Abstract

During the past 50 years, Fennoscandian populations of spring‐spawning Baltic cisco (Coregonus albula), sympatric to common autumn‐spawners, have declined or disappeared; for example, three out of four known spring‐spawning populations in Sweden are regarded as extinct. Over the same period, the climate has changed and populations have been subject to other anthropogenic stressors. We compared historic (1960s) and recent (1990–2000s) morphological data from the still‐existent sympatric cisco populations in Lake Fegen, Sweden. Phenotypic changes were found for spring‐spawners making them more similar to the sympatric autumn‐spawners that had remained virtually unchanged. Based on results for other salmoniform fishes, a phenotypically plastic response to increased temperature during early development appears unlikely. The recent material was also analyzed with microsatellite markers; long‐term effective population size in spring‐spawners was estimated to be about 20 times lower than autumn‐spawners, with signs of long‐term gene flow in both directions and a recent genetic bottleneck in spring‐spawners. We suggest the change toward a less distinct phenotype in spring‐spawners to reflect a recent increase in gene flow from autumn‐spawners. Time since divergence was estimated to only c. 1,900 years (95% CI: 400–5,900), but still the Fegen populations represent the most morphologically and genetically distinct sympatric populations studied. Consequently, we hypothesize that less distinct population pairs can be even younger and that spring‐spawning may have repeatedly evolved and disappeared in several lakes since the end of the last glaciation, concurrent with changed environmental conditions.

Highlights

  • Vast areas of the northern hemisphere, including the Fennoscandian Peninsula and the Baltic basin, were covered by glacier ice until about 18,000 yBP when the ice started to recede (Storch, Omstedt, Pawlak, & Reckermann, 2015)

  • Several “kinds” of chars, whitefishes and ciscoes are recognized within the Salvelinus alpinus, Coregonus lavaretus, and Coregonus albula complexes, respectively (Jonsson & Jonsson, 2001; Kottelat & Freyhof, 2007; Svärdson, 1998)

  • Using the procedure implemented in Bottleneck, we evaluated the presence of allele frequency mode shifts, as expected following a reduction in effective population size (Luikart & Cornuet, 1998)

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Summary

| INTRODUCTION

Vast areas of the northern hemisphere, including the Fennoscandian Peninsula and the Baltic basin, were covered by glacier ice until about 18,000 yBP when the ice started to recede (Storch, Omstedt, Pawlak, & Reckermann, 2015). Several “kinds” of chars, whitefishes and ciscoes are recognized within the Salvelinus alpinus, Coregonus lavaretus, and Coregonus albula complexes, respectively (Jonsson & Jonsson, 2001; Kottelat & Freyhof, 2007; Svärdson, 1998) Within these complexes sympatric forms are commonly present, segregated with respect to genetic markers, feeding habits, spawning time/‐depth and morphological characters related to ecological adaptation. Within the C. albula complex (ciscoes, vendaces), the most com‐ mon and well‐studied case of sympatric forms is related to differ‐ ences in spawning period In these cases, a common autumn‐spawner typically coexists with a spring‐ or winter‐spawning population (Schulz et al, 2006; Svärdson, 1979; Vuorinen et al, 1981). By combining data from detailed morphological and genetic analyses with results from previous stud‐ ies of other sympatric Baltic cisco populations, an overall aim was to gain further understandings of the evolution, maintenance, and pos‐ sible reasons for recent collapses of these two‐population systems

| MATERIAL AND METHODS
| DISCUSSION
CONFLICT OF INTEREST
FISH FAUNA IN LAKE FEGEN
COMPAR ATIVE MATERIAL
COMPARISON OF METHODS TO OBTAIN MORPHOLOGICAL DATA
PCA FOR RECENT MATERIAL FROM L AKE FEGEN
PC A FOR HISTORIC AL MATERIAL FROM L AKE FEG EN
ISOL ATION WITH MIGR ATION MODEL
10. DIFFERENCE IN VC BETWEEN SS AND AS IN HISTORICAL AND RECENT MATERIAL
11. MORPHOMETRY OF RECENT AND HISTORICAL MATERIAL FROM L AKE FEGEN
13. TEST FOR NON‐NEUTRAL LOCI
Findings
14. GENETIC BOTTLENECKS
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