Dataset: Picoeukaryotic phytoplankton observations
Data Citation:
Martiny, A., Flombaum, P. (2019) Picoeukaryotic phytoplankton observations from available public repositories and primary sources from from 1988-2007. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2019-12-04 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.783463.1 [access date]
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This dataset is licensed under Creative Commons Attribution 4.0.
If you wish to use this dataset, it is highly recommended that you contact the original principal investigators (PI). Should the relevant PI be unavailable, please contact BCO-DMO (info@bco-dmo.org) for additional guidance. For general guidance please see the BCO-DMO Terms of Use document.
DOI:10.1575/1912/bco-dmo.783463.1
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Spatial Extent: N:73.06 E:180 S:-66.1 W:-180
Temporal Extent: 1988-01-06 - 2007-08-20
Project:
Principal Investigator:
Adam Martiny (University of California-Irvine, UC Irvine)
Co-Principal Investigator:
Pedro Flombaum (Universidad de Buenos Aires)
BCO-DMO Data Manager:
Shannon Rauch (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version:
1
Version Date:
2019-12-04
Restricted:
No
Validated:
Yes
Current State:
Final no updates expected
Picoeukaryotic phytoplankton observations from available public repositories and primary sources from from 1988-2007
Abstract:
Picoeukaryotic phytoplankton observations from available public repositories and primary sources. Picoeukaryotic phytoplankton are defined as red fluorescent cells larger than Prochlorococcus and less than 2-3 µm in cell diameter. We only considered cell counts by flow cytometry. Samples covered a latitudinal range from 71.4˚N to 66.1˚S up to 400 m depth. Ancillary temperature and nitrate records were available for all but 2,334 and 6,530 observations, respectively, which we complemented with 1° monthly depth-dependent averages from the World Ocean Atlas (www.nodc.noaa.gov). To avoid analytical issues with detection limits, we imposed a minimum nitrate concentration of 0.01 μM. We calculated surface PAR (8 d averaged, 0.047° grid cell) using SeaWiFS and MODIS observations. Downward PAR was estimated using the attenuation coefficient K₄₉₀ from SeaWiFS and MODIS (http://oceancolor.gsfc.nasa.gov) and corrected for chlorophyll a³⁰, and a minimum of 10⁻³ E/m²d was imposed. Latitude, longitude, sample year, date and depth are provided with the field sample.