The distribution of zinc, cadmium, copper and iron in seawater of the Iceland-Faroe Ridge area

• Main Authors: Kremling, Klaus, Petersen, Hauke
• Format: Dataset
• Language: English
• Published: PANGAEA 1977
• Subjects: Iceland-Faroe Ridge; M31; M31_254; M31_257; M31_260; M31_262; M31_264; M31_266; M31_270; M31_272; M31_274; M31_277; M31_283; M31_298; M31_299; M31_300; M31_302; M31_304; M31_305; M31_306; Meteor (1964); Overflow 73; Water sample; WS; Arctic; Norwegian Sea; Iceland; North Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.604013; https://doi.org/10.1594/PANGAEA.604013

During the International ICES Expedition "Overflow '73" a total of 174 samples from 18 stations were collected by R. V. "Meteor" in the waters of the Iceland-Faroe Ridge area. They were filtered on board ship (through 0.4 mym „Nuclepore“ filters), then stored in 500 cm**3 quartz bottles (at -20 °C) and analyzed in air-filtered laboratories on land for zinc and cadmium by means of the differential pulse anodic stripping voltammetry technique and copper and iron by flameless atomic absorption spectrometry. The overall averages of 1.9 myg Zn l**-1, 0.07 myg Cd l**-1, 0.5 myg Cu l**-1 and 0.9 myg Fe l**-1 are in good agreement with recent "baseline" studies of open-ocean waters. The mixture of low salinity water masses from the North Iceland Shelf/Arctic Intermediate Waters seem to maintain distinctly lower concentration of Cd, Cu and Fe than the waters from the North Atlantic and the Norwegian Sea where quite similar mean values are found. There is only little evidence for the assumption that overflow events on the ridge are influencing the concentrations of dissolved metals in the near-bottom layers.