Grain-size distribution and grain-size dependent magnetic susceptibility of sediment core GeoB18530-1
Since the weight percentages of (classifiable) IRD particles > 1 mm and (unclassifiable, but separable) IRD particles > 125 µm both largely underestimate the total content and magnetic impact of IRD, it is important to quantify also the finer IRD fractions and their magnetic susceptibilities....
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.971771 2024-09-15T18:02:34+00:00 Grain-size distribution and grain-size dependent magnetic susceptibility of sediment core GeoB18530-1 Bukar, Shettima von Dobeneck, Tilo LATITUDE: 42.839500 * LONGITUDE: -49.234833 * DATE/TIME START: 2014-06-14T13:58:00 * DATE/TIME END: 2014-06-14T13:58:00 * MINIMUM DEPTH, sediment/rock: 5.8330 m * MAXIMUM DEPTH, sediment/rock: 6.6035 m text/tab-separated-values, 336 data points https://doi.pangaea.de/10.1594/PANGAEA.971771 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.971785 Bukar, Shettima; von Dobeneck, Tilo; Wang, Yiyun; Frederichs, Thomas; Dallanave, Edoardo; St-Onge, Guillaume (submitted): Ice-Rafted Detritus (IRD) of the SE Grand Banks Slope, Newfoundland, Throughout Heinrich Layers 1 to 6 - Part II: Magnetic Properties. Geochemistry, Geophysics, Geosystems von Dobeneck, Tilo; Bukar, Shettima: Petrological classification and lithology-specific abundance analysis of ice-rafted detritus (IRD) of sediment core GeoB18530-1 [dataset bundled publication]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.971290 https://doi.pangaea.de/10.1594/PANGAEA.971771 CC-BY-4.0: Creative Commons Attribution 4.0 International (License comes into effect after moratorium ends) Access constraints: access rights needed info:eu-repo/semantics/restrictedAccess 509-1 ArcTrain Calculated DEPTH sediment/rock bottom/maximum top/minimum GC GeoB18530-1 Geochemistry Grain size maximum minimum grain size distribution Grand Banks Margin Gravity corer Heinrich event Heinrich events Ice-Rafted Detritus Kappabridge AGICO KLY-2 Magnetic susceptibility Maria S. Merian MSM39 Precision scale Sartorius Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic rock magnetism SE Grand Banks Slope Size fraction Wet sieve shaker dataset ftpangaea 2024-08-21T00:02:28Z Since the weight percentages of (classifiable) IRD particles > 1 mm and (unclassifiable, but separable) IRD particles > 125 µm both largely underestimate the total content and magnetic impact of IRD, it is important to quantify also the finer IRD fractions and their magnetic susceptibilities. From each of the IRD-rich sediment units H1, I1 and H2, six magnetic cube samples of 6.2 cm³ each were combined, dried, weighed and ultrasonically suspended in water. These three slurries were successively washed through 16 stacked sieves with mesh sizes in approximately 0.5 phi steps from 4000 µm to 5 µm using a Fritsch wet sieve shaker. The sieve fractions were carefully collected, dried, weighed and measured in a Kappabridge KLY2 susceptometer. The data and therefrom-derived partial susceptibilities and cumulative distributions clearly demonstrate that the magnetically most dominant and "volatile" sediment particles fall into the 40-125 µm range. Detrital particles of such sizes are too coarse to have been current-transported over long distances and were therefore probably at least partially ice-rafted. Dataset Climate change Magnetic susceptibility North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-49.234833,-49.234833,42.839500,42.839500) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
509-1 ArcTrain Calculated DEPTH sediment/rock bottom/maximum top/minimum GC GeoB18530-1 Geochemistry Grain size maximum minimum grain size distribution Grand Banks Margin Gravity corer Heinrich event Heinrich events Ice-Rafted Detritus Kappabridge AGICO KLY-2 Magnetic susceptibility Maria S. Merian MSM39 Precision scale Sartorius Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic rock magnetism SE Grand Banks Slope Size fraction Wet sieve shaker |
spellingShingle |
509-1 ArcTrain Calculated DEPTH sediment/rock bottom/maximum top/minimum GC GeoB18530-1 Geochemistry Grain size maximum minimum grain size distribution Grand Banks Margin Gravity corer Heinrich event Heinrich events Ice-Rafted Detritus Kappabridge AGICO KLY-2 Magnetic susceptibility Maria S. Merian MSM39 Precision scale Sartorius Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic rock magnetism SE Grand Banks Slope Size fraction Wet sieve shaker Bukar, Shettima von Dobeneck, Tilo Grain-size distribution and grain-size dependent magnetic susceptibility of sediment core GeoB18530-1 |
topic_facet |
509-1 ArcTrain Calculated DEPTH sediment/rock bottom/maximum top/minimum GC GeoB18530-1 Geochemistry Grain size maximum minimum grain size distribution Grand Banks Margin Gravity corer Heinrich event Heinrich events Ice-Rafted Detritus Kappabridge AGICO KLY-2 Magnetic susceptibility Maria S. Merian MSM39 Precision scale Sartorius Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic rock magnetism SE Grand Banks Slope Size fraction Wet sieve shaker |
description |
Since the weight percentages of (classifiable) IRD particles > 1 mm and (unclassifiable, but separable) IRD particles > 125 µm both largely underestimate the total content and magnetic impact of IRD, it is important to quantify also the finer IRD fractions and their magnetic susceptibilities. From each of the IRD-rich sediment units H1, I1 and H2, six magnetic cube samples of 6.2 cm³ each were combined, dried, weighed and ultrasonically suspended in water. These three slurries were successively washed through 16 stacked sieves with mesh sizes in approximately 0.5 phi steps from 4000 µm to 5 µm using a Fritsch wet sieve shaker. The sieve fractions were carefully collected, dried, weighed and measured in a Kappabridge KLY2 susceptometer. The data and therefrom-derived partial susceptibilities and cumulative distributions clearly demonstrate that the magnetically most dominant and "volatile" sediment particles fall into the 40-125 µm range. Detrital particles of such sizes are too coarse to have been current-transported over long distances and were therefore probably at least partially ice-rafted. |
format |
Dataset |
author |
Bukar, Shettima von Dobeneck, Tilo |
author_facet |
Bukar, Shettima von Dobeneck, Tilo |
author_sort |
Bukar, Shettima |
title |
Grain-size distribution and grain-size dependent magnetic susceptibility of sediment core GeoB18530-1 |
title_short |
Grain-size distribution and grain-size dependent magnetic susceptibility of sediment core GeoB18530-1 |
title_full |
Grain-size distribution and grain-size dependent magnetic susceptibility of sediment core GeoB18530-1 |
title_fullStr |
Grain-size distribution and grain-size dependent magnetic susceptibility of sediment core GeoB18530-1 |
title_full_unstemmed |
Grain-size distribution and grain-size dependent magnetic susceptibility of sediment core GeoB18530-1 |
title_sort |
grain-size distribution and grain-size dependent magnetic susceptibility of sediment core geob18530-1 |
publisher |
PANGAEA |
url |
https://doi.pangaea.de/10.1594/PANGAEA.971771 |
op_coverage |
LATITUDE: 42.839500 * LONGITUDE: -49.234833 * DATE/TIME START: 2014-06-14T13:58:00 * DATE/TIME END: 2014-06-14T13:58:00 * MINIMUM DEPTH, sediment/rock: 5.8330 m * MAXIMUM DEPTH, sediment/rock: 6.6035 m |
long_lat |
ENVELOPE(-49.234833,-49.234833,42.839500,42.839500) |
genre |
Climate change Magnetic susceptibility North Atlantic |
genre_facet |
Climate change Magnetic susceptibility North Atlantic |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.971785 Bukar, Shettima; von Dobeneck, Tilo; Wang, Yiyun; Frederichs, Thomas; Dallanave, Edoardo; St-Onge, Guillaume (submitted): Ice-Rafted Detritus (IRD) of the SE Grand Banks Slope, Newfoundland, Throughout Heinrich Layers 1 to 6 - Part II: Magnetic Properties. Geochemistry, Geophysics, Geosystems von Dobeneck, Tilo; Bukar, Shettima: Petrological classification and lithology-specific abundance analysis of ice-rafted detritus (IRD) of sediment core GeoB18530-1 [dataset bundled publication]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.971290 https://doi.pangaea.de/10.1594/PANGAEA.971771 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International (License comes into effect after moratorium ends) Access constraints: access rights needed info:eu-repo/semantics/restrictedAccess |
_version_ |
1810440016444260352 |