Predictive modelling along a biogeographic transition zone revealed that species with tropical affinities have increased in frequency compared to cold-temperate species.
Credits: Jeremy Bishop on Unsplash
Multivariate predictive modelling developed with fish assemblages data for the last 50 yr revealed that species with tropical affinities have increased in frequency compared to cold-temperate species.
Biogeographic transition zones in marine temperate systems are often hotspots of biodiversity, with high levels of resilience to short-term climate shifts due to naturally occurring cyclic oscillations of oceanographic conditions. However, these environments are likely vulnerable to a steady global warming scenario in which these cyclical conditions could be disrupted.
In a recent publication we evaluated how changes in local oceanography affect the structure of rocky reef fish assemblages over a period of 50 yr in Arrábida Marine Park. Using a 12 yr time series of rocky reef fish assemblage structure, we identified the set of oceanographic variables that most influenced assemblage dynamics. Winter northward wind stress (Upwelling) and Sea Surface Temperature were the most important drivers of change in assemblage structure. Only warmer years had indicator species with warm-temperate or tropical affinities.
Predictive modelling for a novel fish assemblage ‘tropicalization’ index over the last 50 yr revealed that species with tropical affinities have increased in frequency compared to cold-temperate species, coinciding with the trend of increasing mean winter SST. Since the mid-1980s, warm-temperate and tropical species have responded rapidly to more frequent warm winters, suggesting that species distributions are shifting polewards.
These results support a hypothesis that cold affinity species retreat more slowly than the advance of warm affinity species.
Horta E Costa, B., Assis, J., Franco, G., Erzini, K., Henriques, M., Gonçalves, E. J., et al. (2014). Tropicalization of fish assemblages in temperate biogeographic transition zones. Marine Ecology Progress Series 504, 241–252.
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