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  • 2015-2019  (1,530,547)
  • 1985-1989  (12)
  • 1980-1984  (12)
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  • 2015  (742,578)
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  • 1
    Publication Date: 2024-07-06
    Keywords: DATE/TIME; DEPTH, sediment/rock; GCUWI; Gravity corer, UWITEC; Grevelingen Lake, Netherlands; Porosity; Scharendijke_Site
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-07-06
    Description: The Ocean Sampling Day (OSD) is a simultaneous sampling campaign of the world's oceans which took place (for the first time) on the summer solstice (June 21st) in the year 2014. These cumulative samples, related in time, space and environmental parameters, provide insights into fundamental rules describing microbial diversity and function and contribute to the blue economy through the identification of novel, ocean-derived biotechnologies. We see OSD data as a reference data set for generations of experiments to follow in the coming decade. The present data set includes a description of each sample collected during the Ocean Sampling Day 2014 and provides contextual environmental data measured concurrently with the collection of water samples for genomic analyses.
    Keywords: [BUCKET-10]; [BUCKET-20]; [BUCKET-40]; [BUCKET-5]; [HVP-PUMP]; Accession number, genetics; Ammonium; Bacteria, production as carbon; Biogeographical province; Biome; BOT; BOT_10L; BOT_20L; BOT_2L; BOT_4L; BOT_5L; Bottle, Kemmerer; Bottle, Nalgene 10-L; Bottle, Nalgene 4-L; Bottle, Nalgene 5-L; Bottle, Nansen; Bottle, Niskin; Bottle, Niskin 1.6-L; Bottle, Niskin 10-L; Bottle, Niskin 12-L; Bottle, Niskin 20-L; Bottle, Niskin 2-L; Bottle, Niskin 30-L; Bottle, Niskin 3-L; Bottle, Niskin 5-L; Bottle, Niskin 8-L; Bottle, Ruttner; Bottle, unknown; Bottle, unknown 10-L; Bottle, unknown 20-L; Bottle, unknown 2-L; Bottle, unknown 4-L; Bottle, unknown 5-L; Bottle, Van Dorn; Bottle, Van Dorn 2.2-L; Bucket, plastic; Bucket, plastic 10-L; Bucket, plastic 20-L; Bucket, plastic 40-L; Bucket, plastic 5-L; Campaign of event; Carbon, organic, dissolved; Carbon, organic, particulate; Chlorophyll a; Comment of event; Conductivity; Country; CTD/Rosette; CTD-RO; Date/Time of event; Date/Time of event 2; DEPTH, water; Environmental feature; Event label; Fluorometer; Geographic name/locality; High Volume Peristaltic Pump; HORIZON; Horizontal water sampler; IHO General Sea Areas (1953) registered at www.marineregions.org; KEM; Large Marine ecosystem; Latitude of event; Latitude of event 2; LIMNOS water sampler; LIMNOSWS; Local Time; Longhurst (2007) registered at marineregions.org; Longitude of event; Longitude of event 2; Material; Method/Device of event; MicroB3; MicroB3 - Microbial Biodiversity, Bioinformatics and Biotechnology; NAS; NB_10L; NB_4L; NB_5L; NIS; NIS_1.6L; NIS_10L; NIS_12L; NIS_20L; NIS_2L; NIS_30L; NIS_3L; NIS_5L; NIS_8L; Nitrate; Nitrite; Nitrogen, organic, dissolved; Nitrogen, organic, particulate; OSD1_20140621T1110Z; OSD10_20140621T2050Z; OSD100_20140622T0800Z; OSD101_20140621T1105Z; OSD102_20140621T1200Z; OSD103_20140621T1015Z; OSD105_20140621T1839Z; OSD106_20140620T1100Z; OSD106_20140620T1130Z; OSD107_20140620T0950Z; OSD108_20140620T1140Z; OSD109_20140620T1100Z; OSD11_20140617T1503Z; OSD110_20140621T1030Z; OSD111_20140621T0830Z; OSD113_20140621T1125Z; OSD114_20140621T1005Z; OSD115_20140621T1430Z; OSD116_20140621T1330Z; OSD117_20140621T1610Z; OSD118_20140621T1214Z; OSD119_20140621T1800Z; OSD120_20140621T1813Z; OSD121_20140621T1759Z; OSD122_20140622T0745Z; OSD123_20140622T0900Z; OSD124_20140621T0325Z; OSD125_20140621T1300Z; OSD126_20140621T1215Z; OSD127_20140621T1143Z; OSD128_20140621T1705Z; OSD129_20140621T1638Z; OSD13_20140621T0630Z; OSD130_20140621T1141Z; OSD131_20140621T0824Z; OSD132_20140622T0845Z; OSD133_20140621T0724Z; OSD135_20140621T0303Z; OSD136_20140621T1056Z; OSD137_20140621T1401Z; OSD14_20140623T0805Z; OSD141_20140620T0845Z; OSD142_20140621T1500Z; OSD143_20140621T1845Z; OSD143_20140621T1900Z; OSD144_20140624T0608Z; OSD145_20140621T1045Z; OSD146_20140621T0542Z; OSD147_20140621T0533Z; OSD148_20140621T0845Z; OSD149_20140621T1440Z; OSD15_20140621T0730Z; OSD150_20140621T1500Z; OSD151_20140621T1430Z; OSD152_20140620T1554Z; OSD152_20140620T1610Z; OSD152_20140620T1630Z; OSD152_20140620T1650Z; OSD153_20140621T1015Z; OSD154_20140620T1120Z; OSD155_20140621T0700Z; OSD156_20140621T1000Z; OSD157_20140620T0900Z; OSD158_20140621T1120Z; OSD159_20140621T1000Z; OSD162_20140623T1100Z; OSD163_20140620T1200Z; OSD164_20140613T1000Z; OSD165_20140623T0900Z; OSD166_20140621T0948Z; OSD167_20140621T1415Z; OSD168_20140621T0915Z; OSD169_20140621T1149Z; OSD17_20140620T0700Z; OSD170_20140625T0504Z; OSD171_20140625T0423Z; OSD172_20140625T0245Z; OSD173_20140625T0139Z; OSD174_20140625T0047Z; OSD175_20140624T1313Z; OSD176_20140624T1127Z; OSD177_20140624T1035Z; OSD178_20140624T2320Z; OSD18_20140620T0800Z; OSD182_20140624T1316Z; OSD183_20140624T2158Z; OSD184_20140624T1806Z; OSD185_20140624T1434Z; OSD186_20140621T1704Z; OSD188_20140624T2148Z; OSD189_20140624T1605Z; OSD19_20140623T0730Z; OSD190_20140713T0722Z; OSD191_20140702T1433Z; OSD2_20140620T1126Z; OSD20_20140620T1030Z; OSD21_20140621T1055Z; OSD22_20140623T0800Z; OSD24_20140621T1230Z; OSD25_20140621T0900Z; OSD26_20140621T1245Z; OSD28_20140621T0415Z; OSD29_20140621T1500Z; OSD3_20140620T0540Z; OSD30_20140620T0815Z; OSD31_20140612T1120Z; OSD32_20140623T1520Z; OSD33_20140619T1535Z; OSD34_20140621T0930Z; OSD35_20140621T1701Z; OSD36_20140621T1730Z; OSD37_20140619T1311Z; OSD38_20140620T1655Z; OSD39_20140619T0500Z; OSD4_20140620T0900Z; OSD41_20140621T1840Z; OSD42_20140621T1000Z; OSD43_20140621T1849Z; OSD45_20140622T2130Z; OSD46_20140621T2000Z; OSD47_20140621T1256Z; OSD48_20140621T0950Z; OSD49_20140621T0930Z; OSD5_20140619T0515Z; OSD5_20140619T1100Z; OSD50_20140620T0709Z; OSD51_20140621T1556Z; OSD52_20140621T1007Z; OSD53_20140621T0843Z; OSD54_20140621T1545Z; OSD55_20140621T1630Z; OSD56_20140624T0720Z; OSD57_20140624T0738Z; OSD58_20140621T1530Z; OSD6_20140621T0930Z; OSD60_20140619T1545Z; OSD61_20140621T2108Z; OSD62_20140621T1000Z; OSD63_20140620T1130Z; OSD64_20140621T0930Z; OSD65_20140620T2230Z; OSD69_20140621T1508Z; OSD7_20140621T2000Z; OSD70_20140621T1111Z; OSD71_20140621T2335Z; OSD72_20140621T0912Z; OSD73_20140621T1115Z; OSD74_20140621T1115Z; OSD76_20140620T0915Z; OSD77_20140620T1100Z; OSD78_20140621T0900Z; OSD80_20140621T1730Z; OSD80_20140621T1830Z; OSD80_20140621T1930Z; OSD81_20140621T1058Z; OSD87_20140621T1107Z; OSD9_20140618T0418Z; OSD90_20140621T0800Z; OSD91_20140621T1100Z; OSD92_20140621T1100Z; OSD93_20140621T1100Z; OSD94_20140621T0930Z; OSD95_20140621T0825Z; OSD96_20140621T1250Z; OSD97_20140621T1235Z; OSD98_20140621T1240Z; OSD99_20140621T1024Z; OSD-Jun-2014; Oxygen; pH; Phosphate; Plankton abundance; Primary production of carbon; published at the European Nucleotides Archive; PUMP; Radiation, photosynthetically active; registered at the European Nucleotides Archive (ENA); RWS; Salinity; Sample code/label; Sample ID; Sample method; Silicate; Site; Temperature, water; terms registered at EnvO, the Environmental Ontology; Time zone; Turbidity (Formazin Turbidity Unit); Uniform resource locator/link to reference; URI of event; VDB; VDB_2.2L; Water pump; WB
    Type: Dataset
    Format: text/tab-separated-values, 7078 data points
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2024-07-06
    Keywords: DEPTH, sediment/rock; GEMAX; GNC_X; Gulf of Bothnia, Baltic sea; Hydrogen sulfide; Iron 2+; Methane; Sulfate; US5B; δ13C, methane; δ Deuterium, methane
    Type: Dataset
    Format: text/tab-separated-values, 170 data points
    Location Call Number Expected Availability
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  • 4
    Publication Date: 2024-07-06
    Keywords: Acid volatile sulfides; Chromium reducible sulfur; DEPTH, sediment/rock; GEMAX; GNC_X; Gulf of Bothnia, Baltic sea; Iron; Iron, total; Iron/Aluminium ratio; Porosity; Sulfur, total; US5B
    Type: Dataset
    Format: text/tab-separated-values, 309 data points
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2024-07-06
    Keywords: Acid volatile sulfides; Chromium reducible sulfides; DATE/TIME; DEPTH, sediment/rock; GCUWI; Gravity corer, UWITEC; Grevelingen Lake, Netherlands; Iron; Iron, total; Iron oxides; Molybdenum; Sample comment; Scharendijke_Site; Sulfur, total; Thorium-232
    Type: Dataset
    Format: text/tab-separated-values, 1364 data points
    Location Call Number Expected Availability
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  • 6
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    PANGAEA
    In:  Supplement to: Yang, Yan; Hansson, L; Gattuso, Jean-Pierre (2016): Data compilation on the biological response to ocean acidification: an update. Earth System Science Data, 8(1), 79-87, https://doi.org/10.5194/essd-8-79-2016
    Publication Date: 2024-07-06
    Description: The exponential growth of studies on the biological response to ocean acidification over the last few decades has generated a large amount of data. To facilitate data comparison, a data compilation hosted at the data publisher PANGAEA was initiated in 2008 and is updated on a regular basis (doi:10.1594/PANGAEA.149999). By January 2015, a total of 581 data sets (over 4 000 000 data points) from 539 papers had been archived. Here we present the developments of this data compilation five years since its first description by Nisumaa et al. (2010). Most of study sites from which data archived are still in the Northern Hemisphere and the number of archived data from studies from the Southern Hemisphere and polar oceans are still relatively low. Data from 60 studies that investigated the response of a mix of organisms or natural communities were all added after 2010, indicating a welcomed shift from the study of individual organisms to communities and ecosystems. The initial imbalance of considerably more data archived on calcification and primary production than on other processes has improved. There is also a clear tendency towards more data archived from multifactorial studies after 2010. For easier and more effective access to ocean acidification data, the ocean acidification community is strongly encouraged to contribute to the data archiving effort, and help develop standard vocabularies describing the variables and define best practices for archiving ocean acidification data.
    Keywords: Biological process; Country; Experimental treatment; Geographic name/locality; Number; Persistent Identifier; Taxon/taxa; Title
    Type: Dataset
    Format: text/tab-separated-values, 4644 data points
    Location Call Number Expected Availability
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  • 7
    Publication Date: 2024-07-06
    Keywords: Ammonium; DATE/TIME; DEPTH, sediment/rock; GCUWI; Gravity corer, UWITEC; Grevelingen Lake, Netherlands; Hydrogen sulfide; Iron 2+; Methane; Sample comment; Scharendijke_Site; Sulfate; Sulfate reduction rate; δ13C, methane; δ13C, methane, standard deviation; δ Deuterium, methane; δ Deuterium, methane, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 1054 data points
    Location Call Number Expected Availability
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Egger, Matthias; Lenstra, Wytze K; Jong, Dirk; Meysman, Filip J R; Sapart, Célia-Julia; van der Veen, Carina; Röckmann, Thomas; Gonzales, S; Slomp, Caroline P (2015): Rapid sediment accumulation results in high methane effluxes from coastal sediments. PLoS ONE, 11(8), e0161609, https://doi.org/10.1371/journal.pone.0161609
    Publication Date: 2024-07-06
    Description: Will be submitted by the author
    Keywords: GCUWI; Gravity corer, UWITEC; Grevelingen Lake, Netherlands; Scharendijke_Site
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 9
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    Unknown
    PANGAEA
    In:  Supplement to: Egger, Matthias; Rasigraf, Olivia; Sapart, Célia-Julia; Jilbert, Tom; Jetten, Mike S M; Röckmann, Thomas; van der Veen, Carina; Bânda, Narcisa; Kartal, Boran; Ettwig, Katharina; Slomp, Caroline P (2015): Iron-Mediated Anaerobic Oxidation of Methane in Brackish Coastal Sediments. Environmental Science & Technology, 49(1), 277-283, https://doi.org/10.1021/es503663z
    Publication Date: 2024-07-06
    Description: Methane is a powerful greenhouse gas and its biological conversion in marine sediments, largely controlled by anaerobic oxidation of methane (AOM), is a crucial part of the global carbon cycle. However, little is known about the role of iron oxides as an oxidant for AOM. Here we provide the first field evidence for iron-dependent AOM in brackish coastal surface sediments and show that methane produced in Bothnian Sea sediments is oxidized in distinct zones of iron- and sulfate-dependent AOM. At our study site, anthropogenic eutrophication over recent decades has led to an upward migration of the sulfate/methane transition zone in the sediment. Abundant iron oxides and high dissolved ferrous iron indicate iron reduction in the methanogenic sediments below the newly established sulfate/methane transition. Laboratory incubation studies of these sediments strongly suggest that the in situ microbial community is capable of linking methane oxidation to iron oxide reduction. Eutrophication of coastal environments may therefore create geochemical conditions favorable for iron-mediated AOM and thus increase the relevance of iron-dependent methane oxidation in the future. Besides its role in mitigating methane emissions, iron-dependent AOM strongly impacts sedimentary iron cycling and related biogeochemical processes through the reduction of large quantities of iron oxides.
    Keywords: GEMAX; GNC_X; Gulf of Bothnia, Baltic sea; US5B
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 10
    Publication Date: 2024-07-05
    Type: info:eu-repo/semantics/article
    Location Call Number Expected Availability
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