Decoupling of ΔO₂∕Ar and particulate organic carbon dynamics in nearshore surface ocean waters

• Main Authors: S. Z. Rosengard, R. W. Izett, W. J. Burt, N. Schuback, P. D. Tortell
• Format: Article
• Language: English
• Published: Copernicus Publications 2020-06-01
• Series: Biogeosciences
• Online Access: https://www.biogeosciences.net/17/3277/2020/bg-17-3277-2020.pdf
• ISSN: 1726-4170; 1726-4189

<p>We report results from two Lagrangian drifter surveys off the Oregon coast, using continuous shipboard sensors to estimate mixed-layer gross primary productivity (GPP), community respiration (CR), and net community production (NCP) from variations in biological oxygen saturation (<span class="inline-formula">ΔO₂∕Ar</span>) and optically derived particulate organic carbon (POC). At the first drifter survey, conducted in a nearshore upwelling zone during the development of a microplankton bloom, net changes in <span class="inline-formula">ΔO₂∕Ar</span> and [POC] were significantly decoupled. Differences in GPP and NCP derived from <span class="inline-formula">ΔO₂∕Ar</span> (NCP<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><msub><mi/><mrow class="chem"><msub><mi mathvariant="normal">O</mi><mn mathvariant="normal">2</mn></msub><mo>/</mo><mi mathvariant="normal">Ar</mi></mrow></msub></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="25pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="67fef0273d3d84bca1f32fb398316be3"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-17-3277-2020-ie00001.svg" width="25pt" height="11pt" src="bg-17-3277-2020-ie00001.png"/></svg:svg></span></span>) and POC (NCP<span class="inline-formula">_POC)</span> time series suggest the presence of large POC losses from the mixed layer. At this site, we utilized the discrepancy between NCP<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M10" display="inline" overflow="scroll" dspmath="mathml"><msub><mi/><mrow class="chem"><msub><mi mathvariant="normal">O</mi><mn mathvariant="normal">2</mn></msub><mo>/</mo><mi mathvariant="normal">Ar</mi></mrow></msub></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="25pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="54ed17aa040db4b169e8163e5062ce15"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-17-3277-2020-ie00002.svg" width="25pt" height="11pt" src="bg-17-3277-2020-ie00002.png"/></svg:svg></span></span> and NCP<span class="inline-formula">_POC</span>, and additional constraints derived from surface water excess nitrous oxide (<span class="inline-formula">N₂O</span>), to evaluate POC loss through particle export, DOC production, and vertical mixing fluxes. At the second drifter survey, conducted in lower-productivity, density-stratified offshore waters, we also observed offsets between <span class="inline-formula">ΔO₂∕Ar</span> and POC-derived GPP and CR rates. At this site, however, net [POC] and <span class="inline-formula">ΔO₂∕Ar</span> changes yielded closer agreement in NCP estimates, suggesting a tighter relationship between production and community respiration, as well as lower POC loss rates. These results provide insight into the possibilities and limitations of estimating productivity from continuous underway POC and <span class="inline-formula">ΔO₂∕Ar</span> data in contrasting oceanic waters. Our observations support the use of diel POC measurements to estimate NCP in lower-productivity waters with limited vertical carbon export and the potential utility of coupled <span class="inline-formula">O₂</span> and optical measurements to estimate the fate of POC in high-productivity regions with significant POC export.</p>