From 2016 through to the end of 2025, the Hakai Institute Oceanography Program monitored surface (0-1 or 5m depth) protistan plankton community composition, via optical microscopy, at multiple stations in the northern Salish Sea (Strait of Georgia) and central coast of British Columbia. In the northern Salish Sea, data were collected weekly to bi-weekly in surface waters at a fixed central strait location (QU39, 2016 - 2025) and at a nearshore station located offshore the Hakai Quadra Island field station (QU38, 2019-2023). Shorter monthly time-series and spatial data are also provided for stations within Toba, Bute and Knight Inlets including data from the 2019 Achiever Cruise.
On the central coast, time-series data were collected monthly at four locations: within a fjord (River’s Inlet, DFO2), within Fitz-Hugh (KC10) and Kwakshua (PRUTH) channels and on the shelf (QCS01). Data are also included from the Big Melt Process Study sampling transects outwards from Dean and Burke Inlets to the shelf through Hakai Pass in July and August 2023 and April 2024 to characterize summer and spring bloom conditions, respectively.
This dataset also includes transect data from the False Creek Bioblitz Survey conducted in False Creek, Vancouver, in September 2022.
Water samples were collected using a Niskin bottle from small research vessels (less than 40 ft). Sample water was transferred into 250 mL amber glass bottles and immediately fixed using Lugol's acid-iodine solution (1% concentration) (Edler & Elbrächter 2010; Del Bel Belluz et al., 2021). Samples were kept cool and stored in a dark fridge until analysis was performed at LCLJ Marine Ecological Services in Victoria, BC, by Dr. Louis Hobson. Protistan plankton were enumerated following the Utermöhl method (Utermöhl, 1931; Edler & Elbrächter 2010) using 50 mL settling chambers and phase contrast microscopy on an inverted light microscope (Hobson & Galbraith, 2018). The analysis targets autotrophic protists, but includes all visible taxa including mixotrophic and heterotrophic microzooplankton species. In addition, harmful algae species are enumerated. The analyst is generally able to resolve species as small as 4 um and taxa are classified to the lowest taxonomic level usually to genus or species. Results are provided as abundance of species in cells/L.
These data are published on the Ocean Biodiversity Information System (OBIS) following the required Darwin Core biodiversity data standards (https://manual.obis.org/). In accordance with these standards, taxa name (scientificName) represent the currently accepted name on the World Register of Marine Species (WoRMs). Data are freely available for download from OBIS at https://ipt.iobis.org/obiscanada/resource?r=hakai_protistan_plankton_qu39&v=1.4 and from the Global Biodiversity Information Facility at https://doi.org/10.15468/q748tc.
These time series are maintained to characterize and monitor protistan plankton diversity and investigate links to environmental drivers, the food web and carbon dynamics. Additionally, data are used to support group level phytoplankton composition derived via HPLC phytoplankton pigment analysis, particulate organic matter fatty acid analysis, molecular methods (eDNA) and to validate remote sensing products.
In the northern Salish Sea, portions of this time series have been published in Del Bel Belluz et al. (2021) and Mclaskey et al. (2022). On the central coast, data have been used to investigate trends and drivers of protistan plankton communities across a fjord to shelf gradient (Del Bel Belluz, submitted).
Phytoplankton form the base of the marine food web and drive marine biogeochemical cycling. These species have high turnover rates and quickly respond to environmental perturbation. As a result they are valuable indicators of ecological change. High temporal resolution long term time series are invaluable for investigating dynamic coastal waters with highly variable protistan plankton communities.
10.21966/jv5k-3k59
