id ftdatacite:10.1594/pangaea.942078
record_format openpolar
spelling ftdatacite:10.1594/pangaea.942078 2024-09-09T19:22:30+00:00 Mineral composition of sediment core PG2208 ... Biskaborn, Boris K Nazarova, Larisa B Kröger, Tim Pestryakova, Luidmila A Syrykh, Luidmila S Pfalz, Gregor Herzschuh, Ulrike Diekmann, Bernhard 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.942078 https://doi.pangaea.de/10.1594/PANGAEA.942078 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.942083 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 diatoms Lake sediment core lake sediment proxies Siberia Siberian Arctic DEPTH, sediment/rock Intensity, total Quartz Intensity, 3.34Å Quartz Intensity, 4.26Å Plagioclase Intensity, 3.19Å Kalifeldspar Intensity, 3.24Å Hornblende Intensity, 8.4Å Calcite Intensity, 3.024Å Dolomite Intensity, 2.88Å Illite Intensity, 10Å Illite Intensity, 5Å Chlorite Intensity, 14Å Chlorite Intensity, 7Å Composite Core X-ray diffractometry XRD PHILIPS PW1820 goniometer RU-Land_2013_Yakutia AWI Arctic Land Expedition Paleo Modelling PalMod Polar Terrestrial Environmental Systems @ AWI AWI_Envi Dataset dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.94207810.1594/pangaea.942083 2024-07-03T10:20:00Z To analyze the mineralogical composition of sediments we freeze-dried and milled 19 samples for X-ray diffractometry (XRD) using a PHILIPS PW1820 goniometer (40 kV, 40 mA, from 3 to 100°, step-rate 0.05°, Co ka radiation). Data processing was performed using the free software MacDiff 4.0.7. To avoid influence of opal and organic matter in the samples (Voigt, 2009), we used the ratio of the peak area intensities of each mineral to the sum of the peak area intensities of all detected minerals, and used this value to estimate percentages. ... Dataset Arctic Siberia DataCite Arctic
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic diatoms
Lake sediment core
lake sediment proxies
Siberia
Siberian Arctic
DEPTH, sediment/rock
Intensity, total
Quartz Intensity, 3.34Å
Quartz Intensity, 4.26Å
Plagioclase Intensity, 3.19Å
Kalifeldspar Intensity, 3.24Å
Hornblende Intensity, 8.4Å
Calcite Intensity, 3.024Å
Dolomite Intensity, 2.88Å
Illite Intensity, 10Å
Illite Intensity, 5Å
Chlorite Intensity, 14Å
Chlorite Intensity, 7Å
Composite Core
X-ray diffractometry XRD PHILIPS PW1820 goniometer
RU-Land_2013_Yakutia
AWI Arctic Land Expedition
Paleo Modelling PalMod
Polar Terrestrial Environmental Systems @ AWI AWI_Envi
spellingShingle diatoms
Lake sediment core
lake sediment proxies
Siberia
Siberian Arctic
DEPTH, sediment/rock
Intensity, total
Quartz Intensity, 3.34Å
Quartz Intensity, 4.26Å
Plagioclase Intensity, 3.19Å
Kalifeldspar Intensity, 3.24Å
Hornblende Intensity, 8.4Å
Calcite Intensity, 3.024Å
Dolomite Intensity, 2.88Å
Illite Intensity, 10Å
Illite Intensity, 5Å
Chlorite Intensity, 14Å
Chlorite Intensity, 7Å
Composite Core
X-ray diffractometry XRD PHILIPS PW1820 goniometer
RU-Land_2013_Yakutia
AWI Arctic Land Expedition
Paleo Modelling PalMod
Polar Terrestrial Environmental Systems @ AWI AWI_Envi
Biskaborn, Boris K
Nazarova, Larisa B
Kröger, Tim
Pestryakova, Luidmila A
Syrykh, Luidmila S
Pfalz, Gregor
Herzschuh, Ulrike
Diekmann, Bernhard
Mineral composition of sediment core PG2208 ...
topic_facet diatoms
Lake sediment core
lake sediment proxies
Siberia
Siberian Arctic
DEPTH, sediment/rock
Intensity, total
Quartz Intensity, 3.34Å
Quartz Intensity, 4.26Å
Plagioclase Intensity, 3.19Å
Kalifeldspar Intensity, 3.24Å
Hornblende Intensity, 8.4Å
Calcite Intensity, 3.024Å
Dolomite Intensity, 2.88Å
Illite Intensity, 10Å
Illite Intensity, 5Å
Chlorite Intensity, 14Å
Chlorite Intensity, 7Å
Composite Core
X-ray diffractometry XRD PHILIPS PW1820 goniometer
RU-Land_2013_Yakutia
AWI Arctic Land Expedition
Paleo Modelling PalMod
Polar Terrestrial Environmental Systems @ AWI AWI_Envi
description To analyze the mineralogical composition of sediments we freeze-dried and milled 19 samples for X-ray diffractometry (XRD) using a PHILIPS PW1820 goniometer (40 kV, 40 mA, from 3 to 100°, step-rate 0.05°, Co ka radiation). Data processing was performed using the free software MacDiff 4.0.7. To avoid influence of opal and organic matter in the samples (Voigt, 2009), we used the ratio of the peak area intensities of each mineral to the sum of the peak area intensities of all detected minerals, and used this value to estimate percentages. ...
format Dataset
author Biskaborn, Boris K
Nazarova, Larisa B
Kröger, Tim
Pestryakova, Luidmila A
Syrykh, Luidmila S
Pfalz, Gregor
Herzschuh, Ulrike
Diekmann, Bernhard
author_facet Biskaborn, Boris K
Nazarova, Larisa B
Kröger, Tim
Pestryakova, Luidmila A
Syrykh, Luidmila S
Pfalz, Gregor
Herzschuh, Ulrike
Diekmann, Bernhard
author_sort Biskaborn, Boris K
title Mineral composition of sediment core PG2208 ...
title_short Mineral composition of sediment core PG2208 ...
title_full Mineral composition of sediment core PG2208 ...
title_fullStr Mineral composition of sediment core PG2208 ...
title_full_unstemmed Mineral composition of sediment core PG2208 ...
title_sort mineral composition of sediment core pg2208 ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.942078
https://doi.pangaea.de/10.1594/PANGAEA.942078
geographic Arctic
geographic_facet Arctic
genre Arctic
Siberia
genre_facet Arctic
Siberia
op_relation https://dx.doi.org/10.1594/pangaea.942083
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.94207810.1594/pangaea.942083
_version_ 1809762796110348288