The clonal mat-forming fern, Dicranopteris linearis (N. L. Burm.) Underw.,
dominates vast areas of rainforests on the windward slopes of Mauna Loa Vol
cano on the island of Hawai'i. Because clone size has important ecological
and evolutionary consequences in such a dominant species, we used isozyme a
nalysis to investigate clone size and other aspects of genetic diversity an
d reproduction over a broad range of environmental conditions on primary su
ccessional sites (pahoehoe lava substrates).
Isozyme analysis provided a measure of the upper limit of clonal size in th
is int interdigitating clonal species. Each 0.5-ha primary successional sit
e on Mauna Loa was comprised of a minimum of two to four clones. Genetic di
versity in Dicranopteris was low; of 32 purative loci investigated, only 4
were polymorphic, with 2 or 3 alleles/locus. Over the 17 study locations on
Mauna Loa and Kilauea Volcanoes, we identified nine multilocus genotypes b
ased on unique combinations of allozymes. Seven of the nine genotypes were
heterozygous for at least one locus, evidence of an intergametophytic matin
g system. Highly dispersible spores, coupled with intergametophytic mating
should promote higher genetic diversity We propose that the Following facto
rs contributed to low genetic diversity: founder effects; extreme isolation
from mainland gene pools; high potential for mating among different gameto
phytes produced from the same sporophyte; relatively low numbers of safe si
tes for gametophyte establishment over space and time; and long-term relian
ce on vegetative growth. Leaf phenotypes were associated with genotype, bur
also with environmental conditions. Enough variability within a genotype e
xisted to support the current treatment of Hawaiian Dicranopteris as one sp
ecies.
Vegetative growth was the primary means by which Dicranopteris covered the
landscape. Nevertheless, spore production, gametophyte establishment, and s
exual reproduction were absolutely essential for colonization of the few fa
vorable microsites available on pahoehoe lava substrates of Mauna Loa follo
wing lava eruptions, dieback, and similar landscape-level disturbances.