- 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 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
- Page 64 and 65:
Transport and deposition of dissolv
- Page 66 and 67:
Water mass stratification hinderpar
- Page 68 and 69:
Sedimentation ratesdetermine time r
- Page 70:
What causes the Gulfstream?Circulat
- Page 73 and 74:
• Transport of sediments to the o
- Page 75 and 76:
Sediment drifts• A major step in
- Page 78 and 79: Sediment waves or mud waves
- Page 81 and 82: Bottom currents and sediment drifto
- 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
- Page 91 and 92: Slide headwalls ArcticShelf
- Page 93 and 94: Rotational slumps/faults at Stornes
- Page 95 and 96: Glide planes and sediment typesThe
- Page 97 and 98: Debris flow
- Page 101 and 102: Downslopesedimenttransport•TMF•
- Page 103 and 104: Sidescan Sonar and Seismic Images
- Page 105 and 106: Continental margin slope failuresDo
- Page 107 and 108: Solsikke - Seabed topographySlide d
- Page 109 and 110: Key questions for the understanding
- Page 111 and 112: Slope angles - Section B
- Page 113 and 114: Summary•Geological, morphological
- Page 115 and 116: Mienert, J. & Weaver, P.P.W., eds.,
- Page 117 and 118: Ice margin 18 000 BPGrand BanksSour
- Page 119 and 120: Scotian Slope multibeamDownloaded f
- Page 121 and 122: From Pickrill et al., 2001. OTC pap
- Page 123 and 124: Upper and middle slope canyonseast
- Page 125 and 126: Single channel airgun profile over
- Page 127: Slope canyon incisions and sediment
- 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