Water chemistry
Cobertura |
MEDIAN LATITUDE: 0.436364 * MEDIAN LONGITUDE: -127.624545 * SOUTH-BOUND LATITUDE: -12.000000 * WEST-BOUND LONGITUDE: -145.400000 * NORTH-BOUND LATITUDE: 9.000000 * EAST-BOUND LONGITUDE: -92.000000 * DATE/TIME START: 1990-06-26T00:00:00 * DATE/TIME END: 1993-11-15T00:00:00 * MINIMUM DEPTH, water: 20 m * MAXIMUM DEPTH, water: 2400 m |
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Data(s) |
18/04/2000
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Formato |
text/tab-separated-values, 1002 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.56600 doi:10.1594/PANGAEA.56600 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
Johnson, Kenneth S; Gordon, R Michael; Coale, Kenneth H (1997): What controls dissolved iron in the world ocean? Marine Chemistry, 57(3-4), 137-162, doi:10.1016/S0304-4203(97)00043-1 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #compiled data; DATE/TIME; DEPTH, water; Event label; FeLine3N; FeLine3S; FeLine6N; FeLine9N; FeLineO; GOFLO; Go-Flo bottles; Iron, dissolved; Iron, particulate; JGOFSEqPacFall; JGOFSEqPacSpringA; JGOFSEqPacSpringB; Latitude of event; Longitude of event; Nitrate; Oxygen; Oxygen, apparent utilization; Phosphate; PlumExStation11; PlumExStation8; PlumExStation9; Salinity; see reference(s); Silicate; Silicon Cycling in the World Ocean; SINOPS; Temperature, water; World Ocean |
Tipo |
Dataset |