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Evolution toward a new adaptive optimum: phenotypic evolution in a fossil stickleback lineage
Gene Hunt1, Michael A Bell, Matthew P Travis
1Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20013, USA. hunte@si.edu
Evolution; International Journal of Organic Evolution
|December 18, 2007
Summary
Natural selection
Area of Science:
- Evolutionary biology
- Paleontology
- Quantitative genetics
Background:
- Demonstrating natural selection's role in fossil lineages is challenging.
- Previous analyses of stickleback armor reduction were inconclusive, indistinguishable from neutral drift.
- Indirect evidence suggested natural selection, but direct proof was lacking.
Purpose of the Study:
- To re-evaluate the stickleback armor reduction case study using novel analytical approaches.
- To compare neutral evolution with adaptive evolution models on equal footing.
- To infer the relationship between evolutionary change and the adaptive landscape in fossil lineages.
Main Methods:
- Utilized the Akaike Information Criterion (AIC) to compare neutral and adaptive models.
- Modeled adaptive evolution as an Ornstein-Uhlenbeck process (population ascending an adaptive peak).
- Analyzed an evolutionary time series of skeletal features in a fossil stickleback lineage.
Main Results:
- The adaptive model, incorporating an Ornstein-Uhlenbeck process, significantly outperformed neutral evolution for all measured skeletal features.
- This adaptive model provided a better explanation for the observed evolutionary trajectories than neutral drift.
- The study successfully inferred the influence of natural selection on trait evolution.
Conclusions:
- Natural selection plays a significant role in shaping evolutionary trajectories in fossil lineages, even in cases previously attributed to neutral drift.
- The applied analytical framework, comparing adaptive and neutral models using AIC and Ornstein-Uhlenbeck processes, is effective for inferring selection in paleontology.
- This study demonstrates the possibility of linking fossil evolutionary changes to adaptive landscape dynamics under favorable conditions.
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