On land Pioneering
fauna will colonize an area only after
flora and
fungi have inhabited the area. Soil fauna, ranging from microscopic
protists to larger
invertebrates, have a role in
soil formation and
nutrient cycling.
Bacteria and fungi are the most important groups in the breakdown of organic detritus left by
primary producing plants such as
skeletal soil,
moss and
algae. Soil invertebrates enhance fungal activity by breaking down detritus. As soil develops,
earthworms and
ants alter soil characteristics. Worm burrows aerate soil and ant hills alter sediment particle size dispersal, altering soil character profoundly. Though
vertebrates in general are not considered pioneer species, there are exceptions.
Natterjack toads (
Epidalea calamita) are specialists in open, sparsely vegetated habitats which may be at an early
seral stage. Wide-ranging generalists visit early succession stage habitats, but are not obligate species of those habitats because they use a mosaic of different habitats. Vertebrates can affect early seral stages.
Herbivores may alter plant growth.
Fossorial mammals could alter soil and plant community development. In a profound example, a
seabird colony transfers considerable nitrogen into infertile soils, thereby altering plant growth. A
keystone species may facilitate the introduction of pioneer species by creating new
niches. For example,
beavers may flood an area, allowing new species to immigrate.
Underwater The concept of ecologic succession also applies to underwater habitats. If a space becomes newly available in a reef surrounding,
haplosclerid and
calcareous sponges are the first animals to initially occur in this environment in greater numbers than other species. These types of sponges grow faster and have a shorter life-span than the species which follow them in this habitat. == Pioneer species in the anthropocene ==