1 / 14

Sulfur Cycle Facts

Sulfur Cycle Facts. Sulfur Oxidation States Sulfide and organic sulfhydryl groups = -2 Elemental sulfur = 0 Thiosulfate (S 2 O 3 -2 ) = +2 Sulfite (SO 3 -2 ) = +4 Sulfate (SO 4 -2 ) = +6 Sources of sulfur to the global cycle? Weathering & volcanism & sea-spray

Télécharger la présentation

Sulfur Cycle Facts

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Sulfur Cycle Facts • Sulfur Oxidation States • Sulfide and organic sulfhydryl groups = -2 • Elemental sulfur = 0 • Thiosulfate (S2O3-2) = +2 • Sulfite (SO3-2) = +4 • Sulfate (SO4-2) = +6 • Sources of sulfur to the global cycle? • Weathering & volcanism & sea-spray • Biological emission of Dimethyl Sulfide (DMS) from oceans. • Fossil fuel combustion (photo-oxidation of SO2). • Most sulfur is in seawater and sedimentary rocks. • Assimilatory sulfate reduction: • Incorporates sulfate into methionine and cystein (amino acids). • Only some anaerobes assimilate S-2 directly to organic matter.

  2. Global Input and Outputs

  3. Sulfur Cycling Sº Desulfuromonas

  4. Hypereutrophic Lakes • Very high primary production at the surface and thermocline. • Organic particles sink to hypolimnion and sediments, which have become anaerobic by summer due to stratification. • Anaerobic decomposition will release sulfide by desulfurylation and sulfate reducing bacteria; the later is more dominant with increasing sulfate of Sº supply. • Diffusion of sulfide to illuminated water supports anoxygenic phototrophy and Sº . • Diffusion of sulfide to microaerobic zone supports SOB and Sº. Sº

  5. Protocooperation

  6. Lake Fryxell • Appearances are similar. • Although reverse stratification. • Sulfide source from the bottom and oxygen at the “surface”. • Why no sulfur phototrophs? • - purple sulfur (Chromatium) • - green sulfur (Chlorobium) • How does the S-cycle complete itself?

  7. Sulfide OxidizersLike IOBs, these SOBs favor microaerobic conditions and may be isolated by gradient tubes. What about SOAs (A=archaea)?

  8. Symbiotic Sulfide Oxidizing Bacteria Infers protection of animal tissues from toxic sulfides. Animal feeds off of the organic matter produced by these chemolithoautotrophs. There’s a happy marine nematode woven inside this filamentous SOB!

  9. Endosymbiotic SOB of marine invertebrates Solemya velum, the Atlantic Awningclam is a salt marsh clam without feeding gills. Riftia pachyptilaGiant Tube Worms …

  10. Microbial Mats(No not me!)

  11. Coral Disease (e.g. BBD)

  12. Black Band Disease’s mobile microbial mat community DEAD CORAL Phormidium corallyticum Spread rate ~1 cm/d LIVE CORAL Beggiatoa spp.

More Related