Dataset: Heterotrophic Production Rates collected from CliOMZ AT50-10 in the Eastern Pacific Ocean from May to June 2023 (CliOMZ project)

ValidatedFinal no updates expectedDOI: 10.26008/1912/bco-dmo.948411.1Version 1 (2025-01-13)Dataset Type:Cruise Results

Principal Investigator: Alyson E. Santoro (University of California-Santa Barbara)

Scientist, Contact: Barbara Bayer (University of Vienna)

Data Manager: Sawyer Newman (Woods Hole Oceanographic Institution)


Project: Collaborative Research: Underexplored Connections between Nitrogen and Trace Metal Cycling in Oxygen Minimum Zones Mediated by Metalloenzyme Inventories (CliOMZ)


Abstract

These data include heterotrophic production rates measured on R/V Atlantis (CliOMZ AT50-10 expedition) from Golfito, Costa Rica to San Diego, USA in May-June 2023. We aimed at comparing heterotrophic and chemoautotrophic microbial activities at the selected study sites. Instruments used were a CTD profiler and a scintillation counter (Perkin-Elmer Tri-Carb 2910 TR).

Discrete water samples were collected using a rosette sampler equipped with 24×10 L Niskin bottles. Different depths were sampled ranging from 55 meters to 1500 meters. The sampling strategy specifically focused on targeting low oxygen zones within the water column. Water was dispensed into 2 mL microcentrifuge tubes in the laboratory. Microbial heterotrophic production was measured via the incorporation of [3H]-leucine into microbial biomass using a modified version of the microcentrifuge method (Baetge et. al., 2021). [3H]-leucine (specific activity 44.9 Ci mmol-1; Perkin Elmer) was added to 1.7 mL of sample at a final concentration of 20 nM and incubated for 2-3 h at in situ temperature. For each depth and station, triplicate live incubations and one killed control, to which 100 µL of trichloroacetic acid (TCA) was added immediately, were carried out. At one station, the effect of phenylacetylene and DMSO additions on heterotrophic production activities was tested over a time-span of 24h as described in detail in Bayer et al. 2024.

Incubations were terminated by addition of cold 100 µL 100% TCA and stored at 4°C until extraction following established procedures (Baetge et. al., 2021). DPM were measured on a scintillation counter (Perkin-Elmer Tri-Carb 2910 TR) for 2 min, and [3H]-leucine incorporation rates were converted to units of carbon using a conversion factor of 1.5 kg C (mol leucine incorporated)-1 (Simon and Azam 1989).


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Methods

Baetge, N., Behrenfeld, M. J., Fox, J., Halsey, K. H., Mojica, K. D. A., Novoa, A., Stephens, B. M., & Carlson, C. A. (2021). The Seasonal Flux and Fate of Dissolved Organic Carbon Through Bacterioplankton in the Western North Atlantic. Frontiers in Microbiology, 12. https://doi.org/10.3389/fmicb.2021.669883
Methods

Bayer, B., Kitzinger, K., Paul, N. L., Albers, J. B., Saito, M. A., Wagner, M., Carlson, C. A., & Santoro, A. E. (2024). Contribution of ammonia oxidizers to inorganic carbon fixation in the dark ocean. https://doi.org/10.1101/2024.11.16.623942
Methods

Simon, M., & Azam, F. (1989). Protein content and protein synthesis rates of planktonic marine bacteria . Marine Ecology Progress Series, 51, 201–213. doi:10.3354/meps051201