only nutrient cycling, toxin mediation, and predation for the ecosystem, but also roles that would enable other life to thrive in the water and on the shore. Many genera that we discovered may help other organisms in alleviating salinity stress, promoting growth, or affording protection from dehydration. The diverse taxa of Great Salt Lake fungi provide important benefits for the ecosystem.