FN Archimer Export Format
PT J
TI Seabed image acquisition and survey design for cold water coral mound characterisation
BT 
AF LIM, Aaron
   KANE, Adam
   ARNAUBEC, Aurelien
   WHEELER, Andrew J.
AS 1:1,3;2:1;3:2;4:1,3;
FF 1:;2:;3:PDG-DFO-SM-PRAO;4:;
C1 Univ Coll Cork, Sch Biol Earth & Environm Sci, Cork, Ireland.
   IFREMER, Ctr Mediterranee, Unite Syst Marins, CS 20330, F-83507 La Seyne Sur Mer, France.
   Univ Coll Cork, Irish Ctr Res Appl Geosci, Cork, Ireland.
C2 UNIV COLL CORK, IRELAND
   IFREMER, FRANCE
   UNIV COLL CORK, IRELAND
SI TOULON
SE PDG-DFO-SM-PRAO
IN WOS Ifremer jusqu'en 2018
   copubli-europe
IF 3.349
TC 13
UR https://archimer.ifremer.fr/doc/00403/51482/53728.pdf
LA English
DT Article
DE ;Cold water corals;Mounds;Video survey design;Sediments;Habitat mapping
AB 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. 
PY 2018
PD JAN
SO Marine Geology
SN 0025-3227
PU Elsevier Science Bv
VL 395
UT 000423645300004
BP 22
EP 32
DI 10.1016/j.margeo.2017.09.008
ID 51482
ER

EF