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Biodiversity of Fishes Death in the Sea Understanding Natural Mortality

Rainer Froese GEOMAR 08.01.2015

What is Natural Mortality?

Proportion of fishes dying from natural causes, such as: • Predation • Disease / parasites • Accidents, natural disasters • Old age

The

M

Equation

Instantaneous rate of natural mortality of

M

:

D t / N t = M t

Where

t

is the age in years

D t N t

is the number of deaths at age

t

is the population size at age

t

The

M

Equation

Probability of survival (

l t

) to age

t

:

l t

=

e

M t

Where

t M

is the instantaneous rate of natural mortality is the age in years

l t

ranges from 1.0 at birth to near zero at maximum age

The

M

Equation

Number of survivors

N

to age

t

:

N t

=

N 0 e

M t

Where

N 0

is the number of individuals at start age

t=

0

N t

is the number of individuals at age

t

Cohort numbers if

M

= 0.2

1200 Nt = Nts * exp(-M*(t - ts)) 1000 800 600 400 200 0 0 5 10 15

Cohort age (years)

20 25

Constant Value of

M

for Adults

(in species with indeterminate growth: fishes, reptiles, invertebrates, ..) •

M

is typically higher for larvae, juveniles, and very old individuals, but reasonably constant during adult life • This stems from a balance between intrinsic and extrinsic mortality: – Intrinsic mortality increases with age due to wear and tear and accumulation of harmful mutations acting late in life – Extrinsic mortality decreases with size and experience

The

M

Equations

If

M

is different in years 1, 2, 3 and constant thereafter

l t

=

e

–(

M 1 +M 2 +M 3 +M constant* (t-3)) N t

=

N 0 e

–(

M 1 +M 2 +M 3 +M constant* (t-3))

M

is Death Rate in a Stable Population

In a stable,

equilibrium

population – The number of spawners dying per year must equal the number of ‘new’ spawners per year – Every spawner, when it dies, is replaced by one new spawner, the life-time reproductive rate is 1/1 = 1 – If the average duration of reproductive life

d r

is several years, the annual reproductive rate α is α = 1 /

d r

The

P/B

ratio is

M (Allen 1971)

In a stable,

equilibrium

population – Biomass gained by production (

P

) must equal biomass lost (

B lost

) due to mortality –

M

is the instantaneous loss in numbers relative to the initial number:

N lost

/

N

– If we assume an average weight per =

M

individual, then we have biomass: – If

B lost

=

P

then

P

/

B

=

M B lost

/

B

=

M

Reference: Allen, K.R. 1971. Relation between production and biomass. Journal of the Fisheries Research Board of Canada, 1971, 28(10): 1573-1581

Pauly’s 1980 Equation

log

M

= -0.0066 – 0.279 log

L ∞

+ 0.6543 log

K

+ 0.4634 log

T

Where

L ∞

and

K

are parameters of the von Bertalanffy growth function and

T

is the mean annual surface temperature in °C Reference: Pauly, D. 1980. On the interrelationships between natural mortality, growth parameters, and mean environmental temperature in 175 fish stocks. J. Cons. Int. Explor. Mer. 39(2):175-192.

Jensen’s 1996 Equation

M

= 1.5

K

Where

K

is a parameter of the von Bertalanffy growth function Reference: Jensen, A.L. 1996. Beverton and Holt life history invariants result from optimal trade-off of reproduction and survival. Canadian Journal of Fisheries and Aquatic Sciences:53:820-822

M

= 1.5

K

100 10 1 1 : 1 0.1

0.01

0.01

0.1

1

M = 1.5 K

10 100

M

versus estimates from growth coefficient

K

with

M

= 1.5

K

, for 272 populations of 181 species of fishes. The 1:1 line where observations equal estimates is shown. Robust regression analysis of log observed

M

versus log(1.5

K

) with intercept removed explained 82% of the variance with a slope not significantly different from unity (slope = 0.977, 95% CL = 0.923 – 1.03, n = 272, r2 = 0.8230). Data from FishBase 11/2006 [File: M_Data.xls]

Hoenig’s 1984 Equation

ln

M

= 1.44 – 0.984 * ln

t max

Where

t max

is the longevity or maximum age reported for a population Reference: Hoenig, J.M., 1984. Empirical use of longevity data to estimate mortality rates. Fish. Bull. (US) 81(4).

Charnov’s 1993 Equation

Life History Summary

Note: Blue line is not to scale. Froese and Pauly 2013. Fish Stocks, p. 477-487

In

Encyclopedia of Biodiversity, Academic Press

Fishing Kills Fish

Z

=

M

+

F

Where

Z

= total mortality rate

F

= mortality caused my fishing

Total Mortality of Turbot

Numbers at age in survey catches of North Sea turbot (

Scophthalmus maximus

).

Points at the left are not fully selected by the gear. The point at the right is a single, rare survivor of fishing. The absolute slope

Z

= 0.82 represents total mortality from natural causes

M

and from fishing

F

.

Conclusions

• • Natural mortality

M

is high in early life and near constant in adults

M

determines life expectancy, growth and reproduction (and everything else) • Total mortality is

Z

=

M

+

F

• Death rules

Exercises

• Select a species from FishBase with several estimates of natural mortality (

M

is under Growth) • Discuss

M

relative to other species (

M-K

Graph) • Determine mean

M/K

ratio • Determine adult life expectancy

E