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Ocean chemistryanddeep-sea sediment
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1. Introduction - Type of deep-sea
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Biogenic sedimentsBeneath high-prod
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Sediments in the open ocean are cal
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Carbonate oozePhytoplankton - Cocco
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Gastropod molluscs- pteropodsAragon
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Cold-water coral reefsExamples of d
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Zooplankton - Radiolaria
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Calcareous and Siliceousmicrofossil
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Nutrients and δ 13 C13δ C =1313(
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Modern and glacial Atlantic interme
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Clay mineralsKaolinite is formed by
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Turbidites
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LGM ice sheet extentIRD input
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Sedimentation rates
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2. Chemical cycles in the Oceans
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Steady state oceanWhat do the nutri
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Dissolved constituents arecoming fr
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A large part of the decomposed mate
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Phosphate distribution in oceansat
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Upper right: Nutrients areenriched
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3. Accumulation of pelagic biogenic
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Preservation of pelagic carbonatese
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1 2Ca 2+ concentrations inseawater
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Preservation of pelagic carbonatese
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The Lysoclineand the Carbonate Comp
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SUMMARY:• The solubility of calci
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Transport and deposition of dissolv
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Water mass stratification hinderpar
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Sedimentation ratesdetermine time r
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What causes the Gulfstream?Circulat
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- Page 83 and 84: Downslope transport by gravitation
- Page 85 and 86: IntroductionTwo factors are crucial
- Page 87 and 88: Tsunami deposits on landIcelandStor
- Page 89 and 90: Continental margin slope failuresDo
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- Page 101 and 102: Downslopesedimenttransport•TMF•
- Page 103 and 104: Sidescan Sonar and Seismic Images
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- Page 107 and 108: Solsikke - Seabed topographySlide d
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- Page 111 and 112: Slope angles - Section B
- Page 113 and 114: Summary•Geological, morphological
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- Page 119 and 120: Scotian Slope multibeamDownloaded f
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- Page 130 and 131: Diagenesisof sediments after burial
- Page 132: Diagenesisof sediments after burial
- Page 136 and 137: Diagenesisof sediments after burial
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