The Ocean Archive System searches our original datasets as they were submitted to us, not individual points or profiles. If you want to search and retrieve ocean profiles in a common format, or objectively analyzed fields, your better option may be to use one of our project applications. See: Access Data
OAS accession Detail for 0278256
| << previous | |revision: 1 |
| accessions_id: | 0278256 | archive |
|---|---|
| Title: | Bacterioplankton data from coral and coral mucus aquaria experiments conducted at Bermuda Institute of Ocean Sciences in 2013 (NCEI Accession 0278256) |
| Abstract: | This dataset contains chemical and physical data collected at BIOS during deployment Apprill_2013 at Bermuda, Red Sea, Federated States of Micronesia, Florida Keys, and Australia from 2013-01-01 to 2013-12-31. These data include Ammonium, Nitrite, Silicate, dissolved organic Carbon, nitrate plus nitrite, reactive phosphorus (PO4), salinity calculated from CTD primary sensors, and water temperature. The instruments used to collect these data include Microscope-Fluorescence and PCR Thermal Cycler. These data were collected by Dr Amy Apprill of Woods Hole Oceanographic Institution as part of the "Fundamental Coral-Microbial Associations (Coral Microbial Relationships)" project. The Biological and Chemical Oceanography Data Management Office (BCO-DMO) submitted these data to NCEI on 2019-06-05. The following is the text of the dataset description provided by BCO-DMO: Bacterioplankton data from coral and coral mucus aquaria experiments. Dataset Description: Bacterioplankton data from corals and coral mucus in aquaria experiments conducted at the Bermuda Institute of Ocean Sciences ( 32.3705 degrees N, 64.6966 degrees W). |
| Date received: | 20190605 |
| Start date: | 20130101 |
| End date: | 20131231 |
| Seanames: | |
| West boundary: | |
| East boundary: | |
| North boundary: | |
| South boundary: | |
| Observation types: | chemical, physical |
| Instrument types: | fluorescence microscope, PCR machine |
| Datatypes: | AMMONIUM (NH4), DISSOLVED ORGANIC CARBON, nitrate + nitrite content (concentration), NITRITE, phosphate, SALINITY, silicate, WATER TEMPERATURE |
| Submitter: | |
| Submitting institution: | Biological and Chemical Oceanography Data Management Office |
| Collecting institutions: | Woods Hole Oceanographic Institution |
| Contributing projects: | |
| Platforms: | |
| Number of observations: | |
| Supplementary information: | Acquisition Description: Colonies of Porites astreoides corals (5-20 cm diameter, 30-90 g wet weight) were removed from 3-9 m depth on the Bermudian reefs Hog Breaker (N 32 27.5’ W 64 49.8’), an unnamed reef (N 32 26.042’ W 64 49.248’), and Three Hills Shoal (N 32 41’ W 64 73.3’) in July 2013. Ten colonies were taken from each site in compliance with the Bermuda Institute of Ocean Sciences (BIOS) Collection and Experimental Ethics Policy and were considered Limited Impact Research and as such a collection permit was not required. The colonies were immediately placed in collection bags at depth, sealed and transported in a large collection cooler (greater than 1 h) to the laboratory. At BIOS, the colonies were allowed to acclimate to a mesocosm housing and held in aerated, outdoor fiberglass mesocosms with a flow-through seawater system fed with reef water for two (Three Hills Shoal Reef colonies) or 15 days (all other colonies) prior to the start of the experimental period. For the experiment, the mesocosms consisted of nine, 30 L static aquaria that were set up as previously described (de Putron et al. 2010). Inshore water from 20 meters off shore and one meter in depth was used to fill the aquaria and was pumped through a BIOS flow-through sample system that consisted of a coarse mesh filter and holding tanks followed by a step filtration system of 50 um, then 5 um, to remove larger organisms including some planktonic grazers. Mesocosms were then left static for the 12-day experiment. Mesocosms were randomly arranged to consist of three control, three mucus addition, and three coral mesocosms, with artificial lights providing 61 mol quanta m-2 s-1 photosynthetically active radiation during sunlight hours consistent with the low end of known compensation ranges (3-233 mol quanta m-2 s-1 according to Mass and colleagues (2007) to minimize bleaching. Mesocosms were covered with a transparent plastic film cover and aerated with an air wand bubbler (de Putron et al. 2010). Water was collected from the mesocosms via a syringe-siphon system using silicon tubing. Inline, combusted GF/F filters (Whatman, Maidstone, UK) were attached for samples intended for dissolved organic carbon (DOC) analysis. The reef water temperature, salinity, and conductivity in all mesocosms was monitored daily throughout the experiment using a YSI Professional Plus probe (Yellow Springs, Ohio). Over the course of 12 days, the mesocosms were subjected to one of three conditions: coral (presence/absence of colonies), mucus additions or control (no additions). For the coral mesocosms, the experimental corals (four colonies per mesocosm, three mesocosms) were placed within the mesocosms on days 0 through 4 and removed after water sampling on day 4. Corals were removed for 48-hour until after the sampling procedure on day 6, where they were held in running seawater similarly filtered as in the mesocosms, and reintroduced back into their respective mesocosms from days 6 to 10 and removed again after the sampling procedure on day 10. P. astreoides colonies were not fed over the course of the 12-day experimental period. For the mucus addition mesocosms, mucus was extracted from P. astreoides colonies (n = 18) that were not utilized in the experiment and were maintained in a separate, flow-through seawater tank. These corals (n=18) were taken into the lab and inverted on a funnel to collect mucus for 2 h, a timeframe determined from a preliminary experiment, and the corals returned to the holding aquaria with flow through seawater. Mucus from the additional colonies was pooled and 5 ml was added to each mucus addition mesocosm on days 0.2, 2, 6 and 8. Mucus from the experimental corals (n = 12; named corals A-L from coral tanks 4, 5 and 6) was sampled for community composition prior to day 0, as well as at the end of day 4 and at the end of day 10 of the experiment. For the latter two timepoints, the corals were removed from the experimental mesocosms for 48 hours. Seawater samples (50 ml) for cell counts and fluorescence in situ hybridization (FISH) analyses were taken daily from all mesocosms, fixed with formalin to a final concentration of 10% in the dark for 20 min, and stored at -80C. Samples were thawed and 3-5 ml were filtered onto Irgalan Black stained 25 mm, 0.2 um polycarbonate filters (Nucleopore, Whatman) under gentle vacuum (100 mmHg) and stained with 1 ml of 0, 6-diamidino-2-phenyl dihydrochloride (5 ug ml-1, DAPI, SIGMA-Aldrich, St. Louis, MO) (Porter and Feig 1980). The filters were mounted onto slides with Resolve immersion oil (high viscosity) (Resolve, Richard-Allan Scientific, Kalamazoo, MI) and stored at –20 degrees celsius. Slides were then enumerated using an AX70 epifluorescent microscope (Olympus, Tokyo, Japan) under ultraviolet excitation at 100x magnification. At least 500 cells (10 fields) were counted for picoplankton abundance. FISH was utilized to quantify the abundance of the major picoplankton phylotypes present in the seawater and mucus, and was conducted using previously published protocols and Cy3 labeled probes (Parsons et al. 2014). The bacterial and archaeal groups quantified included the SAR11 clade (152R, 441R, 542R, 732R probes), Alteromonas spp. (AC137R), Vibrio spp. (127R), Rhodobacteracea (536R), Euryarchaeota (Eury806) and Thaumarchaeota (Cren537). Fixed seawater samples (3–5 ml) were filtered onto 25 mm, 0.2 um polycarbonate filters and stored at −20 degrees celcius with desiccant. Quarter filters were washed in 95% ethanol and then probed according to previous protocols (Morris et al. 2002; Parsons et al. 2011, 2014). The cell abundances of the picoplankton phylotypes mentioned above were then determined using image analysis (Parsons et al. 2011, 2014). Detection of Cy3-positive cells and their ratio to DAPI-positive cells was aided by image analysis using an Olympus AX70 microscope (Olympus, Japan) equipped with a Toshiba 3CCD video camera (IK-TU40A Toshiba, Japan), a computer assisted frame grabber and appropriate dichroic filters (Morris et al. 2002; Carlson et al. 2010). Brief exposure times of 1 and 5 seconds were used for DAPI and Cy3 image channels, respectively. Cy3 images were segmented with Image Pro Plus software (Media Cybernetics, Bethesda, MD) and overlaid onto corresponding segmented DAPI images (Parsons et al. 2014). Objects with overlapping signals in both Cy3 and DAPI images were counted as probe positive. The negative control was determined similarly and subtracted from the positive probe counts to correct for autofluorescence and non-specific binding. (For Grazing Rates Processing, see below) Seawater picoplankton biomass for nucleic acids was taken from all experimental mesocosms on days 0, 2, 4, 6, 8, 10 and 12 of the experiment, and from coral mucus extracted from the experimental corals on days 2, 4, and 10 and processing followed a method modified from Giovannoni and colleagues (1990, 1996). 500 ml of water or 1 ml of coral mucus was filtered through a 47 mm, 0.2 um pore filter under gentle vacuum (100 mm Hg), placed into a 4 ml cryovial and stored in 1 ml of sterile sucrose lysis buffer (20 mM EDTA, 400 mM NaCl, 0.75 M sucrose, 50 mM Tris.HCl) at -80 degrees celsius. For DNA extractions of the tissue, mucus and coral samples, sodium dodecyl sulfate to 1% and proteinase K to 200 ug ml-1 were added to the sample and incubated at 37 degrees celsius for 30 min and then at 55 degrees celsius for 30 min. The lysates were extracted with an equal volume of phenol:isoamylalcohol:chloroform (25:1:24) followed by two subsequent equal volumes of isoamylalcohol:chloroform (1:24). The DNA was purified by precipitation using sodium acetate (3M) and isopropanol (100%) for at least 1 hour at -20oC and centrifuged at room temperature for 30 min at 20,000 x g. The resulting pellet was washed with 80% ethanol, vortexed for 30 s and centrifuged at 16,000 x g for 10 min. The pellet was dried and stored at -20C. (See below for Microbial Processing description.) Seawater samples were analyzed for macronutrients (nitrate + nitrite, nitrite, ammonium, ortho phosphate, and silicic acid) at Oregon State University using a continuous segmented flow system consisting of a Technicon AutoAnalyzer II (SEAL Analytical) and an Alpkem RFA 300 Rapid Flow Analyzer (Alpkem) as conducted previously (Apprill and Rappé 2011). DOC was determined via high temperature combustion on a modified Shimadzu TOC-V (Shimadzu Scientific Instruments, Columbia, MD) (Carlson et al. 2010). Flow cytometry was performed on 1 ml seawater preserved to a final concentration of 4% paraformaldehyde to enumerate pigmented picoeukaryotes, Synechococcus, and non-pigmented picoplankton using methods described in Apprill and Rappé (2011). High and low DNA-containing cells were enumerated following SybrGreen staining. The ANOVA and Tukey’s HSD statistics were conducted as described below. |
| Availability date: | |
| Metadata version: | 1 |
| Keydate: | 2023-05-15 04:46:54+00 |
| Editdate: | 2023-05-15 04:47:54+00 |