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Laboratory and Field Culture of Larvae of The Slipper Limpet, Crepidula fornicata
Published on: January 5, 2024
Nonrandom larval dispersal can steepen marine clines
Matthew P Hare1, Christopher Guenther, William F Fagan
1Department of Biology, University of Maryland, College Park, Maryland 20742, USA. matthare@umd.edu
Evolution; International Journal of Organic Evolution
|March 11, 2006
Summary
Nonrandom larval dispersal, driven by coastal currents, can create sharp phenotypic clines in marine species. This occurs even with high gene flow, challenging traditional population genetic models.
Area of Science:
- Population Genetics
- Marine Ecology
- Evolutionary Biology
Background:
- Classical models assume random gene flow homogenizes populations, hindering local adaptation across environmental gradients.
- Marine species with larval dispersal often exhibit sharp phenotypic and genotypic clines, contradicting random gene flow expectations.
- Coastal hydrodynamics can lead to nonrandom larval dispersal patterns, potentially explaining these sharp clines.
Purpose of the Study:
- To investigate how nonrandom larval dispersal, influenced by hydrodynamics, can accentuate sharp phenotypic clines in marine species.
- To model the interplay between directional dispersal, selection gradients, and dispersal barriers in shaping clinal variation.
- To understand the conditions under which marine transition zones generate steep clines despite high gene flow.
Main Methods:
- Developed a population genetic model for a linear species range with a selection gradient and uniform population densities.
- Incorporated convergent larval advection and semipermeable dispersal barriers to simulate nonrandom dispersal patterns.
- Analyzed the impact of factors like current speed, barrier permeability, and advection distance on phenotypic differentiation.
Main Results:
- Convergent larval advection coupled with a dispersal barrier can amplify phenotypic differentiation, creating sharp clines.
- Directional dispersal introduces migration load, shifting phenotypic means away from local optima near convergence zones.
- Disjunctions in quantitative traits were enlarged by faster currents or more complete dispersal barriers, with significant trait differences observed.
Conclusions:
- Nonrandom larval dispersal, particularly convergent advection near dispersal barriers, can generate surprisingly steep phenotypic clines in marine species.
- Hydrographic phenomena in marine transition zones play a crucial role in balancing gene flow and selection, leading to pronounced local adaptation.
- These findings challenge the assumption of random gene flow in marine systems and highlight the importance of hydrodynamics in evolutionary processes.
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