Data Name (This will be the displayed title in Catalog)
Phytoplankton Size Class
Indicator Name (as exists in ecodata)
phyto_size
Family (Which group is this indicator associated with?)
[ ] Oceanographic
[ ] Habitat
[X] Lower trophic levels
[ ] Megafauna
[ ] Social
[ ] Economic
Data Description
Satellite derived phytoplankton size class for the Northeast Continental Shelf and ecological production units.
Introduction to Indicator (Please explain your indicator)
Phytoplankton are key biological regulators of the structure and function of most marine ecosystems. They are the foundation of the marine food web and are the primary food source for zooplankton and filter feeders such as shellfish. Numerous environmental and oceanographic factors interact to drive the abundance, composition, spatial distribution, seasonal timing and productivity of phytoplankton. The size structure of the phytoplankton community influences important biogeochemical and ecological processes, including transfer of energy through the marine food web.
The unique physical characteristics of the Northeast U.S. continental shelf help make it among the most productive continental shelf systems in the world influenced by both bottom-up (e.g. nutrient concentrations, light availability, and mixing/stratification) and top-down (e.g. grazing) controls. Phytoplankton biomass, composition, and productivity all have high spatial, seasonal and interannual variability. The most pronounced spatial pattern is the decrease in phytoplankton biomass from the coast to the shelf break. Georges Bank and Nantucket Shoals are shallow regions that are well mixed by tides. This mixing supplies sufficient nutrients to support phytoplankton growth throughout the year. In other regions, blooms of large diatom species occur on a seasonal cycle when growing conditions are ideal.
Key Results and Visualization
The seasonal cycles of phytoplankton size distribution are typically dominated by larger-celled microplankton during the winter-spring and fall bloom periods, while smaller-celled nanoplankton dominate during the warmer summer months. Phytoplankton size class distributions were near average for most of the year, except during the early fall bloom.
On Georges Bank, the early winter bloom was most likely associated with diatoms, however the above average microplankton fraction from April through August can be attributed to the dinoflagellate Tripos muelleri.
In the Gulf of Maine, the early winter bloom was most likely associated with diatoms, however the record high microplankton fraction from April through August can be attributed to the dinoflagellate Tripos muelleri.
Implications
Phytoplankton abundance, productivity, diversity, cell size, phenology, and carbon fluxes are regulated by the local physical and chemical environment and grazing. Interannual and climatological changes in temperature, freshwater inputs (due to ice sheet melting and/or enhanced river discharge), wind direction, and wind speed can alter the circulation patterns, upwelling conditions, and nutrient fluxes, directly affecting the timing, location, species composition of phytoplankton blooms in the NES. As the NES responds to warming, changing phenologies, changing chemistry, and changes in circulation patterns, we must understand how varying biophysical interactions control phytoplankton and subsequently affect fisheries, their habitats and the people, businesses and communities that depend on them.
Spatial Scale
By EPU and gridded for the entire shelf
Temporal Scale
Daily, weekly, monthly, annual, climatology (1998 to current year)
Synthesis Theme
[X] Multiple System Drivers
[ ] Regime Shifts
[ ] Ecosystem Reorganization
Define Variables
1) Microplankton fraction; The fraction of total chlorophyll concentration in the near surface (first euphotic depth) waters from microplankton (20-200 µm); (percent)
2) Nanoplankton fraction; The fraction of total chlorophyll concentration in the near surface (first euphotic depth) waters from nanoplankton (2-20 µm); (percent)
3) Picoplankton fraction; The fraction of total chlorophyll concentration in the near surface (first euphotic depth) waters from picoplankton (0.2-2 µm); (percent)
Indicator Category
[X] Published Methods
[ ] Extensive analysis, not yet published
[ ] Syntheses of published information
[ ] Database pull
[ ] Database pull with analysis
[X] Other
If other, please specify indicator category
Publicly available satellite data that are processed and analyzed
Primary Contact
kimberly.hyde@noaa.gov
Secondary Contact
No response
Data Name (This will be the displayed title in Catalog)
Phytoplankton Size Class
Indicator Name (as exists in ecodata)
phyto_size
Family (Which group is this indicator associated with?)
Data Description
Satellite derived phytoplankton size class for the Northeast Continental Shelf and ecological production units.
Introduction to Indicator (Please explain your indicator)
Phytoplankton are key biological regulators of the structure and function of most marine ecosystems. They are the foundation of the marine food web and are the primary food source for zooplankton and filter feeders such as shellfish. Numerous environmental and oceanographic factors interact to drive the abundance, composition, spatial distribution, seasonal timing and productivity of phytoplankton. The size structure of the phytoplankton community influences important biogeochemical and ecological processes, including transfer of energy through the marine food web.
The unique physical characteristics of the Northeast U.S. continental shelf help make it among the most productive continental shelf systems in the world influenced by both bottom-up (e.g. nutrient concentrations, light availability, and mixing/stratification) and top-down (e.g. grazing) controls. Phytoplankton biomass, composition, and productivity all have high spatial, seasonal and interannual variability. The most pronounced spatial pattern is the decrease in phytoplankton biomass from the coast to the shelf break. Georges Bank and Nantucket Shoals are shallow regions that are well mixed by tides. This mixing supplies sufficient nutrients to support phytoplankton growth throughout the year. In other regions, blooms of large diatom species occur on a seasonal cycle when growing conditions are ideal.
Key Results and Visualization
The seasonal cycles of phytoplankton size distribution are typically dominated by larger-celled microplankton during the winter-spring and fall bloom periods, while smaller-celled nanoplankton dominate during the warmer summer months. Phytoplankton size class distributions were near average for most of the year, except during the early fall bloom.
On Georges Bank, the early winter bloom was most likely associated with diatoms, however the above average microplankton fraction from April through August can be attributed to the dinoflagellate Tripos muelleri.
In the Gulf of Maine, the early winter bloom was most likely associated with diatoms, however the record high microplankton fraction from April through August can be attributed to the dinoflagellate Tripos muelleri.
Implications
Phytoplankton abundance, productivity, diversity, cell size, phenology, and carbon fluxes are regulated by the local physical and chemical environment and grazing. Interannual and climatological changes in temperature, freshwater inputs (due to ice sheet melting and/or enhanced river discharge), wind direction, and wind speed can alter the circulation patterns, upwelling conditions, and nutrient fluxes, directly affecting the timing, location, species composition of phytoplankton blooms in the NES. As the NES responds to warming, changing phenologies, changing chemistry, and changes in circulation patterns, we must understand how varying biophysical interactions control phytoplankton and subsequently affect fisheries, their habitats and the people, businesses and communities that depend on them.
Spatial Scale
By EPU and gridded for the entire shelf
Temporal Scale
Daily, weekly, monthly, annual, climatology (1998 to current year)
Synthesis Theme
Define Variables
1) Microplankton fraction; The fraction of total chlorophyll concentration in the near surface (first euphotic depth) waters from microplankton (20-200 µm); (percent) 2) Nanoplankton fraction; The fraction of total chlorophyll concentration in the near surface (first euphotic depth) waters from nanoplankton (2-20 µm); (percent) 3) Picoplankton fraction; The fraction of total chlorophyll concentration in the near surface (first euphotic depth) waters from picoplankton (0.2-2 µm); (percent)
Indicator Category
If other, please specify indicator category
Publicly available satellite data that are processed and analyzed
Data Contributors
Kimberly Hyde
Point(s) of Contact
kimberly.hyde@noaa.gov
Affiliation
NEFSC
Public Availability
Source data are publicly available.
Accessibility and Constraints
No response