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Antitropical distribution and evolution in the Indo-West Pacific Ocean
1Department of Marine Science, University of South Florida, St. Petersburg 33701, USA.
Systematic Zoology
|January 1, 1987
Summary
The relict theory best explains antitropical distributions in Indo-West Pacific species. Older species become restricted to isolated areas as younger species evolve and supplant them.
Area of Science:
- Marine Biology
- Biogeography
- Evolutionary Biology
Background:
- Antitropical distributions, where species inhabit regions north and south of the tropics but not the tropics themselves, are observed in Indo-West Pacific continental shelf species.
- Previous hypotheses for these distributions, including glacial transgression, isothermic submergence, island integration, Neogene warming, and Mesozoic continental drift, are not well-supported by evidence.
Purpose of the Study:
- To evaluate existing hypotheses for antitropical distributions in Indo-West Pacific species.
- To identify the most plausible mechanism explaining these disjunct biogeographic patterns.
Main Methods:
- Review of evidence from systematic studies across diverse animal and plant groups.
- Analysis of characteristics common to antitropical distribution patterns.
- Re-evaluation of the historical "relict theory" proposed by Theel (1885).
Main Results:
- Common antitropical patterns and systematic data suggest that established hypotheses are inadequate.
- The "relict theory" provides a viable mechanism for generating antitropical distributions.
- This theory aligns with the Indo-West Pacific, particularly the East Indies, functioning as a center of evolutionary origin.
Conclusions:
- Antitropical and disjunct distributions arise when an ancestral species with a wide range is gradually replaced by a descendant species that evolved in the East Indies.
- The older species becomes relegated to isolated populations at the edges of its former range, often north and south of the equator.
- This process can also result in relict populations in areas like the western Indian Ocean.
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