Verhalten von Radiolarienschalen aus dem Zentralpazifik bei der Diagenese

Marchig, Vesna; Gundlach, H.; Schnier, C.

doi:10.1007/bf02274686

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Equatorial N Pacific Nodules1

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1979

1982

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Cited by 11 publications

(1 citation statement)

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“…The enhanced concentration of Mn, Ni, Cu and Zn in these nodules is due to the dissolution of siliceous tests within the sediment column which leads to the enhanced concentration of these elements in the nodule structure [35]. The incorporation of these divalent transition metal ions in the nodule structure in turn stabilizes 10 A manganite as the principal manganese oxide phase within the nodule [36].…”

Section: Equatorial N Pacific Nodulesmentioning

confidence: 99%

Manganese nodule formation in the Pacific Ocean: a general theory

et al. 1982

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An attempt is made to outline a satisfactory general theory for the formation of Pacific deep-sea manganese nodules based on a consideration of the time of initiation of formation of the nodules, a mechanism of maintenance of the nodules at the sediment surface and the role of biological productivity of the surface waters in influencing nodule characteristics. Using this model, the principal physical, chemical and distributional features of the nodules and reasons for their differences on a regional scale in the Pacific can be interpreted.

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Section: Equatorial N Pacific Nodulesmentioning

confidence: 99%