Petrography and Magnetic Susceptibility of Recent Litoral Sediments on the Island of Usedom

Fuente: PANGAEA
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Auteurs principaux: Pirrung, Michael, Böhm, Marcus, Merten, Dirk, Kunz-Pirrung, Martina
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2019
Sujets:
Aluminium, oxalate-solvable fraction; Anatase; Calcium, oxalate-solvable fraction; Color code HLS-system; Comment; Counting, stereo microscope; Curie temperature; DEPTH, sediment/rock; Distance; Elevation of event; Epidote; Event label; Feldspar; FM_Ostsee2017-11; FM_Ostsee2017-12; FM_Ostsee2017-13; FM_Ostsee2017-14; FM_Ostsee2017-3; FM_Ostsee2017-4; FM_Ostsee2017-5; FM_Ostsee2017-6; FM_Ostsee2017-7; FM_Ostsee2017-8; FM_Ostsee2017-9; FM_Ostsee2018-1; FM_Ostsee2018-2; FM_Ostsee2018-3; FM_Sackkanal (Usedom)2017-1; FM_Sackkanal2017-1; FM_Swine2017-1; FM_Swine2017-2; Fraction, magnetic; Fraction, non-magnetic; Garnet; Grain size, mean radius; Grain size, median radius; Heavy minerals; Hornblende; Inductively coupled plasma-optical emission spectrometer, ICP-OES; Iron, oxalate-solvable fraction; Latitude of event; Lithoclasts; Lithology/composition/facies; Longitude of event; Magnesium, oxalate-solvable fraction; Magnetic susceptibility meter, Bartington MS2C sensor; Manganese, oxalate-solvable fraction; Marine litter, plastic; Minerals; Munsell Color System (1994); Phosphorus, oxalate-solvable fraction; Potassium, oxalate-solvable fraction; Quartz; Roundness; Sediment sample; SES; Shell debris; Silicon, oxalate-solvable fraction; Skewness; Sodium, oxalate-solvable fraction; Sorting in phi; Sphericity; Susceptibility, frequency dependence; Susceptibility, specific; Susceptibility, specific, ferromagnetic; Susceptibility, specific, non-ferromagnetic; Titanium, oxalate-solvable fraction
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_version_ 1867168200631779328
author Pirrung, Michael
Böhm, Marcus
Merten, Dirk
Kunz-Pirrung, Martina
author_facet Pirrung, Michael
Böhm, Marcus
Merten, Dirk
Kunz-Pirrung, Martina
collection Datos científicos de ciencias marinas y ambientales
contents With reference to the starting questions and aims of this study the following results can be given: 1. Anthropogenic metal fragments and magnetic spherules, present in low concentrations only in the southeastern part of the island of Usedom, probably originate from ships in the harbour of Świnoujście. 2. The heavy mineral garnet in litoral sands is highly correlated with mass-specific magnetic susceptibility, therefore this method is suitable for the detection of placers at Usedom. 3. For spring 2017, lithoclast-rich sands at Ahlbeck indicate coast-parallel net transport from the next cliff with moraine material in a southeastern direction over a distance of several kilometers. 4. Studies in the recent litoral zone of the Island of Usedom demonstrate that by means of the parameters magnetic susceptibility, Munsell value, Mg and Si content of oxalate-solvable fraction, all of them determinable with relatively sparse amount of lab work, an attribution of coastal sands to the sedimentary environments: dunes, beach, fluvial-estuarine zone, is possible; this could help for the interpretation of quaternary sediment sequences with respect to shore distance in sediment cores where no bedding structures or fossils are preserved.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_907802
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Petrography and Magnetic Susceptibility of Recent Litoral Sediments on the Island of Usedom
Pirrung, Michael
Böhm, Marcus
Merten, Dirk
Kunz-Pirrung, Martina
Aluminium, oxalate-solvable fraction; Anatase; Calcium, oxalate-solvable fraction; Color code HLS-system; Comment; Counting, stereo microscope; Curie temperature; DEPTH, sediment/rock; Distance; Elevation of event; Epidote; Event label; Feldspar; FM_Ostsee2017-11; FM_Ostsee2017-12; FM_Ostsee2017-13; FM_Ostsee2017-14; FM_Ostsee2017-3; FM_Ostsee2017-4; FM_Ostsee2017-5; FM_Ostsee2017-6; FM_Ostsee2017-7; FM_Ostsee2017-8; FM_Ostsee2017-9; FM_Ostsee2018-1; FM_Ostsee2018-2; FM_Ostsee2018-3; FM_Sackkanal (Usedom)2017-1; FM_Sackkanal2017-1; FM_Swine2017-1; FM_Swine2017-2; Fraction, magnetic; Fraction, non-magnetic; Garnet; Grain size, mean radius; Grain size, median radius; Heavy minerals; Hornblende; Inductively coupled plasma-optical emission spectrometer, ICP-OES; Iron, oxalate-solvable fraction; Latitude of event; Lithoclasts; Lithology/composition/facies; Longitude of event; Magnesium, oxalate-solvable fraction; Magnetic susceptibility meter, Bartington MS2C sensor; Manganese, oxalate-solvable fraction; Marine litter, plastic; Minerals; Munsell Color System (1994); Phosphorus, oxalate-solvable fraction; Potassium, oxalate-solvable fraction; Quartz; Roundness; Sediment sample; SES; Shell debris; Silicon, oxalate-solvable fraction; Skewness; Sodium, oxalate-solvable fraction; Sorting in phi; Sphericity; Susceptibility, frequency dependence; Susceptibility, specific; Susceptibility, specific, ferromagnetic; Susceptibility, specific, non-ferromagnetic; Titanium, oxalate-solvable fraction
With reference to the starting questions and aims of this study the following results can be given: 1. Anthropogenic metal fragments and magnetic spherules, present in low concentrations only in the southeastern part of the island of Usedom, probably originate from ships in the harbour of Świnoujście. 2. The heavy mineral garnet in litoral sands is highly correlated with mass-specific magnetic susceptibility, therefore this method is suitable for the detection of placers at Usedom. 3. For spring 2017, lithoclast-rich sands at Ahlbeck indicate coast-parallel net transport from the next cliff with moraine material in a southeastern direction over a distance of several kilometers. 4. Studies in the recent litoral zone of the Island of Usedom demonstrate that by means of the parameters magnetic susceptibility, Munsell value, Mg and Si content of oxalate-solvable fraction, all of them determinable with relatively sparse amount of lab work, an attribution of coastal sands to the sedimentary environments: dunes, beach, fluvial-estuarine zone, is possible; this could help for the interpretation of quaternary sediment sequences with respect to shore distance in sediment cores where no bedding structures or fossils are preserved.
title Petrography and Magnetic Susceptibility of Recent Litoral Sediments on the Island of Usedom
topic Aluminium, oxalate-solvable fraction; Anatase; Calcium, oxalate-solvable fraction; Color code HLS-system; Comment; Counting, stereo microscope; Curie temperature; DEPTH, sediment/rock; Distance; Elevation of event; Epidote; Event label; Feldspar; FM_Ostsee2017-11; FM_Ostsee2017-12; FM_Ostsee2017-13; FM_Ostsee2017-14; FM_Ostsee2017-3; FM_Ostsee2017-4; FM_Ostsee2017-5; FM_Ostsee2017-6; FM_Ostsee2017-7; FM_Ostsee2017-8; FM_Ostsee2017-9; FM_Ostsee2018-1; FM_Ostsee2018-2; FM_Ostsee2018-3; FM_Sackkanal (Usedom)2017-1; FM_Sackkanal2017-1; FM_Swine2017-1; FM_Swine2017-2; Fraction, magnetic; Fraction, non-magnetic; Garnet; Grain size, mean radius; Grain size, median radius; Heavy minerals; Hornblende; Inductively coupled plasma-optical emission spectrometer, ICP-OES; Iron, oxalate-solvable fraction; Latitude of event; Lithoclasts; Lithology/composition/facies; Longitude of event; Magnesium, oxalate-solvable fraction; Magnetic susceptibility meter, Bartington MS2C sensor; Manganese, oxalate-solvable fraction; Marine litter, plastic; Minerals; Munsell Color System (1994); Phosphorus, oxalate-solvable fraction; Potassium, oxalate-solvable fraction; Quartz; Roundness; Sediment sample; SES; Shell debris; Silicon, oxalate-solvable fraction; Skewness; Sodium, oxalate-solvable fraction; Sorting in phi; Sphericity; Susceptibility, frequency dependence; Susceptibility, specific; Susceptibility, specific, ferromagnetic; Susceptibility, specific, non-ferromagnetic; Titanium, oxalate-solvable fraction
url https://doi.org/10.1594/PANGAEA.907802