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Abstract Allometric scaling describes the relationship of trait size to body size within and among taxa. The slope of the population‐level regression of trait size against body size (i.e. static allometry) is typically invariant among closely related populations and species. Such invariance is commonly interpreted to reflect a combination of developmental and selective constraints that delimit a phenotypic space into which evolution could proceed most easily. Thus, understanding how allometric relationships do eventually evolve is important to understanding phenotypic diversification. In a lineage of fossil Threespine Stickleback (Gasterosteus doryssus), we investigated the evolvability of static allometric slopes for nine traits (five armour and four non‐armour) that evolved significant trait differences across 10 samples over 8500 years. The armour traits showed weak static allometric relationships and a mismatch between those slopes and observed evolution. This suggests that observed evolution in these traits was not constrained by relationships with body size, perhaps because prior, repeated adaptation to freshwater habitats by Threespine Stickleback had generated strong selection to break constraint. In contrast, for non‐armour traits, we found stronger allometric relationships. Those allometric slopes did evolve on short time scales. However, those changes were small and fluctuating and the slopes remained strong predictors of the evolutionary trajectory of trait means over time (i.e. evolutionary allometry), supporting the hypothesis of allometry as constraint. 

Homing behavior allows individuals to return to a home site when displaced, presumably increasing fitness by increasing access to known food resources, refuges from predators, and breeding opportunities. Homing has been demonstrated in Gasterosteus aculeatus, also known as the threespine stickleback. We hypothesized that because stickleback males guard a nest and tend to the eggs and fry, they should be particularly incentivized to home. In an experiment, we marked and displaced nesting male stickleback over a variety of distances to see how far they were able to home and whether homing success declined with distance displaced. We found that stickleback males did home, which is consistent with other studies. Additionally, we found that the return probability decreased with distance displaced, though not significantly. However, some nests were clearly occupied by new, unmarked males after displacement, meaning that even if an experimentally displaced fish returned, they might not have been able to regain their nest. Removing these cases from the data strengthened the expected negative relationship between distance and return, suggesting that stickleback use landmark cues to navigate home. 

Darwin attributed the absence of species transitions in the fossil record to his hypothesis that speciation occurs within isolated habitat patches too geographically restricted to be captured by fossil sequences. Mayr's peripatric speciation model added that such speciation would be rapid, further explaining missing evidence of diversification. Indeed, Eldredge and Gould's original punctuated equilibrium model combined Darwin's conjecture, Mayr's model and 124 years of unsuccessfully sampling the fossil record for transitions. Observing such divergence, however, could illustrate the tempo and mode of evolution during early speciation. Here, we investigate peripatric divergence in a Miocene stickleback fish,Gasterosteus doryssus.This lineage appeared and, over approximately 8000 generations, evolved significant reduction of 12 of 16 traits related to armour, swimming and diet, relative to its ancestral population. This was greater morphological divergence than we observed between reproductively isolated, benthic-limnetic ecotypes of extantGasterosteus aculeatus. Therefore, we infer that reproductive isolation was evolving.However, local extinction ofG. doryssuslineages shows how young, isolated, speciating populations often disappear, supporting Darwin's explanation for missing evidence and revealing a mechanism behind morphological stasis. Extinction may also account for limited sustained divergence within the stickleback species complex and help reconcile speciation rate variation observed across time scales. 

Phytoliths are opal silica particles formed within plant tis- sues. Diatoms are aquatic, single-celled photosynthetic algae with silica skeletons. Phytolith and diatom morphotypes vary depending on local environmental and climatic conditions and because their silicate structures preserve well, the study of phytolith and diatom morphotypes can be used to better understand paleoclimatic and paleoenvironmental dynam- ics and changes. This article presents original data from an 820cm-deep stratigraphy excavated at the Hazen diatomite deposits, a high-elevation desert paleolake in the Fernley Dis- trict, Northern Nevada, USA. The site has been studied for an assemblage of fossilized threespine stickleback, Gasterosteus doryssus , that reveal adaptive evolution. For this study, a to- tal of 157 samples were extracted at 20 cm intervals cover- ing approximately 24,500 years. After extraction, the samples were mounted on slides and viewed under 40 0-10 0 0x light microscopy, enabling classification of 14 phytolith and 45 di- atom morphotypes. Our data support paleoenvironmental re- constructions of the Hazen Miocene paleolake. ∗