Sensitivity analysis of a mathematical model of phytoplankton growth and nutrient distribution in the Pacific Ocean off the northwestern U.S. coast

In a recent publication (Jamart el al., Deep-Sea Research, 24,753–773, 1977) we describe a numerical two-dimensional(time and depth) model of phytoplankton growth and nutrientdistribution in the Pacific Ocean off the northwestern U.S.coast. The numerical model consists of coupled integro-partialdifferential equations expressing conservation of chlorophyll, nitrate, and ammonium. The relevant physical and biologicalprocesses are represented by conventional functions and parameters.The system is "closed" by specification of grazing pressureand light intensity. A long-term simulation ova spring and summermonths (for convenience, called the "standard run") representswell the main features of observed chemical data and biologicalvariables, including the formation and deepening of a subsurfacechlorophyll maximum. In this paper, a sensitivity analysis of the system is carriedout by comparing the "standard run" with the results of twentynumerical experiments, in each of which a single function orparameter in the model is modified. The formation of the subsurfacechlorophyll maximum is simulated, more or less realistically,in all experiments. Moreover, the results suggest that the chlorophylldistribution adjusts in time and depth so as to optimize thetransfer of carbon to secondary producers. The level of thecarbon output is determined mainly by the resources availableto the primary producers.     

A mathematical model for insulin kinetics. III. Sensitivity analysis of the model

A non-linear mathematical model involving four variables and several constants incorporating beta-cell kinetics, a glucose-insulin feedback system and a gastrointestinal absorption term had been applied in earlier papers to various forms of diabetes mellitus. In this paper, we examine the response of the system to variations in the parameters and to initial conditions using sensitivity analysis. It is found that such a method leads to results that are consistent with clinical findings. Further, it is suggested that such an analysis could help in making some predictions regarding future directions in the therapy of diabetes mellitus.     

Description of phytoplankton and nutrient in spring in the western North Atlantic Ocean

Abundance of diatoms in the northern Sargasso Sea in springhas been observed in a 4-year period between 1981 and 1985 andthen again in 1987. A theory is presented that if stratificationblocks get-through of deep nutrients to the surface, as in thesouthern Sargasso, then in-situ cycling via non-diatoms andammonia dominates. The theory is that if in-situ cycling doesnot dominate, as northward, then stratification does not blockget-through of deep nutrients to the surface, which, in combinationwith the marked growth capacity of diatoms, produce an abundanceof cells. This abundance consumes nitrate, phosphate and silicateat the surface and ultimately this nutrient-depleted water arrivesin the southern Sargasso via the gyre circulation. Thus thenutrient-depleted water of the western Atlantic gyre is consideredto be primarily achieved only by diatoms, in spring and in thenorthern Sargasso. A transect during April 13–16, 1985,north from the Virgin Islands along 63°–64°W showsa great change in the diatom species plus Emiliania huxleyifrom negligible concentrations in the southern half of the sectionto large concentrations in the northern half. This unevennessof distribution can be rephrased by indicating that these speciesare narrow-niched with regard to nutrient availability. Theother species, coccolithophores and dinoflagellates, are evenlydistributed at low concentrations south-north (though some diminishslightly) and so they are broad-niched with respect to nutrient.High species diversity depends on broadness of nutrient nicheand equilibrium conditions of hydrographically stable water(i), implying that when non-equilibrium conditions occur (ii),when niche breadth is less (iii) or both (iv), then diversityis less marked, (i) is confirmed by broad-niched species southward,(ii) is confirmed by broad-niched species northward, (iii) isconfirmed by narrow-niched species southward and (iv) by narrow-nichedspecies northward.     

Yessotoxin detected in mussel (Mytilus californicus) and phytoplankton samples from the U.S. west coast

Yessotoxin (YTX) was detected in an algal sample and two mussel samples (0.07–0.10 μg g⁻¹) collected from Scripps Pier in La Jolla, California during a bloom of Lingulodinium polyedrum. Mussel samples collected from Monterey Bay, California also contained measurable YTX (levels up to 0.06 μg g⁻¹) in samples obtained during a 6-month (weekly) sampling period. Gonyaulax spinifera and L. polyedrum were identified in background concentrations in Monterey Bay during the time of contamination. An algal sample from Washington coastal waters collected during non-bloom conditions also contained YTX, possibly originating from Protoceratium reticulatum.Three strains of L. polyedrum (CCMP1931, CCMP1936, 104A) isolated from southern California coastal waters and one strain of G. spinifera (CCMP409) isolated from Maine were tested for YTX production using two methods, competitive ELISA and liquid chromatography–mass spectrometry (LC–MS). The ELISA method detected YTX in the particulate phase in two of three L. polyedrum strains. The LC–MS method did not detect YTX in the particulate or dissolved phase of any of the strains.To our knowledge, this is the first study to test and confirm YTX in environmental samples from California and Washington coastal waters. It is highly likely that L. polyedrum was responsible for the YTX contamination in the southern California samples. Future research needs to conclusively determine the biological origin(s) of YTX contamination in central California and Washington coastal waters.     

Growth and mortality rates of phytoplankton in the northwestern North Pacific estimated by the dilution method and HPLC pigment analysis

Pigment-based growth rates of phytoplankton and mortality rates due to microzooplankton grazing were estimated using a dilution method combined with high-performance liquid chromatography (HPLC) pigment analysis in the northwestern North Pacific in autumn 1998. The dilution experiments were conducted at different hydrographic stations in both colder and warmer water masses. No significant difference was found between the growth rate of the phytoplankton community (0.38–0.70 day⁻¹; estimated by chlorophyll a) at the colder and warmer water stations, while the mortality rate (0.15–0.88 day⁻¹; estimated by chlorophyll a) tended to be higher at warmer water stations. The combination of estimates of daily chlorophyll a production and particulate organic carbon (POC) production enabled us to assess the carbon to chlorophyll a ratio (C/chl a) of “new” organic matter produced by living phytoplankton. The method provided an implicit value of the C/chl a of in situ living phytoplankton. The rate estimates from taxon-specific pigments suggested a possibility that chlorophyll b-containing green algae were grazed preferentially by microzooplankton during their active growth, and the standing stock of green algae was more strictly controlled by micrograzer than other algal groups such as diatoms. This result is one possible explanation for the fact that blooms of green algae have not been reported in the open ocean, in contrast with diatoms.     

Larval fish assemblages in waters off the central Pacific coast of Mexico

Spatial and seasonal variation of the ichthyoplankton assemblageswas analysed using monthly samples collected during a 1 yearcycle off the central Pacific coast of Mexico. Zooplankton sampleswere collected at 12 stations during 11 months, from December1995 to December 1996. The analysis of coastal oceanographicconditions revealed two main seasonal patterns, one relatedto the California Current influence and the other a tropicalone. A temporal recomposition of the ichthyoplankton assemblageswas found to be related to each oceanographic pattern. Duringthe California Current period (January–May) the larvalfish assemblage was respresented mainly by Auxis sp., Bentosemapanamense, Cetengraulis mysticetus, Opistonema sp., Symphuruselongatus, Gobionellus sp., Dormitator latifrons and Bregmacerosbathymaster. The tropical season assemblage (July, October andNovember) was represented by Harengula thrissina, Euthynnuslineatus, Vinciguerria lucetia, Syacium ovale, and representativesof the Eleotridae and Pomacentridae. An inshore–offshoregradient was observed during the tropical oceanographic periods,with a thermic stratification of the water column over the shelf.Conversely, during the California Current period, with coastaladvective processes, the assemblages of fish larvae were morehomogeneous. Although a mixed, richer faunistic compositionwas expected in this transitional area, the overall biogeographicaffinity of the surveyed community remained stable even in contrastingconditions.     

Oxidative stress indicators and trace elements in the blue shark (Prionace glauca) off the east coast of the Mexican Pacific Ocean

Trace element concentrations and oxidative stress indicators (including production of reactive oxygen species (ROS), antioxidant enzyme activities and oxidative damage) were measured in muscle of blue sharks collected along the west coast of Baja California Sur to determine potential differences by sex and maturity cohorts. Mercury (Hg) concentration in muscle samples from larger sharks (>200 cm LT) exceeded the permissible limit (>1 ppm wet weight) for human consumption set by numerous international agencies. Significant differences were found in Hg concentrations (mature>immature; males>females), and in protein carbonyl concentrations (male>female); however, except for carbonyl protein levels, no significant differences by sex or maturity stage were found in the oxidative stress indicators. Differences between sexes and maturity stages in trace element concentration and carbonyl protein levels in blue shark muscle may be related to variations in diet within different cohorts.     

The food supply of the Pacific salmon of the genus Oncorhynchus in the northwestern Pacific Ocean. 2. Comparative characterization and general state

The interannual variations and general state of the food supply of Pacific salmon (Oncorhynchus spp.) in the 2000s in the northwestern Pacific Ocean (including the Bering Sea and the Sea of Okhotsk) were analyzed based on indirect characteristics that indicate the variability of their forage base, feeding habits, growth, and biomass. A new index for the quantitative evaluation of food supply was suggested. The food supply of the Pacific salmon during the 2000s was found to be sufficient to maintain the normal functioning of populations. With high abundance of Pacific salmon, the food supply tended to decrease. However, this caused no negative consequences for the survival of major salmon stocks during the marine period of life and, as a rule, no marked decrease in the food consumption and growth rates of fish. A relative increase in food competition was compensated by adaptive changes in the diet and diel feeding rhythm of salmon. With the shortage of preferred food organisms (amphipods, euphausiids, and pteropods), Pacific salmon changed to consuming minor prey (copepods and chaetognaths), and numerous mesopelagic species of macroplankton and micronekton in the evening hours.     

Analogous nutrient limitations in unicellular diazotrophs and Prochlorococcus in the South Pacific Ocean

Growth limitation of phytoplankton and unicellular nitrogen (N₂) fixers (diazotrophs) were investigated in the oligotrophic Western South Pacific Ocean. Based on change in abundances of nifH or 23S rRNA gene copies during nutrient-enrichment experiments, the factors limiting net growth of the unicellular diazotrophs UCYN-A (Group A), Crocosphaera watsonii, γ-Proteobacterium 24774A11, and the non-diazotrophic picocyanobacterium Prochlorococcus, varied within the region. At the westernmost stations, numbers were enhanced by organic carbon added as simple sugars, a combination of iron and an organic chelator, or iron added with phosphate. At stations nearest the equator, the nutrient-limiting growth was not apparent. Maximum net growth rates for UCYN-A, C. watsonii and γ-24774A11 were 0.19, 0.61 and 0.52 d⁻¹, respectively, which are the first known empirical growth rates reported for the uncultivated UCYN-A and the γ-24774A11. The addition of N enhanced total phytoplankton biomass up to 5-fold, and the non-N₂-fixing Synechococcus was among the groups that responded favorably to N addition. Nitrogen was the major nutrient-limiting phytoplankton biomass in the Western South Pacific Ocean, while availability of organic carbon or iron and organic chelator appear to limit abundances of unicellular diazotrophs. Lack of phytoplankton response to nutrient additions in the Pacific warm pool waters suggests diazotroph growth in this area is controlled by different factors than in the higher latitudes, which may partially explain previously observed variability in community composition in the region.     

Zooplankton composition and distribution off the coast of Galicia, Spain

During June and September 1984, zooplankton samples were collectedwith other hydrographic and biological data along the Galiciancoast (NW of Spain). In June copepods contributed {small tilde}60%to the total zooplankton community, with larvaceans, siphonophoresand cladocerans also abundant. In September >90% of the zooplanktonsampled were copepods. The dominant species of copepods in bothJune and September were Acartia clausi, Paracalanus parvus andTemora longicornis. The meroplankton was dominated by echinoderms,bryozoans, barnacle larvae and bivalve larvae. In June the averagezooplankton biomass was 31.08 mg C m^–3; the Septemberaverage was 41.69 mg C m^–3. The relationship between theslopes of the regression equations (biomass versus abundance)suggests that the zooplankton assemblage in June was composedby larger animals than in September. The major concentrationof zooplankton was between 0 and 50 m, with both June and Septemberdaytime surface samples having 6–7 times the amount oforganisms than the lower water column (50–100 m). Therewere no distinct differences in total zooplankton abundancesat the inshore and offshore stations; however, the inshore stationsoften had a higher percentage of meroplankton than the offshorestations. In June zooplankton abundance at the northern transectsand the western transects was similar. In September there weregreater concentrations of zooplankton in the western Galicianshelf as compared with the northern shelf. These differencesin the horizontal distribution of the zooplankton were relatedto upwelling events.     

Biochemical polymorphism of starry flounder, Platichthys stellatus, from the northwestern and northeastern Pacific Ocean.

Three enzyme systems, MDH, PGM and AGPDH, were investigated in starry flounder collected from off northwestern Hokkaido Island, Japan; western Kamchatka; USSR; Puget Sound, Washington, USA; and Yaquina Bay, Oregon, USA. Significant differences in MDH allele distribution were found between the Asian-Puget Sound and Yaquina Bay-Puget Sound samples suggesting that this system may be useful to separate different population units. The allele frequencies of MDH and PGM did not show significant variation with body length and handedness in starry flounder collected from Puget Sound, Washington, and did not support the hypothesis of differential viability between dextral and sinistrial forms of starry flounder.     

Patterns in species richness,species density,and evenness in groundfish assemblages on the continental slope of the U.S. Pacific coast

For many taxa, diversity, often measured as species richness, decreases with latitude. In this report patterns of diversity (species richness, species diversity, and evenness) in groundfish assemblages were investigated in relation to depth (200–1200 m) and latitude (33–47°N) on the continental slope of the U.S. Pacific coast. The data originated from the 1999–2002 upper continental slope groundfish surveys conducted by the National Marine Fisheries Service. When the data were pooled across depths, species density and evenness were found to decline with latitude. All three diversity measures declined with depth, with the lowest overall diversity in the 600- to 900-m depth range where longspine thornyhead Sebastolobus altivelis constituted close to 70% of the catch. When latitudinal gradients were examined within four depth zones (200–300 m, 400–500 m, 600–900 m, and 1000–1200 m) more complex patterns emerged. At depth species richness and evenness were inversely correlated with latitude as longspine thornyhead dominated catches to the north. However, in shallower areas of the slope, species richness and evenness were positively correlated with latitude. Latitudinal patterns of diversity in the deeper zones and when pooled across depths were positively correlated with temperature and broadly consistent with the Ambient Energy hypothesis discussed by Willig et al. [Annu Rev Ecol System 34:273–309 (2003)].     

Comparison of phytoplankton concentrations and cell volume measurements from the continental shelf off Cape Cod,Massachusetts, U.S.A.

Phytoplankton composition and concentrations varied at stations across the shelf with maximum phytoplankton volumes not necessarily related to maximum concentration values. The shelf phytoplankton off Cape Cod, Massachusetts was composed of two major size classes: the ultraplankton (cells less than 10 microns in size), and net phytoplankton. Cell concentrations decreased along transects seaward, to increase near the shelf margin. Higher cell volume values coincided with increased cell counts east of Cape Cod, but were lower southward, increasing in the mid-shelf region, to decrease along the shelf margin. The shelf ultraplankton component typically represented over 90% of the standing crop, but less than 1% of its phytovolume. Associations are made between cell volumes and concentration combinations and different phytoplankton assemblages.     

Diversity of culturable filamentous Ascomycetes in the eastern South Pacific Ocean off Chile

Our study reports the diversity of culturable mycoplankton in the eastern South Pacific Ocean off Chile to contribute with novel knowledge on taxonomy of filamentous fungi isolated from distinct physicochemical and biological marine environments. We characterized spatial distribution of isolates, evaluated their viability and assessed the influence of organic substrate availability on fungal development. Thirty-nine Operational Taxonomic Units were identified from 99 fungal strains isolated from coastal and oceanic waters by using Automatic Barcode Gap Discovery. All Operational Taxonomic Units belonged to phylum Ascomycota and orders Eurotiales, Dothideales, Sordariales and Hypocreales, mainly Penicillium sp. (82%); 11 sequences did not match existing species in GenBank, suggesting occurrence of novel fungal taxa. Our results suggest that fungal communities in the South Pacific Ocean off Chile appear to thrive in a wide range of environmental conditions in the ocean and that substrate availability may be a factor influencing fungal viability in the ocean.     

Spatial distribution and dynamics of catches of Sebastes glaucus, S. iracundus, and S. polyspinis in Pacific waters off the Kuril Islands and Kamchatka

Based on studies of the years 1992–2001, quantitative indices characterizing the occurrence of three rare or little-studied species of rockfish (Sebastes glaucus, S. iracundus, and S. polyspinis) in Pacific waters off the northern Kuril Islands and southeastern Kamchatka are provided. Specific features of distribution (spatial, vertical, and dependence on near-bottom temperatures) are considered. New data on the diurnal, seasonal, and multiyear dynamics of their catches and occurrence, as well as on the length and weight of the body, sex ratio, and sexual dimorphism in the amount and intensity of feeding are cited.     

Production of viruses during a spring phytoplankton bloom in the South Pacific Ocean near of New Zealand

Lagrangian studies of virus activity in pelagic environments over extended temporal scales are rare. To address this, viruses and bacteria were examined during the course of a natural phytoplankton bloom in the pelagic South Pacific Ocean east of New Zealand. Daily samples were collected in a mesoscale eddy from year days 263-278 (September 19th-October 4th, 2008). The productive bloom transitioned from a diatom to a pico- and nanoplankton-dominated system, resulting in chlorophyll a concentrations up to 2.43?μg?L(-1) . Virus abundances fluctuated c.?10-fold (1.8?×?10(10) -1.3?×?10(11) L(-1) ) over 16?days. The production rates of virus particles were high compared with those reported in other marine systems, ranging from 1.4?×?10(10) to 2.1?×?10(11) L(-1) day(-1) . Our observations suggest viruses contributed significantly to the mortality of bacteria throughout the bloom, with 19-216% of the bacterial standing stock being lysed daily. This mortality released nutrient elements (N, Fe) that likely helped sustain the bloom through the sampling period. Parametric analyses found significant correlations with both biotic (e.g. potential host abundances) and abiotic parameters (e.g. nutrient concentrations, temperature). These observations demonstrate that viruses may be critical in the extended maintenance of regeneration-driven biological production.     

Differences in cell viabilities of phytoplankton between spring and late summer in the northwest Pacific Ocean

Cell viabilities of phytoplankton in the Oyashio and Kuroshio-Oyashio transition regions of the northwest Pacific Ocean were examined in September 2003 (late summer) and May 2005 (spring) using a membrane permeability test. Specific lysis rates of the phytoplankton during late summer were also assessed by an esterase activity assay. In late summer, cyanobacteria Synechococcus spp. were > 2 × 10⁴ cells ml^− 1 and numerically dominated the phytoplankton communities. The cell viabilities of Synechococcus spp. and eukaryotic ultraphytoplankton (< 10 μm in size) were 60-79% and 26-41% in surface waters, respectively. The specific lysis rates of the phytoplankton were 0.12-0.67 d^− 1 in late summer. By contrast, in spring, eukaryotic cells were predominant in the phytoplankton communities. The cell viabilities of surface eukaryotic ultraphytoplankton in spring were > 70% and significantly higher than those in late summer. During spring, Synechococcus spp. only occurred with < 1 × 10⁴ cells ml^− 1 in the Kuroshio-Oyashio transition region, and their viabilities were 80%. In the Oyashio region where a spring diatom bloom developed, the viability of fucoxanthin-containing algae (mainly diatoms and prymnesiophytes) was ca. 90%. These results suggested that the cell viability of phytoplankton could vary seasonally with their community structure in the study area. The phytoplankton cell death in late summer was particularly significant for their loss process and could support the microbial food webs by supplying dissolved organic carbon (DOC) derived from the dead cells.