Dataset: Biogenic Silica from CTD samples collected during R/V Hugh R. Sharp cruise HRS2204 from Apr to May 2022

Final no updates expectedDOI: 10.26008/1912/bco-dmo.945973.1Version 1 (2025-02-27)Dataset Type:Cruise Results

Principal Investigator: Matthew Rau (Pennsylvania State University)

Scientist: Kimberlee Thamatrakoln (Rutgers University)

Student: Austin Grubb (Rutgers University)

BCO-DMO Data Manager: Audrey Mickle (Woods Hole Oceanographic Institution)


Project: Collaborative Research: The importance of particle disaggregation on biogeochemical flux predictions (Disaggregation)


Abstract

These data include measurements of biogenic silica from CTD bottle water samples collected during a cruise on the Northeast Continental Shelf to study particle disaggregation. One cruise was completed aboard the R/V Hugh R. Sharp from 2022-04-21 through 2022-05-02 (HRS22-04), which visited a variety of stations and hydrodynamic environments associated with the Northeast Continental Shelf of the United States. Stations ranged from Georges Bank and the Great South Channel near the Gulf of Maine, M...

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This cruise visited eight stations on the Northeastern U.S. Continental Shelf. Latitudes and longitudes provided per sample in the data, but general station descriptions are below.

  • Station 1 - Station 3: Georges Bank near the Gulf of Maine. Approximate location was 41.7 N, 68 W. Samples acquired from 0 m to 25 m depths.
  • Station 4: The Great South Channel near the Gulf of Maine. Approximate location was 41.6 N, 69 W. Samples acquired from 0 m to 150 m depths.
  • Station 5: Only one CTD profile was taken before this station was aborted due to weather. No data acquired. Station location was 40.8 N, 70.5 W.
  • Station 6: Off the coast of Martha's Vineyard. Approximate location was 41.3 N, 70.5 W. Samples acquired from 0 m to 10 m depths.
  • Station 7: At the mouth of the Sakonnet River near Newport, Rhode Island. Approximate location was 41.5 N, 71.2 W. Samples acquired from 0 m to 10 m depths.
  • Station 8: Hudson Canyon near New York. Approximate location was 39.5 N, 72.3 W. Samples acquired from 0 m to 200 m depths.

Samples for biogenic silica measurements were collected via filtration onto 1.2 µm pore-size, polycarbonate filters (Millipore) and stored at -20 degree C until processing. Downstream analysis was done using a modified sodium hydroxide digestion method as described in Krause et al. 2009. Micro-molar of silicon was calculated from transmission using a spectrophotometer with a 1 cm cuvette.


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Methods

Krause, J. W., Lomas, M. W., & Nelson, D. M. (2009). Biogenic silica at the Bermuda Atlantic Time‐series Study site in the Sargasso Sea: Temporal changes and their inferred controls based on a 15‐year record. Global Biogeochemical Cycles, 23(3). Portico. https://doi.org/10.1029/2008gb003236