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  • Articles  (10)
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  • 1
    Publication Date: 2024-04-03
    Description: Marine planktonic eukaryotes play critical roles in global biogeochemical cycles and climate. However, their poor representation in culture collections limits our understanding of the evolutionary history and genomic underpinnings of planktonic ecosystems. Here, we used 280 billion Tara Oceans metagenomic reads from polar, temperate, and tropical sunlit oceans to reconstruct and manually curate more than 700 abundant and widespread eukaryotic environmental genomes ranging from 10 Mbp to 1.3 Gbp. This genomic resource covers a wide range of poorly characterized eukaryotic lineages that complement long-standing contributions from culture collections while better representing plankton in the upper layer of the oceans. We performed the first, to our knowledge, comprehensive genome-wide functional classification of abundant unicellular eukaryotic plankton, revealing four major groups connecting distantly related lineages. Neither trophic modes of plankton nor its vertical evolutionary history could completely explain the functional repertoire convergence of major eukaryotic lineages that coexisted within oceanic currents for millions of years.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
    Format: application/pdf
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Development genes and evolution 209 (1999), S. 186-197 
    ISSN: 1432-041X
    Keywords: Key words Cnidaria ; Paired class ; Paired-like ; Homeobox gene ; Evolution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract  The genes belonging to the Paired class exert primary developmental functions. They are characterized by six invariant amino acid residues in the homeodomain, while the residue at position 50 can be a serine, glutamine or lysine as in the Pax-type, Q50 Paired-like or the K50 Paired-like homeodomains respectively. Genes in this class emerged early in animal evolution: three distinct Pax genes and two Q50 Paired-like genes have recently been characterised from cnidarians. Phylogenetic molecular reconstructions taking into account homeodomain and paired-domain sequences provide some new perspectives on the evolution of the Paired-class genes. Analysis of 146 Paired-class homeodomains from a wide range of metazoan taxa allowed us to identify 18 families among the three sub-classes from which the aristaless family displays the least diverged position. Both Pax-type and K50 families branch within the Q50 Paired-like sequences implying that these are the most ancestral. Consequently, most Pax genes arose from a Paired-like ancestor, via fusion of a Paired-like homebox gene with a gene encoding only a paired domain; the Cnidaria appear to contain genes representing the ’before’ and ’after’ fusion events.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-1432
    Keywords: Key words: Planktonic foraminifera — Molecular phylogenetics — Rates of substitution — Ribosomal DNA
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract. Planktonic foraminifera are marine protists, whose calcareous shells form oceanic sediments and are widely used for stratigraphic and paleoenvironmental analyses. The fossil record of planktonic foraminifera is compared here to their molecular phylogeny inferred from ribosomal DNA sequences. Eighteen partial SSU rDNA sequences from species representing all modern planktonic families (Globigerinidae, Hastigerinidae, Globorotaliidae, Candeinidae) were obtained and compared to seven sequences representing the major groups of benthic foraminifera. The phylogenetic analyses indicate a polyphyletic origin for the planktonic foraminifera. The Candeinidae, the Globorotaliidae, and the clade Globigerinidae + Hastigerinidae seem to have originated independently, at different epochs in the evolution of foraminifera. Inference of their relationships, however, is limited by substitution rates of heterogeneity. Rates of SSU rDNA evolution vary from 4.0 × 10−9 substitutions/site/year in the Globigerinidae to less than 1.0 × 10−9 substitutions/site/year in the Globorotaliidae. These variations may be related to different levels of adaptation to the planktonic mode of life. A clock-like evolution is observed among the Globigerinidae, for which molecular and paleontological data are congruent. Phylogeny of the Globorotaliidae is clearly biased by rapid rates of substitution in two species (G. truncatulinoides and G. menardii). Our study reveals differences in absolute rates of evolution at all taxonomic levels in planktonic foraminifera and demonstrates their effect on phylogenetic reconstructions.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillan Magazines Ltd.
    Nature 405 (2000), S. 23-24 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Planktonic organisms evolve in continuous motion. Drifting passively in oceanic currents, their distributions seem to be limited mostly by changes in the temperature, nutrients and structure of the water masses in which they live. Or are they? The long distances separating species in the Arctic ...
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2013-01-01
    Description: Previous genetic studies of extant planktonic foraminifera have provided evidence that the traditional, strictly morphological definition of species in these organisms underestimates their biodiversity. Here, we report the first case where this pattern is reversed. The modern (sub)tropical species plexus Globigerinoides sacculifer is characterized by large morphological variability, which has led to the proliferation of taxonomic names attributed to morphological end-members within the plexus. In order to clarify the taxonomic status of its morphotypes and to investigate the genetic connectivity among its currently partly disjunct (sub)tropical populations, we carried out a global survey of two ribosomal RNA regions (SSU and ITS-1) in all recent morphotypes of the plexus collected throughout (sub)tropical surface waters of the global ocean. Unexpectedly, we find an extremely reduced genetic variation within the plexus and no correlation between genetic and morphological divergence, suggesting taxonomical overinterpretation. The genetic homogeneity within the morphospecies is unexpected, considering its partly disjunct range in the (sub)tropical Atlantic and Indo-Pacific and its old age (early Miocene). A sequence variant in the rapidly evolving ITS-1 region indicates the existence of an exclusively Atlantic haplotype, which suggests an episode of relatively recent (last glacial) isolation, followed by subsequent resumption of unidirectional gene flow from the Indo-Pacific into the Atlantic. This is the first example in planktonic foraminifera where the morphological variability in a morphospecies exceeds its rDNA genetic variability. Such evidence for inconsistent scaling of morphological and genetic diversity in planktonic foraminifera could complicate the interpretation of evolutionary patterns in their fossil record.
    Print ISSN: 0094-8373
    Electronic ISSN: 0094-8373
    Topics: Geosciences
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  • 6
    Publication Date: 2024-07-19
    Description: The present data set provides a tab separated text file compressed in a zip archive. The file includes metadata for each TaraOceans V9 rDNA metabarcode including the following fields:md5sum = unique identifier; lineage = taxonomic path associated to the metabarcode; pid = % identity to the closest reference barcode from V9_PR2; sequence = nucleotide sequence of the metabarcode; refs = identity of the best hit reference sequence(s); TARA_xxx = number of occurrences of this barcode in each of the 334 samples; totab = total abundance of the barcode ; cid = identifier of the OTU to which the barcode belongs; and taxogroup = high-taxonomic level assignation of this barcode. The file also includes three categories of functional annotations: (1) Chloroplast: yes, presence of permanent chloroplast; no, absence of permanent chloroplast ; NA, undetermined. (2) Symbiont (small partner): parasite, the species is a parasite; commensal, the species is a commensal; mutualist, the species is a mutualist symbiont, most often a microalgal taxon involved in photosymbiosis; no the species is not involved in a symbiosis as small partner; NA, undetermined. (3) Symbiont (host): photo, the host species relies on a mutualistic microalgal photosymbiont to survive (obligatory photosymbiosis); photo_falc, same as photo, but facultative relationship; photo_klep, the host species maintains chloroplasts from microalgal prey(s) to survive; photo_klep_falc, same as photo_klep, but facultative; Nfix, the host species must interact with a mutualistic symbiont providing N2 fixation to survive; Nfix_falc, same as Nfix, but facultative; no, the species is not involved in any mutualistic symbioses; NA, undetermined. For example, the collodarian/Brandtodinium symbiosis is annotated: Chloroplast, "no"; Symbiont (small), "no"; Symbiont (host), "photo", for the collodarian host; and: Chloroplast, "yes"; Symbiont (small), "mutualist"; Symbiont (host), "no", for the dinoflagellate microalgal endosymbiont.chloroplast = "yes", "no" or "NA"; symbiont.small = "parasite", "commensal", "mutualist", "no" or "NA"; symbiont.host = "photo", "photo_falc", "photo_klep", "Nfix", no or NA; benef = "Nfix", "no" or "NA"; trophism = Metazoa , heterotroph , NA , photosymbiosis , phototroph according to the previous fields.
    Keywords: Fondation Tara Expeditions; FondTara; Tara_Oceans_2009-2013; Tara Oceans Expedition
    Type: dataset
    Format: application/zip, 710.6 MBytes
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  • 7
    Publication Date: 2024-07-19
    Description: The Tara Pacific expedition (2016-2018) sampled coral ecosystems around 32 islands in the Pacific Ocean, and sampled the surface of oceanic waters at 249 locations, resulting in the collection of nearly 58,000 samples. The expedition was designed to systematically study corals, fish, plankton, and seawater, and included the collection of samples for advanced biogeochemical, molecular, and imaging analysis. Here we provide the continuous dataset originating from backscattering sensor [BB3] (WETLabs ECO-BB3) instruments acquiring continuously during the full course of the campaign. Surface seawater was pumped continuously through a hull inlet located 1.5 m under the waterline using a membrane pump (10 LPM; Shurflo), circulated through a vortex debubbler, a flow meter, and distributed to a number of flow-through instruments. The backscattering sensor [BB3] (WETLabs ECO-BB3) was added to the underway system to measure the volume scattering function [VSF] at 124° and 3 wavelengths (470, 532, 650 nm). The flow was automatically directed through a 0.2 µm filter for 10 minutes every hour before being circulated through the [BB3] allowing the calculation of particulate backscattering [bbp] by removing the signal due to dissolved matter, drift, and biofouling (Slade et al. 2010, doi:10.1175/2010JTECHO755.1). The particulate organic carbon concentration [poc] was estimated by applying an empirical relation between measured [poc] and [bbp] (Cetinić et al. 2012, doi:10.1175/2010JTECHO755.1). Phytoplankton organic carbon [cphyto] was estimated by an empirical relationship with [bbp] (Graff et al. 2015, doi:10.1016/j.dsr.2015.04.006).
    Keywords: According to Cetinić et al. (2012); According to Graff et al. (2015); Backscatter; Backscattering coefficient of particles, 470 nm; Backscattering coefficient of particles, 532 nm; Backscattering coefficient of particles, 650 nm; Carbon, organic, particulate; CTD, Sea-Bird; measured with Thermosalinograph (TSG) sensor; DATE/TIME; Fondation Tara Expeditions; FondTara; LATITUDE; LONGITUDE; Number; Pacific Ocean; Phytoplankton, biomass as carbon; phytoplankton carbon; POC; Salinity; Spectral backscattering sensor (WET Labs, Eco-bb3); SV Tara; TARA_2016-2018; Tara_Pacific; TARA_PACIFIC_2016-2018; Tara Pacific Expedition; Temperature, water; UMS; Underway, multiple sensors; Volume scattering function at 124°, 470 nm; Volume scattering function at 124°, 470 nm, standard deviation; Volume scattering function at 124°, 532 nm; Volume scattering function at 124°, 532 nm, standard deviation; Volume scattering function at 124°, 650 nm; Volume scattering function at 124°, 650 nm, standard deviation
    Type: dataset
    Format: text/tab-separated-values, 6020692 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-07-19
    Description: The Tara Pacific expedition (2016-2018) sampled coral ecosystems around 32 islands in the Pacific Ocean, and sampled the surface of oceanic waters at 249 locations, resulting in the collection of nearly 58,000 samples. The expedition was designed to systematically study corals, fish, plankton, and seawater, and included the collection of samples for advanced biogeochemical, molecular, and imaging analysis. Here we provide the continuous dataset originating from navigation and meteorological instruments acquiring continuously during the full course of the campaign.
    Keywords: Course; DATE/TIME; Humidity, relative; LATITUDE; LONGITUDE; meteorological data; Navigation; Navigation and meteorological acquiring during the full course of the campaign; Pacific Ocean; position; Pressure, atmospheric; Solar azimuth angle; Solar zenith angle; Speed; SV Tara; TARA_2016-2018; Tara_Pacific; TARA_PACIFIC_2016-2018; Tara Pacific Expedition; Temperature, air; Temperature, water; UMS; Underway, multiple sensors; Validation flag/comment; Wind apparent direction, reference angle, bow; Wind apparent direction, reference angle, north; Wind apparent speed; Wind direction, true; Wind speed, true
    Type: dataset
    Format: text/tab-separated-values, 10873547 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-07-19
    Description: The Tara Pacific expedition (2016-2018) sampled coral ecosystems around 32 islands in the Pacific Ocean, and sampled the surface of oceanic waters at 249 locations, resulting in the collection of nearly 58,000 samples. The expedition was designed to systematically study corals, fish, plankton, and seawater, and included the collection of samples for advanced biogeochemical, molecular, and imaging analysis. Here we provide the continuous dataset originating from scanning mobility particle sizer ([SMPS], SMPS-C GRIMM Aerosol Technik Ainring GmbH & Co. KG, Ainring, Germany) instruments acquiring continuously during the full course of the campaign. Aerosols pumped through one of the ([MAST-PUMP]) inlets were channeled through a conductive tubing of 1.9 cm inner diameter to four parallel 47mm filter holders installed in the rear hold using a vacuum pump (Diaphragm pumpME16 NT, VACUUBRAND BmbH & Co KG, Wertheim, Germany) at a minimum flow rate of 30 lpm (20lpm prior to may 2016). Air was conducted to a scanning mobility particle sizer ([SMPS], SMPS-C GRIMM Aerosol Technik Ainring GmbH & Co. KG, Ainring, Germany) measuring particles in the size range 0.025 – 0.70 µm. The SMPS was set to perform a full scan of particle distribution every 5 min. Data from [SMPS] are averaged at the 30 minute scale and provided both at the scale of particle concentration (nb cm-3) together with its normalized size distribution (dN/dlogDp (nb cm-3) i.e., the concentration divided by the log of the width of the bin).
    Keywords: aerosols; DATE/TIME; Fondation Tara Expeditions; FondTara; LATITUDE; Log-normal particle size distribution, normalized concentration at particle diameter 101.82 nm; Log-normal particle size distribution, normalized concentration at particle diameter 101.82 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 105.54 nm; Log-normal particle size distribution, normalized concentration at particle diameter 105.54 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 109.41 nm; Log-normal particle size distribution, normalized concentration at particle diameter 109.41 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 113.42 nm; Log-normal particle size distribution, normalized concentration at particle diameter 113.42 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 117.57 nm; Log-normal particle size distribution, normalized concentration at particle diameter 117.57 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 121.88 nm; Log-normal particle size distribution, normalized concentration at particle diameter 121.88 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 126.35 nm; Log-normal particle size distribution, normalized concentration at particle diameter 126.35 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 130.97 nm; Log-normal particle size distribution, normalized concentration at particle diameter 130.97 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 135.77 nm; Log-normal particle size distribution, normalized concentration at particle diameter 135.77 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 140.75 nm; Log-normal particle size distribution, normalized concentration at particle diameter 140.75 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 145.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 145.9 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 151.25 nm; Log-normal particle size distribution, normalized concentration at particle diameter 151.25 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 156.79 nm; Log-normal particle size distribution, normalized concentration at particle diameter 156.79 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 162.53 nm; Log-normal particle size distribution, normalized concentration at particle diameter 162.53 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 168.49 nm; Log-normal particle size distribution, normalized concentration at particle diameter 168.49 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 174.66 nm; Log-normal particle size distribution, normalized concentration at particle diameter 174.66 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 181.06 nm; Log-normal particle size distribution, normalized concentration at particle diameter 181.06 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 187.69 nm; Log-normal particle size distribution, normalized concentration at particle diameter 187.69 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 194.56 nm; Log-normal particle size distribution, normalized concentration at particle diameter 194.56 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 201.69 nm; Log-normal particle size distribution, normalized concentration at particle diameter 201.69 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 209.08 nm; Log-normal particle size distribution, normalized concentration at particle diameter 209.08 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 216.74 nm; Log-normal particle size distribution, normalized concentration at particle diameter 216.74 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 224.68 nm; Log-normal particle size distribution, normalized concentration at particle diameter 224.68 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 232.91 nm; Log-normal particle size distribution, normalized concentration at particle diameter 232.91 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 241.44 nm; Log-normal particle size distribution, normalized concentration at particle diameter 241.44 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 25.03 nm; Log-normal particle size distribution, normalized concentration at particle diameter 25.03 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 25.95 nm; Log-normal particle size distribution, normalized concentration at particle diameter 25.95 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 250.29 nm; Log-normal particle size distribution, normalized concentration at particle diameter 250.29 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 259.46 nm; Log-normal particle size distribution, normalized concentration at particle diameter 259.46 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 26.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 26.9 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 268.96 nm; Log-normal particle size distribution, normalized concentration at particle diameter 268.96 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 27.88 nm; Log-normal particle size distribution, normalized concentration at particle diameter 27.88 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 278.81 nm; Log-normal particle size distribution, normalized concentration at particle diameter 278.81 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 28.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 28.9 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 289.03 nm; Log-normal particle size distribution, normalized concentration at particle diameter 289.03 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 29.96 nm; Log-normal particle size distribution, normalized concentration at particle diameter 29.96 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 299.61 nm; Log-normal particle size distribution, normalized concentration at particle diameter 299.61 nm, standard deviation; Log-normal particle size distribution, normalized concentration at particle diameter 31.06 nm; Log-
    Type: dataset
    Format: text/tab-separated-values, 2410457 data points
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  • 10
    Publication Date: 2024-07-19
    Description: The Tara Pacific expedition (2016-2018) sampled coral ecosystems around 32 islands in the Pacific Ocean, and sampled the surface of oceanic waters at 249 locations, resulting in the collection of nearly 58,000 samples. The expedition was designed to systematically study corals, fish, plankton, and seawater, and included the collection of samples for advanced biogeochemical, molecular, and imaging analysis. Here we provide the dataset obtained with a small CTD probe (Castaway CTD) deployed from the dinghy down to the reef (generally ~5 to 10m) to record temperature and conductivity profiles.
    Keywords: Binary Object; BOAT-PIPE; Conductivity; DATE/TIME; Device type; Distance; DOLPHIN-CARBOY; DOLPHIN-CARTRIDGE-300; DOLPHIN-DECKNET-20; DOLPHIN-UBAT; Event label; EXP; Experiment; Fondation Tara Expeditions; FondTara; HANDHELD-BOW-POLE; HANDHELD-BUCKET; HANDHELD-CTD; HANDHELD-MICROTOPS; HANDHELD-NISKIN; HANDHELD-SIMBADA; HSN-NET-20; HSN-NET-300; INLINE-PUMP; INSITU-UBAT; LATITUDE; LONGITUDE; MANTA-NET-300; MAST-PUMP; OA000-I00-S00; OA000-I01-S01; OA000-I01-S02; OA000-I01-S03; OA000-I02-S01; OA000-I02-S02; OA000-I02-S03; OA000-I03-S00; OA000-I03-S01; OA000-I03-S02; OA000-I04-S00; OA000-I04-S01; OA000-I04-S02; OA000-I04-S03; OA000-I04-S04; OA000-I05-S00; OA000-I05-S01; OA000-I05-S02; OA000-I05-S03; OA000-I05-S04; OA000-I06-S01; OA000-I06-S02; OA000-I06-S03; OA000-I06-S04; OA000-I07-S00; OA000-I07-S01; OA000-I07-S02; OA000-I07-S03; OA000-I07-S04; OA000-I08-S00; OA000-I08-S01; OA000-I08-S02; OA000-I08-S03; OA000-I09-S00; OA000-I09-S01; OA000-I09-S02; OA000-I09-S03; OA000-I10-S00; OA000-I10-S01; OA000-I10-S02; OA000-I10-S03; OA000-I10-S04; OA000-I10-S05; OA000-I11-S00; OA000-I11-S01; OA000-I11-S02; OA000-I11-S03; OA000-I12-S00; OA000-I12-S01; OA000-I12-S02; OA000-I12-S03; OA000-I12-S04; OA000-I13-S00; OA000-I13-S01; OA000-I13-S02; OA000-I13-S03; OA000-I13-S04; OA000-I14-S00; OA000-I14-S01; OA000-I14-S02; OA000-I14-S03; OA000-I15-S00; OA000-I15-S01; OA000-I15-S02; OA000-I15-S03; OA000-I16-S00; OA000-I16-S01; OA000-I16-S02; OA000-I16-S03; OA000-I17-S01; OA000-I17-S02; OA000-I17-S03; OA000-I18-S00; OA000-I18-S01; OA000-I18-S02; OA000-I18-S03; OA000-I19-S00; OA000-I19-S01; OA000-I19-S02; OA000-I19-S03; OA000-I19-S04; OA000-I20-S00; OA000-I20-S01; OA000-I20-S02; OA000-I20-S03; OA000-I21-S00; OA000-I21-S01; OA000-I21-S02; OA000-I21-S03; OA000-I22-S00; OA000-I22-S01; OA000-I22-S02; OA000-I22-S03; OA000-I23-S00; OA000-I23-S01; OA000-I23-S02; OA000-I23-S03; OA000-I23-S11; OA000-I23-S12; OA000-I23-S13; OA000-I23-S14; OA000-I23-S15; OA000-I23-S16; OA000-I23-S21; OA000-I23-S22; OA000-I23-S23; OA000-I23-S24; OA000-I23-S25; OA000-I23-S26; OA000-I23-S31; OA000-I23-S32; OA000-I23-S33; OA000-I23-S34; OA000-I23-S35; OA000-I23-S36; OA000-I24-S00; OA000-I24-S01; OA000-I24-S02; OA000-I24-S03; OA000-I24-S04; OA000-I25-S00; OA000-I25-S01; OA000-I25-S02; OA000-I25-S03; OA000-I25-S04; OA000-I25-S05; OA000-I26-S00; OA000-I26-S01; OA000-I26-S02; OA000-I26-S03; OA000-I26-S04; OA000-I27-S00; OA000-I27-S01; OA000-I27-S02; OA000-I28-S00; OA000-I28-S01; OA000-I28-S02; OA000-I28-S03; OA000-I29-S00; OA000-I29-S01; OA000-I29-S02; OA000-I29-S03; OA000-I30-S00; OA000-I30-S01; OA000-I30-S02; OA000-I30-S03; OA000-I30-S04; OA000-I31-S00; OA000-I31-S01; OA000-I31-S02; OA000-I31-S03; OA000-I31-S04; OA000-I32-S00; OA000-I32-S01; OA000-I32-S02; OA000-I32-S03; OA000-I32-S04; OA000-I32-S05; OA000-TS2-FA1; OA000-TS2-FA2; OA000-TS2-FA3; OA000-TS2-HI1; OA000-TS2-HI2; OA000-TS2-KA1; OA000-TS2-KA2; OA000-TS2-KA3; OA000-TS2-MA1; OA000-TS2-MA2; OA000-TS2-MA3; OA000-TS2-MT1; OA000-TS2-MT2; OA000-TS2-MT3; OA000-TS2-MT4; OA000-TS2-S11; OA000-TS2-S12; OA000-TS2-S21; OA000-TS2-S22; OA000-TS2-S23; OA000-TS2-S24; OA000-TS2-S31; OA000-TS2-S33; OA000-TS2-S41; OA000-TS2-S42; OA000-TS2-S43; OA000-TS2-S51; OA000-TS2-S52; OA000-TS2-S53; OA000-TS2-S54; OA000-TS2-S61; OA000-TS2-S62; OA000-TS2-TA1; OA000-TS2-TA2; OA000-TS2-TA3; OA000-TS3-S99; OA000-TS4-S00; OA000-TS4-S03; OA000-TS4-S12; OA000-TS4-S15; OA000-TS4-S17; OA000-TS4-S18; OA000-TS4-S20; OA000-TS5-S00; OA000-TS5-S11; OA000-TS5-S12; OA000-TS5-S21; OA000-TS5-S22; OA000-TS5-S31; OA000-TS5-S41; OA000-TS5-S51; OA000-TS6-S00; OA000-TS6-S11; OA000-TS6-S12; OA000-TS6-S21; OA000-TS6-S22; OA000-TS7-P01; OA000-TS7-P02; OA000-TS7-P03; OA000-TS7-P04; OA000-TS7-P05; OA000-TS7-P06; OA000-TS7-P07; OA000-TS7-P08; OA000-TS7-P09; OA000-TS7-S00; OA000-TS9-S00; OA000-TS9-S1A; OA000-TS9-S1C; OA000-TS9-S2A; OA000-TS9-S2C; OA000-TS9-S3C; OA000-TS9-S99; OA001-I00-S00; OA002-I00-S00; OA003-I00-S00; OA004-I00-S00; OA005-I00-S00; OA006-I00-S00; OA007-I00-S00; OA008-I00-S00; OA009-I00-S00; OA010-I00-S00; OA011-I00-S00; OA012-I00-S00; OA013-I00-S00; OA014-I00-S00; OA015-I00-S00; OA016-I00-S00; OA017-I00-S00; OA018-I00-S00; OA019-I00-S00; OA020-I00-S00; OA021-I00-S00; OA022-I00-S00; OA023-I00-S00; OA024-I00-S00; OA025-I00-S00; OA026-I00-S00; OA027-I00-S00; OA028-I00-S00; OA029-I03-S00; OA030-I03-S00; OA031-I00-S00; OA032-I00-S00; OA033-I00-S00; OA034-I00-S00; OA035-I00-S00; OA036-I00-S00; OA037-I00-S00; OA038-I00-S00; OA039-I00-S00; OA040-I00-S00; OA041-I04-S00; OA042-I04-S00; OA043-I04-S00; OA044-I04-S00; OA045-I00-S00; OA046-I00-S00; OA047-I00-S00; OA048-I05-S00; OA048-I05-S01; OA049-I05-S00; OA050-I05-S00; OA051-I00-S00; OA052-I00-S00; OA053-I06-S00; OA054-I06-S00; OA055-I06-S00; OA056-I00-S00; OA057-I00-S00; OA058-I00-S00; OA059-I07-S00; OA060-I07-S00; OA061-I07-S00; OA062-I00-S00; OA063-I08-S00; OA063-I08-S01; OA064-I08-S00; OA065-I00-S00; OA066-I09-S00; OA067-I09-S00; OA068-I10-S00; OA069-I10-S00; OA070-I10-S00; OA071-I10-S00; OA072-I11-S00; OA073-I11-S00; OA074-I11-S00; OA075-I12-S00; OA076-I12-S00; OA076-I12-S01; OA077-I12-S00; OA078-I00-S00; OA079-I00-S00; OA080-I13-S00; OA081-I13-S00; OA082-I13-S00; OA083-I13-S00; OA084-I00-S00; OA085-I00-S00; OA086-I00-S00; OA087-I00-S00; OA088-I00-S00; OA089-I14-S00; OA090-I14-S00; OA091-I14-S00; OA092-I15-S00; OA093-I15-S00; OA094-I00-S00; OA095-I00-S00; OA095-I16-S00; OA096-I00-S00; OA097-I00-S00; OA098-I00-S00; OA099-I00-S00; OA100-I00-S00; OA101-I00-S00; OA102-I00-S00; OA103-I00-S00; OA104-I00-S00; OA105-I00-S00; OA106-I00-S00; OA107-I00-S00; OA108-I00-S00; OA109-I00-S00; OA110-I00-S00; OA111-I00-S00; OA112-I00-S00; OA113-I00-S00; OA114-I00-S00; OA115-I00-S00; OA116-I00-S00; OA117-I00-S00; OA118-I00-S00; OA119-I00-S00; OA120-I00-S00; OA121-I00-S00; OA122-I00-S00; OA123-I00-S00; OA124-I00-S00; OA125-I00-S00; OA126-I00-S00; OA127-I18-S00; OA128-I18-S00; OA129-I18-S00; OA130-I18-S00; OA131-I00-S00; OA132-I00-S00; OA133-I00-S00; OA134-I00-S00; OA135-I00-S00; OA136-I00-S00; OA137-I00-S00; OA138-I00-S00; OA139-I00-S00; OA140-I19-S00; OA141-I19-S00; OA142-I19-S00; OA143-I19-S00; OA144-I00-S00; OA145-I00-S00; OA145-I20-S00; OA146-I20-S00; OA147-I00-S00; OA148-I21-S00; OA149-I21-S00; OA150-I00-S00; OA151-I00-S00; OA152-I00-S00; OA153-I00-S00; OA154-I00-S00; OA155-I22-S00; OA156-I23-S00; OA157-I23-S00; OA158-I23-S00; OA159-I23-S00; OA160-I24-S00; OA161-I24-S00; OA162-I24-S00; OA163-I00-S00; OA164-I00-S00; OA165-I00-S00; OA166-I25-S00; OA167-I26-S00; OA168-I26-S00; OA169-I00-S00; OA170-I27-S00; OA171-I27-S00; OA172-I28-S00; OA173-I00-S00; OA174-I00-S00; OA175-I00-S00; OA176-I00-S00; OA177-I00-S00; OA178-I00-S00; OA179-I00-S00; OA180-I00-S00; OA181-I00-S00; OA182-I00-S00; OA183-I00-S00; OA184-I00-S00; OA185-I00-S00; OA186-I00-S00; OA187-I00-S00; OA188-I00-S00; OA189-I00-S00; OA190-I29-S00; OA191-I29-S00; OA192-I00-S00; OA193-I00-S00; OA194-I00-S00; OA195-I00-S00; OA196-I00-S00; OA197-I00-S00; OA198-I00-S00; OA199-I00-S00; OA200-I00-S00; OA201-I00-S00; OA202-I00-S00; OA203-I00-S00; OA204-I00-S00; OA205-I00-S00; OA206-I00-S00; OA207-I00-S00; OA208-I00-S00; OA209-I00-S00; OA210-I00-S00; OA211-I00-S00; OA212-I00-S00; OA213-I00-S00; OA214-I00-S00; OA216-I30-S00; OA217-I00-S00; OA218-I00-S00; OA220-I31-S00; OA221-I31-S00; OA222-I00-S00; OA223-I00-S00; OA224-I00-S00; OA225-I00-S00; OA226-I00-S00; OA227-I00-S00; OA228-I00-S00; OA229-I00-S00; OA230-I32-S00; OA232-I32-S00; OA233-I00-S00; OA234-I00-S00; OA235-I00-S00; OA236-I00-S00; OA237-I00-S00; OA238-I00-S00; OA239-I00-S00; OA240-I00-S00; OA241-I00-S00; OA242-I00-S00; OA243-I00-S00; OA244-I00-S00; OA245-I00-S00; OA246-I00-S00; OA247-I00-S00; OA249-I00-S00; Pacific; Reference/source; Salinity; Sample code/label; Sample comment; Sampling date; SCUBA-3X10; SCUBA-CORER; SCUBA-NET-20; SCUBA-PUMP; SCUBA-SURVEY; SNORKLE-SPEAR; Speed; stanopump-UBAT; SV Tara; TARA_20160528T1915Z_ND_O-ATM_MAST-PUMP; TARA_20160529T0725Z_D_O-SRF_HSN-NET-300; TARA_20160529T1513Z_D_O-SRF_DOLPHIN-CARBOY; TARA_20160529T1543Z_D_O-SRF_DOLPHIN-
    Type: dataset
    Format: text/tab-separated-values, 75470 data points
    Location Call Number Limitation Availability
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