Deep-sea temperate-tropical faunal transition across uniform environmental gradients.

The biogeography of the deep-sea benthic fauna is uncertain due to the vast size and incomplete exploration of these environments. While shallow water assemblages are differentiated into tropical, temperate and polar faunas, it is unknown whether these units extend to lower depths. Here we use model-based and multivariate statistics to analyse megafaunal benthic samples along a 2300 km transect off the eastern Australian continental margin. We show that a temperate-tropical transition between 33-30°S occurs at both lower bathyal (~2500 m) and abyssal (~4000 m) depths. This transition occurs despite almost uniform temperature, salinity and dissolved oxygen concentrations occurring across latitudes at these depths. Conversely, the patterns are consistent with the flux of organic matter to the seafloor, which varies from being relatively high in the productive temperate off SE Australia to low levels in more-oligotrophic tropical waters. Biodiversity is not uniform across the deep-sea and regional-scale heterogeneity needs to be incorporated into marine park designs. • There is a significant temperate-tropical transition in benthic assemblages at bathyal-abyssal depths off eastern Australia • The transition is congruent with variation in net primary productivity but not gradients of temperature, salinity or oxygen • The deep-sea habitats are not uniform and assemblage composition differs at regional scales [ABSTRACT FROM AUTHOR]