Near bottom current velocity and water temperature and associated surface meteorological measurements in the Vazella pourtalesii glass sponge grounds of the Scotian Shelf (2017-2018)

• Main Authors: Hanz, Ulrike, Beazley, Lindsay, Kenchington, Ellen L, Duineveld, Gerard C A, Rapp, Hans Tore, Mienis, Furu
• Format: Dataset
• Language: English
• Published: PANGAEA 2021
• Subjects: ARO-USB oxygen sensor (JFE-AdvantechTM); B_LANDER; Bottom lander; CM; Current direction; Current meter; Current velocity; east-west; north-south; DATE/TIME; Deep-sea Sponge Grounds Ecosystems of the North Atlantic; DEPTH; water; Martha L. Black; MLB2017001; MLB2017001_019; North Atlantic Ocean; Oxygen; dissolved; Salinity; SB_01; SEA-BIRD; SBE37SM-RS232; SponGES; Temperature; Wave height; Wind direction; Wind speed; Wind velocity; south-north; west-east; North Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.928509; https://doi.org/10.1594/PANGAEA.928509

The Scotian Shelf harbors unique aggregations of the glass sponge Vazella pourtalesii providing an important habitat for benthic and pelagic fauna. Recent studies have shown that these sponge grounds have persisted in the face of strong inter-annual and multi-decadal variability in temperature and salinity. However, little is known of the environmental characteristics on hourly-seasonal time scales. This study presents the first hydrodynamic observations and associated (food) particle supply mechanisms for the Vazella sponge grounds, highlighting the influence of natural variability in environmental conditions on sponge growth and resilience. Near-bottom environmental conditions were characterized by high temporal resolution data collected with a benthic lander, deployed during a period of 10-months in the Sambro Bank Sponge Conservation Area. The lander was equipped with temperature and oxygen sensors, a current meter, a sediment trap and a video camera. In addition, water column profiles of temperature and salinity were recorded along a transect, conducted in a gradient from high to lower sponge presence probability. Over the course of the lander deployment, temperature fluctuated between 8.8-12 °C with an average of 10.6 °C ± 0.4 °C. The water contained on average 6.3 mg/l oxygen and near bottom current speed was on average 0.12 m/s, with peaks up to 0.47 m/s. Semi-diurnal tidal flow was observed to result in constant resuspension of particulate matter in the benthic boundary layer. Surface storm events episodically caused extremely turbid conditions on the seafloor that persisted for several days, with particles being resuspended to more than 13 m above the seabed. The carbon flux in the near-bottom sediment trap peaked during storm events and also after a spring bloom in April, when fresh phytodetritus was observed in the bottom boundary layer. While resuspension events can represent a major stressor for sponges, limiting their filtration capability and remobilizing them, episodes of strong currents and ...