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dc.contributor.authorKuenzler, Edward J.  Concept link
dc.date.accessioned2020-01-22T20:39:04Z
dc.date.available2020-01-22T20:39:04Z
dc.date.issued1965-02
dc.identifier.urihttps://hdl.handle.net/1912/25237
dc.description.abstractAn evaluation was made of the importance of marine zooplankton in elemental cycling and transport of elements through the thermocline. Zooplankton density was measured in the eastern Pacific Ocean. Some measurement of elemental elimination rates were made using zooplankton labeled by fallout from a nuclear test; other measurements used animals tagged with tracer Il31 or ca58. The turnover time for cobalt in the upper 100 m of the sea is not more than 100 years based on cobalt flux rates in zooplankton alone (U).en_US
dc.description.sponsorshipU. S. Atomic Energy Commission contract AT(30-l) -3145en_US
dc.language.isoen_USen_US
dc.publisherWoods Hole Oceanographic Institutionen_US
dc.relation.ispartofseriesWHOI Technical Reportsen_US
dc.relation.ispartofseriesWHOI-en_US
dc.subjectZooplankton
dc.subjectMarine ecology
dc.titleZooplankton distribution and isotope turnover during Operation Swordfishen_US
dc.typeTechnical Reporten_US
dc.identifier.doi10.1575/1912/25237


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