Microstructure and composition of marine aggregates as co-determinants for vertical particulate organic carbon transfer in the global ocean

• Published in: Biogeosciences
• Main Authors: Maerz, Joeran, Six, Katharina D., Stemmler, Irene, Ahmerkamp, Soeren, Ilyina, Tatiana
• Format: Text
• Language: English
• Published: 2020
• Subjects: Southern Ocean
• Online Access: https://doi.org/10.5194/bg-17-1765-2020; https://www.biogeosciences.net/17/1765/2020/

Marine aggregates are the vector for biogenically bound carbon and nutrients from the euphotic zone to the interior of the oceans. To improve the representation of this biological carbon pump in the global biogeochemical HAMburg Ocean Carbon Cycle (HAMOCC) model, we implemented a novel Microstructure, Multiscale, Mechanistic, Marine Aggregates in the Global Ocean (M 4 AGO) sinking scheme. M 4 AGO explicitly represents the size, microstructure, heterogeneous composition, density and porosity of aggregates and ties ballasting mineral and particulate organic carbon (POC) fluxes together. Additionally, we incorporated temperature-dependent remineralization of POC. We compare M 4 AGO with the standard HAMOCC version, where POC fluxes follow a Martin curve approach with (i) linearly increasing sinking velocity with depth and (ii) temperature-independent remineralization. Minerals descend separately with a constant speed. In contrast to the standard HAMOCC, M 4 AGO reproduces the latitudinal pattern of POC transfer efficiency, as recently constrained by Weber et al. ( 2016 ) . High latitudes show transfer efficiencies of <math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>≈</mo><mn mathvariant="normal">0.25</mn><mo>±</mo><mn mathvariant="normal">0.04</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="66pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="9efcba71259000e22b65ef00b12fb838"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-17-1765-2020-ie00001.svg" width="66pt" height="10pt" src="bg-17-1765-2020-ie00001.png"/></svg:svg> , and the subtropical gyres show lower values of about 0.10±0.03 . In addition to temperature as a driving factor for remineralization, diatom frustule size co-determines POC fluxes in silicifier-dominated ocean regions, while calcium carbonate enhances the aggregate excess density and thus sinking velocity in subtropical gyres. Prescribing rising carbon dioxide ( CO 2 ) concentrations in stand-alone runs (without climate feedback), M 4 AGO alters the regional ocean atmosphere CO 2 fluxes compared to the standard model. M 4 AGO exhibits higher CO 2 uptake in the Southern Ocean compared to the standard run, while in subtropical gyres, less CO 2 is taken up. Overall, the global oceanic CO 2 uptake remains the same. With the explicit representation of measurable aggregate properties, M 4 AGO can serve as a test bed for evaluating the impact of aggregate-associated processes on global biogeochemical cycles and, in particular, on the biological carbon pump.