Herbivorous protist abundances under simultaneous manipulation of temperature and nutrients from the Long-term Plankton Time Series site in Narragansett Bay, RI in 2017 (NCEI Accession 0291402)

This dataset contains biological and survey - biological data collected on 2017-03-20. These data include abundance and species. The instruments used to collect these data include Inverted Microscope, Microscope - Optical, and Turner Designs Fluorometer 10-AU. These data were collected by Elena Litchman and Paul Wilburn of Michigan State University, Joshua D. Kling of University of California-Berkeley, Gayantonia Franzè, Stephanie I. Anderson, Susanne Menden-Deuer, and Tatiana A. Rynearson of University of Rhode Island, and David A. Hutchins of University of Southern California as part of the "Dimensions: Collaborative Research: Genetic, functional and phylogenetic diversity determines marine phytoplankton community responses to changing temperature and nutrients (Phytoplankton Community Responses)" and "Quantifying Temperature Dependence In Growth & Grazing Rates of Planktonic Herbivores (Planktonic Herbivore Temp Dependence)" projects and "Dimensions of Biodiversity (Dimensions of Biodiversity)" program. The Biological and Chemical Oceanography Data Management Office (BCO-DMO) submitted these data to NCEI on 2023-04-13.

The following is the text of the dataset description provided by BCO-DMO:

Acquisition Description:
This dataset represents abundances of several morphospecies herbivorous protists under initial conditions (day0) and after 10 days of incubation under modified temperature and nutrient conditions from seawater collected from the Narragansett Bay (NB) Long-term Plankton Time Series site (41.57 ºN, 71.39 ºW).

The experimental set-up consisted of a nested design: source water with plankton communities (less than 200 microns) was used to set up long-term (10-day) microcosm incubations at three temperatures and two nutrient concentrations to monitor the community response to temperature and nutrient manipulations in terms of species composition and abundance over the incubation period. Seawater was filtered through a 200 micrometer (µm) mesh to eliminate macrozooplankton grazers. The 20-liter (L) acid-washed carboys were immediately transported to the laboratory. Seawater from each microcosm was used to assess phytoplankton growth and microzooplankton herbivory rates following the two-point modification of the dilution method (Landry and Hassett 1982) with 100 percent and 10 percent SW dilution levels. The initial dilution experiment conducted on day 0 (D0) was used to assess metabolic rates under in situ temperature and nutrient load. Then, on day 3 (D3), day 6 (D6), and day 10 (D10) using water from each microcosm, 6 dilution experiments per day (one per each temperature and nutrient level) were conducted for a total of 19 dilution experiments in 10 days.

Experimental bottles were incubated for 24 hours at -0.5 degrees C, 2.6 degrees C, and 6 degrees C under a 12:12 light: dark cycle of cool white fluorescent lights at 115 µmol photons m -2 s -1 . Triplicate subsamples were taken from the 100 percent SW stocks after 24 hours from each incubation bottle for chlorophyll a and microscopy analysis. Chlorophyll a extraction and determination followed Graff and Rynearson (2011) and measurements were performed on a Turner Designs AU10 fluorometer. Plankton community enumeration and composition was performed on samples preserved in 2 percent acid Lugol’s iodine final concentration (Menden-Deuer et al., 2001). Phytoplankton cells were enumerated using a Sedgewick-Rafter slide (1-milliliter volume) and a Nikon Eclipse E800 light microscope while herbivorous protists were enumerated following the Utermöhl (1958) method settling between 2.5 and 15 milliliters. The entire surface area of the settling chamber was examined at 200x with a Nikon Diaphot 300 inverted microscope. Ciliates and dinoflagellates were identified and classified to the lowest possible taxonomic level by consulting several taxonomic guides (Kofoid and Campbell 1929; Tomas 1997; Strüder-Kypke et al. 2002).

Phytoplankton growth and herbivorous grazing rates were estimated from changes in total chlorophyll a concentration over the 24-hour incubation. The instantaneous phytoplankton growth rate (μ) depends on the assumption of unlimited, exponential growth and was calculated following the equation: μ = 1/t ln (N t /N 0 ), where t is the incubation time in days and N t and N 0 are the chlorophyll a concentration at the beginning and at the end of the experiment. Herbivory rates due to microzooplankton grazing were estimated as the difference between μ measured in the diluted (μ 10% ) and whole (μ 100 percent ) seawater sample g = μ 10 percent - μ 100 percent .