cockroaches and thylacines : the hazards of species extinction christopher g. small, university of...
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Cockroaches and Thylacines: The Hazards of Species Extinction
Christopher G. Small, University of Waterloo(joint with Sheena Zhang & Grace Chiu)
In this talk, I shall examine the problems of species extinction at the macro- and micro-levels. At the macro-level, I shall consider the
statistics of extinction in the fossil record. At the micro-level, I shall try to extract a
few facts from the limited data we have about the thylacine population in the late nineteenth and early twentieth centuries.
Extinctions of families over time Time measured in millions of years (Ma) before present. Graph shows the number of families of organisms which went extinct in each time period. Source: The Fossil Record 2 Database, M. J. Benton.
Extinctions (EXT) against time interval (INT):
Taxonomic families have become extinct at a rate of 5.858 families/Ma over the last 550 MY.
Pearson residuals of extinctions
Permian-Triassic (251 Ma).
Ordovician-Silurian (444 Ma).
Triassic-Jurassic (200 Ma). Devonian-Carboniferous
series of extinctions (360 Ma).
Cretaceous-Tertiary (65 Ma). Goodbye T-rex!
End Eocene event (33 Ma).
Holocene extinction (0 Ma). Goodbye us?
INTˆ
INTˆEXTPRES
Mass extinctions: standard?
Variation in size of extinctions far exceeds “background noise.” I.e., extinctions of taxa are clustered not independent.
Mass extinctions are extreme but not exceptional. (David Raup, 1991).
Mass extinctions are both extreme and exceptional (Richard Bambach & Andrew Knoll, 2001).
Extinctions have occurred at a fairly constant rate on average over time despite occasional mass extinctions.
New taxa have been appearing at a fairly constant rate over time (with a slight increase in speed over the last 50 Ma).
Diversity over time (Ma)The diversity of taxa (in this case families) at any given time has been steadily increasing (with a slight drop at the end of the Palaeozoic).
The hazards of extinction
The statistical approach to studying these extinctions is to treat each species or family as subject to an ongoing hazard of extinction.
This hazard is quantified by means of a hazard function whose value can change over time.
The probability of extinction will depend upon the value of the hazard integrated over time.
Hazards of extinction
Let )(t denote the hazard f unction f or extinction of a
randomly chosen taxon (species, f amily, phylum …) at
time t. That is, dtt)( is the probability of extinction
of the taxon in a time interval of length dt given its
survival up to time t .
For example, if the extinction rate is constant over
time, then )(t f or all t, and the probability of
extinction by time tt of a species extant at time t
is
te 1 .
Estimating nonconstant hazard functions To estimate the hazard function, we would like to
observe extinctions in the fossil record and when they happened.
So we would like to know the precise number of taxa that are extant at different times.
Unfortunately, this is difficult: counts are binned into time periods, dating of individual fossils is uncertain pseudoextinction, Lazarus taxa, Elvis taxa.
At best we use proxy variables at any time we can determine the taxa that appear
before and after that time.
STAGE DURATION MIDPOINT ORIGINS EXTINCTIONS DIVERSITY
VENDIAN 40 590 4 1 16
CAERFAI 34 555.5 230 170 245
ST DAVID'S 19 527 68 52 143
MERIONETH 7 513.6 70 59 161
TREMADOC 17 501.5 62 25 164
ARENIG 17 484.5 142 34 281
LLANVIRN 7.5 472.3 74 35 321
LLANDEILO 4.5 466.3 57 17 343
CARADOC 21 453.5 108 55 434
ASHGILL 4 441 54 99 433
LLANDOVERY 8.5 434.7 66 29 400
WENLOCK 6.5 427.2 63 40 434
Let )(tN be the number of taxa that are extant a
time t . Proxy variables will henceforth be represented
by using a tilde.
A proxy f or )(tN is )(~ tN : the number of taxa
that appear in the f ossil record both before and
af ter time t . Let
)(~)(~)(~ ttNtNtN
)(~ln)(~ln)(~ln ttNtNtN
Let )(~ tE be the cumulative number of taxa that
appear before time t but not af ter time t . Defi ne
)(~ tE similarly.
Define )(~tO be the number of taxa that appear
af ter time t but not before t , and )(~tO similarly.
Generalized Birth and Death Process
Assumptions (D. Stoyan, 1980):
Let )(t be the hazard f unction f or a
taxon to become extinct at time t .
Similarly, )()()( tttt
Let )(t be the rate of speciation of a
given taxon into new taxa at time t .
Similarly, )()()( tttt .
Given all the information about extant
taxa at time t , the expected number of
extinctions between t and tt is
ds
dxxxe
tt
ttNstE
st
)()(
)()()(
E.
Given all the information about extant
taxa at time t , the expected number of
originations between t and tt is
ds
dxxxe
tt
ttNstO
st
)()(
)()()(
E.
.
When t is small these integrals
reduce to
)()(1
)]()([)()()(
tt
ttte
tNttE
E
and
)()(1
)]()([)()()(
tt
ttte
tNttO
E
So estimators f or and are f ound by
substituting proxies and solving
)(ˆ)(ˆ1
)](ˆ)(ˆ[)(~)(ˆ)(~
tt
ttte
tNttE
and
)(ˆ)(ˆ1
)](ˆ)(ˆ[)(~)(ˆ)(
~tt
ttte
tNttO
These simultaneous equations have
solutions
ttN
tNtE
t
)(~ln
)(~)(~
)(̂
and
ttN
tNtO
t
)(~ln
)(~)(
~)(̂
An approximate 95% conditional confi dence
interval f or the hazard f unction can be
obtained f rom the delta method and a
variance stabilizing transformation to be
ttN
tN
tEtE
)(~ln
)(~)(~2)(~
Comments
Most extinctions are “mass extinctions.” The Generalised BD model is useful for hazards, but does not fit other aspects of
data well. Models for extinctions must explain the homogeneity of extinctions and
originations in the face of increasing diversity of taxa. Research may be concentrating too much on taxa and not enough on ecological
niches (D. H. Erwin, 2006).
We should be modelling hazards and not simply fitting them. Current work is investigating modelling the extinction rate as a nonnegative
strongly stationary process. Without modelling there are no null hypotheses: 26 Ma cycles of extinction?
(Raup and Sepkoski,1984). Statistical artefact? (Stigler and Wagner).
The error analysis of proxy variables is nontrivial. It is formally equivalent to the problem of estimating the support of a distribution. C. Marshall (1994), but more work necessary!
Possible sources of thylacine decline:
Hunting and trapping (the latter for zoos worldwide).
Destruction of habitat. Competition with wild dogs. Disease (esp. reports of a “distemper-
like” disease, 1910).
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TasmaniaWoolnorth
Thylacines presented for govt. bounty & thylacines killed at Woolnorth
This time series is the outcome of a number of factors including thylacine demographics human demographics, and socio-economic factors associated with the settlement of Tasmania
at the time. It is difficult to extract information about the thylacine from
such data sets because they have information about both humans and thylacines.
These factors are confounded. To extract information about the thylacine demographics alone, we must either find additional ancillary information about the socio-economic
activity, or find a mathematical model for the socio-economic activity.
Both approaches can be viable, but the second is difficult because, to put it simply, human beings rarely obey the equations imposed on them.
Records at VDL Company, Woolnorth (E. Guiler, 1985)
1899 26 Aug. Tom went to the Mount to look after a tiger with his dogs.
2 Nov. Sent some men to hunt tiger out of Studland Bay run.
11 Nov. All hands in a.m. hunting a tiger out of the Forest. Set snares for a tiger on Saltwater Creek fence.
1890 6 Feb. Tracks seen in Forest.
27 May Chasing tiger in the Forest.
17 July Tiger at Studland Bay, at the Knolls.
1891 1 Aug. Laid poison at Harcus for hunters’ dogs.
1892 26 Aug. Two men to Studland Bay to shift tiger.
1893 No comments.
Records at VDL Company, Woolnorth (continued)
1898 20 Feb. One tiger caught, no locality given.
20 July One tiger caught, McCabe’s Paddock
31 Dec. Snaring in the Forest.
1899 3 July Saw two tigers at Swan Bay.
6 July Caught two tigers in Forest and Three Sticks
22 July Tiger scaring on Three Sticks and Studland Bay
23 Nov. One tiger caught, probably at the Mount.
1900 24 Jan. One tiger caught, locality not stated.
8 Feb. Tiger scaring at Three Sticks
Hunting Record at Woolnorth (1898—1906)
189818991900190119021903190419051906
0
5
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35
Year
Hunting Record in Woolnorth Thylacines caughtHunting attempts
We model the number of potential encounters of thylacines in year t as binomial with parameters )(tn and p , where )(tn is
the (unknown) number of thylacines in the area at time t and p
is the (unknown) probability of killing per individual. Let )(th be
the probability that a thylacine hunt at time t is “successful.”
.1
}0)),((BinPr{1
}0)),((BinPr{)(
)(tnpe
ptn
ptnth
Theref ore, )(tn will be
p
thtn
)](1[ln)(
.
Suppose we model the rate of decline of )(tn as
)()(
tndt
tndE
E ,
which implies that 0)(ln Cttn . Then
.error
errorln)](1[lnln 0
Ct
pCtth
Therefore, we model using the regression equation:
jjj Ctth )](1[lnln
which can be fi t by usual least square methods.
Rate of thylacines h(t) successfully be hunted
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
1898 1899 1900 1901 1902 1903 1904 1905 1906Year
original 3 Step smoothed regression
Thylacine Population around Woolnorth
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
1898 1899 1900 1901 1902 1903 1904 1905 1906
Year
Population estimate Exponential fit from regression
Comments
The data suggest that by the beginning of the twentieth century the decline in the thylacine population was substantial.
While a “distemper-like” disease may have contributed to thylacine decline, the evidence is that the thylacine was disappearing before this.
Habitat, dogs and hunting are the main factors to be considered.
References Bambach, R. K. & Knoll, H. (2001). “Is there a separate class of `mass
extinctions?’” GSA Annual Meeting, 5—8 November 2001. Erwin, Douglas H. (2006). Extinction: How Life on Earth Nearly Ended
250 Million Years Ago. Princeton University. Guiler, Eric R. (1985). Thylacine: The Tragedy of the Tasmanian
Tiger, Oxford University. Marshall, C. R. (1994). “Confidence intervals on stratigraphic ranges:
partial relaxation of the assumption of randomly distributed fossil horizons.” Paleobiology 20, 459—469.
Raup, D. M. (1991). Extinction: Bad Genes or Bad Luck? Norton. Raup, D. M. & Sepkoski, J. J. Jr. (1984). “Periodicity of extinction in the
geologic past.” Proc. Nat. Acad. Sci. USA 81, 801—805. Stigler, S. M. & Wagner, M. J. (1987). “A substantial bias in
nonparametric tests for periodicity in geophysical data.” Science 13, 940—945.
Stoyan, D. (1980). “Estimation of transition rates of inhomogeneous birth-death processes with a paleontological application.” Elektronische Informationsverabeitung u. Kybernetic 16, 647—649.