ocean sediments Flashcards
significance of ocean sediments
- continents are sites of erosion, oceans are sites of deposition
- oceans retain more complete record of history
- law of superposition
law of superposition
sedimentary layers deposited in time sequence , oldest on top
name the 3 types of marine sediments
- authigenic: formed in situ by precipitation of submarine alteration
- terrigenous- detritus from continental erosion and explosive vulcanism
- biogenic - shells or skeletons that sink ( silicate or carbonate)
name the 4 origins of marinesediment
- volcanogenic particles : from eruptions
- lithogenous particles: weathering
- glacially derived particles: rock beds from moving
- biogenic particles: shells or skeletons from animals
what controls the distribution of various kinds of seafloor sediments?
- Delivery: no delivery- the wouldnt fucking be there
- Dilution: too much sediment: high dilution rate, other sediment becomes unimportant
- Destruction: certain processes destroy particles and remove them from seafloor sediment
Authigenic Sediment Sources
- Evaporites
- phosphorites
Terrigenous Sediment Sources
- TO the continental margins
- sediments funneled across margins though submarine canyons to deep sea fans - To the deep sea
- volcanic ash, tephra- was transported by wind
Biogenic Sediment sources
- organisms use dissolved materials - they remove these to build shells and skeletons
-carbonate and silica
** foraminifera, coccolithophorids, diatoms , radiolaria, pteropods
what are siliceous sediments controlled by
delivery
what are carbonate sediments controlled by
sediment depth, it will dissolve below CCD bc of acidity
why is it important to understand CO2 in system
-builds organic matter
- controls ocean pH
-GHG effect
-affects calcium carbonate deposited on the sea floor
what are the major dissolved forms of CO2
- co2 (aqueous carbon dioxide)
- HCO3- ( bicarbonate ion)
- CO32- ( carbonate ion)
explain calcium carbonate distribution
Ω= 1 is called the saturation horizon; , <1 undersaturated so net dissolution of caco3, =1 saturated so equilibrium, >1 supersaturated so net precipitation
- the upper icean is supersaturated
-the saturation horizon is shallower in pacific
factors affecting ccd
temp, depth, concentration of co2, pH, carbonate supply, terrigenous supply
explain lysocline
where dissolution effects first appear in carbonate grains
- ccd is when deposition rate= dissolution rate