Photosynthesis in the surface ocean and subsequent export of a fraction of this fixed carbon leads to carbon dioxide sequestration in the deep ocean. Ecological relationships among plankton functional groups and theoretical relationships between particle size and sinking rate suggest that carbon export from the euphotic zone is more efficient when communities are dominated by large organisms. However, this hypothesis has never been tested against measured size spectra spanning the >5 orders of magnitude found in plankton communities. Using data from five ocean regions (California Current Ecosystem, North Pacific subtropical gyre, Costa Rica Dome, Gulf of Mexico, and Southern Ocean subtropical front), we quantified carbon‐based plankton size spectra from heterotrophic bacteria to metazoan zooplankton (size class cutoffs varied slightly between regions) and their relationship to net primary production and sinking particle flux. Slopes of the normalized biomass size spectra (NBSS) varied from −1.6 to −1.2 (median slope of −1.4 equates to large 1–10 mm organisms having a biomass equal to only 7.6% of the biomass in small 1–10 μm organisms). Net primary production was positively correlated with the NBSS slope, with a particularly strong relationship in the microbial portion of the size spectra. While organic carbon export co‐varied with NBSS slope, we found only weak evidence that export efficiency is related to plankton community size spectra. Multi‐variate statistical analysis suggested that properties of the NBSS added no explanatory power over chlorophyll, primary production, and temperature. Rather, the results suggest that both plankton size spectra and carbon export increase with increasing system productivity.
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Abstract Free, publicly-accessible full text available April 1, 2025 -
Picophytoplankton populations [
Prochlorococcus ,Synechococcus (SYN), and picoeukaryotes] are dominant primary producers in the open ocean and projected to become more important with climate change. Their fates can vary, however, with microbial food web complexities. In the California Current Ecosystem, picophytoplankton biomass and abundance peak in waters of intermediate productivity and decrease at higher production. Using experimental data from eight cruises crossing the pronounced CCE trophic gradient, we tested the hypothesis that these declines are driven by intensified grazing on heterotrophic bacteria (HBAC) passed to similarly sized picophytoplankton via shared predators. Results confirm previously observed distributions as well as significant increases in bacterial abundance, cell growth, and grazing mortality with primary production. Mortalities of picophytoplankton, however, diverge from the bacterial mortality trend such that relative grazing rates on SYN compared to HBAC decline by 12-fold between low and high productivity waters. The large shifts in mortality rate ratios for coexisting populations are not explained by size variability but rather suggest high selectivity of grazer assemblages or tightly coupled tradeoffs in microbial growth advantages and grazing vulnerabilities. These findings challenge the long-held view that protistan grazing mainly determines overall biomass of microbial communities while viruses uniquely regulate diversity by “killing the winners”. -
Abstract The Southern Ocean contributes substantially to the global biological carbon pump (BCP). Salps in the Southern Ocean, in particular Salpa thompsoni , are important grazers that produce large, fast-sinking fecal pellets. Here, we quantify the salp bloom impacts on microbial dynamics and the BCP, by contrasting locations differing in salp bloom presence/absence. Salp blooms coincide with phytoplankton dominated by diatoms or prymnesiophytes, depending on water mass characteristics. Their grazing is comparable to microzooplankton during their early bloom, resulting in a decrease of ~1/3 of primary production, and negative phytoplankton rates of change are associated with all salp locations. Particle export in salp waters is always higher, ranging 2- to 8- fold (average 5-fold), compared to non-salp locations, exporting up to 46% of primary production out of the euphotic zone. BCP efficiency increases from 5 to 28% in salp areas, which is among the highest recorded in the global ocean.more » « less
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Abstract Multiple processes transport carbon into the deep ocean as part of the biological carbon pump, leading to long-term carbon sequestration. However, our ability to predict future changes in these processes is hampered by the absence of studies that have simultaneously quantified all carbon pump pathways. Here, we quantify carbon export and sequestration in the California Current Ecosystem resulting from (1) sinking particles, (2) active transport by diel vertical migration, and (3) the physical pump (subduction + vertical mixing of particles). We find that sinking particles are the most important and export 9.0 mmol C m−2d−1across 100-m depth while sequestering 3.9 Pg C. The physical pump exports more carbon from the shallow ocean than active transport (3.8 vs. 2.9 mmol C m−2d−1), although active transport sequesters more carbon (1.0 vs. 0.8 Pg C) because of deeper remineralization depths. We discuss the implications of these results for understanding biological carbon pump responses to climate change.
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Abstract. The ability to constrain the mechanisms that transport organiccarbon into the deep ocean is complicated by the multiple physical,chemical, and ecological processes that intersect to create, transform, andtransport particles in the ocean. In this paper we develop andparameterize a data-assimilative model of the multiple pathways of thebiological carbon pump (NEMUROBCP). The mechanistic model is designedto represent sinking particle flux, active transport by vertically migratingzooplankton, and passive transport by subduction and vertical mixing, whilealso explicitly representing multiple biological and chemical propertiesmeasured directly in the field (including nutrients, phytoplankton andzooplankton taxa, carbon dioxide and oxygen, nitrogen isotopes, and234Thorium). Using 30 different data types (including standing stockand rate measurements related to nutrients, phytoplankton, zooplankton, andnon-living organic matter) from Lagrangian experiments conducted on 11cruises from four ocean regions, we conduct an objective statisticalparameterization of the model and generate 1 million different potentialparameter sets that are used for ensemble model simulations. The modelsimulates in situ parameters that were assimilated (net primary productionand gravitational particle flux) and parameters that were withheld(234Thorium and nitrogen isotopes) with reasonable accuracy. Modelresults show that gravitational flux of sinking particles and verticalmixing of organic matter from the euphotic zone are more importantbiological pump pathways than active transport by vertically migratingzooplankton. However, these processes are regionally variable, with sinkingparticles most important in oligotrophic areas of the Gulf of Mexico andCalifornia Current, sinking particles and vertical mixing roughly equivalentin productive coastal upwelling regions and the subtropical front in theSouthern Ocean, and active transport an important contributor in the easterntropical Pacific. We further find that mortality at depth is an importantcomponent of active transport when mesozooplankton biomass is high, but itis negligible in regions with low mesozooplankton biomass. Our results alsohighlight the high degree of uncertainty, particularly amongstmesozooplankton functional groups, that is derived from uncertainty in modelparameters. Indeed, variability in BCP pathways between simulations for aspecific location using different parameter sets (all with approximatelyequal misfit relative to observations) is comparable to variability in BCPpathways between regions. We discuss the implications of these results forother data-assimilation approaches and for studies that rely on non-ensemblemodel outputs.more » « less
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Irigoien, Xabier (Ed.)Abstract Larval abundances of Atlantic bluefin tuna (ABT) in the Gulf of Mexico are currently utilized to inform future recruitment by providing a proxy for the spawning potential of western ABT stock. Inclusion of interannual variations in larval growth is a key advance needed to translate larval abundance to recruitment success. However, little is known about the drivers of growth variations during the first weeks of life. We sampled patches of western ABT larvae in 3–4 day Lagrangian experiments in May 2017 and 2018, and assessed age and growth rates from sagittal otoliths relative to size categories of zooplankton biomass and larval feeding behaviors from stomach contents. Growth rates were similar, on average, between patches (0.37 versus 0.39 mm d−1) but differed significantly through ontogeny and were correlated with a food limitation index, highlighting the importance of prey availability. Otolith increment widths were larger for postflexion stages in 2018, coincident with high feeding on preferred prey (mainly cladocerans) and presumably higher biomass of more favorable prey type. Faster growth reflected in the otolith microstructures may improve survival during the highly vulnerable larval stages of ABT, with direct implications for recruitment processes.more » « less