natural selection in a model ocean
DESCRIPTION
Ocean productivity regulates distribution and storage of nutrients and carbon: biological pumpsTRANSCRIPT
Natural Selection in a Model Ocean
Mick Follows, Scott Grant, Stephanie Dutkiewicz, Penny Chisholm MIT
Ocean productivity regulates distribution and storageof nutrients
and carbon: biological pumps Composition and functional
characteristics of pelagic
ecosystem vary in space and time... coccolithophores CaCO3
structural material diatoms Si structural material diazotrophs fix
nitrogen picoplankton ...affecting efficiency/quality of
export:
e.g. recycling microbial loop vs. exporting diatom blooms
Biogeography: What are the dynamics underlying provinces?
(Longhurst) Johnson et al., (2006) Prochlorococcus ecotypes along
AMT section Models of the Marine Ecosystem
Volterra (1928), Cushing (1935) Riley(1946) Nutrient
conservation
NPZ models... e.g. Fasham et al. (1990) recent biogeochemical
models begin to represent functional diversity in the
ecosystem
(e.g. Moore et al., 2002; Gregg et al., 2002; Chai et al.; 2002;
Dutkiewicz et al., 2005) Multiple functional groups of
phytoplankton
simplified example... Functional group characteristics imposed by
parameter values Prochlorococcus ecotypes (Johnson et al., 2006)
AMT observations Johnson et al. (2006) From modeling point of view,
reveals... More complexity: functional diversity within species
More simplicity: well defined functional differences between
otherwise very closely related organisms Simplify modeling approach
by introducing explicit natural selection:
Many possible functional groups (10's 100's) Nutrient
conservation(physical principle) Natural selection (ecological
principle) Generic phytoplankton assign functions randomly choose
sensitivities randomly within prescribed ranges Multiple functional
groups:
generalized system... Parameter values assigned with some
randomness Successful functional groups determined by competition
Random assignment of functional properties(trade-offs?)
sub-tropical 1-dimensional model seasonal cycle initially 100
functional groups phyto (log scale) temp & PAR nutrients
Ensemble averages phyto nutrients max growth rate Kpo4 Kno3
Kpar
Kinhib Npref Topt Why do only a handful of functional groups
persist in each case?
Reflects number ofpotentially limitingresources (Tilman,1977) Also
sensitive tophysical environment,e.g. scales of turbulentvariation
(Tozzi et al.,2004) Tilman (1977) Applying principle of competition
simplifies model construction
Level of diversity emerges, not imposed Self-selects functional
groups according to physical conditions and nutrient availability
Do plausible biological regimes and ecotypes emerge? Johnson et
al., (2006) Prochlorococcus ecotypes along AMT section global
circulation model
30 functional groups of phytoplankton 2 grazers nutrients NO3, NH4,
NO2, PO4, Si, Fe phytoplankton functions and parameter values set
by random process ensemble approach Single ensemble member (Iseed
5007)
annual mean surface phyto (uM P) after 5 yrs annual mean phyto (P),
0-120m(Iseed 5007) annual mean nutrients, 0-120m(Iseed 5007)
Prochlorococcus Synechococcus
obs (log) model (log) (linear) Observed Modeled NO3 NH4 NO2 Johnson
et al., (2006) observed modeled Outlook Natural selection approach
appropriate for modeling ocean ecosystems and biogeochemical cycles
Enables focus on underlying dynamics of model, not tuning of
parameter values Dynamic ecosystem approach can adapt to different
climate/nutrient environments Ensemble approach provides
statistical viewpoint (c.f. adaptive approach?) Prochlorococcus
ecotype observations provide well defined system can model help
interpret the observed structures? Single ensemble member (Iseed
17656)
annual mean surface phyto (uM P) after 5 yrs annual mean phyto(P),
0-120m(Iseed 17656) annual mean nutrients, 0-120m(Iseed 17656)
Prochlorococcus Diversity within species... Productivity of the
oceans controlled by
Availability of nutrients (light, phosphorus, nitrogen iron...)
Significant role for wind-driven, upper ocean circulation ... and
quality of sinking particulate material
association of organic carbon with CaCO3 and opal,>2000m Klaas
and Archer (2002)