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The process of soil coloration in wetlands due to the reduction of iron in soil and the role of bacteria in sulfur cycling. It also discusses the formation of salt marshes and the importance of sediment transport and deposition in their development. The document also mentions the difference between dendritic and lattice-style drainage basins and the role of headwaters and deltas in the process.
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Week 8 Low Chroma In soil, when iron receives protons and electrons (gets reduced) that were once a part of organic matter (which is thus oxidized), that soil iron turns grey. so THAT’S why wetlands have gray soil! Q: What do bacterial cells really need? A: A place to dump the hydrogens (a proton and an electron) Noble gasses are stable/inert There is sulfur in seawater Bacteria gets rid of the sulfur by eating the organic matter Where so salt marshes form? -behind barrier islands Salt marshes are not dunes. Rivers flow through two types of drainage basins 2 Types of Drainage Basins: -Dendritic -Lattice-Style Which came first? Rivers or the mountains? – RIVERS 3 things needed for salt-marsh formation: Sediments get eroded, transported, and deposited Mountains erode and the sediments are carried by the high order streams of the watershed. Headwaters -not much wetland acreage -Rivers transport the eroded sediments -Sediments are deposited as water slows in “low gradient” streams of the coastal plain Deposits: Deltas The 64,000 square mile watershed that is drained and provides fresh water to Chesapeake Bay. This is involved in erosion, sediment transport, and deposition. Sediments are deposited in the sluggish, mixing waters of Chesapeake Bay’s mainstem and tributaries. Sal marshes near the mouths of rivers