- 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 15 and 16: Cold-water coral reefsExamples of d
- Page 17: Zooplankton - Radiolaria
- 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
- Page 67 and 68: Currents cause erosion, transport o
- Page 69 and 70:
After the lectures a student askedW
- Page 72 and 73:
4. Supply of terrigenous sediments
- Page 74 and 75:
Alongslope transport by currents
- Page 76:
In- outflow regime at the Faeroe-Sh
- Page 79:
Sediment drift
- Page 82 and 83:
Seismic Image
- Page 84 and 85:
Passive Continental Margin
- Page 86 and 87:
Downslopesedimenttransport•TMF•
- Page 88 and 89:
Slide headwall shapes and run out
- Page 90 and 91:
Slide headwalls StoreggaWhat do we
- Page 92 and 93:
Down slope transport of sediments:
- Page 94 and 95:
Glide planes in the Storegga SlideS
- Page 96 and 97:
Continental margin slope failuresDo
- Page 98:
Submarine slides and sea level chan
- Page 102 and 103:
Bear Island Trough Mouth Fan
- Page 104 and 105:
I present the seafloor morphologyof
- Page 106 and 107:
Turbidites
- Page 108 and 109:
Ormen Lange - Seabed TopographyStor
- Page 110 and 111:
Age of major submarine landslides45
- Page 112 and 113:
Why is the continental slope angle
- Page 114 and 115:
Mienert, J. & Weaver, P.P.W., eds.,
- Page 116 and 117:
Ice sheets and submarine canyonson
- Page 118 and 119:
ScotianSlopeIce margin 18 000 BP
- Page 120 and 121:
Scotian Slope: Details West of the
- Page 122 and 123:
Head of Logan CanyonFrom Pickrill e
- Page 124 and 125:
3D seismic seabed rendercourtesy of
- Page 126 and 127:
Slope canyon incisions and sediment
- Page 129 and 130:
5. Diagenesis of deep-sea sediments
- Page 131 and 132:
Diagenesisof sediments after burial
- Page 135 and 136:
Diagenetic potential(Schlanger & Do
- Page 137:
How many years does it taketo devel