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  • Data  (11)
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  • 1
    Publication Date: 2023-05-12
    Description: For a reliable simulation of the time and space dependent CO2 redistribution between ocean and atmosphere an appropriate time dependent simulation of particle dynamics processes is essential but has not been carried out so far. The major difficulties were the lack of suitable modules for particle dynamics and early diagenesis (in order to close the carbon and nutrient budget) in ocean general circulation models, and the lack of an understanding of biogeochemical processes, such as the partial dissolution of calcareous particles in oversaturated water. The main target of ORFOIS was to fill in this gap in our knowledge and prediction capability infrastructure. This goal has been achieved step by step. At first comprehensive data bases (already existing data) of observations of relevance for the three major types of biogenic particles, organic carbon (POC), calcium carbonate (CaCO3), and biogenic silica (BSi or opal), as well as for refractory particles of terrestrial origin were collated and made publicly available.
    Keywords: ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean
    Type: Dataset
    Format: application/octet-stream, 506.9 MBytes
    Location Call Number Expected Availability
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  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Dittert, Nicolas; Corrin, Lydie; Diepenbroek, Michael; Grobe, Hannes; Heinze, Christoph; Ragueneau, Olivier (2002): Management of (pale-)oceanographic data sets using the PANGAEA information system: the SINOPS example. Computers & Geosciences, 28(7), 789-798, https://doi.org/10.1016/S0098-3004(01)00112-1
    Publication Date: 2023-06-08
    Description: During the SINOPS project, an optimal state of the art simulation of the marine silicon cycle is attempted employing a biogeochemical ocean general circulation model (BOGCM) through three particular time steps relevant for global (paleo-) climate. In order to tune the model optimally, results of the simulations are compared to a comprehensive data set of 'real' observations. SINOPS' scientific data management ensures that data structure becomes homogeneous throughout the project. Practical work routine comprises systematic progress from data acquisition, through preparation, processing, quality check and archiving, up to the presentation of data to the scientific community. Meta-information and analytical data are mapped by an n-dimensional catalogue in order to itemize the analytical value and to serve as an unambiguous identifier. In practice, data management is carried out by means of the online-accessible information system PANGAEA, which offers a tool set comprising a data warehouse, Graphical Information System (GIS), 2-D plot, cross-section plot, etc. and whose multidimensional data model promotes scientific data mining. Besides scientific and technical aspects, this alliance between scientific project team and data management crew serves to integrate the participants and allows them to gain mutual respect and appreciation.
    Keywords: Silicon Cycling in the World Ocean; SINOPS
    Type: Dataset
    Format: unknown
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  • 3
    Publication Date: 2023-08-15
    Keywords: Barcelona Coast; Carbon, inorganic, particulate, flux; Carbon, organic, particulate, flux; DEPTH, water; MULT; Multiple investigations; Opal, flux; PAP; Pertuis Charentais; Porcupine Abyssal Plain; Taranto Mare Piccolo
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
    Location Call Number Expected Availability
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  • 4
    Publication Date: 2023-08-15
    Keywords: Carbon, inorganic, particulate, flux; Carbon, organic, particulate, flux; DEPTH, water; Duration, number of days; Opal, flux; POOZ; POOZ_trap; Southern Ocean - Indian sector; Trap, sediment; TRAPS
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
    Location Call Number Expected Availability
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Ragueneau, Olivier; Tréguer, Paul; Leynaert, Aude; Anderson, Robert F; Brzezinski, Mark A; DeMaster, David J; Dugdale, Richard; Dymond, Jack R; Fischer, Gerhard; Francois, Roger; Heinze, Christoph; Maier-Reimer, Ernst; Martin-Jézéquel, Véronique; Nelson, David M; Quéguiner, Bernard (2000): A review of the Si cycle in the modern ocean: recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy. Global and Planetary Change, 26(4), 317-365, https://doi.org/10.1016/S0921-8181(00)00052-7
    Publication Date: 2023-08-15
    Description: Due to the major role played by diatoms in the biological pump of CO2, and to the presence of silica-rich sediments in areas that play a major role in air-sea CO2 exchange (e.g. the Southern Ocean and the Equatorial Pacific), opal has a strong potential as a proxy for paleoproductivity reconstructions. However, because of spatial variations in the biogenic silica preservation, and in the degree of coupling between the marine Si and C biogeochemical cycles, paleoreconstructions are not straitghtforward. A better calibration of this proxy in the modern ocean is required, which needs a good understanding of the mechanisms that control the Si cycle, in close relation to the carbon cycle. This review of the Si cycle in the modern ocean starts with the mechanisms that control the uptake of silicic acid (Si(OH)4) by diatoms and the subsequent silicification processes, the regulatory mechanisms of which are uncoupled. This has strong implications for the direct measurement in the field of the kinetics of Si(OH)4 uptake and diatom growth. It also strongly influences the Si:C ratio within diatoms, clearly linked to environmental conditions. Diatoms tend to dominate new production at marine ergoclines. At depth, they also succeed to form mats, which sedimentation is at the origin of laminated sediments and marine sapropels. The concentration of Si(OH)4 with respect to other macronutrients exerts a major influence on diatom dominance and on the rain ratio between siliceous and calcareous material, which severely impacts surface waters pCO2. A compilation of biogenic fluxes collected at about 40 sites by means of sediment traps also shows a remarkable pattern of increasing BSi:Corg ratio along the path of the "conveyor belt", accompanying the relative enrichment of waters in Si compared to N and P. This observation suggests an extension of the Si pump model described by Dugdale and Wilkerson (1989, doi:10.1038/34630), giving to Si(OH)4 a major role in the control of the rain ratio, which is of major importance in the global carbon cycle. The fate of the BSi produced in surface waters is then described, in relation to Corg, in terms of both dissolution and preservation mechanisms. Difficulties in quantifying the dissolution of biogenic silica in the water column as well as the sinking rates and forms of BSi to the deep, provide evidence for a major gap in our understanding of the mechanisms controlling the competition between retention in and export from surface waters. The relative influences of environmental conditions, seasonality, food web structure or aggregation are however explored. Quantitatively, assuming steady state, the measurements of the opal rain rate by means of sediment traps matches reasonably well those obtained by adding the recycling and burial fluxes in the underlying abyssal sediments, for most of the sites where such a comparison is possible. The major exception is the Southern Ocean where sediment focusing precludes the closing of mass balances. Focusing in fact is also an important aspect of the downward revision of the importance of Southern Ocean sediments in the global biogenic silica accumulation. Qualitatively, little is known about the duration of the transfer through the deep and the quality of the material that reaches the seabed, which is suggested to represent a major gap in our understanding of the processes governing the early diagenesis of BSi in sediments. The sediment composition (special emphasis on Al availability), the sedimentation rate or bioturbation are shown to exert an important control on the competition between dissolution and preservation of BSi in sediments. It is suggested that a primary control on the kinetic and thermodynamic properties of BSi dissolution, both in coastal and abyssal sediments, is exerted by water column processes, either occuring in surface waters during the formation of the frustules, or linked to the transfer of the particles through the water column, which duration may influence the quality of the biogenic rain. This highlights the importance of studying the factors controlling the degree of coupling between pelagic and benthic processes in various regions of the world ocean, and its consequences, not only in terms of benthic biology but also for the constitution of the sediment archive. The last section, first calls for the end of the "NPZD" models, and for the introduction of processes linked to the Si cycle, into models describing the phytoplankton cycles in surface waters and the early diagenesis of BSi in sediments. It also calls for the creation of an integrated 1-D diagnostic model of the Si:C coupling, for a better understanding of the interactions between surface waters, deep waters and the upper sedimentary column. The importance of Si(OH)4 in the control of the rain ratio and the improved parametrization of the Si cycle in the 1-D diagnostic models should lead to a reasonable incorporation of the Si cycle into 3-D regional circulation models and OGCMs, with important implications for climate change studies and paleoreconstructions at regional and global scale.
    Keywords: Barcelona Coast; ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean; Pertuis Charentais; Silicon Cycling in the World Ocean; SINOPS; Taranto Mare Piccolo
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
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  • 6
    Publication Date: 2023-12-16
    Keywords: 104-643A; 10-87; 10-90; 10-91; 10-97; 11-104; 11-106B; 12-112; 12-116; 12-118; 12-119; 13-120; 13-126; 13-133; 14-135; 14-136; 14-138; 14-139; 14-140; 14-142; 15-149; 15-153; 16-158; 16-159; 17-166; 17-167; 17-171; 18-173; 18-178; 19-183; 20-199; 21-204; 21-205; 21-208; 21-209; 21-210; 22-213; 22-216; 22-216A; 22-218; 23-219; 23-223; 24-231; 24-234; 24-235; 24-236; 24-237; 24-238; 25-240; 25-240A; 25-241; 25-242; 25-245; 25-249; 26-251A; 26-253; 26-254; 26-255; 27-260; 28-265; 28-266; 28-267B; 28-269; 28-270; 28-274; 29-278; 29-279A; 29-281; 29-282; 30-285; 30-285A; 30-288; 30-288B; 30-289; 31-296; 31-297; 3-14; 3-15; 3-17A; 32-305; 33-315A; 33-317B; 33-318; 34-319; 34-320; 35-323; 36-328; 36-328B; 36-329; 37-335; 38-338; 38-341; 38-342; 38-345; 38-346; 38-348; 38-350; 39-354; 39-356; 39-356A; 40-360; 40-362; 40-364; 41-366; 41-366A; 41-367; 41-368; 41-369; 41-369A; 41-370; 4-23; 42-375; 4-24; 4-30; 4-31; 43-382; 43-386; 44-388A; 44-391; 45-396; 47-397; 47-398; 48-400; 48-404; 48-406; 49-407; 49-408; 50-415; 5-32; 5-33; 5-34; 56-434; 56-436; 57-438A; 57-439; 58-442A; 58-442B; 59-447A; 59-448A; 59-449; 59-450; 60-458; 60-459B; 63-469; 63-470; 63-470A; 63-472; 6-53; 6-54; 6-55; 6-56B; 67-495; 67-496; 67-499; 71-512; 72-515B; 72-516; 73-522; 74-525A; 74-525B; 74-526A; 74-527; 74-528A; 74-529; 77-536; 77-540; 80-548A; 80-549A; 81-552; 81-555; 82-563; 84-569; 85-572D; 85-573B; 85-574; 85-575; 86-578; 86-581; 8-69; 8-70; 8-71; 8-72; 8-73; 8-75; 87-584; 90-588A; 90-590B; 90-591B; 90-592; 90-593; 90-594; 90-594A; 91-596; 92-597; 92-597A; 92-598; 93-603; 93-603B; 94-608; 94-610; 94-611C; 9-77B; 9-78; 9-79; 9-80; 9-80A; Age model; Antarctic Ocean; Antarctic Ocean/BASIN; Antarctic Ocean/CONT RISE; Antarctic Ocean/PLAIN; Antarctic Ocean/RIDGE; Antarctic Ocean/Tasman Sea/CONT RISE; Antarctic Ocean/Tasman Sea/RIDGE; ANT-IV/4; Calculated, see reference(s); Caribbean Sea/BASIN; Caribbean Sea/GAP; Caribbean Sea/RIDGE; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP JOIDES Screen classifiation; Elevation of event; Event label; Glomar Challenger; Gravity corer (Kiel type); Gulf of Mexico; Gulf of Mexico/BANK; Gulf of Mexico/BASIN; Gulf of Mexico/PLAIN; Gulf of Mexico/SLOPE; Indian Ocean//BASIN; Indian Ocean//CHANNEL; Indian Ocean//FAN; Indian Ocean//FRACTURE ZONE; Indian Ocean//PLAIN; Indian Ocean//PLATEAU; Indian Ocean//RIDGE; Indian Ocean/Arabian Sea/RIDGE; Indian Ocean/Gulf of Aden/BASIN; Joides Resolution; LATITUDE; Leg10; Leg104; Leg11; Leg12; Leg13; Leg14; Leg15; Leg16; Leg17; Leg18; Leg19; Leg20; Leg21; Leg22; Leg23; Leg24; Leg25; Leg26; Leg27; Leg28; Leg29; Leg3; Leg30; Leg31; Leg32; Leg33; Leg34; Leg35; Leg36; Leg37; Leg38; Leg39; Leg4; Leg40; Leg41; Leg42; Leg43; Leg44; Leg45; Leg47; Leg48; Leg49; Leg5; Leg50; Leg56; Leg57; Leg58; Leg59; Leg6; Leg60; Leg63; Leg67; Leg71; Leg72; Leg73; Leg74; Leg77; Leg8; Leg80; Leg81; Leg82; Leg84; Leg85; Leg86; Leg87; Leg9; Leg90; Leg91; Leg92; Leg93; Leg94; LONGITUDE; Maud Rise; Mediterranean Sea/BASIN; Mediterranean Sea/RIDGE; Mediterranean Sea/SLOPE; North Atlantic; North Atlantic/BANK; North Atlantic/BASIN; North Atlantic/CONT RISE; North Atlantic/CONT SLOPE; North Atlantic/FLANK; North Atlantic/HILL; North Atlantic/Norwegian Sea; North Atlantic/Norwegian Sea/BASIN; North Atlantic/Norwegian Sea/PLATEAU; North Atlantic/Norwegian Sea/RIDGE; North Atlantic/PLAIN; North Atlantic/PLATEAU; North Atlantic/RIDGE; North Atlantic/SEAMOUNT; North Atlantic/SEDIMENT POND; North Atlantic/SPUR; North Pacific; North Pacific/ABYSSAL FLOOR; North Pacific/BASIN; North Pacific/CONT RISE; North Pacific/ESCARPMENT; North Pacific/FAN; North Pacific/FLANK; North Pacific/GUYOT; North Pacific/HILL; North Pacific/Philippine Sea/BASIN; North Pacific/Philippine Sea/RIDGE; North Pacific/PLAIN; North Pacific/PLATEAU; North Pacific/RIDGE; North Pacific/SEDIMENT POND; North Pacific/SLOPE; North Pacific/TRENCH; North Pacific/TROUGH; North Pacific/VALLEY; Norwegian Sea; Opal, biogenic silica; Polarstern; PS08; PS08/646; PS1466-1; Reference/source; Sample code/label; Silicon Cycling in the World Ocean; SINOPS; SL; South Atlantic; South Atlantic/BANK; South Atlantic/BASIN; South Atlantic/CONT RISE; South Atlantic/CREST; South Atlantic/HILL; South Atlantic/PLATEAU; South Atlantic/RIDGE; South Atlantic/SLOPE; South Atlantic/SYNCLINE; South Pacific; South Pacific/BASIN; South Pacific/CONT RISE; South Pacific/Coral Sea/BASIN; South Pacific/Coral Sea/PLATEAU; South Pacific/PLATEAU; South Pacific/RIDGE; South Pacific/Tasman Sea/CONT RISE; South Pacific/Tasman Sea/PLATEAU; South Pacific/TRENCH; South Pacific/VALLEY
    Type: Dataset
    Format: text/tab-separated-values, 7562 data points
    Location Call Number Expected Availability
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  • 7
    Publication Date: 2024-02-29
    Keywords: 114-704A; 67-499; 7-64; 86-578; 90-594; 94-607; 94-609; 94-610; A150/180; A152-118; AGE; Age model; Age model, lithological correlation; ANTA91-8; APSARA2; APSARA4; AR001-032; AR002-002; AR003-006; AR003-007; AR003-008; AR003-014; AR003-017; AR003-018; AR003-019; AR003-020; AR003-021; AR003-022; AR003-023; AR003-024; AR003-026; AR003-027; AR003-028; AR004-009; Atlantic Ocean; Comment; DRILL; Drilling/drill rig; ELT45; ELT45.027-PC; ELT45.029-PC; ELT45.029-TC; ELT45.063-PC; ELT45.064-PC; ELT45.071-PC; ELT45.074-PC; ELT45.079-PC; ELT48; ELT48.022-PC; ELT48.027-PC; ELT49; ELT49.006-PC; ELT49.008-PC; ELT49.023-PC; ELT49.029-PC; ELT50; ELT50.013-PC; ELT50.017-PC; Eltanin; Event label; GC; Glomar Challenger; Gravity corer; Joides Resolution; LATITUDE; Leg114; Leg67; Leg7; Leg86; Leg90; Leg94; LONGITUDE; Marion Dufresne (1972); MD38; MD84-527; MD84-552; MD88-773; MUC; MultiCorer; North Atlantic/FLANK; North Atlantic/RIDGE; Northeast Pacific; North Pacific; North Pacific/TRENCH; NR-54; Opal, biogenic silica; PC; Piston corer; RC08; RC08-102; RC08-103; RC08-145; RC08-18; RC08-48; RC08-63; RC08-78; RC08-79; RC08-94; RC09; RC09-110; RC09-124; RC09-126; RC09-129; RC09-162; RC09-49; RC09-62; RC09-64; RC09-65; RC09-66; RC09-67; RC09-68; RC10; RC10-139; RC10-140; RC10-216; RC10-250; RC10-252; RC10-253; RC10-254; RC10-288; RC10-289; RC10-50; RC10-52; RC10-97; RC11; RC11-118; RC11-119; RC1112; RC11-120; RC11-121; RC11-170; RC11-172; RC11-179; RC11-21; RC11-213; RC11-220; RC11-237; RC11-238; RC11-76; RC11-91; RC11-96; RC12; RC12-103; RC12-107; RC12-109; RC12-121; RC12-179; RC12-225; RC12-241; RC12-291; RC12-328; RC12-340; RC12-341; RC12-343; RC12-344; RC12-361; RC12-401; RC12-412; RC12-413; RC12-416; RC12-419; RC13; RC13-113; RC13-151; RC13-152; RC13-153; RC13-159; RC13-189; RC13-190; RC13-253; RC13-254; RC13-259; RC13-271; RC13-273; RC13-38; RC13-63; RC13-81; RC14; RC14-106; RC14-11; RC14-12; RC14-39; RC14-99; RC15; RC15-23; RC15-52; RC15-93; RC15-94; RC17; RC17-113; RC17-60; RC17-61; RC17-63; RC17-73; RC17-98; Reference/source; Robert Conrad; Silicon Cycling in the World Ocean; SINOPS; SK-226; SK-657; South Atlantic Ocean; Southern East Pacific Rise; South Indian Ocean; South Pacific; South Pacific/CONT RISE; South Pacific/PLATEAU; V14; V14-101; V14-81; V15; V15-11; V15-12; V15-13; V15-14; V15-15; V15-16; V15-29; V15-30; V15-31; V16; V16-122; V17; V17-165; V17-40; V17-41; V17-42; V17-43; V17-44; V18; V18-312; V18-318; V18-337; V18-350; V18-351; V18-352; V18-353; V18-354; V18-355; V19; V19-19; V19-204; V19-21; V19-22; V19-23; V19-24; V19-25; V19-27; V19-65; V20; V20-103; V20-121; V20-122; V20-123; V20-124; V20-126; V20-129; V20-14; V20-15; V20-170; V20-212; V20-227; V20-241; V20-242; V21; V21-151; V21-171; V21-211; V21-212; V21-213; V21-214; V21-215; V21-216; V21-217; V21-218; V21-219; V21-25; V21-26; V21-28; V21-29; V21-30; V21-59; V22; V22-108; V22-168; V22-186; V22-188; V22-197; V22-219; V22-222; V22-234; V22-26; V22-38; V22-83; V23; V23-58; V23-59; V23-60; V23-74; V23-81; V23-98; V24; V24-166; V24-203; V24-229; V24-235; V24-237; V24-35; V24-36; V25; V25-21; V25-42; V25-44; V25-60; V25-75; V26; V26-175; V26-176; V26-177; V26-37; V26-63; V26-82; V27; V27-110; V27-171; V27-175; V27-228; V27-232; V27-238; V27-239; V27-240; V27-263; V27-264; V27-265; V27-85; V27-86; V28; V28-108; V28-129; V28-229; V28-230; V28-235; V28-249; V28-294; V28-304; V28-35; V28-56; V28-89; V29; V29-144; V29-15; V29-153; V29-210; V29-29; V29-30; V29-48; V29-84; V29-86; V29-89; V29-90; V30; V30-99; V31; V31-166; V32; V32-126; V34; V34-101; V34-111; V34-34; V34-48; V34-51; V34-53; V34-55; V34-89; V34-91; V34-92; Vema; Y0001; Y0001-005; Y6004; Y6004-010; Y6009; Y6009-005; Y9001; Y9001-071; Y9001-072; Y9001-073; Y9001-074; Y9001-075; Y9001-076; Y9001-080; Y9001-083; Y9001-084; Y9001-086; Y9001-097; Y9001-102; Y9001-103; Y9001-104; Y9001-105; Y9001-106; Y9001-107; Y9001-108; Y9001-109; Y9001-110; Y9001-111; Y9001-112; Y9001-114; Y9010; Y9010-002; Y9010-004; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 737 data points
    Location Call Number Expected Availability
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  • 8
    Publication Date: 2024-03-02
    Description: In this dataset we present a global compilation of over 1000 sedimentary records of 230Th from across the global ocean at two time slices, the Late Holocene (0-5000 years ago, or 0-5 ka) and the Last Glacial Maximum (18.5-23.5 ka). Data have been screened for age control, errors, and lithogenic corrections. Overall quality levels were computed by summing each record's scores on the individual criteria. A record is optimal if it is based on a chronology that is constrained by δ18O or 14C and it provides both the raw nuclide concentrations and the associated errors. About one quarter of the records in the database achieved this highest quality level. The large majority of the records in the database are good, passing two of the three criteria, while the remaining quarter are of fair or poor quality.
    Keywords: Comment; DEPTH, water; Distance; Flag; Focusing factor; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; Identification; LATITUDE; LONGITUDE; Ocean; ORDINAL NUMBER; Quality level; Ratio; Reference/source; Thorium-230 excess, decay-corrected; Total sediment, flux; Uranium/Thorium ratio
    Type: Dataset
    Format: text/tab-separated-values, 15667 data points
    Location Call Number Expected Availability
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  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Pfeil, Benjamin; Olsen, Are; Bakker, Dorothee C E; Hankin, Steven; Koyuk, Heather; Kozyr, Alexander; Malczyk, Jeremy; Manke, Ansley; Metzl, Nicolas; Sabine, Christopher L; Akl, John; Alin, Simone R; Bellerby, Richard G J; Borges, Alberto Vieira; Boutin, Jacqueline; Brown, Peter J; Cai, Wei-Jun; Chavez, Francisco P; Chen, Arthur; Cosca, Catherine E; Fassbender, Andrea J; Feely, Richard A; González-Dávila, Melchor; Goyet, Catherine; Hardman-Mountford, Nicolas J; Heinze, Christoph; Hood, E Maria; Hoppema, Mario; Hunt, Christopher W; Hydes, David; Ishii, Masao; Johannessen, Truls; Jones, Steve D; Key, Robert M; Körtzinger, Arne; Landschützer, Peter; Lauvset, Siv K; Lefèvre, Nathalie; Lenton, Andrew; Lourantou, Anna; Merlivat, Liliane; Midorikawa, Takashi; Mintrop, Ludger J; Miyazaki, Chihiro; Murata, Akihiko; Nakadate, Akira; Nakano, Yoshiyuki; Nakaoka, Shin-Ichiro; Nojiri, Yukihiro; Omar, Abdirahman M; Padín, Xose Antonio; Park, Geun-Ha; Paterson, Kristina; Pérez, Fiz F; Pierrot, Denis; Poisson, Alain; Ríos, Aida F; Santana-Casiano, Juana Magdalena; Salisbury, Joe; Sarma, Vedula V S S; Schlitzer, Reiner; Schneider, Bernd; Schuster, Ute; Sieger, Rainer; Skjelvan, Ingunn; Steinhoff, Tobias; Suzuki, Toru; Takahashi, Taro; Tedesco, Kathy; Telszewski, Maciej; Thomas, Helmuth; Tilbrook, Bronte; Tjiputra, Jerry; Vandemark, Doug; Veness, Tony; Wanninkhof, Rik; Watson, Andrew J; Weiss, Ray F; Wong, Chi Shing; Yoshikawa-Inoue, Hisayuki (2013): A uniform, quality controlled Surface Ocean CO2 Atlas (SOCAT). Earth System Science Data, 5(1), 125-143, https://doi.org/10.5194/essd-5-125-2013
    Publication Date: 2024-02-02
    Description: A well-documented, publicly available, global data set of surface ocean carbon dioxide (CO2) parameters has been called for by international groups for nearly two decades. The Surface Ocean CO2 Atlas (SOCAT) project was initiated by the international marine carbon science community in 2007 with the aim of providing a comprehensive, publicly available, regularly updated, global data set of marine surface CO2, which had been subject to quality control (QC). Many additional CO2 data, not yet made public via the Carbon Dioxide Information Analysis Center (CDIAC), were retrieved from data originators, public websites and other data centres. All data were put in a uniform format following a strict protocol. Quality control was carried out according to clearly defined criteria. Regional specialists performed the quality control, using state-of-the-art web-based tools, specially developed for accomplishing this global team effort. SOCAT version 1.5 was made public in September 2011 and holds 6.3 million quality controlled surface CO2 data points from the global oceans and coastal seas, spanning four decades (1968-2007). Three types of data products are available: individual cruise files, a merged complete data set and gridded products. With the rapid expansion of marine CO2 data collection and the importance of quantifying net global oceanic CO2 uptake and its changes, sustained data synthesis and data access are priorities.
    Keywords: 0306SFC_PRT; 061ASFC_PRT; 06AQ19860627-track; 06AQ19860928-track; 06AQ19911114-track; 06AQ19911210-track; 06AQ19921005-track; 06AQ19930128-track; 06AQ19930228-track; 06AQ19931019-track; 06AQ19940524-track; 06AQ19951206-track; 06AQ19960320-track; 06AQ19980411-track; 06AQ19990327-track; 06AQ20001004-track; 06AQ20001026-track; 06BE19961010-track; 06CK20060523-track; 06CK20060715-track; 06CK20060821-track; 06GA19960613-track; 06GA276_3; 06LB19831130-track; 06LB19840107-track; 06LB19840629-track; 06LB19850110-track; 06LB19850313-track; 06LB19850812-track; 06LB19860116-track; 06LB19860323-track; 06LB19860801-track; 06LB19861011-track; 06LB19861214-track; 06LB19870221-track; 06LB19870501-track; 06LB19870721-track; 06LB19870920-track; 06LB19871126-track; 06LB19871231-track; 06LB19880204-track; 06MT18_1; 06MT19910903-track; 06MT19920510-track; 06MT19921229-track; 06MT19941012-track; 06MT19941119-track; 06MT19950714-track; 06MT19960607-track; 06MT19960622-track; 06MT19970106-track; 06MT19970516-track; 06MT19970707-track; 06MT19970814-track; 06MT19981228-track; 06MT20021015-track; 06MT20060714; 06MT20060714-track; 06MT22_5; 06MT30_2; 06MT30_3; 06MT37_2; 06MT39_4; 06MT39_5; 06P119910616-track; 06P119950901-track; 06PO20050321; 06PO20050322-track; 07AL19951011-track; 07AL19960218-track; 07AL19970503-track; 07AL19990718-track; 07AL19991101-track; 07AL19991129-track; 07AL20000113-track; 07AL20000210-track; 07AL20000305-track; 07AL20010513-track; 07AL20010607-track; 07AL20010709-track; 07AL20010802-track; 09AR0103; 09AR19910926-track; 09AR19921019-track; 09AR19930105-track; 09AR19930311-track; 09AR19930807-track; 09AR19931119-track; 09AR19940101-track; 09AR19940831-track; 09AR19941213-track; 09AR19950717-track; 09AR19950916-track; 09AR19960119-track; 09AR19960822-track; 09AR19970910-track; 09AR19971114-track; 09AR19980228-track; 09AR19980404-track; 09AR19980715-track; 09AR19990716-track; 09AR20011031-track; 09AR9401; 09AR9404; 09AR9407; 09AR9501; 09AR9502; 09AR9601; 09AR9604; 09AR9701; 09AR9703; 09AR9707; 09AR9801; 09AR9806; 09AR9901; 09FA20000927-track; 09SS19951116-track; 09SS19990205-track; 11BE19940413-track; 11BE19950303-track; 11BE19950912-track; 11BE19970513-track; 11BE19970527-track; 11BE19970609-track; 11BE19970618-track; 11BE19970621; 11BE19970621-track; 11BE19970702-track; 11BE19980107-track; 11BE19980614-track; 11BE19980625-track; 11BE19980710-track; 11BE19990830-track; 11BE19990904-track; 11BE19990914-track; 11BE19990918-track; 11BE20010502-track; 11BE20010514-track; 11BE20010522-track; 11BE20020422-track; 11BE20020511-track; 11BE20020528-track; 11BE20021104-track; 11BE20030331-track; 11BE20030901; 11BE20030901-track; 11BE20031027; 11BE20031027-track; 11BE20031208; 11BE20031208-track; 11BE20040223; 11BE20040223-track; 11BE20040329; 11BE20040329-track; 11BE20040524; 11BE20040524-track; 11BE20040601-track; 11BE20041004; 11BE20041004-track; 11BE20060425; 11BE20060425-track; 11BE20060529-track; 11BE20070507-track; 18QA19730812-track; 18QA19731028-track; 18QA19760111-track; 18QA19760619-track; 18QA19760911-track; 18QA19761204-track; 18VC19740105-track; 18VC19740216-track; 18VC19741113-track; 18VC19750622-track; 18VC19750913-track; 1995-10-BS; 1996-02-BS; 1997-05-BS; 1999-07-BS; 1999-11-BS; 1999-12-BS; 2000-01-BS; 2000-02-BS; 2000-03-BS; 2001-05-BS; 2001-06-BS; 2001-07-BS; 2001-08-BS; 2003-06-BS; 2003-07-BS; 2003-08-BS; 2003-09-BS; 2003-10-BS; 2004-02-BS; 2004-03-BS; 2004-04-BS; 2004-05-BS; 2004-06-BS; 2004-07-BS; 2004-08-BS; 2004-09-BS; 2004-10-BS; 2005-01-BS; 2005-02-BS; 2005-03-BS; 2005-04-BS; 2005-05-BS; 2005-06-BS; 2005-07-BS; 2005-08-BS; 2005-09-BS; 2005-10-BS; 2005-11-BS; 2005-12-BS; 2006-03-BS; 2006-04-BS; 2006-05-BS; 2006-06-BS; 2006-07-BS; 2006-08-BS; 2006-09-BS; 20070110_TC2; 20070117_TC2; 20070123_TC2; 20070130_TC2; 20070207_TC2; 20070219_TC2; 20070227_TC2; 20070305_TC2; 20070320_TC2; 20070327_TC2; 20070402_TC2; 20070409_TC2; 20070416_TC2; 20070423_TC2; 20070430_TC2; 20070508_TC2; 20070515_TC2; 20070521_TC2; 20070529_TC2; 20070604_TC2; 20070613_TC2; 20070620_TC2; 20070627_TC2; 20070703_TC2; 20070709_TC2; 20070716_TC2; 20070723_TC2; 20070730_TC2; 2007-07-BS; 20070806_TC2; 20070815_TC2; 20070820_TC2; 20070827_TC2; 2007-08-BS; 20070903_TC2; 20070910_TC2; 20070917_TC2; 20071001_TC2; 20071008_TC2; 20071010_TC2; 20071015_TC2; 20071023_TC2; 20071105_TC2; 20071115_TC2; 20071120_TC2; 20071128_TC2; 20071204_TC2; 20071211_TC2; 20071218_TC2; 20071225_TC2; 24N98L1; 24N98L2; 26GC20010421-track; 26GC20010831-track; 26NA20050107; 26NA20050107-track; 26NA20050115; 26NA20050115-track; 26NA20050130; 26NA20050130-track; 26NA20050207; 26NA20050207-track; 26NA20050317; 26NA20050317-track; 26NA20050321; 26NA20050321-track; 26NA20050402; 26NA20050402-track; 26NA20050420; 26NA20050420-track; 26NA20050502; 26NA20050502-track; 26NA20050511; 26NA20050511-track; 26NA20050523; 26NA20050523-track; 26NA20050531; 26NA20050531-track; 26NA20050614; 26NA20050614-track; 26NA20050624; 26NA20050624-track; 26NA20050714; 26NA20050714-track; 26NA20050720; 26NA20050720-track; 26NA20050730; 26NA20050730-track; 26NA20050805; 26NA20050805-track; 26NA20050815; 26NA20050815-track; 26NA20050824; 26NA20050824-track; 26NA20050914; 26NA20050914-track; 26NA20050927; 26NA20050927-track; 26NA20051005; 26NA20051005-track; 26NA20051018; 26NA20051018-track; 26NA20051026; 26NA20051026-track; 26NA20051110; 26NA20051110-track; 26NA20051117; 26NA20051117-track; 26NA20051130; 26NA20051130-track; 26NA20060518; 26NA20060518-track; 26NA20060527; 26NA20060527-track; 26NA20060607; 26NA20060607-track; 26NA20060617; 26NA20060617-track; 26NA20060628; 26NA20060628-track; 26NA20060708; 26NA20060708-track; 26NA20060719; 26NA20060719-track; 26NA20060728; 26NA20060728-track; 26NA20060809; 26NA20060809-track; 26NA20060818; 26NA20060818-track; 26NA20060830; 26NA20060830-track; 26NA20060908; 26NA20060908-track; 26NA20060920; 26NA20060920-track; 26NA20061011; 26NA20061011-track; 26NA20061021; 26NA20061021-track; 26NA20061128; 26NA20061128-track; 26NA20061202; 26NA20061202-track; 26NA20061214; 26NA20061214-track; 26NA20061225; 26NA20061225-track; 26NA20070103; 26NA20070103-track; 26NA20070112; 26NA20070112-track; 26NA20070125; 26NA20070125-track; 26NA20070205; 26NA20070205-track; 26NA20070216; 26NA20070216-track; 26NA20070323; 26NA20070323-track; 26NA20070329; 26NA20070329-track; 26NA20070410; 26NA20070410-track; 26NA20070418; 26NA20070418-track; 26NA20070427; 26NA20070427-track; 26NA20070509; 26NA20070509-track; 26NA20070518; 26NA20070518-track; 26NA20070530; 26NA20070530-track; 26NA20070610; 26NA20070610-track; 26NA20070622; 26NA20070622-track; 26NA20070701; 26NA20070701-track; 26NA20070712; 26NA20070712-track; 26NA20070721; 26NA20070721-track; 26NA20070802; 26NA20070802-track; 26NA20070811; 26NA20070811-track; 26NA20070901; 26NA20070901-track; 26NA20070912; 26NA20070912-track; 26NA20070923; 26NA20070923-track; 26NA20071003; 26NA20071003-track; 26NA20071014; 26NA20071014-track; 26NA20071024; 26NA20071024-track; 26NA20071103; 26NA20071103-track; 26NA20071114; 26NA20071114-track; 26NA20071124; 26NA20071124-track; 29HE050; 29HE19980729-track; 29HE20001028; 29HE20001028-track; 29HE20010306; 29HE20010306-track; 29HE20011027; 29HE20011027-track; 29HE20020305; 29HE20020305-track; 29HE20021028; 29HE20021028-track; 29HE20030409; 29HE20030409-track; 29HE20041021; 29HE20041021-track; 316N0154; 316N19810401-track; 316N19810416-track; 316N19810516-track; 316N19810619-track; 316N19810721-track; 316N19810821-track; 316N19810923-track; 316N19821202-track; 316N19821230-track; 316N19830130-track; 316N19831007-track; 316N19840111-track; 316N19871030-track; 316N19871123-track; 316N19871218-track; 316N19880128-track; 316N19940404-track; 316N19941201-track; 316N19950124-track; 316N19950310-track; 316N19950423-track; 316N19950611-track; 316N19950715-track; 316N19950829-track; 316N19951111-track; 316N19951205-track; 316N19961102-track; 316N19971005-track; 318M19780921-track; 318M19780928-track; 318M19790210-track; 318M19790308-track;
    Type: Dataset
    Format: application/zip, 1851 datasets
    Location Call Number Expected Availability
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  • 10
    Publication Date: 2024-02-02
    Keywords: ANT-III/2; ANT-IX/2; ANT-VII/5; ANT-VIII/3; Atlantis II (1963); Bering91; Bering91_trap; BO1_trap; Bouvet_1; Bouvet Island, Southern Ocean (Atlantic sector); Carbon, inorganic, particulate, flux; Carbon, organic, particulate, flux; CB3_trap; DEPTH, water; Duration, number of days; EA8; EA8_trap; EP1_12S_3594m; EP1_2N_2200m; EP1_2S_3593m; EP1_5N_1200m; EP1_5N_2100m; EP1_5N_3800m; EP1_5S_2209m; EP1_9N_2250m; EP1_EQ_2284m; EP1_EQ_3618m; Equatorial Pacific; Event label; G; G_trap; GBN3_trap; GBZ5_trap; H; HAP-13; HAP-13_trap; HAP-4; HAP-4_trap; Jan-Mayen Current; JDF-1; KG1_trap; LATITUDE; LONGITUDE; M; M12/1; M2; M23/3; M3; M4; M5; M9/4; MANOP; MANOP_C; MANOP_C_trap; MANOP_S; MANOP_S_trap; Meteor (1986); MFZ-11; MFZ-11_trap; MFZ-4; MFZ-4_trap; MOOR; Mooring; Mooring (long time); Mooring-EQPAC-1; MOORY; MW; MW_trap; N34-Phase_I; N48-Phase_I; NABE-Mooring; NABE-N34.1; NABE-N48.1; NAP; NAP_trap; NB2; NB3; NB4; NS; NS_trap; OG2; OG3; OG4; Okhotsk92; Okhotsk92_trap; Opal, flux; P82-3; P82-3_trap; P83-4; P83-4_trap; P84-5; P84-5_trap; PAR94_JDF1_trap; PC85-6; PC85-6_trap; PF3_trap; Polar_Front_3; Polar Front; Polarstern; PS06; PS14; PS16; PS18 06AQANTIX_2; Reference/source; SFB313Moorings; Silicon Cycling in the World Ocean; SINOPS; South Atlantic Ocean; TN043_AS2_trap; TN043_AS3_trap; TN043_AS4_trap; TN043_AS5_trap; Total, flux per year; Trap; TRAP; Trap, sediment; TRAPS; VLCN-1_H_trap; VLCN-1_M_trap; WA3_trap; Walvis Ridge, Southeast Atlantic Ocean; Wecoma; WR2_trap; WS1_trap; WS3_trap
    Type: Dataset
    Format: text/tab-separated-values, 431 data points
    Location Call Number Expected Availability
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