| Literature DB >> 28811875 |
Hans Recknagel1, Oliver E Hooker1,2, Colin E Adams1, Kathryn R Elmer1.
Abstract
Identifying the processes by which new phenotypes and species emerge has been a long-standing effort in evolutionary biology. Young adaptive radiations provide a model to study patterns of morphological and ecological diversification in environmental context. Here, we use the recent radiation (ca. 12k years old) of the freshwater fish Arctic charr (Salvelinus alpinus) to identify abiotic and biotic environmental factors associated with adaptive morphological variation. Arctic charr are exceptionally diverse, and in postglacial lakes there is strong evidence of repeated parallel evolution of similar morphologies associated with foraging. We measured head depth (a trait reflecting general eco-morphology and foraging ecology) of 1,091 individuals across 30 lake populations to test whether fish morphological variation was associated with lake bathymetry and/or ecological parameters. Across populations, we found a significant relationship between the variation in head depth of the charr and abiotic environmental characteristics: positively with ecosystem size (i.e., lake volume, surface area, depth) and negatively with the amount of littoral zone. In addition, extremely robust-headed phenotypes tended to be associated with larger and deeper lakes. We identified no influence of co-existing biotic community on Arctic charr trophic morphology. This study evidences the role of the extrinsic environment as a facilitator of rapid eco-morphological diversification.Entities:
Keywords: Arctic charr; adaptive morphology; benthic–limnetic; ecological opportunity; environmental heterogeneity; freshwater fish; trophic morphology
Year: 2017 PMID: 28811875 PMCID: PMC5552947 DOI: 10.1002/ece3.3013
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
Figure 1(a) Sampling sites of Arctic charr from the British Isles. Lakes are ranked according to their score on PC1 (or based on surface area in case they could not be included in the PCA), with low numbers indicating small, shallow, and species‐poor lakes while large numbers indicate greater surface area, deeper, and more species‐rich lakes. Lake names are listed with associated number in panel b. (b) Distribution of head depth is shown on the left y‐axis in gray boxes (black bar within box = median; whiskers = ± 1.5 IQR [outliers excluded for visualization]) and variation in head depth (VAR) on the right y‐axis (black dots) for all individuals and across all lakes (total N = 1,091). Abbreviations: a’ Bh. Lua. = a’ Bhaid Luachraich
Statistics for the best performing models (ecosystem size (=PC1), biotic community (=PC2), small, steep shore gradient, deep lakes (=PC3), genetic diversity, and charr abundance) and each morphological variable. Following model simplification, ecosystem size remained as the only significant parameter explaining morphology across all tests. Significant p‐values are shown in italics. Asterisks indicate significance levels, with *p < .05, **p < .01, and ***p < .001
| Morphology | Best model | Estimate |
|
|
|
|
|---|---|---|---|---|---|---|
| MEANHD | MEANHD ~ PC1 | −0.392 | 0.169 | −2.317 |
| 0.189 |
| MINHD | MINHD ~ PC1 | −0.663 | 0.253 | −2.621 |
| 0.230 |
| MAXHD | MAXHD ~ PC1 | 1.306 | 0.443 | 2.949 |
| 0.274 |
| VARHD | VARHD ~ PC1 | 1.524 | 0.296 | 5.156 |
| 0.536 |
Figure 2The relationship between Arctic charr morphological characteristics (a: MEAN, b: MIN, c: MAX, d: VAR) and lake environment parameters (ecosystem size) that were significantly associated in linear regressions