10.17
Mikroben und der Schwefelkreislauf
Schwefel ist ein lebenswichtiges Element in den biogeochemischen Systemen der Erde. Es durchläuft verschiedene anorganische Zustände, darunter Sulfat…
Anorganischer Schwefel zirkuliert durch die Umwelt als Sulfat, elementarer Schwefel und Schwefel.
Vulkane und hydrothermale Quellen stoßen Schwefelgase wie Schwefelwasserstoff aus und leisten so wichtige Beiträge zum Schwefelkreislauf.
Zum Beispiel wandeln sulfatreduzierende Bakterien in anoxischen, organisch reichen Umgebungen nahe hydrothermalen Quellen Sulfat hauptsächlich in Schwefelwasserstoff um.
Dieses Gas, das für die meisten Lebensformen giftig ist, wird von verschiedenen Mikroorganismen in weniger schädliche Sulfate oder elementaren Schwefel umgewandelt.
Unter sauerstoffreichen Bedingungen wandeln schwefeloxidierende Bakterien wie Thiobacillus Schwefelwasserstoff in Schwefel oder Sulfat um, wobei manchmal Schwefelsäure entsteht und der lokale pH-Wert sinkt.
Grüne und violette Schwefelbakterien hingegen wandeln Sulfid in Schwefelkörner um, die Thiomargarita und ähnliche Mikroben weiter zu Sulfat oxidieren.
Elementarer Schwefel kann durch spezialisierte anaerbe Bakterien und Archaeen wieder zu Sulfid umgewandelt werden.
Neben anorganischen Umwandlungen bilden Meeresalgen Dimethylsulfid, eine flüchtige organische Schwefelverbindung, die in der Atmosphäre in Aerosole umgewandelt wird, die die Wolkenbildung fördern und das Erdklima regulieren.
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Q1: What are the main inorganic forms of sulfur in the environment?
Sulfur cycles through the environment in three primary inorganic states: sulfate (SO₄²⁻), the most oxidized form stored in rocks and marine sediments; elemental sulfur (S⁰), an intermediate form; and sulfide (S²⁻), the most reduced form. These transitions occur through both abiotic processes like volcanic emissions and biological transformations mediated by microorganisms across oxic and anoxic environments.
Q2: How do sulfate-reducing bacteria contribute to the sulfur cycle?
In anoxic environments, sulfate-reducing bacteria like Desulfovibrio spp. perform dissimilatory sulfate reduction, converting sulfate to sulfide through sulfite as an intermediate. This process is coupled with organic carbon oxidation and occurs in oxygen-poor conditions near hydrothermal vents and organic-rich sediments, releasing hydrogen sulfide gas that is subsequently transformed by other microorganisms.
Q3: What role do sulfur-oxidizing bacteria play in aerobic environments?
Chemolithoautotrophic bacteria such as Thiobacillus oxidize reduced sulfur compounds like hydrogen sulfide to elemental sulfur or sulfate in oxygen-rich conditions. Green and purple sulfur bacteria convert sulfide into intracellular sulfur granules, which Thiomargarita and similar microbes further oxidize to sulfate. This oxidation sometimes produces sulfuric acid, lowering local pH and making these environments acidic.
Q4: How does dimethyl sulfide affect Earth's climate?
Marine algae produce dimethylsulfoniopropionate (DMSP), which bacteria cleave to form dimethyl sulfide (DMS), a volatile organic sulfur compound. When DMS enters the atmosphere, photooxidation converts it to sulfate aerosols that promote cloud formation and influence cloud condensation. These aerosols help regulate Earth's climate and contribute to atmospheric sulfur deposition onto terrestrial ecosystems.
Q5: What is the ecological significance of sulfur-oxidizing chemoautotrophs at hydrothermal vents?
At hydrothermal vent ecosystems, sulfur-oxidizing chemoautotrophs harness energy from sulfide oxidation to fix carbon dioxide, supporting complex microbial and faunal communities in deep-sea habitats. These microorganisms form the foundation of chemosynthetic food webs, enabling life to thrive in environments lacking sunlight by converting chemical energy from reduced sulfur compounds into usable biological energy.
Q6: How do microorganisms complete the sulfur cycle by synthesizing sulfur-containing compounds?
Plants and microbes assimilate sulfate and reduce it while synthesizing sulfur-containing amino acids such as cysteine and methionine. This process completes the sulfur cycle by incorporating inorganic sulfur into organic molecules. These amino acids are essential for protein synthesis and cellular function across all domains of life.
Q7: Why is the sulfur cycle important alongside other elemental cycles?
The sulfur cycle is a vital biogeochemical process that works in conjunction with other elemental cycles to regulate nutrient availability and energy flow through ecosystems. Sulfur transformations by microorganisms influence pH, support chemosynthetic communities, and contribute to atmospheric composition and climate regulation, making it essential for ecosystem function and global biogeochemical balance.