3rd quarter exam (Gen Bio) Flashcards

1
Q

the basic building blocks of proteins

A

Amino acids

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2
Q

the linking together (or polymerization) of small organic molecules (like amino acids) to form larger ones, called biopolymers (like proteins).

A

Biosynthesis

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3
Q

DNA meaning

A

Deoxyribonucleic acid

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4
Q

a double-chain biopolymer that consists of two twisted chain-like molecules held together by organic molecules. It stores genetics.

A

DNA

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5
Q

RNA meaning

A

Ribonucleic acid

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6
Q

is a single-strand molecule similar to one-half of a DNA strand that transmits genetic info.

A

RNA

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7
Q

contains the information needed to construct an exact duplicate of the protein molecule.

A

RNA

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8
Q

is the set of biochemical reactions by which organisms produce and extract food energy.

A

Metabolism

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9
Q

is anaerobic metabolism - without oxygen.

A

Fermentation

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10
Q

is aerobic metabolism - with oxygen.

A

Respiration

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11
Q

process whereby plants use light energy to cause carbon dioxide to react with water.

A

Photosynthesis

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12
Q

By products of Photosynthesis

A

Organic substances - carbohydrates
and free oxygen

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13
Q

The solar system coalesced 4.6 b.y. ago from a cloud of cosmic dust and gas. Gravitational compaction caused nuclear fusion to begin in the sun.

A

Early Earth 4.6 b.y.

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14
Q

(Early earth) gathered into larger clusters to make planets; leftover material formed asteroids and comets.

A

Planetesimals

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15
Q

Probably molten at first, Earth was battered by repeated impacts of planetesimals. The first atmosphere was stripped away by solar wind or impacts, but was replenished by volcanic eruptions.

A

Early Earth 4.5 b.y.

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16
Q

As Earth cooled, water vapor in the atmosphere condensed and rained out to form oceans - maybe as early as 4.4 b.y. ago.

A

Early Earth 4.4 b.y.

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17
Q

Near the end of the intense bombardment period, about 3.8 b.y. ago, Earth still was wracked by meteorite impacts and volcanic eruptions. It was a tough place to make a living.

A

Early Life 3.8 b.y.

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18
Q

The first life required chemosynthesis of organic compounds - such as amino acids - from inorganic materials like atmospheric gases, to make proteins.

A

Origin of Life

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19
Q

One hypothesis suggests simple microbes first formed in aerosols - tiny liquid droplets or solid particles suspended in the atmosphere.

A

Origin of Life

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20
Q

Because of the adverse surface conditions, the most likely place for life to develop might have been at deep ocean thermal springs, protected from meteorite bombardment. Both the raw materials and the heat needed for chemosynthesis would have been available here.

A

Origin of Life

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21
Q

The first life was microbial.

A

Origin of Life 3.5 b.y. +?

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22
Q

Meteorite ALH84001 was found in Antarctica in 1984. It is 4.5 b.y. old. Its chemistry is unlike Earth rocks - instead, it is like Mars rocks analyzed by remote landers.

A

Mars Life? 4.5-3.6 b.y.

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23
Q

In 1996, tiny tube-like structures were discovered
inside the meteorite. Some scientists have interpreted these structures as fossils of microbes - if so, they would be at least 3.6 b.y. old.

A

Mars Life? 4.5-3.6 b.y.

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24
Q

Chemical sediments from 2.0 to 1.8 b.y. consist of oxygen-poor iron minerals plus oxygen-rich iron minerals

A

Oxygen Atmosphere 1.8 b.y.

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25
All organisms are composed of cells, a complex grouping of chemical compounds enclosed in a membrane, or porous wall.
Early Life
26
(Early life) store their DNA in a poorly defined part of the cell, not separated from the cytoplasm - the main body of the cell - by a membrane.
Prokaryotic cells
27
(Early life) include a distinct nucleus surrounded by a membrane, as well as other membrane-bounded organelles - well defined parts that each have a specific function.
Eukaryotic cells
28
the earliest and simplest cell forms; many are anaerobic.
Prokaryotic cells
29
are larger and more complex; most require oxygen.
Eukaryotic cells
30
bones and other hard parts are replaced by minerals carried in solution by groundwater.
Mineralization
31
has been replaced by mineralization.
Petrified wood
32
indirect evidence of organisms: tracks and trails wormholes and burrows nests feces (coprolites) calcite mounds (stromatolites)
Trace fossils
33
Charles Darwin visited the Galapagos Islands in 1832. He observed many species of finches on the islands, whereas only one lives on the nearby continent of South America.
Evolution
34
(Evolution) Darwin hypothesized that species can adapt to new conditions through
natural selection
35
Over time, the entire population will evolve towards a better adaptation.
Evolution
36
A study of DNA released in mid-1999 showed that all the Galapagos finches are closely related to each other.
Evolution
37
DNA from Galapagos iguanas shows that they have evolved about 7 m.y. since splitting off from their South American cousins.
Evolution
38
3.5 b.y.: The oldest known fossils are chains of prokaryotic cells from a chert in W. Australia.
Fossil Record - Archean
39
(Fossil Record - Precambrian) are layers of calcium carbonate that form in warm, shallow seas by the activities of photosynthetic bacteria.
Stromatolites
40
(Fossil Record - Proterozoic) oldest fossils of larger, multicellular, soft-bodied marine animals.
Ediacara fauna
41
Plants: Land plants probably evolved from green algae about 600 m.y. ago. Life on land may have looked like this.
Fossil Record - Late Proterozoic
42
545-505 m.y.a. - beginning of period of great diversification: Higher atmospheric oxygen affected skeletal biochemistry and supported larger organisms. Ozone developed to level where it blocked ultraviolet radiation. Eukaryotes invented sexual reproduction. Hard parts appeared.
Fossil Record - Cambrian
43
490-443 m.y.a.: Seas held abundant marine invertebrates with sophisticated adaptations to different conditions.
Fossil Record - Ordovician
44
438-408 m.y.a.: This was the “Golden Age” of cephalopods and brachiopods (a clam-like shellfish).
Fossil Record - Silurian
45
408-360 m.y.a.: The “Golden Age” of fishes
Fossil Record - Devonian
46
408-360 m.y.a.: Land plants became common. Vascular plants developed - club mosses and ferns.
Fossil Record - Devonian
47
380-360 m.y.a. - First seed plants - the naked-seed plants - developed. Gymnosperms like Glossopteris developed. Ginkgos are long-lived relics of the ancient family of naked-seed plants, so are conifers.
Fossil Record - Late Devonian
48
360-286 m.y.a.: Age of amphibians; first winged reptiles and first winged insects. Widespread forests and swamps.
Fossil Record - Carboniferous
49
320-290 m.y.a.: peat swamps common, with scale trees, seed ferns, scouring rushes, and large dragonflies
Fossil Record - Pennsylvanian
50
286-248 m.y.a.: Amphibians decline; reptiles and insects increase; first mammal-like reptiles appear. Nonseed plants decline.
Fossil Record - Permian
51
225 m.y.a.: First dinosaurs and mammals; explosive radiation of dinosaurs. (Primitive Ornithischia, an early dinosaur)
Fossil Record - Triassic
52
213-144 m.y.a.: The Age of dinosaurs; forests of gymnosperms and ferns cover most of Earth. Birds appear.
Fossil Record - Jurassic
53
144-65 m.y.a.: Plesiosaurs infested the beaches
Fossil Record - Cretaceous
54
144-65 m.y.a. - first flowering plants appear. After the K-T boundary, flowering plants diversify and spread explosively over the planet, as do mammals.
Fossil Record - Cretaceous and Tertiary
55
65.0 m.y.a.: Cretaceous -Tertiary Boundary Many species and genera, including the dinosaurs, died out at end of Cretaceous One hypothesis: Earth was hit by a meteorite - at Chixulub, in the Yucatan area of Mexico
Fossil Record - K-T Boundary
56
65-54.9 m.y.a.: Beginning of modern life forms following the K-T Boundary extinctions. Age of mammals began, grasslands spread.
Fossil Record - Tertiary: Paleocene
57
38.0-24.6 m.y.a.: horses, antelopes, cats, oreodonts
Fossil Record - Tertiary: Oligocene
58
24.6-5.1 m.y.a.: horses, antelopes, and other mammals.
Fossil Record - Tertiary: Miocene
59
2.0-0.1 m.y.a.: deer family and elephant family
Fossil Record - Quaternary: Pleistocene
60
2.0-0.01 m.y.a.: horses, cats, elephants, bison, dire wolves
Fossil Record - Quaternary: Pleistocene
61
2.0-0.01 m.y.a.: mammals successfully colonized all environments
Fossil Record - Quaternary: Pleistocene
62
2.0-0.01 m.y.a.: subglacial areas, La Brea tar pits, S. CA
Fossil Record - Quaternary: Pleistocene
63
< 0.1 m.y.a.: Western Nebraska when first humans were appearing
Fossil Record - Quaternary: Pleistocene
64
4.4-0 m.y.a.: Hominids diverged from an early ape-like family. (Poor fossil record and missing transitional forms complicate the story and leave many gaps, but new fossils are being found each year.)
Fossil Record - Quaternary
65
Hominids (Cont.) Homo erectus - 1.8-0.4 m.y. (Peking man, Java man: developed large brains, tools, weapons, fire, and learned to cook food.)
Fossil Record - Quaternary
66
Homo sapiens sapiens - 120,000-present
Fossil Record - Quaternary: Holocene
67
invented big bang theory
Georges Lemaitre
68
4 Divisions of Geological Time Scale
Eons, Era, Period, Epoch
69
Largest Division (hundred to thousands mya)
Eons
70
Span-time period (ten to hundred mya)
Era
71
span no more than one hundred mya
Period
72
Smallest division of GTS characterized by distinctive characteristics
Epoch
73
Phanerozoic Eon
Paleozoic(544-250 mya), Cenozoic (250-65 mya), Mesozoic (65- present mya)
74
Middle Animals= Age of Reptiles and Dinosaurs
Paleozoic and Mesozoic
75
Age of Mammals, Age of flowers, Age of insects
Cenozoic
76
The 4 Eras
Precambrian, Paleozoic, Mesozoic, Cenozoic
77
Periods under Paleozoic
Cambrian, Ordovician, Silurian, Devonian, Carboniferous, Permian
78
Periods under Mesozoic
Triassic, Jurassic, Cretaceous
79
Periods under Cenozoic
Tertiary, Quaternary