生物多样性
岩石海岸
地中海气候
地理
生态学
水循环
循环(流体动力学)
环境科学
生物多样性热点
海洋学
渔业
生物
地质学
潮间带
热力学
物理
入口
作者
Alex Rattray,Marco Andrello,Valentina Asnaghi,Stanislao Bevilacqua,Fabio Bulleri,Emma Cebrián,Mariachiara Chiantore,Joachim Claudet,Salud Deudero,Julian Evans,Simonetta Fraschetti,Giuseppe Guarnieri,Luisa Mangialajo,Patrick J. Schembri,Antonio Terlizzi,Lisandro Benedetti‐Cecchi
摘要
Ecological connectivity is important for effective marine planning and biodiversity conservation. Our aim was to identify factors important in influencing variation in benthic community structure on shallow rocky reefs in 2 regions of the Mediterranean Sea with contrasting oceanographic regimes. We assessed beta (β) diversity at 146 sites in the littoral and shallow sublittoral from the Adriatic/Ionian Seas (eastern region) and Ligurian/Tyrrhenian Seas (western region) using a null modelling approach to account for variation in species richness. The distance decay relationship between species turnover within each region and geographic distance by sea was determined using generalised linear models. Mantel tests were used to examine correlations between β diversity and connectivity by ocean currents, estimated from Lagrangian dispersal simulations. Variation in β diversity between sites was partitioned according to environmental and spatial components using a distance-based redundancy approach. Species turnover along a gradient of geographic distance was greater by a factor of 3 to 5 in the western region than the eastern region, suggesting lower connectivity between sites. β diversity was correlated with connectivity by ocean currents at both depths in the eastern region but not in the western region. The influence of spatial and environmental predictors of β diversity varied considerably between regions, but was similar between depths. Our results highlight the interaction of oceanographic, spatial and environmental processes influencing benthic marine β diversity. Persistent currents in the eastern region may be responsible for lower observed β diversity compared to the western region, where patterns of water circulation are more variable
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