(Table 1) Turbidity, temperature, and salinity in the hydrothermal plume and background waters above the northern part of the Mohn's Ridge at Station AMK36-3573-5

In July 1995 geological and biological studies in the axial zone of the northern part of the Mohn's Ridge (72°20'N) were carried out during Cruise 36 of R/V Akademik Mstislav Keldysh. Slopes of the neovolcanic zone, as well as a caldera on its crest were investigated with use of deep-sea m...

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Bibliographic Details
Main Authors: Bogdanov, Yury A, Sagalevich, Anatoly M, Galkin, Sergey V, Chernyaev, Evgeny S, Lukashin, Vyacheslav N, Ivanov, Georgy V
Format: Dataset
Language:English
Published: PANGAEA 1997
Subjects:
Akademik Mstislav Keldysh
AMK36
AMK36-3573-5
Archive of Ocean Data
ARCOD
CTD
Neil Brown
CTD/Rosette
CTD-RO
DEPTH
water
Mohns Ridge
Norwegian Sea
Salinity
Temperature
Turbidity (Nephelometric turbidity unit)
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.760164
https://doi.org/10.1594/PANGAEA.760164
Description
Summary:In July 1995 geological and biological studies in the axial zone of the northern part of the Mohn's Ridge (72°20'N) were carried out during Cruise 36 of R/V Akademik Mstislav Keldysh. Slopes of the neovolcanic zone, as well as a caldera on its crest were investigated with use of deep-sea manned submersibles Mir, geological and biological samples were also collected. Use of the Rosette sounding complex provided recognition of several major hydrothermal plumes. Bottom sediments of the marginal depression are enriched in metals characteristic for hydrothermal metalliferous sediments. Thus, a new unknown hydrothermal field was found.

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