- 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 12 and 13: Gastropod molluscs- pteropodsAragon
- Page 16 and 17: Siliceous oozePhytoplankton - Diato
- Page 18: Ocean desertsThe central subtropica
- Page 21 and 22: High productivity zones
- Page 23 and 24: Nutrient rich intermediate waters
- Page 26: Terrigenous sedimentsOcean circulat
- Page 29 and 30: Fluvial input
- Page 32 and 33: Eolian input
- Page 35: Hydrothermal vent sedimentinput
- Page 39 and 40: Summary:Deep-sea sediments are a mi
- Page 41 and 42: Dissolved constituentsAfter being i
- Page 43 and 44: Steady state oceanDefinition: The r
- Page 45 and 46: • In the photic zone thephytoplan
- Page 47 and 48: Marine snowThe marine snow is compo
- Page 49 and 50: The answers are:• The nutrient-po
- Page 51 and 52: Summary:• Organic matter produced
- Page 53 and 54: Which factors control the distribut
- Page 55 and 56: Preservation of pelagic carbonatese
- Page 57 and 58: Seawater has a pH of ~ 8.2
- Page 59 and 60: Carbonate ion concentrationsBy dire
- Page 61 and 62: We now know that:• The rate of ca
- Page 63 and 64: Preservation of pelagic siliceouspa
- Page 65 and 66:
Only a very few particles reach the
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Currents cause erosion, transport o
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After the lectures a student askedW
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4. Supply of terrigenous sediments
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Alongslope transport by currents
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In- outflow regime at the Faeroe-Sh
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Sediment drift
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Seismic Image
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Passive Continental Margin
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Downslopesedimenttransport•TMF•
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Slide headwall shapes and run out
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Slide headwalls StoreggaWhat do we
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Down slope transport of sediments:
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Glide planes in the Storegga SlideS
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Continental margin slope failuresDo
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Submarine slides and sea level chan
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Bear Island Trough Mouth Fan
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I present the seafloor morphologyof
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Turbidites
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Ormen Lange - Seabed TopographyStor
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Age of major submarine landslides45
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Why is the continental slope angle
- Page 114 and 115:
Mienert, J. & Weaver, P.P.W., eds.,
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Ice sheets and submarine canyonson
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ScotianSlopeIce margin 18 000 BP
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Scotian Slope: Details West of the
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Head of Logan CanyonFrom Pickrill e
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3D seismic seabed rendercourtesy of
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Slope canyon incisions and sediment
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5. Diagenesis of deep-sea sediments
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Diagenesisof sediments after burial
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Diagenetic potential(Schlanger & Do
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How many years does it taketo devel