A seedling and sporeling emergence assay was conducted on 50 soil cores tak
en from within Carer stricta tussocks (intra-tussock) and from paired, adja
cent inter-tussock areas in the Hawkins Conservation Area, South Hadley, Ma
ssachusetts, USA, to test the hypothesis that local heterogeneity in water
levels alters seed bank composition and subsequent seedling emergence patte
rns. Soil cores were sliced into 2.5-cm-thick sections and split into flood
ed and drawn-down treatments. Germination of buried seeds and spores was as
sessed in these treatments under greenhouse conditions for 6 months. Eighte
en species emerged from both treatments combined: 17 from inter-tussock sam
ples and 12 from intra-tussock samples. Pooled across sample depths and wat
ering treatments, more species of grasses, forbs (exclusive of Impatiens ca
pensis), and woody plants germinated from intra-tussock samples, while more
pteridophytes germinated from the inter-tussock samples. Emergence of pter
idophytes, grasses, and forbs was associated significantly with sample dept
h. More pteridophytes germinated from samples close to the swamp surface, w
hile grasses and forbs were most abundant in samples 10-20 cm below the sur
face. In the drawn-down treatment, pteridophyte and forb seedlings were mor
e plentiful from inter-tussock samples. In contrast, more forb seedlings em
erged from intra-tussock samples in the flooded treatment. This variation i
n forb emergence seems to reflect differences in species composition within
and between tussocks. Twenty-two species occurred in the standing vegetati
on of the study area, but only nine of these also occurred in the seed bank
. The composition of standing vegetation atop and between tussocks did not
differ significantly. Grasses, which dominated the seed bank, were absent f
rom standing vegetation. Grasses clearly represent a persistent population
of seeds in the seed bank, while forbs are more transient within the seed b
ank. The depth-stratified species composition of the seed bank also suggest
s patterns of temporal succession in the aboveground vegetation of this New
England tussock swamp.