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Bist abil ity in oy ster diff erential equation model Jing Yi Zhou Advisers: Dr. Shaw, Dr. Shi, and Dr. Lipcius
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Bistability in Oyster Differential Equation Model

Jun 02, 2018

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Page 1: Bistability in Oyster Differential Equation Model

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Bistability in oysterdifferential equation mod

Jing Yi Zhou

Advisers: Dr. Shaw, Dr. Shi, and Dr. Lipcius

Page 2: Bistability in Oyster Differential Equation Model

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Page 3: Bistability in Oyster Differential Equation Model

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Crassostrea virginica

•Filter feeder

• Spawns in early summer when

water temperatures rise

• Simultaneous hermaphrodites

• Adults release eggs and sperm into

the water.• Females can produce about 100

million eggs each year

Figure 1: http://sercblog.si.edu/?p=2842

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F

h

e

lif

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Oyster reefs

• Living reef 

• Composed of clusters of oysters

• Rooted in a mixture of shells andshell fragments

• Cluster

• Colony of 3-7 generations of oysters

•Each generation becomes attachedto the shells of the preceding

Figure 3: Retrieved from 20

Lipcius oyster restoration p

Page 6: Bistability in Oyster Differential Equation Model

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Current status

Ermgassen compared results of fishery-independent surveyChesapeake oysters from about 100 years ago to results of msurveys in 2012.

• Remaining biomass ranged from 3% to 38% in various regioChesapeake Bay.

This is mainly attributed to overfishing and diseases (Examp

Page 7: Bistability in Oyster Differential Equation Model

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Page 8: Bistability in Oyster Differential Equation Model

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Figure 5: http://w

content/uploads/

df 

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Logistic growth

Population growth•

  = 1

 

•   = ℎ

•   =

Figure 6: http://education-portal.com/academy

population-growth-equation-definition-graph.h

Page 10: Bistability in Oyster Differential Equation Model

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Equilibria or steady-states

It is a solution of an ODE that does notchange with time

• Can be classified as stable or unstable bylooking at the signs of the eigenvalue of theJacobian matrix

• Example)

 = 

2   1  

 

• Equilibria located where

  = 0

at P = 0, 10

Figure 7:

http://tutorial.math.lamar.edu/C

spx

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Bifurcations

A small change in the parameter can leadto a drastic change in the long-termbehavior of solutions. Such a change iscalled a bifurcation.

• Types of bifurcations

• Saddle-node (fold) bifurcation

Figure 8: Retrieved from paper. Regime shifts

can occur with no

Warning by Hastings, Ecology Letters, 2010, v

Page 12: Bistability in Oyster Differential Equation Model

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Bistability or alternative stable states

Existence of multiple equilibriagiven a range of constants

• Example: Catastrophic bifurcation

Figure 9: Retrieved from paper. Regime shif

can occur with no

Warning by Hastings, Ecology Letters, 2010

Page 13: Bistability in Oyster Differential Equation Model

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What causes these alternative stable sta

• Usually due to one or more feedback mechanisms

• For example)

• Low sediment: Oysters filter sediment → lowers turbidit

→ increases dissolved oxygen concentration → more oys

• High sediment: Oysters filter sediment → oysters spend

→ increases susceptibility to disease → decreases growt

reproduction

Page 14: Bistability in Oyster Differential Equation Model

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Previous differential equations

  = 1

  1

  = 1

 =

Natural

mortality

Death from

sedimentOyster growth rate

Shells from dead oysters Degradation of shell

Oyster

filtration rate

Sediment

erosion

Page 15: Bistability in Oyster Differential Equation Model

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More equation

  =

 

+ , =

 

2  • Proportion of oyster unaffected by sediment

• (, ) = − +

Modification that depends on reef height

•  = 

 

• Filtration rate per unit oyster volume

Page 16: Bistability in Oyster Differential Equation Model

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Times series

At the initial value (O, B, S) =(0.01, 0.39, 0.01)

Figure 9: Retrieved from paper. Jordan-Cooley, Bistability

in a differential equation model of oyster reef height and

sediment accumulation

Figure 10: Time series generated through Matlab

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Bifurcation diagram for live adult oyster

Figure 12: Bifur

Matcont

Stable

unstable

Page 19: Bistability in Oyster Differential Equation Model

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Current model

  =

 = ()

  1

  = 1

 =

Maturation of

oyster juveniles

Natural

mortality

Death from

sedimentOyster growth rate

Shells from dead oysters Degradation of shell

Oyster

filtration rate

Sediment

erosion

Larvae recruitment and

production

Page 20: Bistability in Oyster Differential Equation Model

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Larval functions

•  =  ×

+

• Larval production

•  =

• Larval recruitment

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Objectives

• Finding all the necessary parameters

• Parameters conversion

• Defining parameters that are biologically plausible

• Do bifurcation analysis on the new model

• Couple populations that interact

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Thank you!