W5L2 Biochemicla chemcial organic rocks Flashcards

1
Q

stabke vs unstable

A

unstable minerals weather/break up/dissolve quickly

stable minerals dissolve after very long transport and/or a rise in pressure

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2
Q

ions carried

A

ions carried in solution in surface water, subsurface water and ocean water
ions can be biomineralised by organisms as shells & skeletons deposited after death
or concentrated by evaporation & precipitated directly from water
or react with other chemical species (eg iron and oxygen) and precipitated

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3
Q

Biomineralised minerals form

A

Biomineralised sediments, form anywhere that suitable organisms exist -
lakes
marine inshore: coral reefs, lagoons, bioclastic limestones
marine offshore (shelf, continental slope, sedimentary basins): oozes (shells)

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4
Q

Chemically precipitated sediment form

A

Chemically precipitated sediment, formed as a byproduct of evaporation -
lake marls – clays and precipitated calcium carbonate (calcite mud/micrite)
pelagic marls – clays and precipitated calcium carbonate (calcite mud/micrite)

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5
Q

Biochemical rocks coral, prerequisites

A

warm, clear, normal salinity, shallow water
no debris from the land but plenty of nutrients
tropical/subtropical environments are ideal
sunlight - corals have photosynthetic symbionts

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6
Q

Coral polyps

A

Coral polyps make skeletons from dissolved mineral ions -
biomineralised calcium and carbonate ions combine to make calcite
Ca+ + HCO32- → CaCO3

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7
Q

Coral reefs

A

Reefs typically build on the outer shelf, fronting the open ocean
Coral polyps are sensitive to changes in -
sea level , suspended sediment, salinity/water temperature
daily growth rings record changes in these parameters and are registers of climate change

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8
Q

chemically precipitated rocks

A

evaporites

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9
Q

the more precipitation

A

the less evaporites

evaporation has to be higher than precipitation levels

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10
Q

evaporation concentrates ions

A

to the point of supersaturation

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11
Q

Evaporite Environments

A

Playa lake or wadi: fed by desert flashfloods, water evaporates and salts are concentrated
Sabkha: low lying coast in arid environment periodically flooded by seawater
Restricted basin in arid environment, periodically flooded by seawater

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12
Q

Organic (Carbonaceaous rocks)

A

Coal is the diagenetically altered remains of swamp material (peat) where low-oxygen conditions prevent organic decay
Organic-rich marine shales (oil shales) are largely composed of marine algae and terrestrial plant material deposited in low-oxygen conditions
diagenetically altered by heat & pressure
oil, with associated gas & water, migrates to a porous reservoir rock

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