
Global Change Biology, Journal Year: 2024, Volume and Issue: 30(7)
Published: July 1, 2024
Abstract As climatic variation re‐shapes global biodiversity, understanding eco‐evolutionary feedbacks during species range shifts is of increasing importance. Theory on expansions distinguishes between two different forms: “pulled” and “pushed” waves. Pulled waves occur when the source expansion comes from low‐density peripheral populations, while pushed recruitment to expanding edge supplied by high‐density populations closer species' core. How extreme events shape pushed/pulled wave events, as well trailing‐edge declines/contractions, remains largely unexplored. We examined responses a marine invertebrate (the owl limpet, Lottia gigantea ) that increased in abundance 2014–2016 heatwaves near poleward its geographic northeastern Pacific. used whole‐genome sequencing 19 across >11 degrees latitude characterize genomic variation, gene flow, demographic histories range. estimated present‐day dispersal potential past stability identify how contemporary historical seascape features characteristics. Consistent with expectations wave, we found little differentiation core leading‐edge higher diversity at edges. A large well‐mixed population northern likely result ocean current anomalies larval settlement high‐dispersal biogeographic boundaries. Trailing‐edge have possibly driven local selection limited high Last Glacial Maximum. Our findings suggest can drive carry adaptive also cautioning extirpations may threaten unique evolutionary variation. This work highlights importance both trailing leading edges respond change events.
Language: Английский