Lecture 5 Flashcards

1
Q

many organisms deposit crystalline or amorphous minerals –

A

inside or outside their cells

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2
Q

minerals are used to –, remove salts and toxic materials, store useful ions, and provide components for sense organs

A

build skeletons

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3
Q

common biominerals: hexagonal

A

calcite

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4
Q

common biominerals: orthorhombic

A

aragonite

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5
Q

common biominerals: CaP

A

apatite

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6
Q

common biominerals: hydrated silica

A

opal

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7
Q

common biominerals: iron oxide

A

magnetite

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8
Q

only – biominerals are commonly fossilized

A

skeletal

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9
Q

most minerals skeletons are

A

stiffened walls (calcite), scaffolds, shells

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10
Q

eggshell is a – formed on a hydrostatic skeleton

A

stiffened wall

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11
Q

vertebrate skeletons are

A

scaffolds

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12
Q

shells are formed by – growth

A

accretionary

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13
Q

Nautilus shells is divided by

A

stiffened walls

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14
Q

nautilus grows in a –spiral

A

logarithmic

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15
Q

open-rooted teeth and horns are –

A

shells

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16
Q

– have a large effect on the use of biominerals in skeletons

A

crystal properties

17
Q

– is more important than symmetry

A

habit

18
Q

in pure solutions, calcite forms

A

equidimensional crystals

19
Q

in pure solutions, aragonite forms

A

fibers

20
Q

some magnesium promotes the formation of

A

fibrous calcite

21
Q

– biomineralization works at the atomic scale in two dimensions

A

matix-mediated

22
Q

structures made of fibers are –

A

weak

23
Q

mother of pearl

A

nacre

24
Q

nacre and foliated calcite are

A

strong

25
Q

nacre and foliated calcite have long fossil record extending back to the

A

Cambrian

26
Q

conversion of a carbonate fiber into a sheet requires a change in

A

crystal habit

27
Q

fibers grow fast at the –

A

tip

28
Q

fiber –> sheet

A

matrix-mediated biomineralization

29
Q

calcite and aragonite seas measured from fluid inclusions in

A

rock salts

30
Q

– are like sealed time capsules (used in ore deposit exploration and the petroleum industry)

A

fluid inclusions

31
Q

percent of – in calcite declines when algae is grown in Cretaceous seawater

A

Mg

32
Q

Cambrian - Ordovician seawater

A

calcite

33
Q

Ediacaran seawater

A

aragonite