Mapping Seascapes in the Deep Ocean

A new, automated method for classifying hundreds of kilometres of the deep sea floor in a way that is more cost efficient, quicker and more objective than previously possible has been developed by researchers

Currently there is very little information about the geographic distribution of life on the sea floor. This is largely because of the practical difficulty in accessing creatures which live at such a great depth in the ocean. However, this research soon to be published in the journal Marine Geology , reveals a new method of estimating this distribution using a combination of: submarine mapping technology, statistics and a 'landscape' ecology technique called 'Niche Theory', which is generally used on land.

The Niche Theory states that biodiversity is driven by spatial variability in environmental conditions, i.e. the greater the range of habitats, the greater the biodiversity. The lead author of this study, Khaira Ismail from the University of Southampton, has used this concept to create broad-scale, full coverage maps of the sea floor. The objective of these maps is to estimate the location of biodiversity hotspots, by identifying areas where the deep-sea landscapes are relatively more varied.

Dr Veerle Huvenne, from the NOC, said "by informing us of where to look and where to plan more detailed surveys, this new method will help to make our deep-sea research more targeted and efficient, by advancing our understanding of life in the deep ocean, which at the moment is still very limited."

These maps cover areas approximately 200km across, and have pixel sizes around 25m. They are created using information on the topography and sediment type of the sea floor, collected from a multi-beam echo sounder and a side scan sonar, respectively. The resulting map is then analysed in order to break down the sea floor into a series of zones, using statistical analysis to identify distinct 'geomorphological terrains' in an objective and repeatable way.

Khaira said "using statistical methods to identify these 'terrain zones' allows us to be more objective than if we were picking them out by hand. This objectivity means that the results are consistent and repeatable, which allows different areas of the sea floor to be compared more easily."

Source: Science Daily

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