http://lod.bco-dmo.org/id/dataset/754508
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2019-01-31
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Phosphorus redox and water column phosphorus data from R/V Neil Armstrong AR16 in the Western North Atlantic from 2017-05-04 to 2017-05-20
2019-01-31
publication
2019-01-31
revision
BCO-DMO Linked Data URI
2019-01-31
creation
http://lod.bco-dmo.org/id/dataset/754508
Benjamin A.S. Van Mooy
Woods Hole Oceanographic Institution
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: Van Mooy, B. A. (2019) Phosphorus redox and water column phosphorus data from R/V Neil Armstrong AR16 in the Western North Atlantic from 2017-05-04 to 2017-05-20. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2019-01-31 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/754508 [access date]
Phosphorus redox and water column phosphorus data Dataset Description: <p>Sampling was conducted aboard the R/V Neil Armstrong during a cruise in May of 2017.&nbsp; Water samples for whole community analyses were collected from Niskin bottles deployed on a rosette with a CTD.&nbsp;</p> Methods and Sampling: <div>All data collected from a modified procedure as described in Van Mooy et al (2015).</div>
<div>Sampling -&nbsp;Samples were taken at depths corresponding to 30% PAR (10-36 m). At Station 6, samples were taken at depths 5 m, 25 m, 60 m, 90 m, 110 m, 150 m, 205 m, 250 m, and 500 m. Subsamples for incubations were dispensed from the Niskin bottle directly into triplicate acid-cleaned 50 mL polycarbonate bottles and processed as described below.</div>
<div>&nbsp;</div>
<div>Phosphate uptake rates - The incubation bottles were carried to a laboratory van that was designated solely for work with radioactive isotopes.&nbsp; Each incubation bottle was spiked with approximately 10 µCi of 33P-phosphoric acid.&nbsp; The final concentration of 33P-phosphate in the incubations was less than 10 pmol L-1, which was likely two orders of magnitude smaller than ambient phosphate concentrations. The bottles were capped and mixed by gently inverting.&nbsp; To account for any abiotic adsorption of the radioactive tracer, additional triplicate 50 mL subsamples were spiked with 10% paraformaldehyde prior to the addition of the 33P-phosphoric acid. These “kill controls” were used for blank subtractions in uptake and reduction rate calculations. All bottles were placed in a flow-through on-deck incubator that was maintained at surface seawater temperatures by continually flushing it with the surface seawater from the ship’s pumping system.&nbsp; Temperature in the incubators was occasionally monitored with a waterproof temperature logger (Onset).&nbsp; The incubators used blue transparent film to achieve a light intensity to mimick 30% PAR. For the depth profile at Station 6, the incubators used a combination of neutral density screening and blue transparent film to achieve a light intensity to mimick PAR throughout the water column while samples with less than 1% PAR were placed in black plastic bags for complete darkness. Incubations proceeded for an average of 3.32 h (0.95 to 10.5 h) then 5 mL of sample was vacuum filtered (approximately 200 mbar) onto 25 mm diameter 0.2 µm pore size polycarbonate membranes (Millipore). The membranes were quickly rinsed three times with freshly filtered (0.2 µm pore size polycarbonate membrane) surface seawater.&nbsp; The membranes were then immediately placed in a liquid scintillation vial containing 10 mL of UltimaGold liquid (Perkin Elmer) scintillation cocktail, which was then shaken vigorously.&nbsp; After resting for a few hours, the 33P-radioacitivity in the vials was determined using a liquid scintillation counter (Perkin Elmer).&nbsp; A steady-state phosphate turnover rate was calculated by dividing the total 33P radioactivity retained on the membranes by the total 33P radioactivity added to the incubations and the incubation time.</div>
<div>&nbsp;</div>
<div>Phosphate reduction to intracellular P(III) compounds – The remaining 45 mL of sample was vacuum filtered as described above. Next, the membranes were immersed in 1.0 mL of ultra-high purity (UHP) deionized water (18 MΩ*cm) in a cryovial (Fisher).&nbsp; The vials were immediately capped and immersed in liquid nitrogen for approximately 10 min, before they were immersed in boiling-hot water for 10 min, and then vigorously shaken.&nbsp; This freeze-thaw cycle was repeated two additional times, after which generally little discernable cellular debris was visible.&nbsp; Next, 100 µL aliquots of the samples were injected onto an IC system (Dionex) which pumped an eluent gradient of 23 mmol L-1 to 90 mmol L-1 sodium hydroxide through an IonPac AS18 (Dionex) column at a rate of 1.0 mL min-1.&nbsp; An ion suppressor using UHP water as a regenerant removed sodium hydroxide from the eluent. Three fractions were collected in 40 second intervals at retention times where pure standards of (1) methyl-phosphonate, 2-hydroxethyl-phosphonate, and (3) phosphite elute (fraction 2 did not have a known phosphonate compound at time of analysis) and the 33P-radioactivity determined as described above. The 33P-radioactivity of the three fractions was summed, corrected for dilution, and then divided by the 33P-radioactivity from the parallel 33P-phosphate uptake subsamples to determine the fraction (%) of 33P uptake that was incorporated into P (III) compounds.&nbsp; Environmental triplicates were averaged, and the standard deviation was propagated as analytical error.&nbsp; All samples were processed at sea in May 2017 except samples from Station 9, which were flash-frozen in liquid nitrogen, transported to the laboratory in a cryogenic dry shipper, and stored in liquid nitrogen until their analysis in June 2017.&nbsp;&nbsp;</div>
<div>&nbsp;</div>
<div>MAGIC Soluble reactive phosphorus (SRP) concentrations.&nbsp; SRP (i.e. phosphate) was determined in seawater samples (done in triplicate) and incubations using MAGnesium Induced Coprecipitation (MAGIC) as described by Karl and Tien (1992).</div>
<div>&nbsp;</div>
<div>Total particulate phosphorus (TTP) concentrations. TPP was determined in seawater samples using a wet chemical oxidation method using potassium persulfate as described in Suzumura (2008). Briefly, 1 to 2 liters of seawater were filtered onto 47 mm 0.2 µm pore size polyvinylidene fluoride membranes (Millipore) and frozen (-80°C) until analysis. One fourth of these filters were cut with clean stainless-steel scissors and placed in 8 mL glass vials for oxidation. 2 mL of 5% (0.19 M) persulfate was added to each vial and the samples were then autoclaved for 30 minutes at 120°C. To remove any residual material, the samples were filtered through 0.45 µm syringe filters (Millipore Millex-HV). The persulfate was shown to inhibit color development when greater than 2%, therefore, the samples were diluted to 0.5% (0.019 M). As with the SRP samples, the TPP samples were analyzed via the molybdenum blue method using a spectrophotometer (Thermo).</div>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1536346 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1536346
completed
Benjamin A.S. Van Mooy
Woods Hole Oceanographic Institution
(508) 289 2322
Department of Marine Chemistry and Geochemistry, MS #4, Fye 117 Woods Hole Oceanographic Institution
Woods Hole
MA
02543
USA
bvanmooy@whoi.edu
pointOfContact
asNeeded
Dataset Version: 1
Unknown
Date
Station
CTD_Cast
lat
lon
Depth
MAGIC_SRP
TPP
Sample_type
P33_phosphate_incorporation_into_P_3_compounds
P33_phosphate_uptake
P33_phosphate_incorporation_into_P3_compounds_pcnt
P33_phosphate_incorporation_into_P3_compounds_analytical_error
liquid scintillation counter (Perkin Elmer)
bottle
spectrophotometer (Thermo)
theme
None, User defined
date
station number
cast
latitude
longitude
depth
reactive phosphorus (PO4)
Total Particulate Phosphorus
sample type
No BCO-DMO term
radiotracer phosphate uptake
featureType
BCO-DMO Standard Parameters
Liquid Scintillation Counter
Niskin bottle
Spectrophotometer
instrument
BCO-DMO Standard Instruments
AR16
service
Deployment Activity
Western North Atlantic
place
Locations
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
Redox Cycling of Phosphorus in the Western North Atlantic Ocean
https://osprey.bco-dmo.org/project/746565
Redox Cycling of Phosphorus in the Western North Atlantic Ocean
<p>NSF Award Abstract:</p>
<p>Redox Cycling of Phosphorus in the Western North Atlantic Ocean<br />
Benjamin Van Mooy<br />
ID: 1536346</p>
<p>Understanding controls on the growth of plankton in the upper ocean, which plays an essential role in the sequestration of carbon dioxide, is an important endeavor for chemical oceanography. Phosphorus is an essential element for marine plankton, and has been a research focus of chemical oceanography for nearly a century. Yet, phosphorus redox cycling rates are almost completely unknown throughout the ocean, and the specific molecular identities of the phosphonates, a form of phosphate, in seawater have defied elucidation. This project will explore and refine entirely new pathways for the biological cycling of phosphorus. This project will support teaching and learning by funding the PhD research of a graduate student, and through the continuation of conducting K-12 classroom laboratory modules and hosting 6-8th grade science fair participants in the investigator's lab.</p>
<p>Phosphorus has never been viewed by oceanographers as an element that actively undergoes chemical redox reactions in the water column, and it was believed to occur only in the +5 valence state, in compounds such as phosphate. However, over the last 17 years, numerous lines of geochemical and genomic information have emerged to show that phosphorus in the +3 valence state (P(+3)), particularly dissolved phosphonate compounds, may play a very important role within open ocean planktonic communities. This is particularly true in oligotrophic gyres such as the Sargasso Sea, where growth of phytoplankton can be limited by the scarcity of phosphate. To better understand these new data, the investigators will design and execute a research program that spans at-sea chemical oceanographic experimentation, state-of-the-art chromatography and mass spectrometry, and novel organic synthesis of 33P-labeled P(+3) compounds. Specifically, they will answer questions about rates of production and consumption of low molecular weight P(+3) compounds, the impact of phosphate availability on the production and consumption of P(+3) compounds, and the groups of phytoplankton that utilize low molecular weight P(+3) compounds. Results of this project have the potential to contribute to the transformation of our understanding of the marine phosphorus cycle.</p>
Phosphorus Redox Cycling
largerWorkCitation
project
eng; USA
oceans
Western North Atlantic
-71.21921
-64.44075
29.16425
40.59278
2017-05-04
2017-05-20
western north Atlantic
0
BCO-DMO catalogue of parameters from Phosphorus redox and water column phosphorus data from R/V Neil Armstrong AR16 in the Western North Atlantic from 2017-05-04 to 2017-05-20
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/754519.rdf
Name: Date
Units: unitless
Description: <p>Sampling date formatted as YYYY-MM-DD</p>
http://lod.bco-dmo.org/id/dataset-parameter/754520.rdf
Name: Station
Units: unitless
Description: <p>numeric identifier for the station where the data was collected</p>
http://lod.bco-dmo.org/id/dataset-parameter/754521.rdf
Name: CTD_Cast
Units: unitless
Description: <p>Numeric identifier for the CTD cast where the data was collected</p>
http://lod.bco-dmo.org/id/dataset-parameter/754522.rdf
Name: lat
Units: decimal degrees
Description: <p>latitude of sampling. Positive values indicate North</p>
http://lod.bco-dmo.org/id/dataset-parameter/754523.rdf
Name: lon
Units: decimal degrees
Description: <p>longitude of sampleing. Negative values indicate West</p>
http://lod.bco-dmo.org/id/dataset-parameter/754524.rdf
Name: Depth
Units: meters (m)
Description: <p>depth at which samples were collected</p>
http://lod.bco-dmo.org/id/dataset-parameter/754525.rdf
Name: MAGIC_SRP
Units: nmol per liter (nM/L)
Description: <p>Soluble reactive phosphorus measured by magnesium induced co-precipitation (nd-not determined; bdl-below detection limit;bdl=1.25 nMol per Liter)</p>
http://lod.bco-dmo.org/id/dataset-parameter/754526.rdf
Name: TPP
Units: nmol per liter
Description: <p>Total particulate phosphorus (nd – not determined; bdl – below detection limit; bdl = 4.07 nmol per liter)</p>
http://lod.bco-dmo.org/id/dataset-parameter/754527.rdf
Name: Sample_type
Units: unitless
Description: <p>type of sample (Comm.=Whole community)</p>
http://lod.bco-dmo.org/id/dataset-parameter/754528.rdf
Name: P33_phosphate_incorporation_into_P_3_compounds
Units: counts per minutes per liter per hour (cpm/(L h))
Description: <p>33P-phosphate incorporation into P(III) compounds (Blank corrected; Average value for given CTD cast; Station 9 data were collected in June 2017 and are decay-corrected to May 2017)</p>
http://lod.bco-dmo.org/id/dataset-parameter/754529.rdf
Name: P33_phosphate_uptake
Units: counts per minutes per liter per hour (cpm/(L h))
Description: <p>33P-phosphate uptake (Blank corrected; Average value for given CTD cast; Station 9 data were collected in June 2017 and are decay-corrected to May 2017)</p>
http://lod.bco-dmo.org/id/dataset-parameter/754530.rdf
Name: P33_phosphate_incorporation_into_P3_compounds_pcnt
Units: unitless
Description: <p>33P-phosphate incorporation into P(III) compounds as percentage</p>
http://lod.bco-dmo.org/id/dataset-parameter/754531.rdf
Name: P33_phosphate_incorporation_into_P3_compounds_analytical_error
Units: unitless
Description: <p>33P-phosphate incorporation into P(III) compounds analytical error as percentage</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
20809
https://datadocs.bco-dmo.org/file/DwwxD02S356lM7/phos.csv
phos.csv
Primary data file for dataset ID 754508
download
https://osprey.bco-dmo.org/dataset/754508/data/download
download
onLine
dataset
<div>All data collected from a modified procedure as described in Van Mooy et al (2015).</div>
<div>Sampling -&nbsp;Samples were taken at depths corresponding to 30% PAR (10-36 m). At Station 6, samples were taken at depths 5 m, 25 m, 60 m, 90 m, 110 m, 150 m, 205 m, 250 m, and 500 m. Subsamples for incubations were dispensed from the Niskin bottle directly into triplicate acid-cleaned 50 mL polycarbonate bottles and processed as described below.</div>
<div>&nbsp;</div>
<div>Phosphate uptake rates - The incubation bottles were carried to a laboratory van that was designated solely for work with radioactive isotopes.&nbsp; Each incubation bottle was spiked with approximately 10 µCi of 33P-phosphoric acid.&nbsp; The final concentration of 33P-phosphate in the incubations was less than 10 pmol L-1, which was likely two orders of magnitude smaller than ambient phosphate concentrations. The bottles were capped and mixed by gently inverting.&nbsp; To account for any abiotic adsorption of the radioactive tracer, additional triplicate 50 mL subsamples were spiked with 10% paraformaldehyde prior to the addition of the 33P-phosphoric acid. These “kill controls” were used for blank subtractions in uptake and reduction rate calculations. All bottles were placed in a flow-through on-deck incubator that was maintained at surface seawater temperatures by continually flushing it with the surface seawater from the ship’s pumping system.&nbsp; Temperature in the incubators was occasionally monitored with a waterproof temperature logger (Onset).&nbsp; The incubators used blue transparent film to achieve a light intensity to mimick 30% PAR. For the depth profile at Station 6, the incubators used a combination of neutral density screening and blue transparent film to achieve a light intensity to mimick PAR throughout the water column while samples with less than 1% PAR were placed in black plastic bags for complete darkness. Incubations proceeded for an average of 3.32 h (0.95 to 10.5 h) then 5 mL of sample was vacuum filtered (approximately 200 mbar) onto 25 mm diameter 0.2 µm pore size polycarbonate membranes (Millipore). The membranes were quickly rinsed three times with freshly filtered (0.2 µm pore size polycarbonate membrane) surface seawater.&nbsp; The membranes were then immediately placed in a liquid scintillation vial containing 10 mL of UltimaGold liquid (Perkin Elmer) scintillation cocktail, which was then shaken vigorously.&nbsp; After resting for a few hours, the 33P-radioacitivity in the vials was determined using a liquid scintillation counter (Perkin Elmer).&nbsp; A steady-state phosphate turnover rate was calculated by dividing the total 33P radioactivity retained on the membranes by the total 33P radioactivity added to the incubations and the incubation time.</div>
<div>&nbsp;</div>
<div>Phosphate reduction to intracellular P(III) compounds – The remaining 45 mL of sample was vacuum filtered as described above. Next, the membranes were immersed in 1.0 mL of ultra-high purity (UHP) deionized water (18 MΩ*cm) in a cryovial (Fisher).&nbsp; The vials were immediately capped and immersed in liquid nitrogen for approximately 10 min, before they were immersed in boiling-hot water for 10 min, and then vigorously shaken.&nbsp; This freeze-thaw cycle was repeated two additional times, after which generally little discernable cellular debris was visible.&nbsp; Next, 100 µL aliquots of the samples were injected onto an IC system (Dionex) which pumped an eluent gradient of 23 mmol L-1 to 90 mmol L-1 sodium hydroxide through an IonPac AS18 (Dionex) column at a rate of 1.0 mL min-1.&nbsp; An ion suppressor using UHP water as a regenerant removed sodium hydroxide from the eluent. Three fractions were collected in 40 second intervals at retention times where pure standards of (1) methyl-phosphonate, 2-hydroxethyl-phosphonate, and (3) phosphite elute (fraction 2 did not have a known phosphonate compound at time of analysis) and the 33P-radioactivity determined as described above. The 33P-radioactivity of the three fractions was summed, corrected for dilution, and then divided by the 33P-radioactivity from the parallel 33P-phosphate uptake subsamples to determine the fraction (%) of 33P uptake that was incorporated into P (III) compounds.&nbsp; Environmental triplicates were averaged, and the standard deviation was propagated as analytical error.&nbsp; All samples were processed at sea in May 2017 except samples from Station 9, which were flash-frozen in liquid nitrogen, transported to the laboratory in a cryogenic dry shipper, and stored in liquid nitrogen until their analysis in June 2017.&nbsp;&nbsp;</div>
<div>&nbsp;</div>
<div>MAGIC Soluble reactive phosphorus (SRP) concentrations.&nbsp; SRP (i.e. phosphate) was determined in seawater samples (done in triplicate) and incubations using MAGnesium Induced Coprecipitation (MAGIC) as described by Karl and Tien (1992).</div>
<div>&nbsp;</div>
<div>Total particulate phosphorus (TTP) concentrations. TPP was determined in seawater samples using a wet chemical oxidation method using potassium persulfate as described in Suzumura (2008). Briefly, 1 to 2 liters of seawater were filtered onto 47 mm 0.2 µm pore size polyvinylidene fluoride membranes (Millipore) and frozen (-80°C) until analysis. One fourth of these filters were cut with clean stainless-steel scissors and placed in 8 mL glass vials for oxidation. 2 mL of 5% (0.19 M) persulfate was added to each vial and the samples were then autoclaved for 30 minutes at 120°C. To remove any residual material, the samples were filtered through 0.45 µm syringe filters (Millipore Millex-HV). The persulfate was shown to inhibit color development when greater than 2%, therefore, the samples were diluted to 0.5% (0.019 M). As with the SRP samples, the TPP samples were analyzed via the molybdenum blue method using a spectrophotometer (Thermo).</div>
Specified by the Principal Investigator(s)
<p>BCO-DMO Processing:</p>
<ul>
<li>Added conventional header with dataset name, PI name, version date.</li>
<li>Modified parameter names to conform with BCO-DMO naming conventions.</li>
<li>Reformatted dates to ISO0861 convention.</li>
<li>Appended latitude/longitude information.</li>
<li>combined the P redox data and water column P data into one dataset using the station and cast number as mapping keys.</li>
</ul>
<p>&nbsp;</p>
Specified by the Principal Investigator(s)
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
liquid scintillation counter (Perkin Elmer)
liquid scintillation counter (Perkin Elmer)
PI Supplied Instrument Name: liquid scintillation counter (Perkin Elmer) PI Supplied Instrument Description:After resting for a few hours, the 33P-radioacitivity in the vials was determined using a liquid scintillation counter (Perkin Elmer). Instrument Name: Liquid Scintillation Counter Instrument Short Name:LSC Instrument Description: Liquid scintillation counting is an analytical technique which is defined by the incorporation of the radiolabeled analyte into uniform distribution with a liquid chemical medium capable of converting the kinetic energy of nuclear emissions into light energy. Although the liquid scintillation counter is a sophisticated laboratory counting system used to quantify the activity of particulate emitting (ß and a) radioactive samples, it can also detect the auger electrons emitted from 51Cr and 125I samples.
Liquid scintillation counters are instruments assaying alpha and beta radiation by quantitative detection of visible light produced by the passage of rays or particles through a suitable scintillant incorporated into the sample. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB21/
bottle
bottle
PI Supplied Instrument Name: bottle PI Supplied Instrument Description:bottle Instrument Name: Niskin bottle Instrument Short Name:Niskin bottle Instrument Description: A Niskin bottle (a next generation water sampler based on the Nansen bottle) is a cylindrical, non-metallic water collection device with stoppers at both ends. The bottles can be attached individually on a hydrowire or deployed in 12, 24, or 36 bottle Rosette systems mounted on a frame and combined with a CTD. Niskin bottles are used to collect discrete water samples for a range of measurements including pigments, nutrients, plankton, etc. Community Standard Description: http://vocab.nerc.ac.uk/collection/L22/current/TOOL0412/
spectrophotometer (Thermo)
spectrophotometer (Thermo)
PI Supplied Instrument Name: spectrophotometer (Thermo) PI Supplied Instrument Description:As with the SRP samples, the TPP samples were analyzed via the molybdenum blue method using a spectrophotometer (Thermo). Instrument Name: Spectrophotometer Instrument Short Name:Spectrophotometer Instrument Description: An instrument used to measure the relative absorption of electromagnetic radiation of different wavelengths in the near infra-red, visible and ultraviolet wavebands by samples. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB20/
Cruise: AR16
AR16
International Council for the Exploration of the Sea
R/V Neil Armstrong
vessel
AR16
Benjamin A.S. Van Mooy
Woods Hole Oceanographic Institution
International Council for the Exploration of the Sea
R/V Neil Armstrong
vessel