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The Ecology of Phytoplankton

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<strong>of</strong> their ecologies. <strong>The</strong> C–S gap is spanned by<br />

genera such as Dinobryon, Dictyosphaerium,<br />

Coenochloris, Pseudosphaerocystis, Eudorina and,<br />

arguably, Volvox (Reynolds, 1983b), and by<br />

Aphanocapsa and Aphanothece. <strong>The</strong> series spans<br />

diminishing sv −1 ratios, maximum growth rates<br />

and low-temperature tolerance but increasing<br />

ability to exploit and conserve nutrient<br />

resources. Algae in the C–R axis include predominantly<br />

centric diatoms <strong>of</strong> varying tolerance <strong>of</strong><br />

turbidity and the Scenedesmus–Pediastrum element<br />

<strong>of</strong> enriched shallow ponds and rivers). <strong>The</strong> R–S<br />

possibility is represented by the slow-growing,<br />

long-surviving, acquisitive but highly acclimated<br />

species <strong>of</strong> density gradients, like Planktothrix<br />

rubescens and Lyngbya limnetica. Certain (not<br />

all) members <strong>of</strong> the genus Cryptomonas show a<br />

blend <strong>of</strong> the characteristics <strong>of</strong> all three primary<br />

strategies in being unicellular, having cells <strong>of</strong><br />

moderate size (1–4 ×10 3 µm 3 )and<strong>of</strong>intermediate<br />

sv −1 (0.3–0.5 µm −1 ), and being capable <strong>of</strong><br />

intermediate replication rates (r20∼10 × 10 −6<br />

s −1 ; r0∼0.9 × 10 −6 s −1 ).<br />

It is right to point out that Grime’s CSR concept<br />

<strong>of</strong> plant stategies is not universally accepted<br />

and it has been subject <strong>of</strong> vehement and challenging<br />

debate (see Tilman, 1977, 1987, 1988;<br />

Loehle, 1988, a.o.). Although there is much common<br />

ground shared by the adversaries and, in<br />

truth, the differences are more <strong>of</strong> perspective<br />

and emphasis (Grace, 1991), the differences have<br />

never been entirely resolved. <strong>The</strong> application to<br />

plankton has not been so criticised and some<br />

(Huszar and Caraco, 1998; Fabbro and Duivenvorden,<br />

2000; Gosselain and Descy, 2000; Kruk<br />

et al., 2002; Padisák, 2003) but by no means<br />

all (Morabito et al., 2002), have found the arguments<br />

convincing and helpful to interpretation.<br />

<strong>The</strong> applicability <strong>of</strong> a scheme devised for plant<br />

species is not a barrier: it is now quite evident<br />

that the idea has a long pedigree among<br />

other ecological schools (Ramenskii, 1938) and<br />

has been applied successfully to the ‘violent’,<br />

‘patient’ and ‘explerent’ strategies <strong>of</strong> zooplankton<br />

(Romanovsky, 1985). <strong>The</strong> CSR model has been<br />

applied to fungi (Pugh, 1980) and periphyton<br />

(Biggs et al., 1998).<br />

An updated application to phytoplankton<br />

is set out in Box 5.1. A notable modifica-<br />

REPLICATION RATES UNDER SUB-IDEAL CONDITIONS 211<br />

tion recognises that motility and large size<br />

are not necessary adaptations to function in<br />

chronically very resource-depleted pelagic environments.<br />

Indeed, resource gathering in spatially<br />

continuous, rarefied environments is favoured<br />

by small size, whereas the low levels <strong>of</strong> diffuse<br />

biomass is an unattractive resource for<br />

direct grazing by mesozooplankters (see Chapter<br />

6). <strong>The</strong> adaptive strategies for surviving<br />

the ‘resource desert’ <strong>of</strong> the ultraoligotrophy <strong>of</strong><br />

the oceanic pelagic are accorded the additional<br />

stress-tolerant category SS.<br />

<strong>The</strong> original ascriptions <strong>of</strong> C, S and R categories<br />

to phytoplankton (Reynolds, 1988a) separate<br />

quite satisfactorily on the plot <strong>of</strong> the areas<br />

projected by various species <strong>of</strong> phytoplankton<br />

and the product <strong>of</strong> maximum dimension and<br />

surface-to-volume ratio (msv −1 ) Fig. 3.12). Nearspherical<br />

forms align close to msv −1 [d × 4π(d/2) 2<br />

÷ 4π(d/2) 3 /3] = 6 but separate broadly in to<br />

C and S species according to size, because the<br />

carbon and chlorophyll contents vary with v =<br />

4π(d/2) 3 /3 but the light interception increases<br />

as a function <strong>of</strong> the disk area, a = π(d/2) 2 .<br />

<strong>The</strong> morphological attenuation <strong>of</strong> the R species<br />

pulls out the plot to much higher msv −1 values.<br />

Thus, we distinguish species that are capable<br />

<strong>of</strong> rapid growth in benign, resource-replete<br />

environments, those that are able to go on<br />

squeezing out increased biomass from diminishing<br />

light income and those who are physiologically<br />

or behaviourally adapted to function in<br />

spite <strong>of</strong> developing nutrient stress. <strong>The</strong> model<br />

appears in various guises later in the book,<br />

demonstrating the power and flexibility <strong>of</strong> the<br />

strategy–process–ecosystem interactions. It even<br />

provides the bridge to the light : nutrient hypothesis<br />

(Sterner et al., 1997) ins<strong>of</strong>arasthespecies<br />

best adapted to cope with low doses <strong>of</strong> I ∗ are most<br />

able to cope with high particulate content in the<br />

water andtheC:Pratio<strong>of</strong>thesestonavailable<br />

to secondary consumers.<br />

5.4.6 Resource exhaustion and survival<br />

It is reasonable to assume that the growth <strong>of</strong><br />

phytoplankters distinguished by efficient, highaffinity<br />

resource-gathering capabilities may continue<br />

until they deplete their growth-limiting<br />

resource to near exhaustion. It was <strong>of</strong>ten and

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