Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306
The data comprise meters composite depth (mcd) versus volume susceptibility (x10-3 SI) and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. The anhysteretic magnetization (ARM) was measu...
Main Authors: | , , , |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2021
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.926657 https://doi.org/10.1594/PANGAEA.926657 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.926657 |
---|---|
record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
303-U1306 Anhysteretic susceptibility/magnetic susceptibility COMPCORE Composite Core Deep Western Boundary Current DEPTH sediment/rock Eirik Drift Exp303 Joides Resolution Magnetic susceptibility volume North Atlantic North Atlantic Climate 1 Northwest Atlantic Oxygen isotopes Quaternary relative paleointensity see Channell et al. (2014) |
spellingShingle |
303-U1306 Anhysteretic susceptibility/magnetic susceptibility COMPCORE Composite Core Deep Western Boundary Current DEPTH sediment/rock Eirik Drift Exp303 Joides Resolution Magnetic susceptibility volume North Atlantic North Atlantic Climate 1 Northwest Atlantic Oxygen isotopes Quaternary relative paleointensity see Channell et al. (2014) Channell, James E T Wright, James D Mazaud, Alain Stoner, Joseph S Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 |
topic_facet |
303-U1306 Anhysteretic susceptibility/magnetic susceptibility COMPCORE Composite Core Deep Western Boundary Current DEPTH sediment/rock Eirik Drift Exp303 Joides Resolution Magnetic susceptibility volume North Atlantic North Atlantic Climate 1 Northwest Atlantic Oxygen isotopes Quaternary relative paleointensity see Channell et al. (2014) |
description |
The data comprise meters composite depth (mcd) versus volume susceptibility (x10-3 SI) and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. The anhysteretic magnetization (ARM) was measured on a pass-through u-channel magnetometer and the volume susceptibilities were measured on a pass-through (u-channel) susceptibility bridge (see Channell et al., 2014). Planktic oxygen isotope (δ18O) and relative paleointensity (RPI) data are used in tandem to generate an age model for the last 1 Myr from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. For the 1-1.5 Ma interval, the age model is based on RPI alone due to insufficient foraminifera for isotope analyses. Utilizing RPI and δ18O in tandem allows recognition of low-δ18O "events" prior to glacial Terminations I, III, IV, V, VII, VIII, IX and X, that are independently supported by radiocarbon dates through the last deglaciation, and are attributed to local or regional surface-water effects. At Site U1306, Quaternary sedimentation rates (mean ~15 cm/kyr) are elevated during peak glacials and glacial onsets, and are reduced during interglacials, in contrast to the pattern at Site U1305 in 3460 m water depth at the distal toe of the drift, 191 km SW of Site U1306. The contrasting sedimentation-rate pattern appears to hold for the entire ~1.5 Myr record. The slackening and/or shoaling (due to lowered salinity) of the Deep Western Boundary Current (DWBC) during glacial intervals coincided with greater sediment supply to Site U1306 whereas the deepening, and possibly increased vigor, of the DWBC during interglacial intervals boosted sediment supply to Site U1305. |
format |
Dataset |
author |
Channell, James E T Wright, James D Mazaud, Alain Stoner, Joseph S |
author_facet |
Channell, James E T Wright, James D Mazaud, Alain Stoner, Joseph S |
author_sort |
Channell, James E T |
title |
Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 |
title_short |
Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 |
title_full |
Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 |
title_fullStr |
Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 |
title_full_unstemmed |
Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 |
title_sort |
meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from integrated ocean drilling program (iodp) site u1306 |
publisher |
PANGAEA |
publishDate |
2021 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.926657 https://doi.org/10.1594/PANGAEA.926657 |
op_coverage |
LATITUDE: 58.208000 * LONGITUDE: -45.630000 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 209.83 m |
long_lat |
ENVELOPE(-45.630000,-45.630000,58.208000,58.208000) |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland North Atlantic Northwest Atlantic |
genre_facet |
Greenland North Atlantic Northwest Atlantic |
op_relation |
Channell, James E T (2020): Age model of IODP Site 303-U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.919739 Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2014): Age through tandem correlation of Quaternary relative paleointensity (RPI) and oxygen isotope data at IODP Site U1306 (Eirik Drift, SW Greenland). Quaternary Science Reviews, 88, 135-146, https://doi.org/10.1016/j.quascirev.2014.01.022 Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus a relative paleointensity (RPI) proxy (NRM/ARM) from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926662 Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus component declination, inclination and maximum angular deviation (MAD) values for natural remanent magnetization (NRM) from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926656 Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus oxygen isotope measurements on Neogloboquadrina pachyderma from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926659 https://doi.pangaea.de/10.1594/PANGAEA.926657 https://doi.org/10.1594/PANGAEA.926657 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.926657 https://doi.org/10.1594/PANGAEA.919739 https://doi.org/10.1016/j.quascirev.2014.01.022 https://doi.org/10.1594/PANGAEA.926662 https://doi.org/10.1594/PANGAEA.926656 https://doi.org/10.1594/PANGAEA.926659 |
_version_ |
1766018691037659136 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.926657 2023-05-15T16:29:00+02:00 Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 Channell, James E T Wright, James D Mazaud, Alain Stoner, Joseph S LATITUDE: 58.208000 * LONGITUDE: -45.630000 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 209.83 m 2021-01-18 text/tab-separated-values, 40746 data points https://doi.pangaea.de/10.1594/PANGAEA.926657 https://doi.org/10.1594/PANGAEA.926657 en eng PANGAEA Channell, James E T (2020): Age model of IODP Site 303-U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.919739 Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2014): Age through tandem correlation of Quaternary relative paleointensity (RPI) and oxygen isotope data at IODP Site U1306 (Eirik Drift, SW Greenland). Quaternary Science Reviews, 88, 135-146, https://doi.org/10.1016/j.quascirev.2014.01.022 Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus a relative paleointensity (RPI) proxy (NRM/ARM) from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926662 Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus component declination, inclination and maximum angular deviation (MAD) values for natural remanent magnetization (NRM) from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926656 Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus oxygen isotope measurements on Neogloboquadrina pachyderma from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926659 https://doi.pangaea.de/10.1594/PANGAEA.926657 https://doi.org/10.1594/PANGAEA.926657 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY 303-U1306 Anhysteretic susceptibility/magnetic susceptibility COMPCORE Composite Core Deep Western Boundary Current DEPTH sediment/rock Eirik Drift Exp303 Joides Resolution Magnetic susceptibility volume North Atlantic North Atlantic Climate 1 Northwest Atlantic Oxygen isotopes Quaternary relative paleointensity see Channell et al. (2014) Dataset 2021 ftpangaea https://doi.org/10.1594/PANGAEA.926657 https://doi.org/10.1594/PANGAEA.919739 https://doi.org/10.1016/j.quascirev.2014.01.022 https://doi.org/10.1594/PANGAEA.926662 https://doi.org/10.1594/PANGAEA.926656 https://doi.org/10.1594/PANGAEA.926659 2023-01-20T09:14:19Z The data comprise meters composite depth (mcd) versus volume susceptibility (x10-3 SI) and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. The anhysteretic magnetization (ARM) was measured on a pass-through u-channel magnetometer and the volume susceptibilities were measured on a pass-through (u-channel) susceptibility bridge (see Channell et al., 2014). Planktic oxygen isotope (δ18O) and relative paleointensity (RPI) data are used in tandem to generate an age model for the last 1 Myr from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. For the 1-1.5 Ma interval, the age model is based on RPI alone due to insufficient foraminifera for isotope analyses. Utilizing RPI and δ18O in tandem allows recognition of low-δ18O "events" prior to glacial Terminations I, III, IV, V, VII, VIII, IX and X, that are independently supported by radiocarbon dates through the last deglaciation, and are attributed to local or regional surface-water effects. At Site U1306, Quaternary sedimentation rates (mean ~15 cm/kyr) are elevated during peak glacials and glacial onsets, and are reduced during interglacials, in contrast to the pattern at Site U1305 in 3460 m water depth at the distal toe of the drift, 191 km SW of Site U1306. The contrasting sedimentation-rate pattern appears to hold for the entire ~1.5 Myr record. The slackening and/or shoaling (due to lowered salinity) of the Deep Western Boundary Current (DWBC) during glacial intervals coincided with greater sediment supply to Site U1306 whereas the deepening, and possibly increased vigor, of the DWBC during interglacial intervals boosted sediment supply to Site U1305. Dataset Greenland North Atlantic Northwest Atlantic PANGAEA - Data Publisher for Earth & Environmental Science Greenland ENVELOPE(-45.630000,-45.630000,58.208000,58.208000) |