Rock magnetic, geochemical and sedimentological properties related to IRD composition and content of sediment core GeoB18530-1
The IRD-rich Heinrich Event (HE) layers of gravity core GeoB18530-1, retrieved from the SE Grand Banks slope of Newfoundland, coincide with bulk magnetic susceptibility maxima. This positive correlation of IRD content and susceptibility is widely observed and at first glance contradictive, since det...
Main Authors: | , |
---|---|
Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.971785 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.971785 |
---|---|
record_format |
openpolar |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.971785 2024-09-15T18:02:34+00:00 Rock magnetic, geochemical and sedimentological properties related to IRD composition and content of sediment core GeoB18530-1 von Dobeneck, Tilo Bukar, Shettima LATITUDE: 42.839500 * LONGITUDE: -49.234833 * DATE/TIME START: 2014-06-14T13:58:00 * DATE/TIME END: 2014-06-14T13:58:00 application/zip, 8 datasets https://doi.pangaea.de/10.1594/PANGAEA.971785 en eng PANGAEA 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.971785 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 ArcTrain Geochemistry grain size distribution Grand Banks Margin Heinrich events Ice-Rafted Detritus Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic rock magnetism dataset bundled publication ftpangaea 2024-08-21T00:02:25Z The IRD-rich Heinrich Event (HE) layers of gravity core GeoB18530-1, retrieved from the SE Grand Banks slope of Newfoundland, coincide with bulk magnetic susceptibility maxima. This positive correlation of IRD content and susceptibility is widely observed and at first glance contradictive, since detrital dolomite, the most common IRD component, is weakly magnetic and should therefore reduce rather than enhance bulk magnetic susceptibility. As Part I of the associated manuscripts (Bukar et al., submitted) showed, the petrology of HLs is rather diverse; some prominent magmatic and metamorphic IRD species should actually have relatively high magnetic susceptibilities. This data set bundle comprises a collection of bulk rock magnetic, geochemical and sedimentological sediment records revealing the influence of specific magnetic mineral fractions, IRD lithologies and textural properties on the magnetic susceptibility signal. Part II of the associated manuscripts (Bukar et al., submitted) also features so far unreported rock magnetic property data of all observed IRD lithologies. These susceptibility, IRM, ARM and HIRM data were acquired from large or pooled (granule to gravel size) classified IRD specimens. Since IRD particles are not limited to larger grain sizes, three composite bulk sediment samples from units H1, I1 and H2 were wet-sieved to reveal the grain-size dependence of magnetic susceptibility. Six linear regression models finally compare the predictability of magnetic susceptibility from rock magnetic, geochemical, sedimentological and petrological data. Other/Unknown Material Climate change Magnetic susceptibility Newfoundland 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 |
ArcTrain Geochemistry grain size distribution Grand Banks Margin Heinrich events Ice-Rafted Detritus Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic rock magnetism |
spellingShingle |
ArcTrain Geochemistry grain size distribution Grand Banks Margin Heinrich events Ice-Rafted Detritus Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic rock magnetism von Dobeneck, Tilo Bukar, Shettima Rock magnetic, geochemical and sedimentological properties related to IRD composition and content of sediment core GeoB18530-1 |
topic_facet |
ArcTrain Geochemistry grain size distribution Grand Banks Margin Heinrich events Ice-Rafted Detritus Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic rock magnetism |
description |
The IRD-rich Heinrich Event (HE) layers of gravity core GeoB18530-1, retrieved from the SE Grand Banks slope of Newfoundland, coincide with bulk magnetic susceptibility maxima. This positive correlation of IRD content and susceptibility is widely observed and at first glance contradictive, since detrital dolomite, the most common IRD component, is weakly magnetic and should therefore reduce rather than enhance bulk magnetic susceptibility. As Part I of the associated manuscripts (Bukar et al., submitted) showed, the petrology of HLs is rather diverse; some prominent magmatic and metamorphic IRD species should actually have relatively high magnetic susceptibilities. This data set bundle comprises a collection of bulk rock magnetic, geochemical and sedimentological sediment records revealing the influence of specific magnetic mineral fractions, IRD lithologies and textural properties on the magnetic susceptibility signal. Part II of the associated manuscripts (Bukar et al., submitted) also features so far unreported rock magnetic property data of all observed IRD lithologies. These susceptibility, IRM, ARM and HIRM data were acquired from large or pooled (granule to gravel size) classified IRD specimens. Since IRD particles are not limited to larger grain sizes, three composite bulk sediment samples from units H1, I1 and H2 were wet-sieved to reveal the grain-size dependence of magnetic susceptibility. Six linear regression models finally compare the predictability of magnetic susceptibility from rock magnetic, geochemical, sedimentological and petrological data. |
format |
Other/Unknown Material |
author |
von Dobeneck, Tilo Bukar, Shettima |
author_facet |
von Dobeneck, Tilo Bukar, Shettima |
author_sort |
von Dobeneck, Tilo |
title |
Rock magnetic, geochemical and sedimentological properties related to IRD composition and content of sediment core GeoB18530-1 |
title_short |
Rock magnetic, geochemical and sedimentological properties related to IRD composition and content of sediment core GeoB18530-1 |
title_full |
Rock magnetic, geochemical and sedimentological properties related to IRD composition and content of sediment core GeoB18530-1 |
title_fullStr |
Rock magnetic, geochemical and sedimentological properties related to IRD composition and content of sediment core GeoB18530-1 |
title_full_unstemmed |
Rock magnetic, geochemical and sedimentological properties related to IRD composition and content of sediment core GeoB18530-1 |
title_sort |
rock magnetic, geochemical and sedimentological properties related to ird composition and content of sediment core geob18530-1 |
publisher |
PANGAEA |
url |
https://doi.pangaea.de/10.1594/PANGAEA.971785 |
op_coverage |
LATITUDE: 42.839500 * LONGITUDE: -49.234833 * DATE/TIME START: 2014-06-14T13:58:00 * DATE/TIME END: 2014-06-14T13:58:00 |
long_lat |
ENVELOPE(-49.234833,-49.234833,42.839500,42.839500) |
genre |
Climate change Magnetic susceptibility Newfoundland North Atlantic |
genre_facet |
Climate change Magnetic susceptibility Newfoundland North Atlantic |
op_relation |
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.971785 |
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_ |
1810440016617275392 |