Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history

M. Drodt; A. X. Trautwein; Iris König; E. Suess; M. J. Dekkers

doi:10.1007/BF02458915

Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history

M. Drodt^*, A. X. Trautwein, Iris König, E. Suess, M. J. Dekkers

^*Corresponding author for this work

Institute of Physics

1 Citation (Scopus)

Abstract

Sediment cores with different sub-bottom depths (I: 45 cm and II: 700 cm) from the Peru Basin have been investigated. From the depth profile of the relative amount of Fe(II) a redox zone is obtained which correlates with the organic carbon flux into the sediment (core I). Mössbauer parameters suggest that the iron in the sediments is mainly contained in clay minerals and to varying extent also in goethite.

Original language	English
Journal	Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics
Volume	18
Issue number	2-3
Pages (from-to)	341-345
Number of pages	5
ISSN	0392-6737
DOIs	https://doi.org/10.1007/BF02458915
Publication status	Published - 01.01.1996

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10.1007/BF02458915

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Drodt, M., Trautwein, A. X., König, I., Suess, E., & Dekkers, M. J. (1996). Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history. Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics, 18(2-3), 341-345. https://doi.org/10.1007/BF02458915

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title = "M{\"o}ssbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history",

abstract = "Sediment cores with different sub-bottom depths (I: 45 cm and II: 700 cm) from the Peru Basin have been investigated. From the depth profile of the relative amount of Fe(II) a redox zone is obtained which correlates with the organic carbon flux into the sediment (core I). M{\"o}ssbauer parameters suggest that the iron in the sediments is mainly contained in clay minerals and to varying extent also in goethite.",

author = "M. Drodt and Trautwein, \{A. X.\} and Iris K{\"o}nig and E. Suess and Dekkers, \{M. J.\}",

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Drodt, M, Trautwein, AX, König, I, Suess, E & Dekkers, MJ 1996, 'Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history', Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics, vol. 18, no. 2-3, pp. 341-345. https://doi.org/10.1007/BF02458915

Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history. / Drodt, M.; Trautwein, A. X.; König, Iris et al.
In: Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics, Vol. 18, No. 2-3, 01.01.1996, p. 341-345.

Research output: Journal Articles › Scientific review articles › Research

TY - JOUR

T1 - Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history

AU - Drodt, M.

AU - Trautwein, A. X.

AU - König, Iris

AU - Suess, E.

AU - Dekkers, M. J.

PY - 1996/1/1

Y1 - 1996/1/1

N2 - Sediment cores with different sub-bottom depths (I: 45 cm and II: 700 cm) from the Peru Basin have been investigated. From the depth profile of the relative amount of Fe(II) a redox zone is obtained which correlates with the organic carbon flux into the sediment (core I). Mössbauer parameters suggest that the iron in the sediments is mainly contained in clay minerals and to varying extent also in goethite.

AB - Sediment cores with different sub-bottom depths (I: 45 cm and II: 700 cm) from the Peru Basin have been investigated. From the depth profile of the relative amount of Fe(II) a redox zone is obtained which correlates with the organic carbon flux into the sediment (core I). Mössbauer parameters suggest that the iron in the sediments is mainly contained in clay minerals and to varying extent also in goethite.

UR - https://www.scopus.com/pages/publications/0040596895

U2 - 10.1007/BF02458915

DO - 10.1007/BF02458915

M3 - Scientific review articles

AN - SCOPUS:0040596895

SN - 0392-6737

VL - 18

SP - 341

EP - 345

JO - Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics

JF - Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics

IS - 2-3

ER -

Drodt M, Trautwein AX, König I, Suess E, Dekkers MJ. Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history. Nuovo Cimento della Societa Italiana di Fisica D - Condensed Matter, Atomic, Molecular and Chemical Physics, Biophysics. 1996 Jan 1;18(2-3):341-345. doi: 10.1007/BF02458915

Mössbauer, X-ray fluorescence and paleomagnetic studies of deep-sea sediments from the Peru Basin: Two million years of sedimentation history

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