Benthic foraminifera contribution to fjord modern carbon pools: A seasonal study in Adventfjorden,Spitsbergen

The aim of this study was to determine the amount of organic and inorganic carbon in foraminifera specimens and to provide quantitative data on the contribution of foraminifera to the sedimentary carbon pool in Adventfjorden. The investigation was based on three calcareous species that occur commonly in Svalbard fjords: Cassidulina reniforme, Elphidium excavatum and Nonionellina labradorica. Our results show that the species investigated did not contribute substantially to the organic carbon pool in Adventfjorden, because they represented only 0.37% of the organic carbon in the sediment. However, foraminiferal biomass could have been underestimated as it did not include arenaceous or monothalamous taxa. Foraminiferal carbonate constituted up to 38% of the inorganic carbon in the sediment, which supports the assumption that in fjords where non‐calcifying organisms dominate the benthic fauna foraminifera are among the major producers of calcium carbonate and that they play crucial roles in the carbon burial process. The results presented in this study contribute to estimations of changes in foraminiferal carbon levels in contemporary environments and could be an important reference for palaeoceanographic studies.     

Effect of photon flux density on inorganic carbon accumulation and net CO2 exchange in a high-CO2-requiring mutant of Chlamydomonas reinhardtii

The effect of photon flux density on inorganic carbon accumulation and photosynthetic CO₂ assimilation was determined by CO₂ exchange studies at three, limiting CO₂ concentrations with a ca-1 mutant of Chlamydomonas reinhardiii. This mutant accumulates a large internal inorganic carbon pool in the light which apparently is unavailable for photosynthetic assimilation. Although steady-state photosynthetic CO₂ assimilation did not respond to the varying photon flux densities because of CO₂ limitation, components of inorganic-carbon accumulation were not clearly light saturated even at 1100 mol photons m^-2 s^-1, indicating a substantial energy requirement for inorganic carbon transport and accumulation. Steady-state photosynthetic CO₂ assimilation responded to external CO₂ concentrations but not to changing internal inorganic carbon concentrations, confirming that diffusion of CO₂ into the cells supplies most of the CO₂ for photosynthetic assimilation and that the internal inorganic carbon pool is essentially unavailable for photosynthetic assimilation. The estimated concentration of the internal inorganic carbon pool was found to be relatively insensitive to the external CO₂ concentration over the small range tested, as would be expected if the concentration of this pool is limited by the internal to external inorganic carbon gradient. An attempt to use this CO₂ exchange method to determine whether inorganic carbon accumulation and photosynthetic CO₂ assimilation compete for energy at low photon flux densities proved inconclusive.     

Nitrogen assimilation by a Citrus tree

Primary assimilation of ¹⁵N-ammonium or ¹⁵N-nitrate by excised leaves of satsuma mandarin (Citrus unshiu Markovitch) was examined under light and dark conditions. Under both conditions both types of nitrogen were most markedly incorporated into glutamine-amide nitrogen in the primary step of the assimilation, and into proline in the later steps. Incorporation of ammonium or nitrate into amino acids was more active in the light than in the dark, although the stimulating effect of light on the incorporation was relatively small in both cases.     

Benthic foraminiferal population fluctuations related to anoxia: Santa Barbara Basin

The pore-water geochemistry and benthic foraminiferal assemblages of sediments from two slope sites and within the central portion of the Santa Barbara Basin were characterized between February 1988 and July 1989. The highest foraminiferal numerical densities (1197 cm^–3 as determined by an ATP assay) occurred at a slope site in June 1988 (550 m) in partially laminated sediments. In continuously laminated sediments from the central basin, foraminifera were found living (as determined by ATP assay) in October 1988 to depths of 4 cm, and specimens prepared for transmission electron microscopy were found with intact organelles to 3 cm, indicating their inhabitation of anoxic pore waters. Ultrastructural data from Nonionella stella is consistent with the hypothesis that this species can survive by anaerobic respiration. However, the benthic foraminifera appear unable to survive prolonged anoxia. The benthic foraminiferal population was completely dead in July 1989 when bottom water O₂ was undetectable.     

Resting Stages of Skeletonema marinoi Assimilate Nitrogen From the Ambient Environment Under Dark,Anoxic Conditions

The planktonic marine diatom Skeletonema marinoi forms resting stages, which can survive for decades buried in aphotic, anoxic sediments and resume growth when re-exposed to light, oxygen, and nutrients. The mechanisms by which they maintain cell viability during dormancy are poorly known. Here, we investigated cell-specific nitrogen (N) and carbon (C) assimilation and survival rate in resting stages of three S. marinoi strains. Resting stages were incubated with stable isotopes of dissolved inorganic N (DIN), in the form of ¹⁵N-ammonium (NH₄⁺) or -nitrate (NO₃⁻) and dissolved inorganic C (DIC) as ¹³C-bicarbonate (HCO₃⁻) under dark and anoxic conditions for 2 months. Particulate C and N concentration remained close to the Redfield ratio (6.6) during the experiment, indicating viable diatoms. However, survival varied between <0.1% and 47.6% among the three different S. marinoi strains, and overall survival was higher when NO₃⁻ was available. One strain did not survive in the NH₄⁺ treatment. Using secondary ion mass spectrometry (SIMS), we quantified assimilation of labeled DIC and DIN from the ambient environment within the resting stages. Dark fixation of DIC was insignificant across all strains. Significant assimilation of ¹⁵N-NO₃⁻ and ¹⁵N-NH₄⁺ occurred in all S. marinoi strains at rates that would double the nitrogenous biomass over 77–380 years depending on strain and treatment. Hence, resting stages of S. marinoi assimilate N from the ambient environment at slow rates during darkness and anoxia. This activity may explain their well-documented long survival and swift resumption of vegetative growth after dormancy in dark and anoxic sediments.     

Nitrate and Ammonium Induced Photosynthetic Suppression in N-Limited Selenastrum minutum

Nitrate-limited chemostat cultures of Selenastrum minutum Naeg. Collins (Chlorophyta) were used to determine the effects of nitrogen addition on photosynthesis, dark respiration, and dark carbon fixation. Addition of NO₃⁻ or NH₄⁺ induced a transient suppression of photosynthetic carbon fixation (70 and 40% respectively). Intracellular ribulose bisphosphate levels decreased during suppression and recovered in parallel with photosynthesis. Photosynthetic oxygen evolution was decreased by N-pulsing under saturating light (650 microeinsteins per square meter per second). Under subsaturating light intensities (<165 microeinsteins per square meter per second) NH₄⁺ addition resulted in O₂ consumption in the light which was alleviated by the presence of the tricarboxylic acid cycle inhibitor fluoroacetate. Addition of NO₃⁻ or NH₄⁺ resulted in a large stimulation of dark respiration (67 and 129%, respectively) and dark carbon fixation (360 and 2080%, respectively). The duration of N-induced perturbations was dependent on the concentration of added N. Inhibition of glutamine 2-oxoglutarate aminotransferase by azaserine alleviated all these effects. It is proposed that suppression of photosynthetic carbon fixation in response to N pulsing was the result of a competition for metabolites between the Calvin cycle and nitrogen assimilation. Carbon skeletons required for nitrogen assimilation would be derived from tricarboxylic acid cycle intermediates. To maintain tricarboxylic acid cycle activity triose phosphates would be exported from the chloroplast. This would decrease the rate of ribulose bisphosphate regeneration and consequently decrease net photosynthetic carbon accumulation. Stoichiometric calculations indicate that the Calvin cycle is one source of triose phosphates for N assimilation; however, during transient N resupply the major demand for triose phosphates must be met by starch or sucrose breakdown. The effects of N-pulsing on O₂ evolution, dark respiration, and dark C-fixation are shown to be consistent with this model.     

The effect of harvesting intensity on the fate of applied 15N-ammonium to the organic horizons of a coniferous forest in N. Wales

¹⁵N-ammonium sulphate equivalent to 0.5 kg N/ha was added as a tracer to lysimeters containing the organic horizons of an acid forest soil. The effect of logging debris (brash), vegetation and second rotationPicea sitchensis seedlings on the amount of the¹⁵N found in various soil, vegetation and leachate pools was followed over a period of 60 days. Transformation of¹⁵N-ammonium to nitrate occurred within 24 hours. Although total nitrate leachate losses were high, tracer-derived nitrate represented only 0.4%–4.2% of the applied¹⁵N-ammonium. The atom % excess of the KCI-extractable organic-N pool was initially lower than for the inorganic species but due to the large pool size, consistently represented 3–6% of the applied¹⁵N-ammonium. The similarity of the atom % excess of the ammonium and nitrate pools indicated an autotrophic nitrification pathway.A significant proportion of the¹⁵N-ammonium passed through the microbial biomass which contained between 16 and 48% of the¹⁵N-ammonium 2 days after addition of the¹⁵N-ammonium. This nitrogen was in a readily available form or short-term pool for the first two weeks (with no change in the overall biomass pool), after which the nitrogen appeared to become transformed into more stable compounds representing a long-term pool. Total recovery of the¹⁵N was between 68% and 99% for the different treatments. The presence of brash reduced microbial immobilisation of the¹⁵N-ammonium and total retention in the organic matter. This is suggested to be a consequence of greater nitrification and denitrificatiion rate in organic horizons beneath a brash covering due to different microclimatic conditions.     

河西走廊沙漠泡泡刺群体光合特征及其与环境因子的关系

以河西走廊沙漠典型的荒漠植物泡泡刺群落为材料,运用LI-8100土壤碳通量测定系统与改进的同化箱联合对其7月和8月中旬的群体光合作用进行了测定,分析群体光合速率与立地环境因子的关系,探讨泡泡刺群体对干旱荒漠环境的光合适应机制。结果表明,7月中旬泡泡刺的土壤呼吸速率和蒸发速率均高于8月中旬,而其同期群体光合速率和水分利用效率也显著高于8月中旬。两时期的光合有效辐射是影响泡泡刺群体光合速率的主要因子,于7、8月中旬对泡泡刺群体的光合速率起着直接作用;同时,实验地8月中旬的空气相对湿度也能通过与大气温度以及光合有效辐射的相互作用对泡泡刺群体的光合速率产生较大影响。在7月中旬高温强光环境下,泡泡刺的群体光合速率高于8月中旬,从而说明泡泡刺对高光强、高温的荒漠环境具有较好的适应性。     

贵州喀斯特森林三种植物对不同坡位环境的光合生理响应

该研究以贵州普定喀斯特森林中、下坡位生长的构树( Broussonetia papyrifera)、朴树( Celtis sinensis)和光滑悬钩子( Rubus tsangii)为材料,通过对碳酸酐酶( CA)活性、光合作用日变化、净光合速率对CO2与光的响应曲线、叶绿素荧光特性以及稳定碳同位素组成等指标的测定,进而对比分析三种植物不同的光合生理响应特性。结果表明：构树光合作用过程的无机碳源既可来自大气中的CO2,也可以在气孔部分闭合的情况下利用细胞内的HCO3－,下坡位的构树较高的CA活性使其利用HCO3－的效率会更高,并能在较低光强下具有较高的光能利用效率。这可能与下坡位的构树具有较高的CA活性有关,对下坡位具有更好的适应性。朴树光合无机碳的同化能力最低,且光合无机碳源较单一,主要利用大气CO2,其较慢的生长速率使其对无机碳的需求最低,且能保持较稳定的无机碳同化速率。相对来说,中坡位的朴树具有相对较高的净光合速率和光能利用效率,对中坡位表现出较好的适应性。光滑悬钩子主要利用大气中的CO2进行光合作用。中坡位的光滑悬钩子具有较强的光能利用效率,并表现出较高的净光合速率,光滑悬钩子对中坡位同样表现出较好的适应性。该研究结果为喀斯特生态脆弱区植被重建过程中树种的选择及合理配置提供了科学依据。     

PLANKTONIC SARCODINES: MICROHABITAT FOR OCEANIC DINOFLAGELLATES1

Two morphologically distinct species of free-swimming dinoflagellates belonging to the genus Gyrodinium utilize the spine and rhizopodial environments of planktonic foraminifera and colonial radiolaria as microhabitats. Up to 84% of the sarcodines examined in a given population were associated with these dinoflagellates at densities up to 20,000 cells per sarcodine in some radiolarian colonies. Both dinoflagellate species possess chloroplasts, indicating they are capable of autotrophy. ¹⁴C-labelling experiments with the radiolarian-associated dinoflagellate demonstrate that it can take up inorganic carbon under both light and dark conditions. Ultrastructural evidence suggests the foraminiferal dinoflagellate may be capable of phagotrophy. Hence, these algae should be considered mixotrophs. An unusual cytoplasmic extension used for attachment and possibly feeding occurs in the foraminiferal-associated Gyrodinium and is documented with electron microscopy. Ultrastructural examination suggests this organelle may be hydrostatically controlled and may be an extension of the sac pusule.     

Interactions between inorganic phosphate (Pi) assimilation,photosynthesis and respiration in the Pi-limited green alga Selenastrum minutum*

Inorganic phosphate (P_i)-limited chemostat cultures of the green alga Selenastrum minutum were employed to investigate interactions between P_i assimilation, respiration and photosynthetic processes. Changes in net and gross gas exchange rates indicated that O₂ evolution decreases during photosynthetic P_i assimilation. Room temperature and 77K Chi a fluorescence measurements revealed that this photosynthetic suppression is correlated with a transition from state 1 to state 2. Substantial photosynthetic P_i uptake rates occur in the presence of DCMU and KCN. Additionally, the cellular ratio of ATP:NADPH increases following P_i enrichment, suggesting that the ratio of cyclic to linear electron flow is enhanced in response to the high energy requirements of P_i uptake. Net starch degradation was observed during photosynthetic P_i assimilation and the cellular pool size of 3-phosphoglycerate increased; however, gross gas exchange parameters and cellular metabolite pool sizes indicated that mitochondrial respiration plays a smaller role during P_i assimilation in the light than it does in the dark. These observations were used to formulate a model depicting possible interactions between photosynthetic electron flow, photosynthetic and respiratory carbon metabolism and metabolite exchange between the chloroplast, cytosol and mitochondrion during photosynthetic P_i assimilation.     

Oxygen respiration rates of benthic foraminifera as measured with oxygen microsensors

Oxygen respiration rates of benthic foraminifera are still badly known, mainly because they are difficult to measure. Oxygen respiration rates of seventeen species of benthic foraminifera were measured using microelectrodes and calculated on the basis of the oxygen fluxes measured in the vicinity of the foraminiferal specimens. The results show a wide range of oxygen respiration rates for the different species (from 0.09 to 5.27 nl cell⁻¹ h⁻¹) and a clear correlation with foraminiferal biovolume showed by the power law relationship: R = 3.98 10⁻³ BioVol^0.88 where the oxygen respiration rate (R) is expressed in nl O₂ h⁻¹ and in μm³ biovolume (BioVol) (n = 44, R² = 0.72, F = 114, p < 0.0001). The results expressed per biovolume unit (1.82 to 15.7 nl O₂ 10⁻⁸ μm⁻³ h⁻¹) allow us to compare our data with the previous published data showing similar ranges. A comparison with available data for other microbenthos groups (nematodes, copepods, ostracods, ciliates and flagellates) suggests that benthic foraminifera have a lower oxygen respiration rates per unit biovolume. The total contribution of benthic foraminifera to the aerobic mineralisation of organic matter is estimated for the studied areas. The results suggest that benthic foraminifera play only a minor role (0.5 to 2.5%) in continental shelf environments, which strongly contrasts with their strong contribution to anaerobic organic matter mineralisation, by denitrification, in the same areas.     

The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World

Ocean acidification (OA) can have adverse effects on marine calcifiers. Yet, phototrophic marine calcifiers elevate their external oxygen and pH microenvironment in daylight, through the uptake of dissolved inorganic carbon (DIC) by photosynthesis. We studied to which extent pH elevation within their microenvironments in daylight can counteract ambient seawater pH reductions, i.e. OA conditions. We measured the O₂ and pH microenvironment of four photosymbiotic and two symbiont-free benthic tropical foraminiferal species at three different OA treatments (∼432, 1141 and 2151 µatm pCO₂). The O₂ concentration difference between the seawater and the test surface (ΔO₂) was taken as a measure for the photosynthetic rate. Our results showed that O₂ and pH levels were significantly higher on photosymbiotic foraminiferal surfaces in light than in dark conditions, and than on surfaces of symbiont-free foraminifera. Rates of photosynthesis at saturated light conditions did not change significantly between OA treatments (except in individuals that exhibited symbiont loss, i.e. bleaching, at elevated pCO₂). The pH at the cell surface decreased during incubations at elevated pCO₂, also during light incubations. Photosynthesis increased the surface pH but this increase was insufficient to compensate for ambient seawater pH decreases. We thus conclude that photosynthesis does only partly protect symbiont bearing foraminifera against OA.     

Photosynthesis and nitrogen utilization in exponentially growing nitrogen-limited cultures of Lemna gibba

The photosynthetic performance and nitrogen utilization of Lemna gibba L. G3 adapted to limited nitrogen supply was studied. The plants were adapted to two levels of nitrogen limitation where the nitrogen addition rates were calculated to sustain relative growth rates (RGR) of 0.15 day^?1 and 0.25 day^?1, respectively. The photosynthetic performance of these cultures was compared to nitrogen-sufficient cultures with an average RGR of 0.32 day^?1. Plants transferred from nitrogen-sufficient conditions attained RGR values corresponding to the nitrogen addition rates after 6 to 10 days. Light-saturated net photosynthesis declined during adaptation according to the drop in growth rate, and a concomitant decrease in the respiration rate was recorded. The efficiency of net photosynthesis on a dry weight basis increased with increased nitrogen supply, whereas it was the same in all cultures when expressed on a chlorophyll basis. The light compensation point was unaffected by the nitrogen regime. Limited nitrogen supply resulted in an increased proportion of dry matter in the roots, which led to decreased leaf area ratios. The net assimilation rates also decreased, but not to the same extent as the leaf area ratios. Growth-limiting amounts of nitrogen were added to the cultures once daily, and the net influx of N was higher than the requirement for N, also in adapted cultures with a steady growth rate. This resulted in transient, periodic fluctuations in the NO₃^?, NH₄⁺ and amino acid pools. Also the rates of NO₃^? reduction and NH₄⁺ assimilation fluctuated as did the amino acid assimilation which paralleled NH₄⁺ assimilation. The role of flux rates over the plasmalemma and tonoplast for control of nitrogen assimilation rates are discussed.     

Carbon and oxygen isotope geochemistry of live (stained) benthic foraminifera from the Aleutian Margin and the Southern Australian Margin

Comparisons of ambient bottom-water geochemistry and stable isotopic values of the tests of living (stained) calcareous benthic foraminifera from the North Pacific (on the Aleutian Margin, water depth 1988 m) and Murray Canyons group in the Southern Indian Ocean (Australian Margin, water depths 2476 m and 1634 m) provide modern environmental analogs to calibrate paleoenvironmental assessments. Consistent with the hypothesis that microhabitat preferences influence foraminiferal isotopic values, benthic foraminifera from both margins were depleted in ¹³C with respect to bottom-water dissolved inorganic carbon (DIC). The carbon isotope values of deep infaunal foraminifera (Chilostomella oolina, Globobulimina pacifica) showed greater differences from estimates of those of DIC than shallow benthic foraminifera (Bulimina mexicana, Bolivinita quadrilatera, Pullenia bulloides). This study provides new isotopic and ecological information for B. quadrilatera. The mean Δδ¹³C value, defined as foraminiferal δ¹³C values minus estimated ambient δ¹³C values from the Aleutian Margin, is 0.97‰ higher for G. pacifica than the mean from the Murray Canyon. This difference may result either from genetic or biological differences between the populations or from differences in environmental isotopic influences (such as pore water differences) that were not accounted for in the equilibrium calculations. These analyses provide calibration information for the evaluation of bottom water conditions and circulation patterns of ancient oceans based on fossil foraminiferal geochemistry.     

Energetics of sulfate transport in Desulfomicrobium baculatum

The freshwater sulfate reducer Desulfomicrobium baculatum accumulated ³⁵S-sulfate up to 120-fold by an energy-dependent transport system, as was concluded from inhibition of transport by tetrachlorosalicylanilide (TCS). Sulfate accumulation was completely reversible and depended on the presence of sodium ions. The sodium ion gradient ([Na⁺]_out/[Na⁺]_in) was eightfold and was built up by electrogenic Na⁺/H⁺ antiport. Together with a membrane potential of-145 m V, the sodium ion motive force was-199 m V, from which a symport stoichiometry of two sodium ions per sulfate was calculated. This is the first report of a freshwater sulfate reducer taking up sulfate electroneutrally in symport with sodium ions and not with protons.Abbreviations ETH 2120 N,N'-Dibenzyl-N,N'-diphenyl-1,2-phenylendioxydiacetamide - TCS Tetrachlorosalicylanilide     

15N-ammonium and 15N-nitrate uptake of a 15-year-old Picea abies plantation

Throughfall nitrogen of a 15-year-old Picea abies (L.) Karst. (Norway spruce) stand in the Fichtelgebirge, Germany, was labeled with either ¹⁵N-ammonium or ¹⁵N-nitrate and uptake of these two tracers was followed during two successive growing seasons (1991 and 1992). ¹⁵N-labeling (62 mg ¹⁵N m^-2 under conditions of 1.5 g N m^-2 atmospheric nitrogen deposition) did not increase N concentrations in plant tissues. The ¹⁵N recovery within the entire stand (including soils) was 94%±6% of the applied ¹⁵N-ammonium tracer and 100%±6% of the applied ¹⁵N-nitrate tracer during the 1st year of investigation. This decreased to 80%±24% and 83%±20%, respectively, during the 2nd year. After 11 days, the ¹⁵N tracer was detectable in 1-year-old spruce needles and leaves of understory species. After 1 month, tracer was detectable in needle litter fall. At the end of the first growing season, more than 50% of the ¹⁵N taken up by spruce was assimilated in needles, and more than 20% in twigs. The relative distribution of recovered tracer of both ¹⁵N-ammonium and ¹⁵N-nitrate was similar within the different foliage age classes (recent to 11-year-old) and other compartments of the trees. ¹⁵N enrichment generally decreased with increasing tissue age. Roots accounted for up to 20% of the recovered ¹⁵N in spruce; no enrichment could be detected in stem wood. Although ¹⁵N-ammonium and ¹⁵N-nitrate were applied in the same molar quantities (¹⁵NH ₄ ⁺ : ¹⁵NO ₃ ^- =1:1), the tracers were diluted differently in the inorganic soil N pools (¹⁵NH ₄ ⁺ /NH ₄ ⁺ : ¹⁵NO ₃ ^- /NO ₃ ^- =1:9). Therefore the measured ¹⁵N amounts retained by the vegetation do not represent the actual fluxes of ammonium and nitrate in the soil solution. Use of the molar ammonium-to-nitrate ratio of 9:1 in the soil water extract to estimate ¹⁵N uptake from inorganic N pools resulted in a 2–4 times higher ammonium than nitrate uptake by P. abies.     

Interaction of benthic microalgae and macrofauna in the control of benthic metabolism, nutrient fluxes and denitrification in a shallow sub-tropical coastal embayment (western Moreton Bay, Australia)

Benthic biogeochemistry and macrofauna were investigated six times over 1 year in a shallow sub-tropical embayment. Benthic fluxes of oxygen (annual mean ?918 μmol O₂ m^?2 h^?1), ammonium (NH₄ ⁺), nitrate (NO₃ ^?), dissolved organic nitrogen, dinitrogen gas (N₂), and dissolved inorganic phosphorus were positively related to OM supply (N mineralisation) and inversely related to benthic light (N assimilation). Ammonium (NH₄ ⁺), NO₃ ^? and N₂ fluxes (annual means +14.6, +15.9 and 44.6 μmol N m^?2 h^?1) accounted for 14, 16 and 53 % of the annual benthic N remineralisation respectively. Denitrification was dominated by coupled nitrification–denitrification throughout the study. Potential assimilation of nitrogen by benthic microalgae (BMA) accounted for between 1 and 30 % of remineralised N, and was greatest during winter when bottom light was higher. Macrofauna biomass tended to be highest at intermediate benthic respiration rates (?1,000 μmol O₂ m^?2 h^?1), and appeared to become limited as respiration increased above this point. While bioturbation did not significantly affect net fluxes, macrofauna biomass was correlated with increased light rates of NH₄ ⁺ flux which may have masked reductions in NH₄ ⁺ flux associated with BMA assimilation during the light. Peaks in net N₂ fluxes at intermediate respiration rates are suggested to be associated with the stimulation of potential denitrification sites due to bioturbation by burrowing macrofauna. NO₃ ^? fluxes suggest that nitrification was not significantly limited within respiration range measured during this study, however comparisons with other parts of Moreton Bay suggest that limitation of coupled nitrification–denitrification may occur in sub-tropical systems at respiration rates exceeding ?1,500 μmol O₂ m^?2 h^?1.     

Seasonal variations in foraminiferal flux in the Southern Ocean, Campbell Plateau, New Zealand

Time-incremental sediment trap moorings were deployed at two sites across Campbell Plateau, New Zealand; one in the relatively quiet waters of the plateau interior (Pukaki Rise) and the other at the Antarctic Circumpolar Current-swept margin (eastern Campbell flank). A continuous record of particle flux over 416 days identifies marked differences in faunal composition and seasonal occurrence in response to these two dynamically different Southern Ocean settings. In the shallow and thermally isolated interior of the Pukaki Rise site, the flux of foraminifera was closely linked to the austral spring pulse of primary production, at which time 97% of the total foraminiferal production for the year occurred. This seasonal flux of foraminifera at Pukaki Rise was dominated by the species Globorotalia inflata and Globigerina bulloides. The collapse of phytoplankton production at the end of spring was most likely a result of a co-limitation of iron and silicic acid. Over the deep and dynamic eastern flank of Campbell Plateau there were four seasonal pulses of foraminiferal flux, the largest in spring when almost half of the foraminiferal production occurred. Most of the spring flux at this site consisted of Globorotalia inflata and Globigerinita glutinata. Summer at eastern Campbell flank, exhibited the lowest flux of foraminifera, but the highest species diversity, while autumn and winter fluxes were dominated by the deep-dwelling Globorotalia truncatulinoides. Although there was only a single pulse of foraminiferal flux at Pukaki Rise, its mass (g m^{− 2}d^{− 1}) was still greater than that which occurred over the flank, summed across all four seasons. However, the overall standing stock (tests m^{− 2}d^{− 1}) on the flank was more than twice that which occurred at the Pukaki Rise site.An examination of core-top material taken from gravity cores collected in the vicinity of the sediment trap locations, revealed typical Southern Ocean foraminiferal assemblages that were markedly dissimilar in proportion to those observed in the sediment traps.     

Oxygen consumption during leaf nitrate assimilation in a C3 and C4 plant: the role of mitochondrial respiration

Measurements of net fluxes of CO₂ and O₂ from leaves and chlorophyll a fluorescence were used to determine the role of mitochondrial respiration during nitrate (NO₃^–) assimilation in both a C₃ (wheat) and a C₄ (maize) plant. Changes in the assimilatory quotient (net CO₂ consumed over net O₂ evolved) when the nitrogen source was shifted from NO₃^– to NH₄⁺ (ΔAQ) provided a measure of shoot NO₃^– assimilation. According to this measure, elevated CO₂ inhibited NO₃^– assimilation in wheat but not maize. Net O₂ exchange under ambient CO₂ concentrations increased in wheat plants receiving NO₃^– instead of NH₄⁺, but gross O₂ evolution from the photosynthetic apparatus (J_O2) was insensitive to nitrogen source. Therefore, O₂ consumption within wheat photosynthetic tissue (ΔΟ₂), the difference between J_O2 and net O₂ exchange, decreased during NO₃^– assimilation. In maize, NO₃^– assimilation was insensitive to changes in intercellular CO₂ concentration (C_i); nonetheless, ΔΟ₂ at low C_i values was significantly higher in NO₃^–‐fed than in NH₄⁺‐fed plants. Changes in O₂ consumption during NO₃^– assimilation may involve one or more of the following processes: (a) Mehler ascorbate peroxidase (MAP) reactions; (b) photorespiration; or (c) mitochondrial respiration. The data presented here indicates that in wheat, the last process, mitochondrial respiration, is decreased during NO₃^– assimilation. In maize, NO₃^– assimilation appears to stimulate mitochondrial respiration when photosynthetic rates are limiting.