(Table 3) Mineral compositions and lengths of mollusk shells from some hydrothermal fields of the Mid-Atlantic Ridge and East Pacific Rise
Cobertura |
MEDIAN LATITUDE: 25.634167 * MEDIAN LONGITUDE: -73.344167 * SOUTH-BOUND LATITUDE: 9.833333 * WEST-BOUND LONGITUDE: -111.400000 * NORTH-BOUND LATITUDE: 37.840000 * EAST-BOUND LONGITUDE: -31.520000 * MINIMUM ELEVATION: -3480.0 m * MAXIMUM ELEVATION: -2250.0 m |
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Data(s) |
07/09/2012
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Formato |
text/tab-separated-values, 108 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.788331 doi:10.1594/PANGAEA.788331 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.788382 Demina, Lyudmila L; Galkin, Sergey V; Dara, OM (2012): Trace metal bioaccumulation in the shells of mussels and clams at deep-sea hydrothermal vent fields. Translated from Geokhimiya, 2012, 50(2), 147-163, Geochemistry International, 50(2), 133-147, doi:10.1134/S0016702911120056 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow |
Palavras-Chave | #Akademik Mstislav Keldysh; AMK49; AMK49-4582; AMK49-4611; AMK49-4623; AMK49-4675; AMK49-4679; AMK50; AMK50-4714; AMK50-4797; AMK50-4819; Aragonite; Archive of Ocean Data; ARCOD; Area/locality; Broken Spur Hydrothermal Field; Calcite; Elevation of event; Elevation of event 2; Event label; Guaymas Basin, Gulf of California; Hydrothermal area 21°N, EPR; Hydrothermal area 9°50N, EPR; Latitude of event; Longitude of event; Menez Gwen hydrothermal field; MIR; MIR deep-sea manned submersible; Rainbow Hydrothermal Field; Ruler tape; Sample, optional label/labor no; Sample comment; Shell length; Snake Pit Hydrothermal Field; Taxon/taxa; X-ray diffraction (XRD) |
Tipo |
Dataset |