Chapter 25 - History of Life on Earth Flashcards

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1
Q

Macroevolution -

A

the broad pattern of evolution above the species level

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2
Q

The four main stages that are hypothesized to have have produced simple cells:

A
  1. The abiotic (nonliving) synthesis of small organic molecules, such as amino acids and nitrogenous bases
  2. The joining of these small molecules into macromolecules, such as proteins and nucleic acids
  3. The packaging of these molecules into protocells, droplets with membranes that maintained internal chemistry different from that of their surroundings
  4. The origin of self-replicating molecules that eventually made inheritance possible
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3
Q

Hypothesis’s by both A. I. Oparin and J. B. S. Haldane:

A

Earth’s early atmosphere was a reducing (electron-adding) environment, in which organic compounds could have formed from simpler molecules

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4
Q

Hydrothermal vents -

A

areas on the seafloor where heated water and minerals gush from Earth’s interior into the ocean

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5
Q

Black smokers -

A

a type of hydrothermal vent that release water so hot that organic compounds formed there may have been unstable

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6
Q

Alkaline vents -

A

a type of hydrothermal vent that release water that has a high pH (9–11) and is warm rather than hot, an environment that may have been more suitable for the origin of life

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7
Q

The first genetic material was most likely _____, not DNA

A

RNA: RNA molecules with certain nucleotide sequences may have shapes that enable them to replicate faster and with fewer errors than other sequences

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8
Q

the known fossil record is biased in favor of species that _______________________________________

A

existed for a long time, were abundant and widespread in certain kinds of environments, and had hard shells, skeletons, or other parts that facilitated their fossilization

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9
Q

Radiometric dating -

A

dating based on the decay of radioactive isotopes

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10
Q

Half-life -

A

the time required for 50% of the parent isotope to decay, which the rate of decay is expressed by

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11
Q

by measuring the ratio of _______ to _______ in a fossil, we can determine the fossil’s age

A

carbon-14; carbon-12

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12
Q

A geologic record -

A

a standard time scale that divides Earth’s history into four eons and further subdivisions

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13
Q

The Phanerozoic eon -

A

roughly the last half billion years, encompasses most of the time that animals have existed on Earth

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14
Q

Three era’s the Phanerozoic eon is subdivided into:

A

the Paleozoic, Mesozoic, and Cenozoic

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15
Q

Mesozoic era -

A

sometimes called the “age of reptiles” because of its abundance of reptilian fossils, including those of dinosaurs

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16
Q

Stromatolites -

A

layered rocks that form when certain prokaryotes bind thin films of sediment together

17
Q

An endosymbiont -

A

a small engulfed cell, a cell that lives within another cell

18
Q

Eukaryotic cells -

A

more complex organism; have a nuclear envelope, mitochondria, endoplasmic reticulum, a well-developed cytoskeleton, and other internal structures. Can engulf other organisms by changing their shape

19
Q

Endosymbiosis -

A

process/theory in which a prokaryotic cell engulfed a small cell that would evolve into an organelle found in all eukaryotes the mitochondrion

20
Q

Serial endosymbiosis hypothesis -

A

hypothesis that mitochondria evolved before plastids through a sequence of endosymbiotic events

21
Q

Supporting evidence for the endosymbiotic origin of mitochondria and plastids

A

The inner membranes have enzymes and transport systems same as those in plasma membranes of living bacteria

Mitochondria and plastids replicate by a splitting process that is similar to that of certain bacteria.

Mitochondria and plastids have cellular machinery needed to transcribe and translate DNA into proteins (separate of larger organism)

Mitochondria and plastid ribosomes are more similar to bacterial ribosomes; size, RNA sequences, and sensitivity to certain antibiotics

22
Q

Larger and more diverse multicellular eukaryotes do not appear in the fossil record until about __________

A

600 million years ago

23
Q

Cambrian explosion -

A

where many present-day animal phyla appear suddenly in fossils formed 535–525 million years ago, early in the Cambrian period.

24
Q

Arthropods -

A

most widespread and diverse land animals

25
Q

Theory of plate tectonics -

A

the continents are part of great plates of Earth’s crust that essentially float on the hot, underlying portion of the mantle

26
Q

Continental drift -

A

process where movements in the mantle cause the plates to move over time

27
Q

Mass extinction -

A
  • in which large numbers of species become extinct worldwide
28
Q

The Permian mass extinction -

A

defines the boundary between the Paleozoic and Mesozoic eras, claimed about 96% of marine animal species

29
Q

The Cretaceous mass extinction -

A

occurred 66 million years ago. This event extinguished more than half of all marine species and eliminated many families of terrestrial plants and animals, including all dinosaurs

30
Q

Adaptive radiations -

A

periods of evolutionary change in which groups of organisms form many new species whose adaptations allow them to fill different ecological roles, or niches, in their communities

31
Q

Heterochrony -

A

an evolutionary change in the rate or timing of developmental events

32
Q

Paedomorphosis -

A

where the sexually mature stage of a species may retain body features that were juvenile structures in an ancestral species

33
Q

Homeotic genes -

A

aka master regulatory genes determine such basic features as where a pair of wings and legs will develop on a bird or how a plant’s flower parts are arranged.

34
Q

Hox genes -

A

one class of homeotic genes provides positional information in an animal embryo. This information prompts cells to develop into structures appropriate for a particular location.