Ma. Hemminga et al., Biomass production in pioneer Spartina anglica patches: Evidence for the importance of seston particle deposition, EST COAST S, 47(6), 1998, pp. 797-805
Salt marsh formation can be initiated by the colonization of bare tidal fla
ts by pioneer halophytes such as Spartina anglica. In the present study, gr
owth of S. anglica in the edge and centre zones of pioneer patches colonizi
ng a tidal flat in a marine bay in the south-west Netherlands was investiga
ted. Average biomass and shoot length was significantly lower in centre zon
es than in edge zones of the patches. Multiple linear regression showed tha
t 84% of the variance in aboveground biomass in the centre zones could be e
xplained by sediment phosphorus and nitrogen concentrations. No such relati
onship existed in the edge zone. This suggests that biomass production in t
he centre zones of the patches is nutrient limited, but that factors other
than sediment nitrogen and phosphorus content determine growth of Spartina
in the edge zones.
The sediment nitrogen and phosphorus concentrations in the centre zones of
the patches were significantly related with sediment carbon concentrations,
indicating that the pool of particle-bound nutrients in the sediment to an
important extent is associated with organic particles. Determination of st
able carbon isotope signatures of the sedimentary organic matter showed tha
t an increasing carbon content of the sediment in the centre zone of the pa
tches land a rise in plant biomass) coincides with a higher contribution of
non-Spartina derived carbon to the sedimentary organic matter pool. Sustai
ned biomass production in the centre zones of the patches, thus, probably d
epends on deposition of allochthonous organic particles and the nutrient in
puts inherent in this process. Due to the construction of large-scale hydro
-engineering works, however, conditions for deposition of waterborne partic
les are currently unfavourable. The consequences of reduced carbon and nutr
ient inputs into the patches will be particularly in the (older) centre zon
es, where the nutrient pools in non-refractory organic matter have been dra
ined in the years of previous growth. Accordingly, it is hypothesized that
the canopy-enhanced sedimentation for which Spartina is well-known, via pos
itive feed-back effects on plant growth can be crucial for plant vitality,
and, hence, for successful colonization of unvegetated areas. (C) 1998 Acad
emic Press.