Seabed image acquisition and survey design for cold water coral mound characterisation

Type Article
Date 2018-01
Language English
Author(s) Lim Aaron1, 3, Kane Adam1, Arnaubec Aurelien2, Wheeler Andrew J.1, 3
Affiliation(s) 1 : Univ Coll Cork, Sch Biol Earth & Environm Sci, Cork, Ireland.
2 : IFREMER, Ctr Mediterranee, Unite Syst Marins, CS 20330, F-83507 La Seyne Sur Mer, France.
3 : Univ Coll Cork, Irish Ctr Res Appl Geosci, Cork, Ireland.
Source Marine Geology (0025-3227) (Elsevier Science Bv), 2018-01 , Vol. 395 , P. 22-32
DOI 10.1016/j.margeo.2017.09.008
WOS© Times Cited 12
Keyword(s) Cold water corals, Mounds, Video survey design, Sediments, Habitat mapping

Cold-water coral (CWC) habitats are commonly regarded as hotspots of biodiversity in the deep-sea. However, a standardised approach to monitoring the effects of climate change, anthropogenic impact and natural variability through video-surveying on these habitats is poorly-established. This study is the first attempt at standardising a cost-effective video-survey design specific to small CWC mounds in order to accurately determine the proportion of facies across their surface. The Piddington Mound of the Moira Mounds, Porcupine Seabight, offshore Ireland has been entirely imaged by downward-facing video in 2011 and 2015. The 2011 video data is navigated into a full-mound, georeferenced video mosaic. A quadrat-based manual classification of this video mosaic at 0.25 m2 resolution shows the exact proportion of facies abundance across the mound surface. The minimum number of random downward-facing images from the mound are determined to accurately characterise mound surface facies proportions. This minimum sample size is used to test the effectiveness of various common survey designs for ROV-video-based habitat investigations. Single-pass video lines are not representative of the mound surface whilst gridded survey designs yield best results, similar to 100% mound coverage. The minimum sample size and manual classification are applied to the 2015 video data to show a 19% mound surface facies change over 4 years at 0.25 m2 resolution. The proportion of live coral facies show little change while coral rubble facies show most change. This highlights an inconsistency between temporally-separated data sets and implies that in 20 years, the mound surface may almost entirely change.

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