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Morphometric variance, evolutionary constraints and their change through time in Late Devonian Palmatolepis conodonts
Sabrina Renaud1, Catherine Girard2, Anne-Béatrice Dufour1
1Laboratoire de Biométrie et Biologie Evolutive, UMR 5558, CNRS, Université Claude Bernard Lyon 1, Université de Lyon, Villeurbanne, 69622, France.
Evolutionary adaptation reshaped phenotypic variation in Palmatolepis conodonts during the Late Devonian. Environmental changes and mass extinctions altered the structure of their variance, demonstrating how selection can reorient evolution.
Area of Science:
- Paleontology
- Evolutionary Biology
- Geometric Morphometrics
Background:
- Phenotypic variation is crucial for evolution, but selection can alter its structure.
- Understanding how selection regimes influence variance is key to evolutionary studies.
Purpose of the Study:
- To investigate the impact of environmental changes and mass extinctions on phenotypic variation in Palmatolepis conodonts.
- To analyze how adaptive optima shifts reorient the structure of phenotypic variance (P-matrix).
Main Methods:
- Quantified conodont shape using 2D geometric morphometrics.
- Characterized patterns of variance using the variance-covariance matrix (P-matrix) and its first axis (Pmax).
- Analyzed data across the Late Devonian, including the Frasnian/Famennian mass extinction event.
Main Results:
- Environmental oscillations and the Frasnian/Famennian mass extinction caused a shape response and altered the P-matrix and Pmax.
- Post-extinction, Palmatolepis mean shape shifted, accompanied by a reorientation of the P-matrix and Pmax.
- Empirical evidence shows that shifting adaptive optima can reorient phenotypic variation, enhancing evolutionary response.
Conclusions:
- Phenotypic variance is not static; it actively responds to changing selection pressures and adaptive optima.
- The study highlights the dynamic interplay between selection, environmental change, and the evolution of phenotypic variation.
- The P-matrix's variability is a critical factor in adaptation over geological timescales.
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