10.18
Mikroben und andere Elementarzyklen
Mikrobielle Aktivität spielt eine entscheidende Rolle im biogeochemischen Kreislauf von Eisen und Mangan, insbesondere bei den Redoxgradienten, die fü…
Mikroben treiben den Kreislauf von Eisen und Mangan an, indem sie diese Elemente zwischen ihrer oxidierten und reduzierten Form verschieben.
In neutralen, sauerstoffreichen Lebensräumen dominiert Eiseneisen in unlöslicher, ausgefällter Form.
Einige Bakterien produzieren kleine Moleküle, sogenannte Siderophore, die an Eiseneisen binden und löslich machen.
Die Zellen nehmen dann dieses lösliche Eisen auf und reduzieren es in die eisenhaltige Form für den metabolischen Gebrauch.
An der oxisch-anoxischen Grenzfläche, wo der Sauerstoffgehalt niedrig ist, nutzen magnetotaktische Bakterien wie Magnetospirillum Eisen, um Magnetitkristalle zu bilden, die sich mit dem Erdmagnetfeld ausrichten, um anoxische Schichten zu erreichen.
In derselben Zone oxidieren filamentöse Bakterien wie Leptothrix eisenhaltiges Eisen und bilden mit Eisenoxiden beschichtete Hüllen.
Sie oxidieren außerdem Mangan(II) zu unlöslichem Mangandioxid, das in tiefere anoxische Schichten absinken kann, wo metallreduzierende Bakterien wie Geobacter es wieder in Mangan (II) umwandeln.
In anoxischen Zonen führen Bakterien wie Shewanella eine dissimilatorische Eisenreduktion durch, wobei Eiseneisen der terminale Elektronenakzeptor ist.
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Q1: How do bacteria access iron in oxygen-rich environments?
In neutral, oxygen-rich habitats, iron exists as insoluble ferric iron. Bacteria secrete siderophores—small organic molecules with high affinity for ferric iron—that bind and solubilize it. Cells then take up this soluble iron and reduce it to ferrous form for metabolic use.
Q2: What role do magnetotactic bacteria play in iron cycling?
Magnetotactic bacteria like Magnetospirillum inhabit the oxic-anoxic interface where oxygen levels are low. They internalize iron to form magnetite crystals that act as intracellular compasses, aligning with Earth's magnetic field to guide cells toward anoxic layers optimal for their metabolism.
Q3: How do filamentous bacteria contribute to manganese cycling?
Filamentous bacteria such as Leptothrix oxidize soluble manganous ions into insoluble manganese dioxide at the oxic-anoxic interface. This manganese dioxide sinks into underlying anoxic sediments, where metal-reducing bacteria like Geobacter enzymatically reduce it back to manganous form, completing the cycle.
Q4: What is the function of iron oxide sheaths produced by Leptothrix?
Leptothrix bacteria oxidize ferrous iron and produce extracellular iron oxide sheaths. These sheaths serve dual purposes: they prevent cell encrustation and provide structural support, allowing bacteria to thrive at the oxic-anoxic interface where redox conditions fluctuate.
Q5: How do metal-reducing bacteria like Shewanella obtain energy in anoxic zones?
In anoxic zones, bacteria like Shewanella perform dissimilatory iron reduction, using ferric iron as the terminal electron acceptor. This metabolic process allows them to extract energy from iron reduction, supporting growth and cellular functions in oxygen-depleted environments.
Q6: Why are redox gradients important for microbial iron and manganese cycling?
Redox gradients in stratified aquatic environments create distinct zones where microbes exploit different oxidation states of iron and manganese for metabolic energy. These gradients enable diverse bacterial communities to thrive at different depths, collectively maintaining metal homeostasis and availability across ecosystems.
Q7: How do acidophilic bacteria like Acidithiobacillus affect iron cycling in acidic environments?
Acidithiobacillus species thrive at low pH in oxygen-rich environments and facilitate iron cycling by oxidizing ferrous iron to ferric iron. This oxidation process is critical in acidic habitats like acid mine drainage systems, where these organisms contribute significantly to iron turnover.