THE FRESHWATER STREAM,A COMPLEX ECOSYSTEM1

A stream is set apart from all other aquatic ecosystems in that the water is continually entering and leaving the stream and is in almost constant motion. Thus, there is essentially a unidirectional flow, a constant mixing of the watery medium, a continuous erosion of the substrate with concomitant changes in the characteristics of the stream bed, and little or no opportunity for the accumulation and retention of the dissolved nutrients. The physical and chemical characteristics of the stream are largely reflections of the physical and chemical makeup of the watershed. Because of the constant replacement of the water as it flows away, new nutrients must be brought into the stream continually in order to support the biotic communities. The kinds and amounts of nutrients that enter the stream determine, to a large extent, the numbers and kinds of organisms in the different communities. The organisms that comprise those communities may be categorized as representative species indigenous to springs, riffles, and pools. Most plants in streams are sessile whereas most of the animals are vagile, at least during some phase of their life cycle. All sessile organisms must depend on the current bringing their foodstuffs to them, but the vagile forms may seek out their foods in different parts of the stream and may even move from one community to another. Each community is adapted to its particular environment. Spring communities, because of the constancy of the physical and chemical environment, may reach what is essentially a “climax” situation and remain stable over long periods of time. Communities that occupy riffle and pool habitats may change from season to season and from year to year depending on changes in temperature, volume of flow, and the character of the substrate. Between each of these kinds of communities there are transitional areas that may be occupied by wider varieties of organisms than any of the three principal kinds of communities. In any event, the continuity of these communities in time and space is determined by the speed of the current which in turn depends upon the volume of flow. On this basis it becomes evident that the characteristics of the biotic communities are different at the source of a stream than at any other location. Similarly, riffle communities are different than those living in pools. The most difficult evaluation to be made in studying a stream ecosystem is that of the interlocking relationships among the many kinds of organisms. The plants, whatever kind they may be, fix carbon and other elements into organic compounds that can be utilized as food by the animals. The multitude of organisms that make up the bottom fauna of any stream are largely supported by the food formed directly by the plants. Such animals as small crustaceans, insect larvae, worms, turbellarians, mollusks, and the like serve as food for the carnivorous species. To determine the role of each organism in maintaining such a complex structure is a tremendous challenge. Many tools and methods are at the disposal of the biologist who dares to undertake such a project. Still, the greatest of all these is the dedication to spending long hours of tedious and, frequently, very hard work.