Dataset: 2019 BAIT Particulate Metals
Data Citation:
Twining, B., Ohnemus, D. C., Sofen, L. (2023) Particulate trace element concentrations measured during four cruises in 2019 at locations around the Bermuda Atlantic Time-series Study (BATS) station. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2023-02-01 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.888772.1 [access date]
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This dataset is licensed under Creative Commons Attribution 4.0.
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DOI:10.26008/1912/bco-dmo.888772.1
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Spatial Extent: N:32.151 E:-63.5636 S:31.1769 W:-64.8234
Temporal Extent: 2019-03-11 - 2019-11-21
Program:
U.S. GEOTRACES (U.S. GEOTRACES)
Principal Investigator:
Benjamin Twining (Bigelow Laboratory for Ocean Sciences)
Co-Principal Investigator:
Daniel C. Ohnemus (Skidaway Institute of Oceanography, SkIO)
Scientist:
Laura Sofen (Bigelow Laboratory for Ocean Sciences)
BCO-DMO Data Manager:
Shannon Rauch (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version:
1
Version Date:
2023-02-01
Restricted:
No
Validated:
Yes
Current State:
Final no updates expected
Particulate trace element concentrations measured during four cruises in 2019 at locations around the Bermuda Atlantic Time-series Study (BATS) station
Abstract:
Particulate trace element concentrations were measured during 4 BATS cruises (March, May, August, November) in 2019 as part of the Bermuda Atlantic Iron Timeseries (BAIT) project. Three stations were sampled around the BATS station to 1800 meters (m) with a trace-metal clean rosette system. Collected water was passed through 0.45-micrometer (um) Supor membranes and subsequently subjected to both a weak acid leach and a total digest. Samples were analyzed via magnetic sector ICPMS for aluminum (Al), phosphorus (P), titanium (Ti), vanadium (V), manganese (Mn), iron (Fe), cobalt (Co), nickel (Ni), copper (Cu), zinc (Zn), cadmium (Cd), barium (Ba), lead (Pb), and thorium (Th). Data have been used to partition particulate Fe into lithogenic, biogenic, and authigenic fractions, and to understand controls on Fe cycling in the upper ocean over a seasonal cycle.