Improved bathymetry leads to >4000 new seamount predictions in the global ocean - but beware of phantom seamounts!

Chris Yesson; Tom B Letessier; Alex Nimmo-Smith; Phil Hosegood; Andrew S Brierley; Marie Hardouin; Roland Proud

doi:10.14324/111.444/ucloe.000030

Improved bathymetry leads to >4000 new seamount predictions in the global ocean - but beware of phantom seamounts!

UCL Open Environ. 2021 Dec 22:3:e030. doi: 10.14324/111.444/ucloe.000030. eCollection 2021.

Authors

Chris Yesson¹, Tom B Letessier¹, Alex Nimmo-Smith², Phil Hosegood², Andrew S Brierley³, Marie Hardouin^{1

4}, Roland Proud³

Affiliations

¹ Institute of Zoology, Zoological Society of London, Regent's Park, London NW1 4RY, UK.
² School of Biological & Marine Science, University of Plymouth, Plymouth, Devon PL4 8AA, UK.
³ Pelagic Ecology Research Group, Scottish Oceans Institute, School of Biology, University of St Andrews, St Andrews, Fife KY16 9TS, UK.
⁴ Imperial College London, Silwood Park, Ascot, Berkshire SL5 7PY, UK.

Abstract

Seamounts are important marine habitats that are hotspots of species diversity. Relatively shallow peaks, increased productivity and offshore locations make seamounts vulnerable to human impact and difficult to protect. Present estimates of seamount numbers vary from anywhere between 10,000 to more than 60,000. Seamount locations can be estimated by extracting large, cone-like features from bathymetry grids (based on criteria of size and shape). These predicted seamounts are a useful reference for marine researchers and can help direct exploratory surveys. However, these predictions are dependent on the quality of the surveys underpinning the bathymetry. Historically, quality has been patchy, but is improving as mapping efforts step up towards the target of complete seabed coverage by 2030. This study presents an update of seamount predictions based on SRTM30 PLUS global bathymetry version 11 and examines a potential source of error in these predictions. This update was prompted by a seamount survey in the British Indian Ocean Territory in 2016, where locations of two putative seamounts were visited. These 'seamounts' were targeted based on previous predictions, but these features were not detected during echosounder surveys. An examination of UK hydrographic office navigational (Admiralty) charts for the area showed that the summits of these putative features had soundings reporting 'no bottom detected at this depth' where 'this depth' was similar to the seabed reported from the bathymetry grids: we suspect that these features likely resulted from an initial misreading of the charts. We show that 15 'phantom seamount' features, derived from a misinterpretation of no bottom sounding data, persist in current global bathymetry grids and updated seamount predictions. Overall, we predict 37,889 seamounts, an increase of 4437 from the previous predictions derived from an older global bathymetry grid (SRTM30 PLUS v6). This increase is due to greater detail in newer bathymetry grids as acoustic mapping of the seabed expands. The new seamount predictions are available at https://doi.pangaea.de/10.1594/PANGAEA.921688.

Keywords: bathymetry; environmental science; knolls; seamounts.