C&C Ch. 4 Flashcards

1
Q

what were the two key insights that led to the successes of early geology?

A
  • the principle of uniformitarianism
  • the invention of stratigraphy as a method of dating
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2
Q

who is uniformitarianism particularly associated with?

A

the late 18th century Edinburgh geologist James Hutton

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3
Q

what does uniformitarianism state?

A

the application to the history of the structure of the earth the principle that the basic physical processes involved are assumed to be the same everywhere and at all times. Geological change over time reflects the operation of the laws of physics, which are themselves unchanging.

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4
Q

is there an independent justification of the assumption of uniformity?

A

no

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5
Q

what does the uniformitarian assumption in geology imply?

A

that the present-day constitution of the earth’s surface reflects the cumulative action of:
- processes of formation of new rocks by volcanic action and deposition of sediments in rivers, lakes and seas
- the erosion of old rocks by the action of wind, water, and ice.

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6
Q

what does the formation of sedimentary rocks like sandstone and limestone depend on?

A

the erosion of other rocks

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7
Q

mountains are formed by

A

volcanic action

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8
Q

earthquake cause

A

uplift of land

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9
Q

how can the order of the events that have led to the present-day appearance of many part of the earth be established?

A

by the principle of stratigraphy

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10
Q

how is stratigraphy useful?

A

information on the mineral composition and arrays of fossils found in different layers of rocks (strata) is used to characterise individual layers.

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11
Q

the types of fossils found in a given sedimentary rock layer provide evidence about

A

the environment that prevailed when it was laid down (eg whether the organisms were marine, freshwater, or terrestrial)

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12
Q

using the principle that older rocks must normally lie below younger ones yields what type of result?

A

a relative, not an absolute, chronology

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13
Q

describe the processes involved in landscape formation

A

very slow; erosion of even a few mm of rock takes many years, and the deposition of sediments is correspondingly slow

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14
Q

how does geology conflict with Biblical chronology?

A
  • sedimentary rocks of the same formation are several km deep in many parts of the world
  • large deposits have been eroded
  • a time-scale of at least many tens of millions years for the existence of the earth is thus necessary
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15
Q

who challenges the long time-scale for the earth? how?

A

the eminent physicist Lord Kelvin; on the grounds that the rate of cooling of an originally molten earth would make the earth’s core much cooler than it actually is if the earth had been formed much more than 100m years ago

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16
Q

how was Lord Kelvin’s theory disproved?

A
  • radioactive decay of unstable elements (eg uranium) into more stable derivatives was discovered.
  • this process is accompanies by the release of energy sufficient to slow the rate of cooling of the earth to a value that agrees with current estimates of its age.
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17
Q

why is radioactivity useful in terms of studying evolution?

A

it provides new and reliable methods for establishing the ages of rock samples.

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18
Q

how can we use radioactivity to establish the age of a rock sample?

A
  • the atoms of radioactive elements have a constant probability per year of decaying to a more stable daughter element, accompanied by the emission of radiation
  • when a rock is laid down, it can be assumed the element is pure
  • if the proportion of the daughter element in the sample is measured and the rate of decay is known, the time since the formation of the rock can be estimated
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19
Q

what happens when a plant, animal, or microbe dies?

A

the soft parts are almost certain to decay rapidly

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20
Q

when are the microbes responsible for decay unable to break down the soft parts?

A

in unusual environments, such as the arid atmosphere of a desert or the preservative chemicals of a piece of amber

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21
Q

what usually happens to skeletal structures (eg the tough chitin which covers the bodies of insects and spiders, or the bones/teeth of vertebrates) after death?

A
  • eventually decay
  • slower rate of disappearance offers an opportunity for minerals to infiltrate them, and eventually replace the original material with a mineralised replica
  • may also create a mould of their shape as minerals are deposited around them
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22
Q

where is fossilisation most likely to happen? why?

A

underwater, where the deposition of sediment and precipitation of minerals occur at the bottom of season, lakes, and river estuaries

23
Q

in what ways is the fossil record biased?

A

marine organisms living in shallow seas, where sediments are continuously formed, have the best fossil record, and flying creatures have the worst.

24
Q

how many the deposition of sediments be interrupted?

A

by a change in climate or by uplift of the seabed.

25
Q

what is the impact of having gaps in the fossil record?

A
  • it is rare to have a long-continued series of remains showing the continuous changes expected under the hypothesis of evolution.
  • in many cases, new groups of animals/plants make their first appearance in the fossil record without any obvious links to earlier forms
26
Q

Cambrian explosion

A

most of the major groups of animals appear for the first time as fossils in the Cambrian period, between 550 and 500MYA

27
Q

Archaeopteryx

A
  • fossil bird-reptile
  • show characteristics like modern birds (wings/feathers), like reptiles (toothed jaw/long tail)
28
Q

how did Darwin argue that humans were most closely related to gorillas and chimpanzees if there were no fossil remains connecting apes and humans?

A

on the base of anatomical similarities

29
Q

extracting DNA for sequencing from bones or teeth of Neanderthals and Denisovans has revealed that…

A

their sequences differ slightly more from ours than do the sequences of two different Homo sapiens individuals

30
Q

describe the possible history of Homo sapiens as shown by ancient DNA data

A
  • possible mating among Neanderthals and Denisovans and humans
  • several migration events
31
Q

describe the major migration events of modern humans

A
  • two major migrations of modern humans from Africa to Europe and Asia about 9000 years ago
  • a migration from northern Asia into the American continent
  • migration back into Africa (DNA variants characteristic of Eurasians are found in the genomes of Africans)
32
Q

give an example of a continuous temporal sequence of fossils which shows a single evolving lineage

A
  • long rocks columns recovered from deposits at the bottom of the sea.
  • this allows very fine-scaled time separation between successive samples of the microorganisms’ fossilised skeletons
33
Q

3.5b years ago - 500MYA

A

3.5b years - evidence for the remains of bacteria and related unicellular orgs

800mya - organisms made up of simple clusters of cells appear at a time of environmental crisis when earth was largely covered w ice

700mya - 500mya vidence of soft-bodied, multicellular animal life.

550mya - Cambrian - animal remains associated w hard skeletons become abundant

500mya - evidence for nearly all major animal groups (eg primitive fish-like vertebrates w/o jaws)

34
Q

440mya - 360mya

A

440mya - evidence for freshwater life, fossil spores (=first land plants), shark-like fish w jaws

400 - Devonian:
- freshwater and land animals become more common and diverse
- primitive insects, spiders, mites, millipedes
- simple vascular plants and fungi
- jawed fish w bony skeletons, inc. lobe-finned fishes
- salamander-like amphibians

35
Q

360mya - 250mya

A

360mya- 280mya: Carboniferous.
- coal deposits (fossilised remains of tree-like plants that grew in tropical swamps)
- remains of primitive reptiles

280-250mya: Permian
- great diversification of reptiles
- some of these have anatomical features that increasingly come to resemble those of mammals
- some modern groups of insects, such as bugs and beetles, appear
- ends with largest set of extinctions in fossil records (eg trilobites)

36
Q

250mya - 65mya

A

250-200mya: Triassic
- plants similar to modern conifers and cycads appear
- dinosaurs, turtles, and primitive crocodiles appear
- at end, first true mammals are found
- bony fishes similar to modern appear in sea

200-140mya: Jurassic:
- mammals diversify
- life on land still dominated by reptiles, esp dinosaurs
- flying reptiles and Archaeopteryx appear
- flies, termites, crabs, lobsters appear

140-65mya: Cretaceous
- flowering plants evolve
- all major modern groups of insects found
- marsupials and placental mammals appear
- dinosaurs still abundant
- at end, asteroid lands in Yucatan peninsula of Mexico: all dinosaurs (except birds) disappear, along with many others

37
Q

65mya - 2mya

A

Tertiary:
- main groups of placental mammals appear (mostly similar to modern insectivores)
- whales and bats, main groups of birds, modern invertebrates, flowering plant groups, bony fishes abundant

38-26:
- grasslands appear
- grazing horse-like animals with 3 toes
- primitive apes
- ungulates

38
Q

why does it make sense that only unicellular organisms related to bacteria existed for more than a billion years?

A

the evolution of the machinery needed to translate the genetic code into protein sequences, and complex organisation of even the simplest cell, must have required many steps

38
Q

what happened between 2mya and 10,000 years ago?

A
  • a series of ice ages.
  • humans become the dominant land animal and many large mammal species become extinct.
  • evolution of dwarf forms of various large mammal species
39
Q

why is the late appearance in the record of eukaryote cells consistent w evolution?

A

they have a much more complex organisation compared with prokaryotes

40
Q

why is the appearance of multicellular organisms after unicellular organisms consistent w evolution?

A

the development of multicellular organisms from a single cell requires elaborate signalling mechanisms to control growth and differentiation. this could not have evolved before single-celled forms existed

41
Q

why is the fact that life was exclusively marine for an immense period understandable?

A
  • geological evidence shows that there was very little O2 in atmosphere
  • lack of protection from UV radiation by atmospheric ozone would have prohibited life on land/fresh water
  • once sufficient O2 had built up as a result of photosynthesis of bacteria and algae possibility of land invasion opened up
42
Q

why does the appearance of fossils of flying insects and vertebrates after the emergence of life on land make sense?

A

it is unlikely that true flying animals could evolve from purely aquatic forms

43
Q

why does the recurrent phenomenon of the emergence of abundant/diverse forms of life, followed by their extinction/reduction make sense?

A

the mechanisms of evolution have no foresight and cannot guarantee that their products can survive sudden large environmental changes

44
Q

the interpretation of the fossil record follows….

A

the same principle of uniformitarianism that is applied by geologists to the history of the structure of the earth

45
Q

how were the Galapagos and Hawaiian islands formed? what does this mean about the present-day inhabitants of such islands?

A
  • by volcanic action and were never connected to a continent
  • present-day inhabitants of such islands must be the descendants of individuals who were able to cross the bast distances separating the new islands from the nearest inhabited land
46
Q

what restrictions are there on what inhabitants the Galapagos/Hawaiian islands can have?

A
  1. few species will be able to establish themselves due do difficulty of colonisation of a remote piece of new land
  2. only types of organism able to cross 100s of 1000s of miles of oceans can become established
  3. highly random element to which species are present, because of small no of species that arrive on the islands
  4. evolution on such remote islands will produce many forms found nowhere else
47
Q

compare the composition of oceanic islands with continents of comparable climates

A

tend to have relatively few species in any major group

48
Q

what species are usually present/not present on oceanic islands before human introductions?

A

present: reptiles and birds
not: terrestrial mammals and amphibians

49
Q

the rampant spread of many species after human introduction shows clearly that

A

local conditions were not unsuitable for their establishment

50
Q

how can we explain the fact that finches form such a great proportion of bird species on the Galapagos?

A

there were only a small number of species of original bird colonists, one of which was a species of finch that became the ancestor of present day species

51
Q

Darwin’s finches have a much greater variety of —- —– and —— than is usually among finches; these are clearly adapted to

A

beak sizes; shapes; different modes of food gathering

52
Q

studies on the DNA of Darwin’s finches show that they are closely related to

A

species on mainland south america

53
Q

how are the observations about Darwin’s finches explicable?

A

if the colonist ancestors of these island species found themselves in environments free from established competitor species.

this situation would permit the evolution of traits that adapted the colonists to new ways of life and allowed diversification of an ancestral species into several descendant species.