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Historical Science M ethodology and D ifferences from E xperim - - PowerPoint PPT Presentation

Historical Science M ethodology and D ifferences from E xperim ental S cience C arol E . C leland C arol E . C leland Philosophy D epartm Philosophy D epartm ent ent C enter for A strobiology C enter for A strobiology U niversity of C


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SLIDE 1

C arol E . C leland C arol E . C leland Philosophy D epartm ent Philosophy D epartm ent C enter for A strobiology C enter for A strobiology U niversity of C olorado (B oulder) U niversity of C olorado (B oulder)

Historical Science

M ethodology and D ifferences from E xperim ental S cience

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SLIDE 2

O VE RVIE W O VE RVIE W

  • D ifferences in the m

ethodology of classical experim ental science and prototypical historical science: two different patterns of evidential reasoning.

  • T he role of com

m

  • n cause explanation in the evaluation
  • f historical hypotheses.
  • T he Principle of the C om

m

  • n C ause and the

asym m etry of overdeterm ination.

  • T he priority of com

m

  • n cause over separate causes

explanation in historical science.

  • D ifferences in the m

ethodology of classical experim ental science and prototypical historical science: two different patterns of evidential reasoning.

  • T he role of com

m

  • n cause explanation in the evaluation
  • f historical hypotheses.
  • T he Principle of the C om

m

  • n C ause and the

asym m etry of overdeterm ination.

  • T he priority of com

m

  • n cause over separate causes

explanation in historical science.

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SLIDE 3

T he structure of C lassical E xperim ental S cience T he structure of C lassical E xperim ental S cience

  • Focus: Is on a single (som

etim es com plex) hypothesis which typically has the form

  • f a universal generalization

(A ll C ’s are E ’s).

  • C entral Research A ctivity: C onsists in repeatedly

bringing about the test conditions specified by the hypothesis and controlling for extraneous conditions that m ight be responsible for false positives and false negatives.

  • Focus: Is on a single (som

etim es com plex) hypothesis which typically has the form

  • f a universal generalization

(A ll C ’s are E ’s).

  • C entral Research A ctivity: C onsists in repeatedly

bringing about the test conditions specified by the hypothesis and controlling for extraneous conditions that m ight be responsible for false positives and false negatives.

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SLIDE 4

T he E xperim ental Program vs. S olitary E xperim ent T he E xperim ental Program vs. S olitary E xperim ent

  • Failed predictions: do not result in the rejection of

hypotheses; they are best interpreted as attem pts to protect the hypothesis from false negatives.

  • S uccessful predictions: A re not followed by risky tests

(in Popper’s sense); they are best interpreted as attem pts to protect the hypothesis from false positives.

  • A cceptance/ rejection of a hypothesis: occurs only

after a hypothesis is subjected to a series of experim ents controlling for plausible auxiliary assum ptions that could explain predictive successes and predictive failures.

  • Failed predictions: do not result in the rejection of

hypotheses; they are best interpreted as attem pts to protect the hypothesis from false negatives.

  • S uccessful predictions: A re not followed by risky tests

(in Popper’s sense); they are best interpreted as attem pts to protect the hypothesis from false positives.

  • A cceptance/ rejection of a hypothesis: occurs only

after a hypothesis is subjected to a series of experim ents controlling for plausible auxiliary assum ptions that could explain predictive successes and predictive failures.

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SLIDE 5

T he structure of Prototypical H istorical S cience T he structure of Prototypical H istorical S cience

Focus:Is on proliferating m ultiple, rival hypotheses to explain a puzzling body of traces encountered in field world. C entral Research A ctivity: C onsists in searching for a ‘sm

  • king gun’ a trace(s) that sets apart
  • ne or m
  • re hypotheses as providing a better

explanation for the observed traces than the

  • thers.

Focus:Is on proliferating m ultiple, rival hypotheses to explain a puzzling body of traces encountered in field world. C entral Research A ctivity: C onsists in searching for a ‘sm

  • king gun’ a trace(s) that sets apart
  • ne or m
  • re hypotheses as providing a better

explanation for the observed traces than the

  • thers.
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SLIDE 6

A C ase S tudy

T he A lvarez H ypothesis

A C ase S tudy

T he A lvarez H ypothesis

  • T wo pronged hypotheses: im

pact, extinction

  • Initially m

any different explanations for the end- C retaceous m ass extinction: pandem ic, evolutionary senescence, clim ate change, supernova, volcanism , and m eteorite Im pact.

  • D iscovery of an iridium

anom aly (“sm

  • king gun”) in

K -T boundary sedim ents narrowed it down to two possibilities: volcanism and m eteorite im pact. D iscovery of extensive quantities of a rare form

  • f

shocked m ineral subsequently cinched the case for im pact over volcanism .

  • T wo pronged hypotheses: im

pact, extinction

  • Initially m

any different explanations for the end- C retaceous m ass extinction: pandem ic, evolutionary senescence, clim ate change, supernova, volcanism , and m eteorite Im pact.

  • D iscovery of an iridium

anom aly (“sm

  • king gun”) in

K -T boundary sedim ents narrowed it down to two possibilities: volcanism and m eteorite im pact. D iscovery of extensive quantities of a rare form

  • f

shocked m ineral subsequently cinched the case for im pact over volcanism .

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SLIDE 7

T he E valuation of H istorical H ypotheses T he E valuation of H istorical H ypotheses

  • N ot grounded in prediction:
  • H istorical predictions are not ‘risky’ in Popper’s

sense; too m any highly plausible extraneous conditions (e.g., iridium poor m eteorite, geological processes, unrepresentative sam ples) capable of defeating them .

  • Predictions are typically vague, e.g., Ward’s

‘prediction’ about C retaceous am m

  • nites; they

serve m

  • re as guides for looking for a sm
  • king gun

than predictions.

  • N ot grounded in prediction:
  • H istorical predictions are not ‘risky’ in Popper’s

sense; too m any highly plausible extraneous conditions (e.g., iridium poor m eteorite, geological processes, unrepresentative sam ples) capable of defeating them .

  • Predictions are typically vague, e.g., Ward’s

‘prediction’ about C retaceous am m

  • nites; they

serve m

  • re as guides for looking for a sm
  • king gun

than predictions.

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SLIDE 8

T he E valuation of H istorical H ypotheses(cont.) T he E valuation of H istorical H ypotheses(cont.)

  • A hypothesis m

ay be rejected on the basis of evidence that does not refute it, e.g., the contagion hypothesis for the end-C retaceous extinctions.

  • T he acceptance of a hypothesis does not

require a successful prediction, e.g., the iridium anom aly was not and could not have been predicted or retrodicted.

  • A hypothesis m

ay be rejected on the basis of evidence that does not refute it, e.g., the contagion hypothesis for the end-C retaceous extinctions.

  • T he acceptance of a hypothesis does not

require a successful prediction, e.g., the iridium anom aly was not and could not have been predicted or retrodicted.

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SLIDE 9

T he E valuation of H istorical H ypotheses(cont.) T he E valuation of H istorical H ypotheses(cont.)

  • G rounded in explanatory power:
  • H ypotheses are accepted and rejected in virtue of

their power to explain (vs.predict) puzzling bodies of traces discovered through field work.

  • T he A lvarez hypothesis explains an otherwise

puzzling association (correlation) am

  • ng traces better

than any of its rivals. It is for this reason that it is viewed as ‘confirm ed’ and its rivals are no longer seriously entertained by scientists.

  • G rounded in explanatory power:
  • H ypotheses are accepted and rejected in virtue of

their power to explain (vs.predict) puzzling bodies of traces discovered through field work.

  • T he A lvarez hypothesis explains an otherwise

puzzling association (correlation) am

  • ng traces better

than any of its rivals. It is for this reason that it is viewed as ‘confirm ed’ and its rivals are no longer seriously entertained by scientists.

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SLIDE 10

C om m

  • n C ause explanation

C om m

  • n C ause explanation
  • C om

m

  • n cause explanations and narrative explanations, e.g.,

sexing a T . rex.

  • Reichenbach’s epistem

ic Principle of the C om m

  • n C ause:

seem ingly im probable associations (correlations or sim ilarities) am

  • ng traces are best explained by reference to a

com m

  • n cause.
  • Presupposes an ostensibly m

etaphysical claim about the tem poral structure of causal relations in our universe: m

  • st

(not all) events form causal forks opening from past to future (leave m any traces in the future).

  • C om

m

  • n cause explanations and narrative explanations, e.g.,

sexing a T . rex.

  • Reichenbach’s epistem

ic Principle of the C om m

  • n C ause:

seem ingly im probable associations (correlations or sim ilarities) am

  • ng traces are best explained by reference to a

com m

  • n cause.
  • Presupposes an ostensibly m

etaphysical claim about the tem poral structure of causal relations in our universe: m

  • st

(not all) events form causal forks opening from past to future (leave m any traces in the future).

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SLIDE 11

T he A sym m etry of O verdeterm ination T he A sym m etry of O verdeterm ination

  • A tim

e asym m etry of causation: M ost local events

  • verdeterm

ine their past causes (because the latter typically leave extensive and diverse effects)and underdeterm ine their future effects (because they rarely constitute the total cause of an effect)

  • M uch easier to infer an ancient volcanic eruption

than a near future volcanic eruption.

  • A tim

e asym m etry of causation: M ost local events

  • verdeterm

ine their past causes (because the latter typically leave extensive and diverse effects)and underdeterm ine their future effects (because they rarely constitute the total cause of an effect)

  • M uch easier to infer an ancient volcanic eruption

than a near future volcanic eruption.

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SLIDE 12

T he A sym m etry of O verdeterm ination (cont.) T he A sym m etry of O verdeterm ination (cont.)

  • Physical source is controversial but it characterizes all wave

(radiativeasym m etry)and particle (2nd law of therm

  • dynam

ics) phenom ena; an objective and pervasive physical feature of world.

  • Physically (vs. logically or strictly m

etaphysically) grounds the Principle of the C om m

  • n C ause and the m

ethodology of historical natural science.

  • A sserts that the present is filled with epistem

ically

  • verdeterm

ining traces of the past; hence one can never com pletely rule out finding a sm

  • king gun for any scientific

hypothesis about the past.

  • Physical source is controversial but it characterizes all wave

(radiativeasym m etry)and particle (2nd law of therm

  • dynam

ics) phenom ena; an objective and pervasive physical feature of world.

  • Physically (vs. logically or strictly m

etaphysically) grounds the Principle of the C om m

  • n C ause and the m

ethodology of historical natural science.

  • A sserts that the present is filled with epistem

ically

  • verdeterm

ining traces of the past; hence one can never com pletely rule out finding a sm

  • king gun for any scientific

hypothesis about the past.

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SLIDE 13

T he priority of com m

  • n cause over

separate causes explanations T he priority of com m

  • n cause over

separate causes explanations

  • T he asym

m etry of overdeterm ination(A of O D ) does not guarantee that every im probable association am

  • ng traces is due

to a last com m

  • n cause; it is a statistical/ probabilistic claim

.

  • T he A of O D does suggest that im

probable associations am

  • ng traces are m
  • re likely to be the result of a com

m

  • n cause

than separate causes

  • In the absence of special theoretical or local background

inform ation, historical natural scientists exhibit a preference for com m

  • n cause over separate causes explanations.
  • T he asym

m etry of overdeterm ination(A of O D ) does not guarantee that every im probable association am

  • ng traces is due

to a last com m

  • n cause; it is a statistical/ probabilistic claim

.

  • T he A of O D does suggest that im

probable associations am

  • ng traces are m
  • re likely to be the result of a com

m

  • n cause

than separate causes

  • In the absence of special theoretical or local background

inform ation, historical natural scientists exhibit a preference for com m

  • n cause over separate causes explanations.
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SLIDE 14

A C ase S tudy

T he end-Perm ian E xtinction (245 m ya)

A C ase S tudy

T he end-Perm ian E xtinction (245 m ya)

  • O n the basis of an initial body of correlated traces,

paleontologists conjectured that there was a single, prolonged extinction event lasting m illions of years, and they proliferated a num ber of rival com m

  • n cause

hypotheses to explain it.

  • A s they accum

ulated m

  • re evidence it becam

e clear that there were actually two extinction pulses separated by a period of around 10 m illion years.

  • O n the basis of an initial body of correlated traces,

paleontologists conjectured that there was a single, prolonged extinction event lasting m illions of years, and they proliferated a num ber of rival com m

  • n cause

hypotheses to explain it.

  • A s they accum

ulated m

  • re evidence it becam

e clear that there were actually two extinction pulses separated by a period of around 10 m illion years.

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SLIDE 15

T he end-Perm ian E xtinction (cont.) T he end-Perm ian E xtinction (cont.)

  • In the absence of specific theoretical reasons or em

pirical evidence that the end-Perm ian extinction was produced by separate causes, paleontologists opted for rival com m

  • n cause

hypotheses.

  • H aving acquired com

pelling local em pirical evidence that there were two extinction events, they opted for separate causes.

  • T hey then returned their focus to com

m

  • n causes: separate

com m

  • n causes of the two extinctions and the possibility that

both resulted from an earlier com m

  • n cause (e.g., Pangaea)
  • In the absence of specific theoretical reasons or em

pirical evidence that the end-Perm ian extinction was produced by separate causes, paleontologists opted for rival com m

  • n cause

hypotheses.

  • H aving acquired com

pelling local em pirical evidence that there were two extinction events, they opted for separate causes.

  • T hey then returned their focus to com

m

  • n causes: separate

com m

  • n causes of the two extinctions and the possibility that

both resulted from an earlier com m

  • n cause (e.g., Pangaea)
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SLIDE 16

C onclusion C onclusion

  • Researchers in historical natural science exhibit a

preference, all other things being equal, for com m

  • n

cause explanation over separate causes explanation

  • T he A of O D underwrites this preference
  • T he objectivity and rationality of the m

ethodology of historical natural science is grounded in a global physical feature of our universe, as opposed to a logical relation between evidence & hypothesis

  • Researchers in historical natural science exhibit a

preference, all other things being equal, for com m

  • n

cause explanation over separate causes explanation

  • T he A of O D underwrites this preference
  • T he objectivity and rationality of the m

ethodology of historical natural science is grounded in a global physical feature of our universe, as opposed to a logical relation between evidence & hypothesis

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SLIDE 17

References References

  • “Prediction and Explanation in Historical Natural Science” (forthcoming in

British Journal of Philosophy of Science)

  • “Philosophical issues in natural history and its historiography” in Tucker,
  • A. (ed), Blackwell Companions to Philosophy: A Companion to the

Philosophy of History and Historiography. Oxford: Blackwell Pub. (2009), pp. 44-62.

  • “Methodological and Epistemic Differences Between Historical Science and

Experimental Science,” Philosophy of Science 69, (2002), pp. 474-496.

  • “Reply to Kevin Kilty’s ‘Comment on: Historical science, experimental

science, and the scientific method’,” Geology 30, (2002), pp. 951-952.

  • “Reply to R. J. Bailey’s ‘ Comment on: Historical science, experimental

science, and the scientific method’,” Geology 30, (2002), pp. 953-954.

  • “Historical science, experimental science, and the scientific method,” Geology

29, (2001), pp. 987-990.

  • “Prediction and Explanation in Historical Natural Science” (forthcoming in

British Journal of Philosophy of Science)

  • “Philosophical issues in natural history and its historiography” in Tucker,
  • A. (ed), Blackwell Companions to Philosophy: A Companion to the

Philosophy of History and Historiography. Oxford: Blackwell Pub. (2009), pp. 44-62.

  • “Methodological and Epistemic Differences Between Historical Science and

Experimental Science,” Philosophy of Science 69, (2002), pp. 474-496.

  • “Reply to Kevin Kilty’s ‘Comment on: Historical science, experimental

science, and the scientific method’,” Geology 30, (2002), pp. 951-952.

  • “Reply to R. J. Bailey’s ‘ Comment on: Historical science, experimental

science, and the scientific method’,” Geology 30, (2002), pp. 953-954.

  • “Historical science, experimental science, and the scientific method,” Geology

29, (2001), pp. 987-990.