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  • 1
    Publication Date: 2023-03-14
    Keywords: Carbon, inorganic, dissolved; Carbon, organic, particulate; Carbon/Nitrogen ratio; Carbon dioxide, partial pressure; Chlorophyll a; CTD; Date/Time of event; DEPTH, water; Environment; Event label; Latitude of event; Longitude of event; LowpHOX-II; Lowphox-II_T3; Lowphox-II_T5; Nitrate; Nitrite; Nitrogen, organic, particulate; Oxygen, dissolved; pH; Phosphate; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 221 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-03-06
    Description: These data are part of the LowpHOX-2 cruise off the northern coast of Chile investigating the distribution of intact polar lipids above, through, and below the oxygen minimum zone at two stations. We report intact polar lipid concentrations in addition to a number of water column chemistry parameters. Used in a manuscript under review at Frontiers in Marine Science.
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-03-06
    Keywords: Archaeol; CTD; Date/Time of event; DEPTH, water; Diacylglyceryl carboxyhydroxymethylcholine 16:0; Diacylglyceryl carboxyhydroxymethylcholine 17:0; Diacylglyceryl carboxyhydroxymethylcholine 19:0; Diacylglyceryl carboxyhydroxymethylcholine 21:0; Diacylglyceryl carboxyhydroxymethylcholine 22:4; Diacylglyceryl carboxyhydroxymethylcholine 23:0; Diacylglyceryl carboxyhydroxymethylcholine 23:1; Diacylglyceryl carboxyhydroxymethylcholine 23:6; Diacylglyceryl carboxyhydroxymethylcholine 24:2; Diacylglyceryl carboxyhydroxymethylcholine 26:0; Diacylglyceryl carboxyhydroxymethylcholine 27:0; Diacylglyceryl carboxyhydroxymethylcholine 28:0; Diacylglyceryl carboxyhydroxymethylcholine 29:0; Diacylglyceryl carboxyhydroxymethylcholine 30:0; Diacylglyceryl carboxyhydroxymethylcholine 31:1; Diacylglyceryl carboxyhydroxymethylcholine 32:0; Diacylglyceryl carboxyhydroxymethylcholine 33:0; Diacylglyceryl carboxyhydroxymethylcholine 36:6; Diacylglyceryl carboxyhydroxymethylcholine 38:6; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 19:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 24:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 25:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 26:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 28:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 29:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 30:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 30:1; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 32:1; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 32:2; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 33:1; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 34:1; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 34:2; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 34:4; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 34:5; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 35:1; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 36:2; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 36:6; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 38:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 38:5; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 39:0; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 40:10; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 42:11; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 44:11; Diacylglyceryl hydroxymethyl-trimethyl-beta-alanine 44:12; Diacylglyceryl trimethylhomoserine 25:0; Diacylglyceryl trimethylhomoserine 26:0; Diacylglyceryl trimethylhomoserine 26:2; Diacylglyceryl trimethylhomoserine 27:0; Diacylglyceryl trimethylhomoserine 28:0; Diacylglyceryl trimethylhomoserine 28:1; Diacylglyceryl trimethylhomoserine 29:0; Diacylglyceryl trimethylhomoserine 29:1; Diacylglyceryl trimethylhomoserine 30:0; Diacylglyceryl trimethylhomoserine 30:1; Diacylglyceryl trimethylhomoserine 31:0; Diacylglyceryl trimethylhomoserine 31:1; Diacylglyceryl trimethylhomoserine 32:0; Diacylglyceryl trimethylhomoserine 32:1; Diacylglyceryl trimethylhomoserine 32:2; Diacylglyceryl trimethylhomoserine 32:3; Diacylglyceryl trimethylhomoserine 32:4; Diacylglyceryl trimethylhomoserine 33:0; Diacylglyceryl trimethylhomoserine 33:1; Diacylglyceryl trimethylhomoserine 34:0; Diacylglyceryl trimethylhomoserine 34:1; Diacylglyceryl trimethylhomoserine 34:2; Diacylglyceryl trimethylhomoserine 34:3; Diacylglyceryl trimethylhomoserine 34:4; Diacylglyceryl trimethylhomoserine 34:5; Diacylglyceryl trimethylhomoserine 34:6; Diacylglyceryl trimethylhomoserine 34:8; Diacylglyceryl trimethylhomoserine 35:0; Diacylglyceryl trimethylhomoserine 35:1; Diacylglyceryl trimethylhomoserine 36:2; Diacylglyceryl trimethylhomoserine 36:3; Diacylglyceryl trimethylhomoserine 36:4; Diacylglyceryl trimethylhomoserine 36:5; Diacylglyceryl trimethylhomoserine 36:6; Diacylglyceryl trimethylhomoserine 37:1; Diacylglyceryl trimethylhomoserine 37:2; Diacylglyceryl trimethylhomoserine 37:5; Diacylglyceryl trimethylhomoserine 37:6; Diacylglyceryl trimethylhomoserine 38:0; Diacylglyceryl trimethylhomoserine 38:1; Diacylglyceryl trimethylhomoserine 39:1; Diacylglyceryl trimethylhomoserine 40:1; Diacylglyceryl trimethylhomoserine OH-34:1; Digalactosyldiacylglycerol 28:0; Digalactosyldiacylglycerol 30:0; Digalactosyldiacylglycerol 30:2; Digalactosyldiacylglycerol 31:1; Digalactosyldiacylglycerol 32:0; Digalactosyldiacylglycerol 32:1; Digalactosyldiacylglycerol 32:2; Digalactosyldiacylglycerol 32:4; Digalactosyldiacylglycerol 32:5; Digalactosyldiacylglycerol 32:6; Digalactosyldiacylglycerol 34:0; Digalactosyldiacylglycerol 34:1; Digalactosyldiacylglycerol 34:2; Digalactosyldiacylglycerol 34:3; Digalactosyldiacylglycerol 34:4; Digalactosyldiacylglycerol 34:6; Digalactosyldiacylglycerol 34:7; Digalactosyldiacylglycerol 35:3; Digalactosyldiacylglycerol 36:0; Diglycosyl dietherglyceride 36:4; Diglycosyl dietherglyceride 37:5; Environment; Event label; Latitude of event; Longitude of event; LowpHOX-II; Lowphox-II_T3; Lowphox-II_T5; Monogalactosyldiacylglycerol 24:0; Monogalactosyldiacylglycerol 27:2; Monogalactosyldiacylglycerol 28:0; Monogalactosyldiacylglycerol 28:1; Monogalactosyldiacylglycerol 30:0; Monogalactosyldiacylglycerol 30:1; Monogalactosyldiacylglycerol 30:2; Monogalactosyldiacylglycerol 30:3; Monogalactosyldiacylglycerol 31:0; Monogalactosyldiacylglycerol 31:1; Monogalactosyldiacylglycerol 32:0; Monogalactosyldiacylglycerol 32:1; Monogalactosyldiacylglycerol 32:2; Monogalactosyldiacylglycerol 33:0; Monogalactosyldiacylglycerol 34:0; Monogalactosyldiacylglycerol 34:1; Monogalactosyldiacylglycerol 34:7; Monogalactosyldiacylglycerol 36:0; Monogalactosyldiacylglycerol 36:10; Monogalactosyldiacylglycerol 36:5; Monogalactosyldiacylglycerol 39:5; Monoglycosyl archaeol; Monoglycosyl ceramide 22:2; Monoglycosyl ceramide 25:6; Monoglycosyl ceramide 29:4; Monoglycosyl ceramide 31:4; Monoglycosyl ceramide 36:1; Monoglycosyl ceramide 37:4; Monoglycosyl ceramide 38:4; Monoglycosyl glyceroldialkylglyceroltetraether 0; Monoglycosyl glyceroldialkylglyceroltetraether 4; Monoglycosyl glyceroldialkylglyceroltetraether 5; Ornithine lipid 33:0; Ornithine lipid 33:1; Ornithine lipid 34:0; Ornithine lipid 35:1; Ornithine lipid 35:6; Ornithine lipid 36:1; Ornithine lipid 36:6; Ornithine lipid 37:1; Ornithine lipid 38:1; Ornithine lipid 38:6; Phosphatidylcholinediacylglycerol 24:0; Phosphatidylcholinediacylglycerol 26:0; Phosphatidylcholinediacylglycerol 27:0; Phosphatidylcholinediacylglycerol 28:0; Phosphatidylcholinediacylglycerol 29:0; Phosphatidylcholinediacylglycerol 29:1; Phosphatidylcholinediacylglycerol 29:2; Phosphatidylcholinediacylglycerol 30:0; Phosphatidylcholinediacylglycerol 30:1; Phosphatidylcholinediacylglycerol 30:2; Phosphatidylcholinediacylglycerol 31:0; Phosphatidylcholinediacylglycerol 31:1; Phosphatidylcholinediacylglycerol 31:2; Phosphatidylcholinediacylglycerol 32:0; Phosphatidylcholinediacylglycerol 32:1; Phosphatidylcholinediacylglycerol 32:2; Phosphatidylcholinediacylglycerol 32:6; Phosphatidylcholinediacylglycerol 33:0; Phosphatidylcholinediacylglycerol 33:1; Phosphatidylcholinediacylglycerol 33:2; Phosphatidylcholinediacylglycerol 33:5; Phosphatidylcholinediacylglycerol 33:6; Phosphatidylcholinediacylglycerol 34:1; Phosphatidylcholinediacylglycerol 34:4; Phosphatidylcholinediacylglycerol 35:0; Phosphatidylcholinediacylglycerol 35:1; Phosphatidylcholinediacylglycerol 36:1; Phosphatidylcholinediacylglycerol 36:10; Phosphatidylcholinediacylglycerol 36:3; Phosphatidylcholinediacylglycerol 36:5; Phosphatidylcholinediacylglycerol 37:6; Phosphatidylcholinediacylglycerol 38:1; Phosphatidylcholinediacylglycerol 38:2; Phosphatidylcholinediacylglycerol 38:5; Phosphatidylcholinediacylglycerol 38:6; Phosphatidylcholinediacylglycerol 39:5; Phosphatidylcholinediacylglycerol 40:10; Phosphatidylcholinediacylglycerol 40:9; Phosphatidylcholinediacylglycerol 42:0; Phosphatidylcholinediacylglycerol 42:11; Phosphatidylcholinediacylglycerol 44:12;
    Type: Dataset
    Format: text/tab-separated-values, 3223 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2022-05-26
    Description: © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Marine Science 4 (2017): 105, doi:10.3389/fmars.2017.00105.
    Description: Little is still known of the impacts of protist grazing on bacterioplankton communities in the dark ocean. Furthermore, the accuracy of assessments of in situ microbial activities, including protist grazing, can be affected by sampling artifacts introduced during sample retrieval and downstream manipulations. Potential artifacts may be increased when working with deep-sea samples or samples from chemically unique water columns such as oxygen minimum zones (OMZs). OMZs are oxygen-depleted regions in the ocean, where oxygen concentrations can drop to 〈20 μM. These regions are typically located near eastern boundary upwelling systems and currently occur in waters occupying below about 8% of total ocean surface area, representing ~1% of the ocean's volume. OMZs have a profound impact not only on the distribution of marine Metazoa, but also on the composition and activities of microbial communities at the base of marine food webs. Here we present an overview of current knowledge of protist phagotrophy below the photic zone, emphasizing studies of oxygen-depleted waters and presenting results of the first attempt to implement new technology for conducting these incubation studies completely in situ (the Microbial Sampling- Submersible Incubation Device, MS-SID). We performed 24-h incubation experiments in the Eastern Tropical South Pacific (ETSP) OMZ. This preliminary study shows that up to 28% of bacterial biomass may be consumed by protists in waters where oxygen concentrations were down to ~4.8 μM and up to 13% at a station with nitrite accumulation where oxygen concentrations were undetectable. Results also show that shipboard measurements of grazing rates were lower than rates measured from the same water using the MS-SID, suggesting that in situ experiments help to minimize artifacts that may be introduced when conducting incubation studies using waters collected from below the photic zone, particularly from oxygen-depleted regions of the water column.
    Description: This work was funded by the Agouron Institute, grant AI-M010.16.1 WHO to OU, M. Sullivan, and VE, and the Millenium Science Initiative, grant IC 120019. Ship time was provided the Chilean National Commission for Scientific and Technological Research (CONICYT) grant AUB 150006/12806.
    Keywords: OMZ ; Phagotrophy ; In situ technology ; Incubation studies ; ETSP ; Eastern Tropical South Pacific OMZ
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 5
    Publication Date: 2023-02-08
    Description: Prochlorococcus and Synechococcus are the most abundant free-living photosynthetic microorganisms in the ocean. Uncultivated lineages of these picocyanobacteria also thrive in the dimly illuminated upper part of oxygen-deficient zones (ODZs), where an important portion of ocean nitrogen (N) loss takes place via denitrification and anaerobic ammonium oxidation. Recent metagenomic studies revealed that ODZ Prochlorococcus have the genetic potential for using different N forms, including nitrate and nitrite, uncommon N sources for Prochlorococcus, but common for Synechococcus. To determine which N sources ODZ picocyanobacteria are actually using in nature, the cellular N-15 natural abundance (delta N-15) and assimilation rates of different N compounds were determined using cell sorting by flow cytometry and mass spectrometry. The natural delta N-15 of the ODZ Prochlorococcus varied from -4.0 parts per thousand to 13.0 parts per thousand (n = 9), with 50% of the values in the range of -2.1-2.6 parts per thousand. While the highest values suggest nitrate use, most observations indicate the use of nitrite, ammonium, or a mixture of N sources. Meanwhile, incubation experiments revealed potential assimilation rates of ammonium and urea in the same order of magnitude as that expected for total N in several environments including ODZs, whereas rates of nitrite and nitrate assimilation were very low. Our results thus indicate that reduced forms of N and nitrite are the dominant sources for ODZ picocyanobacteria, although nitrate might be important on some occasions. ODZ picocyanobacteria might thus represent potential competitors with anammox bacteria for ammonium and nitrite, with ammonia-oxidizing archaea for ammonium, and with nitrite-oxidizing bacteria for nitrite.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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