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  • 1
    Publication Date: 2014-10-23
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 2
    Publication Date: 2015-03-27
    Description: We used bulk tissue δ 13 C and δ 15 N values and δ 15 N values of individual amino acids (AA) to characterize the trophic structure of a pelagic fish assemblage from the North Pacific Subtropical Gyre (NPSG) ecosystem. We focus on energy flow between fishes inhabiting distinct epipelagic, mesopelagic, and upper bathypelagic habitats and on predatory fish foraging across and within these depth habitats. Trophic positions (TPs) estimated from a combination of trophic and source AA δ 15 N values (TP Tr-Src ) spanned a narrow range of 0.7 TP for 10 species of large fishes, including tunas, billfishes, and gempylids (TP Tr-Src 4.3-5.0). Similarly, 13 species of small micronekton fishes encompassed a range of 1.2 TP (TP Tr-Src 2.6-3.8). The δ 15 N values of three source AAs were found to increase with increasing depth of capture across the 13 micronekton fish species ( δ 15 N Phe range = 6.6‰; δ 15 N Gly range = 13.4‰; δ 15 N Ser range = 13.6‰), indicating that some species from epipelagic, mesopelagic, and upper bathypelagic communities access distinct food resources, such as suspended particles. These isotopic depth trends are consistent with previous observations in particulate organic matter and zooplankton from the NPSG, providing new evidence that large pelagic and micronekton fishes access a food web fueled by particles formed in surface waters but that are highly modified by microbes as they slowly settle to remote depths. On the contrary, no significant relationships between the δ 15 N values of source AAs and habitat depth were observed in the large predator fish group, of which many species move and forage across large depth gradients.
    Print ISSN: 0024-3590
    Electronic ISSN: 1939-5590
    Topics: Biology , Geosciences , Physics
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  • 3
    Publication Date: 2015-01-31
    Description: We assess the metabolic demand of mesopelagic zooplankton for carbon, nitrogen, and phosphorus in the North Pacific Subtropical Gyre (NPSG). We compare zooplankton metabolic demand with the attenuation of sinking particle fluxes, and find the average metabolic demand for resident midwater zooplankton can account for 1.3× the loss of sinking particulate organic carbon and particulate nitrogen fluxes, and 2.6× the loss of particulate phosphorus fluxes. Zooplankton metabolic demand for carbon remains significant (0.4-1.9×) relative to the loss in sinking particulate fluxes, even when new depth-specific dry weight conversion factors and recent global-bathymetric models of zooplankton metabolism are applied. These new models reduce zooplankton carbon demands to reasonably match particle flux attenuation in the mesopelagic zone. Zooplankton metabolic demand for phosphorus is particularly large in comparison to particle flux attenuation (1.5-9×), and when temporal change in the molar carbon : phosphorus ratio of the attenuation in particulate fluxes are considered, mesopelagic zooplankton in the NPSG may episodically become phosphorus-limited. Midwater zooplankton have the potential to be important mediators of carbon flux to the deep ocean in the NPSG.
    Print ISSN: 0024-3590
    Electronic ISSN: 1939-5590
    Topics: Biology , Geosciences , Physics
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  • 4
    Publication Date: 2019
    Description: Abstract The oceans are an important global reservoir for mercury (Hg), and marine fish consumption is the dominant human exposure pathway for its toxic methylated form. A more thorough understanding of the global biogeochemical cycle of Hg requires additional information on the mechanisms that control Hg cycling in pelagic marine waters. In this study, Hg isotope ratios and total Hg concentrations are used to explore Hg biogeochemistry in oligotrophic marine environments north of Hawaii. We present the first measurements of the vertical water column distribution of Hg concentrations and the Hg isotopic composition in precipitation, marine particles, and zooplankton near Station ALOHA (22°45′N, 158°W). Our results reveal production and demethylation of methylmercury in both the euphotic (0–175 m) and mesopelagic zones (200–1,000 m). We document a strong relationship between Hg isotopic composition and depth in particles, zooplankton, and fish in the water column and diurnal variations in Δ199Hg values in zooplankton sampled near the surface (25 m). Based on these observations and stable Hg isotope relationships in the marine food web, we suggest that the Hg found in large pelagic fish at Station ALOHA was originally deposited largely by precipitation, transformed into methyl‐Hg, and bioaccumulated in situ in the water column. Our results highlight how Hg isotopic compositions reflect abiotic and biotic production and degradation of methyl‐Hg throughout the water column and the importance of particles and zooplankton in the vertical transport of Hg.
    Print ISSN: 0886-6236
    Electronic ISSN: 1944-9224
    Topics: Biology , Chemistry and Pharmacology , Geography , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 5
    Publication Date: 2014-11-05
    Description: Every night a massive migration takes place in ocean waters. Zooplankton and micronekton, a diverse group of organisms
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 6
    Publication Date: 2019
    Description: Abstract Many species of micronekton perform diel vertical migrations (DVMs), which ultimately contributes to carbon export to the deep sea. However, not all micronekton species perform DVM, and the nonmigrators, which are often understudied, have different energetic requirements that might be reflected in their trophic ecology. We analyze bulk tissue and whole animal stable nitrogen isotopic compositions (δ15N values) of micronekton species collected seasonally between 0 and 1250 m depth to explore differences in the trophic ecology of vertically migrating and nonmigrating micronekton in the central North Pacific. Nonmigrating species exhibit depth‐related increases in δ15N values mirroring their main prey, zooplankton. Higher variance in δ15N values of bathypelagic species points to the increasing reliance of deeper dwelling micronekton on microbially reworked, very small suspended particles. Migrators have higher δ15N values than nonmigrators inhabiting the epipelagic zone, suggesting the consumption of material during the day at depth, not only at night when they migrate closer to the surface. Migrating species also appear to eat larger prey and exhibit a higher range of variation in δ15N values seasonally than nonmigrators, likely because of their higher energy needs. The dependence on material at depth enriched in 15N relative to surface particles is higher in migratory fish that ascend only to the lower epipelagic zone. Our results confirm that stark differences in the food habits and dietary sources of micronekton species are driven by vertical migrations.
    Print ISSN: 0024-3590
    Electronic ISSN: 1939-5590
    Topics: Biology , Geosciences , Physics
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  • 7
    Publication Date: 2016-05-25
    Description: Mucous gels are produced by benthic animals rapidly and in copious amounts, and consequently they are a possible priming substrate whose addition in modest amounts may affect sedimentary organic matter (SOM) remineralization. The priming effect of benthic infaunal mucus was tested using mucus of the common gastropod Neverita duplicata as model substrate. Its composition is typical of marine molluscan mucus, consisting primarily of water (〉 96% by weight). Salt-free dry weight constitutes 0.7% of total mucus. Relationships between C, N, and S content show the presence of N-free and S-free fractions, indicative of mucopolysaccharides, that account for approximately half of the total C present. The C/N ratios of the N-containing fraction (6.1 and 8.75 for pedal and hypobranchial mucus, respectively) are indicative of a carbohydrate-protein complex. Relatively low C/S ratios for the S-containing fraction (21.8 and 10.5 for pedal and hypobranchial mucus, respectively) and positive staining with Alcian Blue dye are indicative of S-ester and alkyl- groups bridging mucopolysaccharide and glycoprotein components. Anaerobic incubations of pedal mucus, sediment, and mucus-sediment mixture resulted in the generation of ΣCO 2 and at ratios lower than substrate C/N ratios, indicating the preferential decomposition of N-rich components. Production rates of ΣCO 2 and in mucus-sediment incubations are higher, by 9% ± 16% and 29% ± 11%, respectively, than those predicted from linear addition of mucus-only and sediment-only rates. The accelerated remineralization rate of N in the presence of modest mucus contribution suggests that benthic mucus addition can affect SOM remineralization processes through a “priming” effect.
    Print ISSN: 0024-3590
    Electronic ISSN: 1939-5590
    Topics: Biology , Geosciences , Physics
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  • 8
    Publication Date: 2017-12-19
    Description: Several studies have found that the respiratory demand for carbon by the mesopelagic community exceeds carbon supply through the particulate sinking flux by up to two to three orders of magnitude, suggesting that mesopelagic communities rely on additional overlooked carbon sources. Suspended particles (defined as 0.7–53 μ m) have been suggested as one of these sources but few studies have evaluated their contribution to the mesopelagic food web. We use amino acid compound-specific nitrogen isotope analysis to investigate whether suspended particles are an important nutritional source to fish, cephalopod, and crustacean micronekton species in the central North Pacific. Our results suggest that micronekton feed from food webs fueled by a variety of nutritional sources including surface dwelling phytoplankton and bacteria, sinking particles, and suspended particles, with micronekton becoming more reliant on suspended particles with increasing habitat depth. Several species were identified as feeding from a primarily suspended particle-based food web including the fishes Cyema atrum , Cyclothone pallida , Melanocetus johnsonii , Serrivomer sector , and the pelagic octopod Japetella diaphana . We also found that micronekton species feeding from a suspended particle food web cannot be identified using bulk tissue δ 15 N values. Our data support the notion that suspended particles are an important nutritional source in the lower mesopelagic and upper bathypelagic and they should be accounted for when estimating carbon supply for these communities.
    Print ISSN: 0024-3590
    Electronic ISSN: 1939-5590
    Topics: Biology , Geosciences , Physics
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  • 9
    Publication Date: 2016-11-22
    Description: The environmental drivers of zooplankton variability are poorly explored for the central subtropical Pacific, where a direct bottom-up food-web connection is suggested by increasing trends in primary production and mesozooplankton biomass at Stn. ALOHA over the past 20 years (1994-2013). Here we use Generalized Additive Models (GAMs) to investigate how these trends relate to the major modes of North Pacific climate variability. A GAM based on monthly mean data explains 43% of the temporal variability in mesozooplankton biomass with significant influences from primary productivity (PP), sea surface temperature (SST), NPGO and El Niño. This result mainly reflects the seasonal plankton cycle at Stn. ALOHA in which increasing light and SST lead to enhanced nitrogen fixation, productivity and zooplankton biomass during summertime. Based on annual mean data, GAMs for two-variables suggest that PP and 3-4 year lagged NPGO individually account for ~40% of zooplankton variability. The full annual mean GAM explains 70% of variability of zooplankton biomass with significant influences from PP, 4-y lagged NPGO and 4-y lagged PDO. The NPGO affects wind stress, sea surface height and subtropical gyre circulation, and has been linked to mid-euphotic zone anomalies in salinity and PP at Stn. ALOHA. Our study broadens the known impact of this climate mode on plankton dynamics in the North Pacific. While lagged transport effects are also evident for subtropical waters, our study highlights a strong coupling between zooplankton fluctuations and PP, which differs from the transport-dominated climate influences that have been found for North Pacific boundary currents.
    Print ISSN: 0148-0227
    Topics: Biology , Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 10
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