(Table 1) Comparison of diatom-bound and bulk sedimentary d15N values of ODP Holes 175-1082A and 175-1084A

The Matuyama Diatom Maximum (MDM) is a time of peak opal accumulation from 2.6 to ~2.0 Ma within the Benguela Current upwelling system that was initiated by increased influence of Southern Ocean water on the eastern South Atlantic. We measured opal, total organic carbon (TOC), and CaCO3 fluxes and C and N stable isotopes in sediments deposited from 2.4 to 1.95 Ma at Sites 1082 and 1084 to explore the biogeochemical dynamics within the Benguela region. The infusion of Southern Ocean water delivered dissolved nutrients and Southern Ocean flora and fauna, resulting in local opal accumulation increasing up to 8 g/cm**2/ky and the production of diatom mats. Some d15N measurements of diatom-bound organic matter indicate that the mats grew within the Benguela region. The bulk sediment d15N records are taken to reflect changes in the d15N of nitrate in the incoming water, where lower values at 2.4 Ma reflect less nitrate utilization in the Antarctic. A long-term increase in relative nitrate uptake in the Southern Ocean is evidenced by the gradual increase in d15N toward 1.9 Ma.

Global distributions of diazotrophs abundance and biomass - Depth integrated values computed from a collection of source datasets - Contribution to the MAREDAT World Ocean Atlas of Plankton Functional Types

The MAREDAT atlas covers 11 types of plankton, ranging in size from bacteria to jellyfish. Together, these plankton groups determine the health and productivity of the global ocean and play a vital role in the global carbon cycle. Working within a uniform and consistent spatial and depth grid (map) of the global ocean, the researchers compiled thousands and tens of thousands of data points to identify regions of plankton abundance and scarcity as well as areas of data abundance and scarcity. At many of the grid points, the MAREDAT team accomplished the difficult conversion from abundance (numbers of organisms) to biomass (carbon mass of organisms). The MAREDAT atlas provides an unprecedented global data set for ecological and biochemical analysis and modeling as well as a clear mandate for compiling additional existing data and for focusing future data gathering efforts on key groups in key areas of the ocean. The present data set presents depth integrated values of diazotrophs abundance and biomass, computed from a collection of source data sets.

(Table 1) Main parameters of consumption of inorganic nitrogen compounds by microplankton in the western Black Sea in April 1993

Parameters of provision of the phytoplankton community with inorganic nitrogen compounds in the western Black Sea in April 1993 are analyzed (specifically, dependence of rates of uptake of nitrates and ammonium by microplankton on substrate concentration, diurnal dynamics of assimilation of mineral nitrogen, values of f-ratios, and proportions of carbon and nitrogen fluxes). In most cases all the parameters of degree of phytoplankton provision with mineral nitrogen are shown to vary unidirectionally, both at the surface and in the photosynthesis zone. Individual areas of a relatively small region studied differed markedly in their level of provision of algae with inorganic nitrogen compounds - from complete saturation to high degree of limitation of phytoplankton development due to nitrogen deficiency in the environment. Obtained results allow to estimate provision of Black Sea phytoplankton with nitrogen in terms of limitation of rates of uptake of its inorganic compounds.

Posibles funciones de la familia génica de la glutamato descarboxilasa en Populus

Aunque hace más de 50 años que se describió que la glutamato descarboxilasa (GAD) lleva a cabo la descarboxilación del glutamato para producir GABA, y en animales ha sido muy estudiada debido al papel del GABA como neurotransmisor, la información disponible sobre las GADs de plantas es aún limitada, conociéndose sólo algunos aspectos de la regulación por calcio de su actividad enzimática o de expresión de algunos de los genes de su familia génica. El GABA es un metabolito que tradicionalmente se ha asociado a estrés, pero su papel en plantas todavía no está claro. En las últimas dos décadas los resultados experimentales obtenidos sobre la GAD y el GABA, destacando las alteraciones fenotípicas mostradas por plantas tratadas con GABA y por plantas transgénicas para GAD, han generado preguntas interesantes sobre el posible papel de este metabolito y la enzima en señalización en plantas. En plantas, son varios los papeles que se han propuesto para el metabolismo del GABA tales como su participación como componente del metabolismo del carbono y del nitrógeno (Fait y col., 2008), protección frente especies reactivas de oxigeno (Liu y col., 2011), regulación de la expresión génica incluyendo la regulación de genes implicados en la síntesis de hormonas (Khatiresan y col., 1997; Shi y col., 2010; Lancien y Roberts, 2006) y señalización a larga distancia (Beuve y col., 2004) y en gradiente guiando el crecimiento del tubo polínico (Palanivelu y col., 2013). Nuestro grupo de investigación ha sugerido un papel novedoso para la producción de GABA durante la xilogénesis en pino (Molina-Rueda y col., 2010, 2015). En base a estos antecedentes, los objetivos planteados para este trabajo han sido: la asignación de posibles funciones a las GADs de Populus en condiciones normales de crecimiento y en estrés abióticos, estudiar la adquisición del dominio de unión a calmodulina (CaMBD) de las GADs de plantas vasculares y analizar el efecto del GABA y del glutamato en las raíces de Populus. Las conclusiones que se derivan de los resultados de este trabajo se detallan a continuación. El dominio de unión a calmodulina de la GAD de plantas esta conservado en GADs de plantas consideradas ancestros de plantas vasculares y ausente en plantas no vasculares, lo que sitúa juntos en la evolución los eventos de adquisición del dominio de unión a CaM y el desarrollo del tejido vascular de plantas. Los resultados similares de la localización de GABA en xilema y una expresión GAD asociada a la formación de madera de reacción tanto en pino como en chopo apuntan a un papel relevante de la producción de GABA durante la xilogénesis en leñosas. La familia génica GAD posee seis genes codificando todos ellos para proteínas aparentemente funcionales y susceptibles de ser reguladas por calcio. Esta familia génica ha sufrido duplicaciones y eventos de especialización durante la evolución de Populus. Este trabajo ha posibilitado la asociación entre papeles específicos y los diferentes genes de esta familia. Beuvé N, Rispail N, Laine P, Cliquet J-B, Ourry A, Deunff F (2004) Putative role of Υ-aminobutyric acid as a long-distance signal in up-regulation of nitrate uptake in Brassica napus L. Plant Cell Environ. 27: 1035-1046 Fait A, Fromm H, Walter D, Galili G, Fernie AR (2008) Highway or byway: the metabolic role of the GABA shunt in plants. Trends in plant science 13: 14-19 Kathiresan A, Tung P, Chinnappa CC, Reid DM (1997) gamma-Aminobutyric acid stimulates ethylene biosynthesis in sunflower. Plant Physiol. 115: 129-135 Lancien M, Roberts MR (2006) Regulation of Arabidopsis thaliana 14-3-3 gene expression by ϒ-aminobutyric acid. Plant Cell Environ. 29: 1430-1436 Liu C, Zhao L, Yu G (2011) The dominant glutamic acid metabolic flux to produce gamma-amino butyric acid over proline in Nicotiana tabacum leaves under water stress relates to its significant role in antioxidant activity. Journal of integrative plant biology 53: 608-618 Molina-Rueda JJ, Pascual MB, Canovas FM, Gallardo F (2010) Characterization and developmental expression of a glutamate decarboxylase from maritime pine. Planta 232: 1471-1483 Molina-Rueda, J.J. y col., 2015. A putative role for γ-aminobutyric acid (GABA) in vascular development in pine seedlings. Planta 241: 257-267 Palanivelu R, Brass L, Edlund AF, D P (2003) Pollen tube growth and guidance is regulated by POP2, an Arabidopsis gene that controls GABA levels. Cell 114: 47-59 Shi SQ, Shi Z, Jiang ZP, Qi LW, Sun XM, Li CX, Liu JF, Xiao WF, Zhang SG (2010) Effects of exogenous GABA on gene expression of Caragana intermedia roots under NaCl stress: regulatory roles for H2O2 and ethylene production. Plant, cell & environment 33: 149-162

Nitrogen isotope fractionation during nitrate, ammonium and urea uptake by marine diatoms and coccolithophores under various conditions of N availability

Stable isotopes of N provide a new approach to the study of algal production in the ocean, yet knowledge of the isotope fractionation (epsilon) in various oceanic regimes is lacking. Here we report large and rapid changes in isotope composition (delta(15)N) of 2 coastal diatoms and 2 clones (open and coastal) of a coccolithophore grown in the simultaneous presence of nitrate, ammonium and urea under varying conditions of N availability (i.e. N-sufficiency and N-starvation followed by N-resupply) and hence different physiological states, During N-sufficiency, the delta(15)N of particulate organic N (PON) was well reproduced, using a model derived from Rayleigh distillation theory, with constant epsilon similar to that for growth on each individual N source. However, following N-resupply, the variations in delta(15)N(PON) could be well explained only in the case of the open ocean Emiliania huxleyi, with epsilon similar to N-sufficient conditions. It was concluded that the mechanism of isotope fractionation changed rapidly with N availability for the 3 coastal clones. However, in the case of E. huxleyi isolated from the Subarctic Pacific Ocean, no evidence of a change in mechanism was found, suggesting that perhaps open ocean species can quickly recover from N-depleted conditions.

Effect of ammonium and nitrate on indigenous mycorrhizal infection, rhizosphere pH change, and phosphorus uptake by sorghum

Sorghum (Sorghum bicolor L.) plants were grown in split pots in three Rothamsted soils with different soil pH values and phosphorus (P) contents. Ammonium addition resulted in higher plant dry weight and P content than comparable nitrate treatments. The pH of soils in the rhizosphere (0.51-mm average thickness) differed from the bulk soil depending on nitrogen (N) form and level. Ammonium application resulted in a pH decrease, but nitrate application slightly increased pH. To examine the effect of rhizosphere acidification on mobilization of phosphate, 0.5 M NaHCO3 extractable phosphate was measured. The lowering rhizosphere pH enhanced the solubility of P in the soil and maybe availability of P to plants. Rhizosphere-P depletion increased with increasing ammonium supply, but when N was supplied as nitrate, P depletion was not related to increasing nitrate supply. Low P status Hoosfield soils developed mycorrhizal infection., and as a result, P inflow was increased. Geescroft soil, which initially had a high P status, did not develop mycorrhizal infection, and P inflow was much smaller and was unaffected by N treatments. Therefore, plant growth and P uptake were influenced by both rhizosphere pH and indigenous mycorrhizal infection.

Size-Fractionated Nitrogen Uptake Measurements in the Equatorial Pacific and Confirmation of the Low Si-High-Nitrate Low-Chlorophyll Condition

The equatorial Pacific Ocean is the largest natural source of CO(2) to the atmosphere, and it significantly impacts the global carbon cycle. Much of the large flux of upwelled CO(2) to the atmosphere is due to incomplete use of the available nitrate (NO(3)) and low net productivity. This high-nutrient low-chlorophyll (HNLC) condition of the equatorial upwelling zone (EUZ) has been interpreted from modeling efforts to be due to low levels of silicate ( Si( OH) 4) that limit the new production of diatoms. These ideas were incorporated into an ecosystem model, CoSINE. This model predicted production by the larger phytoplankton and the picoplankton and effects on air-sea CO(2) fluxes in the Pacific Ocean. However, there were no size-fractionated rates available for verification. Here we report the first size-fractionated new and regenerated production rates (obtained with (15)N - NO(3) and (15)N - NH(4) incubations) for the EUZ with the objective of validating the conceptual basis and functioning of the CoSINE model. Specifically, the larger phytoplankton ( with cell diameters > 5 mu m) had greater rates of new production and higher f-ratios (i.e., the proportion of NO(3) to the sum of NO(3) and NH(4) uptake) than the picoplankton that had high rates of NH(4) uptake and low f-ratios. The way that the larger primary producers are regulated in the EUZ is discussed using a continuous chemostat approach. This combines control of Si(OH)(4) production by supply rate (bottom-up) and control of growth rate ( or dilution) by grazing ( top-down control).