Cyanobacteria and cyanophage contributions to carbon and nitrogen cycling in an oligotrophic oxygen-deficient zone.

Up to half of marine N losses occur in oxygen-deficient zones (ODZs). Organic matter flux from productive surface waters is considered a primary control on N2 production. Here we investigate the offshore Eastern Tropical North Pacific (ETNP) where a secondary chlorophyll a maximum resides within the ODZ. Rates of primary production and carbon export from the mixed layer and productivity in the primary chlorophyll a maximum were consistent with oligotrophic waters. However, sediment trap carbon and nitrogen fluxes increased between 105 and 150 m, indicating organic matter production within the ODZ. Metagenomic and metaproteomic characterization indicated that the secondary chlorophyll a maximum was attributable to the cyanobacterium Prochlorococcus, and numerous photosynthesis and carbon fixation proteins were detected. The presence of chemoautotrophic ammonia-oxidizing archaea and the nitrite oxidizer Nitrospina and detection of nitrate oxidoreductase was consistent with cyanobacterial oxygen production within the ODZ. Cyanobacteria and cyanophage were also present on large (>30 µm) particles and in sediment trap material. Particle cyanophage-to-host ratio exceeded 50, suggesting that viruses help convert cyanobacteria into sinking organic matter. Nitrate reduction and anammox proteins were detected, congruent with previously reported N2 production. We suggest that autochthonous organic matter production within the ODZ contributes to N2 production in the offshore ETNP.

Archaeal Sources of Intact Membrane Lipid Biomarkers in the Oxygen Deficient Zone of the Eastern Tropical South Pacific.

Archaea are ubiquitous in the modern ocean where they are involved in the carbon and nitrogen biogeochemical cycles. However, the majority of Archaea remain uncultured. Archaeal specific membrane intact polar lipids (IPLs) are biomarkers of the presence and abundance of living cells. They comprise archaeol and glycerol dibiphytanyl glycerol tetraethers (GDGTs) attached to various polar headgroups. However, little is known of the IPLs of uncultured marine Archaea, complicating their use as biomarkers. Here, we analyzed suspended particulate matter (SPM) obtained in high depth resolution from a coastal and open ocean site in the eastern tropical South Pacific (ETSP) oxygen deficient zone (ODZ) with the aim of determining possible biological sources of archaeal IPL by comparing their composition by Ultra High Pressure Liquid Chromatography coupled to high resolution mass spectrometry with the archaeal diversity by 16S rRNA gene amplicon sequencing and their abundance by quantitative PCR. Thaumarchaeotal Marine Group I (MGI) closely related to Ca. Nitrosopelagicus and Nitrosopumilus dominated the oxic surface and upper ODZ water together with Marine Euryarchaeota Group II (MGII). High relative abundance of hexose phosphohexose- (HPH) crenarchaeol, the specific biomarker for living Thaumarchaeota, and HPH-GDGT-0, dihexose- (DH) GDGT-3 and -4 were detected in these water masses. Within the ODZ, DPANN (Diapherotrites, Parvarchaeota, Aenigmarchaeota, Nanoarchaeota, and Nanohaloarchaea) of the Woesearchaeota DHVE-6 group and Marine Euryarchaeota Group III (MGIII) were present together with a higher proportion of archaeol-based IPLs, which were likely made by MGIII, since DPANN archaea are supposedly unable to synthesize their own IPLs and possibly have a symbiotic or parasitic partnership with MGIII. Finally, in deep suboxic/oxic waters a different MGI population occurred with HPH-GDGT-1, -2 and DH-GDGT-0 and -crenarchaeol, indicating that here MGI synthesize membranes with IPLs in a different relative abundance which could be attributed to the different detected population or to an environmental adaptation. Our study sheds light on the complex archaeal community of one of the most prominent ODZs and on the IPL biomarkers they potentially synthesize.

Organic matter stoichiometry, flux, and oxygen control nitrogen loss in the ocean.

Biologically available nitrogen limits photosynthesis in much of the world ocean. Organic matter (OM) stoichiometry had been thought to control the balance between the two major nitrogen removal pathways-denitrification and anammox-but the expected proportion of 30% anammox derived from mean oceanic OM is rarely observed in the environment. With incubations designed to directly test the effects of stoichiometry, however, we showed that the ratio of anammox to denitrification depends on the stoichiometry of OM supply, as predicted. Furthermore, observed rates of nitrogen loss increase with the magnitude of OM supply. The variable ratios between denitrification and anammox previously observed in the ocean are thus attributable to localized variations in OM quality and quantity and do not necessitate a revision to the global nitrogen cycle.

A new liquid chromatography/electrospray ionization mass spectrometry method for the analysis of underivatized aliphatic long-chain polyamines: application to diatom-rich sediments.

Natural polyamines are found in all three domains of life and long-chain polyamines (LCPAs) play a special role in silicifying organisms such as diatoms and sponges where they are actively involved in the complex formation and nanopatterning of siliceous structures. With chain lengths extending up to 20 N-methylated propylamine repeat units, diatom LCPAs constitute the longest natural polyamines. Mixtures of natural LCPAs are typically purified in bulk using ion-exchange, size-exclusion and dialysis and then analyzed either by direct infusion mass spectrometry or by MALDI-TOF. Here, we describe a novel ion-pairing liquid chromatographic method that allows baseline separation, detection and structural elucidation of underivatized aliphatic methylated and non-methylated LCPAs with a wide range of chain lengths. Complete separation of synthetic mixtures of LCPA species differing by either a propylamine or an N-methylpropylamine unit is achievable using this method and chromatographic separation of natural, diatom frustule bound LCPAs extracted from sediment core samples is greatly improved. Using electrospray ionization mass spectrometry (ESI-MS), we detected singly [M+H](+) and multiply [M+nH](n+) charged protonated ions. The abundance of multiply charged LCPA species increased linearly as a function of LCPA chain length (N) and multiprotonated ions [M+nH](n+) were more abundant for longer chain polyamines. The abundance of multiply charged LCPAs along with the concomitant disappearance of the singly charged protonated molecular ion significantly increases the complexity of the MS spectra, justifying the need for good chromatographic separation of complex LCPA mixtures. This analytical procedure will likely constitute a powerful tool for the characterization, quantification, as well as the purification of individual LCPAs in natural and synthetic samples for studies of silica precipitation as well as nitrogen and carbon isotopic analysis used in paleoceanographic studies.

HPLC purification of higher plant-dervied lignin phenols for compound specific radiocarbon analysis.

The ability to measure the radiocarbon content of compounds isolated from complex mixtures has begun to revolutionize our understanding of carbon transformations on earth. Because samples are often small, each new compound isolation method must be tested for background carbon contamination (C(ex)). Here, we present a new method for compound-specific radiocarbon analysis (CSRA) of higher plant-derived lignin phenols. To test for C(ex), we compared the Δ(14)C values of unprocessed lignin phenol containing standard materials (woods, leaves, natural vanillin, and synthetic vanillin) with those of lignin phenols liberated by CuO oxidation and purified by two-dimensional high-pressure liquid chromatography (HPLC) coupled to mass spectrometry (MS) and UV detection. We assessed C(ex) associated with (1) microwave assisted CuO oxidation of bulk samples to lignin phenol monomers, (2) HPLC purification, and (3) accelerator mass spectrometry (AMS) sample preparation. The Δ(14)C of purified compounds (corrected for C(ex)) agreed, within error, with those of bulk materials for samples that were >10 µg C. This method will allow routine analysis of the Δ(14)C of lignin phenols isolated from terrestrial, aquatic, and marine settings, revealing the time scale for the processing of one of the single largest components of active organic carbon reservoirs on earth.

Succession and diel transcriptional response of the glycolate-utilizing component of the bacterial community during a spring phytoplankton bloom.

The influence of the phytoplankton-specific organic compound glycolate on bacterial community structure was examined during the 2004 spring phytoplankton bloom (February to April) in Dabob Bay in Washington. The diversity of the bacteria able to utilize glycolate during the phytoplankton bloom was determined using previously developed PCR primers to amplify the gene for the D subunit of glycolate oxidase (glcD). Many of the glcD sequences obtained represented novel sequences that appeared to be specific to marine environments. Overall, the glcD sequence diversity decreased as the phytoplankton bloom progressed. Phylotype-specific glcD quantitative PCR primers were designed for the six most commonly detected glcD phylotypes that represented distinct phylogenetic groups of heterotrophic bacteria. Three patterns of phylotype abundance were detected: four phylotypes were most abundant during the onset of the bloom; the abundance of one phylotype increased as the bloom progressed; and one phylotype was abundant throughout the bloom. Quantitative reverse transcriptase PCR with the same phylotype-specific primers was used to determine the levels of day and night glcD RNA transcription over the course of the bloom. glcD transcripts, when detectable, were always more abundant in the day than at night for each phylotype, suggesting that the bacteria responded to the glycolate produced by phytoplankton during the day. The nearly constant low in situ glycolate concentrations suggested that bacteria rapidly utilized the available glycolate. This study provided evidence for direct phytoplankton-bacterium interactions and the resulting succession in a single functional group of marine bacteria.

Quantifying 3H-thymidine incorporation rates by a phylogenetically defined group of marine planktonic bacteria (Bacteriodetes phylum).

The rate of [(3)H-methyl] thymidine ((3)H-TdR) incorporation into DNA has been applied extensively to measure cell production by bacterial communities in aquatic environments. Here we describe a method to quantify (3)H-TdR incorporation by specific, phylogenetically defined members of the bacterial community. The method involves selectively capturing DNA from targeted groups of bacteria and then quantifying its (3)H radioactivity. The method was applied to measure (3)H-TdR incorporation by the members of the phylum Bacteriodetes whose members, which include the Cytophaga-Flavobacter cluster, are ubiquitous in coastal waters. (3)H-labelled DNA from Bacteriodetes was selectively biotinylated in PCR-like reactions that contained a Bacteriodetes-specific 16S rRNA gene primer, thermostable DNA polymerase and biotinylated dUTP. The biotinylated DNA was then captured on streptavidin-coated beads and its (3)H radioactivity determined by scintillation counting. We have termed this method 'selective nucleic acid polymerase-biotinylation and capture' or 'SNAP-BAC'. Internal (33)P-labelled DNA standards were used to quantify the recovery of (3)H-labelled DNA from the SNAP-BAC reactions. The method was verified by successfully targeting Bacteriodetes in simple laboratory mixtures of (3)H-labelled DNA extracted from pure cultures of Bacteriodetes and gamma-proteobacteria. Field application of this method in Puget Sound and off the Washington coast determined that Bacteriodetes were responsible for 56 +/- 17% and 32 +/- 5% of community (3)H-TdR incorporation (1.3 +/- 0.3 and 9.9 +/- 1.7 pmol l(-1) h(-1)) at these two locations.