2023
DOI: 10.3389/fmicb.2023.1097712
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Emission of cyanobacterial volatile organic compounds and their roles in blooms

Abstract: Cyanobacteria are photosynthetic prokaryotes and one of dominant species in eutrophicated waters, which easily burst blooms in summer with high irradiance and temperature conditions. In response to high irradiance, high temperature, and nutrient conditions, cyanobacteria release abundant of volatile organic compounds (VOCs) by up-regulating related gene expression and oxidatively degrading β-carotene. These VOCs not only increase offensive odor in waters, but also transfer allelopathic signals to algae and aqu… Show more

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Cited by 10 publications
(3 citation statements)
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“…The best geochemical evidence presently available suggests that this light would have been present on Earth's surface from before the origin of life (at ∼3.9 Ga) and for at least 1000 (perhaps even for 1500 [34]) million years until organisms evolved oxygenic photosynthesis which saturated available oxygen sinks [34,35,37], leading to a protective ozone layer in the stratosphere. Additionally, cyanobacteria (and today's plants) emit volatile organic compounds (VOCs) which, together with atmospheric oxides of nitrogen, are the precursors for photochemical production of ozone in the troposphere [38,39]. Oxygen and ozone are thus considered here as biology-procured pigments, today dissipating the UV-C region in the upper atmosphere, thereby allowing the present dissipative structuring of the more delicate (i.e., prone to UV-C disassociation) complex biosynthetic pathways producing visible pigments at Earth's surface using multiple visible photons of lower energy but of much higher intensity.…”
Section: The Photochemistry Of Organic Moleculesmentioning
confidence: 99%
“…The best geochemical evidence presently available suggests that this light would have been present on Earth's surface from before the origin of life (at ∼3.9 Ga) and for at least 1000 (perhaps even for 1500 [34]) million years until organisms evolved oxygenic photosynthesis which saturated available oxygen sinks [34,35,37], leading to a protective ozone layer in the stratosphere. Additionally, cyanobacteria (and today's plants) emit volatile organic compounds (VOCs) which, together with atmospheric oxides of nitrogen, are the precursors for photochemical production of ozone in the troposphere [38,39]. Oxygen and ozone are thus considered here as biology-procured pigments, today dissipating the UV-C region in the upper atmosphere, thereby allowing the present dissipative structuring of the more delicate (i.e., prone to UV-C disassociation) complex biosynthetic pathways producing visible pigments at Earth's surface using multiple visible photons of lower energy but of much higher intensity.…”
Section: The Photochemistry Of Organic Moleculesmentioning
confidence: 99%
“…Cyanobacteria, commonly known as blue-green algae, are single-celled or filamentous organisms capable of oxygenic photosynthesis [1][2][3]. They thrive in various environments, such as soils, freshwater bodies, thermal springs, and marine ecosystems [4].…”
Section: Introductionmentioning
confidence: 99%
“…Among these VOCs, terpenes are the primary type, with isoprene and monoterpenes as the major components and sesquiterpenes and diterpenes as the minor components [11,12]. For isoprene and monoterpenes, they are synthesized via the methylerythritol 4-phosphate pathway (MEP) [13,14]. Tobacco (Nicotiana tabacum) and Arabidopsis thaliana did not release isoprene, but the plants transferred into the isoprene synthase gene (ISPS) gradually increased isoprene emission with temperature elevation [11].…”
Section: Introductionmentioning
confidence: 99%