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

机译:深海温带 - 热带动物群过渡均匀环境梯度

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摘要

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 degrees S occurs at both lower bathyal (similar to 2500 m) and abyssal (similar to 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.
机译:由于对这些环境的巨大尺寸和不完全探索,深海底栖底栖动物的生物地理造影是不确定的。虽然浅水组装差异化为热带,温带和极地的动物群,但是未知这些单位是否延伸到较低的深度。在这里,我们使用模型和多元统计数据来分析澳大利亚大陆边缘东部2300公里的2300 km横断面的梅格法纳甘露底座样本。我们表明,在较低的浴(类似于2500米)和深度(类似于4000米)深度的温带 - 热带过渡。尽管在这些深度上存在几乎均匀的温度,盐度和溶解的氧浓度,但这种过渡发生了这种过渡。相反,该图案与海底的有机物质的助焊剂一致,这在澳大利亚的生产温带中的较高水平在更绵延的热带水中的低水平变化。在深海和区域规模的异质性中,生物多样性并不统一,需要纳入海洋公园设计。

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