- Page 1 and 2: Ocean chemistryanddeep-sea sediment
- Page 3 and 4: 1. Introduction - Type of deep-sea
- Page 5 and 6: Biogenic sedimentsBeneath high-prod
- Page 7 and 8: Sediments in the open ocean are cal
- Page 9: Carbonate oozePhytoplankton - Cocco
- Page 15 and 16: Cold-water coral reefsExamples of d
- Page 17 and 18: Zooplankton - Radiolaria
- Page 20 and 21: Calcareous and Siliceousmicrofossil
- Page 22 and 23: Nutrients and δ 13 C13δ C =1313(
- Page 24: Modern and glacial Atlantic interme
- Page 28 and 29: Clay mineralsKaolinite is formed by
- Page 30: Turbidites
- Page 33: LGM ice sheet extentIRD input
- Page 37: Sedimentation rates
- Page 40 and 41: 2. Chemical cycles in the Oceans
- Page 42 and 43: Steady state oceanWhat do the nutri
- Page 44 and 45: Dissolved constituents arecoming fr
- Page 46 and 47: A large part of the decomposed mate
- Page 48 and 49: Phosphate distribution in oceansat
- Page 50 and 51: Upper right: Nutrients areenriched
- Page 52 and 53: 3. Accumulation of pelagic biogenic
- Page 54 and 55: Preservation of pelagic carbonatese
- Page 56 and 57: 1 2Ca 2+ concentrations inseawater
- Page 58 and 59: Preservation of pelagic carbonatese
- Page 60 and 61: The Lysoclineand the Carbonate Comp
- Page 62 and 63:
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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• Transport of sediments to the o
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Sediment drifts• A major step in
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Sediment waves or mud waves
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Bottom currents and sediment drifto
- Page 83 and 84:
Downslope transport by gravitation
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IntroductionTwo factors are crucial
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Tsunami deposits on landIcelandStor
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Continental margin slope failuresDo
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Slide headwalls ArcticShelf
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Rotational slumps/faults at Stornes
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Glide planes and sediment typesThe
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Debris flow
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Downslopesedimenttransport•TMF•
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Sidescan Sonar and Seismic Images
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Continental margin slope failuresDo
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Solsikke - Seabed topographySlide d
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Key questions for the understanding
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Slope angles - Section B
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Summary•Geological, morphological
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Mienert, J. & Weaver, P.P.W., eds.,
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Ice margin 18 000 BPGrand BanksSour
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Scotian Slope multibeamDownloaded f
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From Pickrill et al., 2001. OTC pap
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Upper and middle slope canyonseast
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Single channel airgun profile over
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Slope canyon incisions and sediment
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Diagenesisof sediments after burial
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Diagenesisof sediments after burial
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Diagenesisof sediments after burial