Abstract
In the last chapter we were concerned with quantitative diurnal and seasonal changes of major components of marine communities. There is a third kind of change over time, largely in composition of species, that takes place when a new resource such as newly upwelled water or recently cleared rock surface is made available. This is the more or less orderly sequence of replacement of some species by others that occurs during colonization or succession. The concept of succession was developed in terrestrial ecosystems, and its characteristics have been summarized by Odum (1969). Many of the properties usually associated with succession are tautological (Peters, 1976). We will examine the most useful, less tautological properties applicable to marine systems.
Keywords
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
References
In terrestrial ecology primary succession is the sequence of species that colonize a new substrate; secondary succession takes place on previously inhabited surfaces that have been cleared of biota by some disturbance.
This seems typical of species of early succession. In terrestrial situations, palatability of plants of early succession is also greater than that of species typical of the later stages (Cates and Orians, 1975). Pioneer plants appear not to invest much effort in chemical or morphological defenses against herbivores.
The result of all these activities is often referred to as “bioturbation.”
This contrasts with some results in terrestrial environments, where it is believed that the succession moves from a nitrate-based to an ammonium-based nitrogen economy, since as succession proceeds, nitrogen may be supplied more and more by internal decay and recycling (mineralization of organic nitrogen) (Rice and Pancholy, 1972; Bormann and Likens, 1979). Such trends are not always found in terrestrial ecosystems (Vitousek et al., 1982).
The terms opportunistic, fugitive, weedy, or pioneer are often applied to these species. The reproductive strategies involved were discussed in Chapter 4, where we also pointed out the r-K continuum was not a complete statement. Species adapted to live in very stressful conditions should also be included.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1984 Springer Science+Business Media New York
About this chapter
Cite this chapter
Valiela, I. (1984). The Structure of Marine Communities Over Time: Colonization and Succession. In: Marine Ecological Processes. Springer Advanced Texts in Life Sciences. Springer, New York, NY. https://doi.org/10.1007/978-1-4757-1833-1_15
Download citation
DOI: https://doi.org/10.1007/978-1-4757-1833-1_15
Publisher Name: Springer, New York, NY
Print ISBN: 978-1-4757-1835-5
Online ISBN: 978-1-4757-1833-1
eBook Packages: Springer Book Archive