GEOSCAN Search Results: Fastlink

GEOSCAN Menu


TitleGeomorphic features and benthos in a deep glacial trough in Atlantic Canada
 
AuthorLacharité, M; Brown, C J; Normandeau, AORCID logo; Todd, B JORCID logo
SourceSeafloor geomorphology as benthic habitat : GeoHab atlas of seafloor geomorphic features and benthic habitats ; by Harris, P T (ed.); Baker, E (ed.); 2019 p. 691-704, https://doi.org/10.1016/B978-0-12-814960-7.00041-5
Image
Year2019
Alt SeriesNatural Resources Canada, Contribution Series 20180232
PublisherElsevier
Edition2
Documentbook
Lang.English
Mediapaper; on-line; digital
File formatpdf (Adobe® Reader®)
ProvinceNewfoundland and Labrador; Nova Scotia; Eastern offshore region
NTS11A; 11B; 11G; 11H; 11I; 11J
AreaLaurentian Channel; Atlantic Ocean
Lat/Long WENS -59.0000 -56.0000 47.0000 44.5000
Subjectsmarine geology; surficial geology/geomorphology; geophysics; Nature and Environment; Science and Technology; submarine features; submarine troughs; glacial features; marine sediments; glacial deposits; moraines; benthos; faunas; geophysical surveys; acoustic surveys, marine; side-scan sonar; bedforms; pockmarks; iceberg gouging; scour marks; bathymetry; photography; grab samples; biological communities; Laurentian Moraine; Marine biology; Habitats; glaciomarine sediments
Illustrationslocation maps; geoscientific sketch maps; geophysical profiles; tables; plots
ProgramOffshore Geoscience
Released2019 11 01
AbstractThe Laurentian Channel is a deep glacial trough located in Atlantic Canada, extending from the St. Lawrence Estuary to the shelf edge between Nova Scotia and Newfoundland. The outer Laurentian Channel close to its entrance at the shelf edge has been designated as an Area of Interest for the establishment of a Marine Protected Area, but baseline information was lacking. Here, a benthoscape map of the outer Laurentian Channel was generated using geomorphic features mapped using multibeam sonar (density of iceberg scours and pockmarks/iceberg pits, depth and slope) and ground truthed with surficial geology samples and underwater imagery. Individual surrogates and mapped patterns were compared to faunal patterns (infauna and epifauna) derived from the ground truthing. Water depth was the main predictor of infauna abundance and richness, while both depth and density of pockmarks/iceberg pits influenced community composition. Some benthoscape classes had close associations with distinct infauna, but diffuse patterns were mostly observed. Epifauna-namely sea pens-were most abundant at the confluence of multiple benthoscape classes.
Summary(Plain Language Summary, not published)
The Laurentian Channel is a deep glacial trough located in Atlantic Canada between Nova Scotia and Newfoundland. The outer Laurentian Channel close to the shelf edge has been designated as an Area of Interest (AOI) for the establishment of a Marine Protected Area, but baseline information was lacking. A map of the outer Laurentian Channel was generated using geomorphic features, surficial geology samples, and underwater imagery.
GEOSCAN ID311327

 
Date modified: