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  • 2010-2014  (73)
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  • 1
    Publication Date: 2012-07-03
    Description: Until recently, the process of denitrification (conversion of nitrate or nitrite to gaseous products) was thought to be performed exclusively by prokaryotes and fungi. The finding that foraminifera perform complete denitrification could impact our understanding of nitrate removal in sediments as well as our understanding of eukaryotic respiration, especially if it is widespread. However, details of this process and the subcellular location of these reactions in foraminifera remain uncertain. For example, prokaryotic endobionts, rather than the foraminifer proper, could perform denitrification, as has been shown recently in an allogromiid foraminifer. Here, intracellular nitrate concentrations and isotope ratios (δ15NNO3 and δ18ONO3) were measured to assess the nitrate dynamics in four benthic foraminiferal species (Bolivina argentea, Buliminella tenuata, Fursenkoina cornuta, Nonionella stella) with differing cellular architecture and associations with microbial endobionts, recovered from Santa Barbara Basin, California. Cellular nitrate concentrations were high (12–217 mM) in each species, and intracellular nitrate often had elevated δ15NNO3 and δ18ONO3 values. Experiments including suboxic and anoxic incubations of B. argentea revealed a decrease in intracellular nitrate concentration and an increase in δ15NNO3 and δ18ONO3 over time, indicating nitrate respiration and/or denitrification within the foraminifera. Results illustrate that nitrate reduction occurs in a range of foraminiferal species, including some possessing endobionts (including a chloroplast-sequestering species) and others lacking endobionts, implying that microbial associates may not solely be responsible for this process in foraminifera. Furthermore, we show that benthic foraminifera may represent important reservoirs of nitrate storage in sediments, as well as mediators of its removal.
    Print ISSN: 0148-0227
    Topics: Biology , Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 2013-01-03
    Description: [1]  Until recently, the process of denitrification (conversion of nitrate or nitrite to gaseous products) was thought to be performed exclusively by prokaryotes and fungi. The finding that foraminifera perform complete denitrification could impact our understanding of nitrate removal in sediments as well as our understanding of eukaryotic respiration, especially if it is widespread. However, details of this process and the subcellular location of these reactions in foraminifera remain uncertain. For example, prokaryotic endobionts, rather than the foraminifer proper, could perform denitrification, as has been shown recently in an allogromiid foraminifer. Here, intracellular nitrate concentrations and isotope ratios ( δ 15 N NO3 and δ 18 O NO3 ) were measured to assess the nitrate dynamics in four benthic foraminiferal species ( Bolivina argentea, Buliminella tenuata, Fursenkoina cornuta, Nonionella stella ) with differing cellular architecture and associations with microbial endobionts, recovered from Santa Barbara Basin, California. Cellular nitrate concentrations were high (12–217 mM) in each species, and intracellular nitrate often had elevated δ 15 N NO3 and δ 18 O NO3 values. Experiments including suboxic and anoxic incubations of B. argentea revealed a decrease in intracellular nitrate concentration and an increase in δ 15 N NO3 and δ 18 O NO3 over time, indicating nitrate respiration and/or denitrification within the foraminifera. Results illustrate that nitrate reduction occurs in a range of foraminiferal species, including some possessing endobionts (including a chloroplast-sequestering species) and others lacking endobionts, implying that microbial associates may not solely be responsible for this process in foraminifera. Furthermore, we show that benthic foraminifera may represent important reservoirs of nitrate storage in sediments, as well as mediators of its removal.
    Print ISSN: 0148-0227
    Topics: Biology , Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 3
    Publication Date: 2014-01-22
    Description: Active eukaryotes in microbialites from Highborne Cay, Bahamas, and Hamelin Pool (Shark Bay), Australia The ISME Journal 8, 418 (February 2014). doi:10.1038/ismej.2013.130 Authors: Virginia P Edgcomb, Joan M Bernhard, Roger E Summons, William Orsi, David Beaudoin & Pieter T Visscher
    Keywords: protiststromatolitethrombolite18S rRNAdiversityforaminifera
    Print ISSN: 1751-7362
    Electronic ISSN: 1751-7370
    Topics: Biology
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Schattenhofer, Martha; Fuchs, Bernhard M; Amann, Rudolf; Zubkov, Mikhail V; Tarran, Glen A; Pernthaler, Jakob (2009): Latitudinal distribution of prokaryotic picoplankton populations in the Atlantic Ocean. Environmental Microbiology, 11(8), 2078-2093, https://doi.org/10.1111/j.1462-2920.2009.01929.x
    Publication Date: 2023-09-23
    Description: Members of the prokaryotic picoplankton are the main drivers of the biogeochemical cycles over large areas of the world's oceans. In order to ascertain changes in picoplankton composition in the euphotic and twilight zones at an ocean basin scale we determined the distribution of 11 marine bacterial and archaeal phyla in three different water layers along a transect across the Atlantic Ocean from South Africa (32.9°S) to the UK (46.4°N) during boreal spring. Depth profiles down to 500 m at 65 stations were analysed by catalysed reporter deposition fluorescence in situ hybridization (CARD-FISH) and automated epifluorescence microscopy. There was no obvious overall difference in microbial community composition between the surface water layer and the deep chlorophyll maximum (DCM) layer. There were, however, significant differences between the two photic water layers and the mesopelagic zone. SAR11 (35 ± 9%) and Prochlorococcus (12 ± 8%) together dominated the surface waters, whereas SAR11 and Crenarchaeota of the marine group I formed equal proportions of the picoplankton community below the DCM (both ~15%). However, due to their small cell sizes Crenarchaeota contributed distinctly less to total microbial biomass than SAR11 in this mesopelagic water layer. Bacteria from the uncultured Chloroflexi-related clade SAR202 occurred preferentially below the DCM (4-6%). Distinct latitudinal distribution patterns were found both in the photic zone and in the mesopelagic waters: in the photic zone, SAR11 was more abundant in the Northern Atlantic Ocean (up to 45%) than in the Southern Atlantic gyre (~25%), the biomass of Prochlorococcus peaked in the tropical Atlantic Ocean, and Bacteroidetes and Gammaproteobacteria bloomed in the nutrient-rich northern temperate waters and in the Benguela upwelling. In mesopelagic waters, higher proportions of SAR202 were present in both central gyre regions, whereas Crenarchaeota were clearly more abundant in the upwelling regions and in higher latitudes. Other phylogenetic groups such as the Planctomycetes, marine group II Euryarchaeota and the uncultured clades SAR406, SAR324 and SAR86 rarely exceeded more than 5% of relative abundance.
    Keywords: Alteromonas/Colwellia, targeted with Alt1413 oligonucleotide FISH-probe; AMT16; AMT16/1; AMT16/11; AMT16/12; AMT16/13; AMT16/14; AMT16/15; AMT16/16; AMT16/17; AMT16/18; AMT16/19; AMT16/2; AMT16/20; AMT16/21; AMT16/22; AMT16/23; AMT16/24; AMT16/25; AMT16/26; AMT16/27; AMT16/28; AMT16/29; AMT16/3; AMT16/30; AMT16/31; AMT16/32; AMT16/33; AMT16/34; AMT16/35; AMT16/37; AMT16/38; AMT16/39; AMT16/4; AMT16/40; AMT16/41; AMT16/42; AMT16/43; AMT16/45; AMT16/46; AMT16/47; AMT16/48; AMT16/49; AMT16/5; AMT16/50; AMT16/51; AMT16/52; AMT16/53; AMT16/54; AMT16/55; AMT16/56; AMT16/57; AMT16/58; AMT16/59; AMT16/6; AMT16/60; AMT16/61; AMT16/62; AMT16/63; AMT16/64; AMT16/65; AMT16/7; AMT16/8; AMT16/9; Bacteria, targed with EUB338(I-III) oligonucleotide FISH-probe; Bacteroidetes, targeted with CF319a oligonucleotide FISH-probe; Benguela Current Coastal Province; Bottle, Niskin; Catalysed reporter deposition-fluorescence in situ hybridization (CARD-FISH); Crenarchaeota marine group I, targeted with Cren554 oligonucleotide FISH-probe; D294; D294/1; D294/11; D294/12; D294/13; D294/14; D294/15; D294/16; D294/17; D294/18; D294/19; D294/2; D294/20; D294/21; D294/22; D294/23; D294/24; D294/25; D294/26; D294/27; D294/28; D294/29; D294/3; D294/30; D294/31; D294/32; D294/33; D294/34; D294/35; D294/37; D294/38; D294/39; D294/4; D294/40; D294/41; D294/42; D294/43; D294/45; D294/46; D294/47; D294/48; D294/49; D294/5; D294/50; D294/51; D294/52; D294/53; D294/54; D294/55; D294/56; D294/57; D294/58; D294/59; D294/6; D294/60; D294/61; D294/62; D294/63; D294/64; D294/65; D294/7; D294/8; D294/9; DEPTH, water; Discovery (1962); Epifluorescence microscopy after DAPI staining; Euryarchaeota marine group II, targeted with Eury806 oligonucleotide FISH-probe; Event label; Gammaproteobacteria, targeted with Gam42a oligonucleotide FISH-probe; Latitude of event; Longitude of event; NIS; North Atlantic Gyral Province; Northern Atlantic Drift; Oceanospirillum, targeted with Oce232 oligonucleotide FISH-probe; Planctomycetes, targeted with Pla46 oligonucleotide FISH-probe; Prochlorococcus, targeted with PRO405 oligonucleotide FISH-probe; Prokaryotes; Pseudoalteromonas, targeted with PSA184 oligonucleotide FISH-probe; SAR11 clade, targeted with SAR11-441 oligonucleotide FISH-probe; SAR202 clade, targeted with SAR202-312R oligonucleotide FISH-probe; SAR324 clade, targeted with SAR324-1412 oligonucleotide FISH-probe; SAR406 clade, targeted with SAR406-97 oligonucleotide FISH-probe; SAR86 clade, targeted with SAR86-1245 oligonucleotide FISH-probe; South Atlantic Gyral Province; Vibrio, targeted with GV841 oligonucleotide FISH-probe; western tropical Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 3986 data points
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Gomez-Pereira, Paola R; Fuchs, Bernhard M; Alonso, Cecilia; Oliver, Matthew J; van Beusekom, Justus; Amann, Rudolf (2010): Distinct flavobacterial communities in contrasting water masses of the North Atlantic Ocean. The ISME Journal, 4(4), 472-487, https://doi.org/10.1038/ismej.2009.142
    Publication Date: 2024-02-02
    Description: Samples were taken along a transect in the North Atlantic Ocean from 66°139.27'N; 29°136.65'W to 34°124.87'N; 28°128.90'W during the VISION cruise (diVersIty, Structure and functION) MSM03/01 on board the research vessel Maria S. Merian from September 21 to September 30, 2006. Along this transect, each station was sampled at 12 depths, from 10m down to 250m or 500m. Samples were collected with a rosette of 20-l Niskin bottles mounted on a conductivity-temperature-density profiler. Water samples for nutrients analysis were filtered directly after sampling through 0.45-µm in-line filters attached to a 60-ml pre-cleaned syringe into two 12-ml polystyrole tubes. Samples were stored at 4°C (dissolved silicate) or 80°C (ammonium, phosphate, nitrate and nitrite) The samples were spectrophotometrically measured with a continuous-flow analyzer using standard AA3 methods (Seal Analytical, Norderstedt, Germany) using a variant of the method of Grasshoff et al. (1983).
    Keywords: Ammonium; CFA; Continuous Flow Analysis; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; Latitude of event; Longitude of event; Maria S. Merian; MSM03/1; MSM03/1_902-1; MSM03/1_903-1; MSM03/1_904-1; MSM03/1_905-1; MSM03/1_906-1; MSM03/1_907-1; MSM03/1_908-1; MSM03/1_909-1; MSM03/1_910-1; MSM03/1_911-1; MSM03/1_912-1; MSM03/1_913-1; MSM03/1_914-1; MSM03/1_915-1; MSM03/1_916-1; MSM03/1_917-1; MSM03/1_918-1; MSM03/1_919-1; Nitrate; Nitrite; North Atlantic; Phosphate; Silicate; VISION
    Type: Dataset
    Format: text/tab-separated-values, 1072 data points
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  • 6
    Publication Date: 2024-02-16
    Keywords: Conductivity; CTD; CTD, Sea-Bird; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; Latitude of event; Longitude of event; Maria S. Merian; MSM03/1; MSM03/1_901-1; MSM03/1_901-2; MSM03/1_902-1; MSM03/1_902-2; MSM03/1_903-1; MSM03/1_903-2; MSM03/1_904-1; MSM03/1_904-2; MSM03/1_905-1; MSM03/1_905-2; MSM03/1_906-1; MSM03/1_906-2; MSM03/1_906-3; MSM03/1_907-1; MSM03/1_907-2; MSM03/1_908-1; MSM03/1_908-2; MSM03/1_909-1; MSM03/1_909-2; MSM03/1_910-1; MSM03/1_910-2; MSM03/1_910-3; MSM03/1_911-1; MSM03/1_911-2; MSM03/1_912-1; MSM03/1_912-2; MSM03/1_913-1; MSM03/1_913-2; MSM03/1_914-1; MSM03/1_914-2; MSM03/1_914-3; MSM03/1_915-1; MSM03/1_915-2; MSM03/1_916-1; MSM03/1_916-2; MSM03/1_917-1; MSM03/1_917-2; MSM03/1_918-1; MSM03/1_918-2; MSM03/1_918-3; MSM03/1_919-1; MSM03/1_919-2; MSM03/1_919-3; North Atlantic; Oxygen; Pressure, water; Radiation, photosynthetically active; Salinity; Sound velocity in water; Temperature, water; VISION
    Type: Dataset
    Format: text/tab-separated-values, 103546 data points
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  • 7
    Publication Date: 2013-08-01
    Print ISSN: 0034-6748
    Electronic ISSN: 1089-7623
    Topics: Electrical Engineering, Measurement and Control Technology , Physics
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  • 8
    Publication Date: 2013-09-17
    Description: Author(s): Bernhard M. Breid and James R. Anglin We develop a Hamiltonian that describes the time-dependent formation of a molecular Bose-Einstein condensate from a Bardeen-Cooper-Schrieffer state of fermionic atoms as a result of slowly sweeping through a Feshbach resonance. In contrast to many other calculations in the field, our Hamiltonian inc... [Phys. Rev. A 88, 033617] Published Mon Sep 16, 2013
    Keywords: Matter waves and collective properties of cold atoms and molecules
    Print ISSN: 1050-2947
    Electronic ISSN: 1094-1622
    Topics: Physics
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  • 9
    Publication Date: 2013-02-20
    Description: Comparable light stimulation of organic nutrient uptake by SAR11 and Prochlorococcus in the North Atlantic subtropical gyre The ISME Journal 7, 603 (March 2013). doi:10.1038/ismej.2012.126 Authors: Paola R Gómez-Pereira, Manuela Hartmann, Carolina Grob, Glen A Tarran, Adrian P Martin, Bernhard M Fuchs, David J Scanlan & Mikhail V Zubkov
    Keywords: SAR11Prochlorococcuslight stimulationflow cytometric sortingradioisotope tracingATP and amino-acid uptake
    Print ISSN: 1751-7362
    Electronic ISSN: 1751-7370
    Topics: Biology
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  • 10
    Publication Date: 2012-07-20
    Description: Journal of Proteome Research DOI: 10.1021/pr300123g
    Print ISSN: 1535-3893
    Electronic ISSN: 1535-3907
    Topics: Chemistry and Pharmacology
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