(Table 1) Summary of general lithology in IODP Exp302 cores ...
The Cenozoic ice-rafted debris (IRD) history of the central Arctic is reconstructed utilizing the terrigenous coarse sand fraction in IODP 302 cores from 0 to 273 meters composite depth. This Holocene - middle Eocene quantitative record of terrigenous sand accumulation on the Lomonosov Ridge, along...
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ftdatacite:10.1594/pangaea.734547 2024-09-15T17:47:24+00:00 (Table 1) Summary of general lithology in IODP Exp302 cores ... St. John, Kristen E Kudless 2010 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.734547 https://doi.pangaea.de/10.1594/PANGAEA.734547 en eng PANGAEA https://dx.doi.org/10.1029/2007pa001483 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Lithology/composition/facies Depth, composite revised bottom Depth, composite revised top Age, minimum/young Age, maximum/old Sedimentation rate Sample comment Density, dry bulk Comment Composite Core Visual description see comment Calculated Exp302 CCGS Captain Molly Kool Vidar Viking Integrated Ocean Drilling Program / International Ocean Discovery Program IODP dataset Dataset 2010 ftdatacite https://doi.org/10.1594/pangaea.73454710.1029/2007pa001483 2024-08-01T10:58:30Z The Cenozoic ice-rafted debris (IRD) history of the central Arctic is reconstructed utilizing the terrigenous coarse sand fraction in IODP 302 cores from 0 to 273 meters composite depth. This Holocene - middle Eocene quantitative record of terrigenous sand accumulation on the Lomonosov Ridge, along with qualitative information on grain texture and composition, confirms the interpretation that ice initiation (sea ice and glacial ice) occurred ~46 Ma in the Arctic, and provides a long-term pattern of Arctic ice expansion and decay since the middle Eocene. IRD mass accumulation rates range from 0 to 0.13 g/cm2/ka in the middle Eocene and from 0 to 0.36 g/cm2/ka in the Neogene. IRD mass accumulation rate (MAR) maxima in the Miocene and Pliocene cooccur with either glacial initiation or intensification in the sub-Arctic. The 46.25 Ma IRD onset in the central Arctic slightly precedes the earliest evidence of ice in the Antarctic, and compares in timing with a >1000 ppm decrease in atmospheric concentrations of ... : A hiatus of 2.2 ma exists between 135 and 140 r-mcd, and a 26-ma hiatus exists at 198 r-mcd [Backman et al., 2008; Frank et al., 2008]. ... Dataset Antarc* Antarctic Lomonosov Ridge Sea ice DataCite |
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Open Polar |
collection |
DataCite |
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ftdatacite |
language |
English |
topic |
Lithology/composition/facies Depth, composite revised bottom Depth, composite revised top Age, minimum/young Age, maximum/old Sedimentation rate Sample comment Density, dry bulk Comment Composite Core Visual description see comment Calculated Exp302 CCGS Captain Molly Kool Vidar Viking Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
spellingShingle |
Lithology/composition/facies Depth, composite revised bottom Depth, composite revised top Age, minimum/young Age, maximum/old Sedimentation rate Sample comment Density, dry bulk Comment Composite Core Visual description see comment Calculated Exp302 CCGS Captain Molly Kool Vidar Viking Integrated Ocean Drilling Program / International Ocean Discovery Program IODP St. John, Kristen E Kudless (Table 1) Summary of general lithology in IODP Exp302 cores ... |
topic_facet |
Lithology/composition/facies Depth, composite revised bottom Depth, composite revised top Age, minimum/young Age, maximum/old Sedimentation rate Sample comment Density, dry bulk Comment Composite Core Visual description see comment Calculated Exp302 CCGS Captain Molly Kool Vidar Viking Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
description |
The Cenozoic ice-rafted debris (IRD) history of the central Arctic is reconstructed utilizing the terrigenous coarse sand fraction in IODP 302 cores from 0 to 273 meters composite depth. This Holocene - middle Eocene quantitative record of terrigenous sand accumulation on the Lomonosov Ridge, along with qualitative information on grain texture and composition, confirms the interpretation that ice initiation (sea ice and glacial ice) occurred ~46 Ma in the Arctic, and provides a long-term pattern of Arctic ice expansion and decay since the middle Eocene. IRD mass accumulation rates range from 0 to 0.13 g/cm2/ka in the middle Eocene and from 0 to 0.36 g/cm2/ka in the Neogene. IRD mass accumulation rate (MAR) maxima in the Miocene and Pliocene cooccur with either glacial initiation or intensification in the sub-Arctic. The 46.25 Ma IRD onset in the central Arctic slightly precedes the earliest evidence of ice in the Antarctic, and compares in timing with a >1000 ppm decrease in atmospheric concentrations of ... : A hiatus of 2.2 ma exists between 135 and 140 r-mcd, and a 26-ma hiatus exists at 198 r-mcd [Backman et al., 2008; Frank et al., 2008]. ... |
format |
Dataset |
author |
St. John, Kristen E Kudless |
author_facet |
St. John, Kristen E Kudless |
author_sort |
St. John, Kristen E Kudless |
title |
(Table 1) Summary of general lithology in IODP Exp302 cores ... |
title_short |
(Table 1) Summary of general lithology in IODP Exp302 cores ... |
title_full |
(Table 1) Summary of general lithology in IODP Exp302 cores ... |
title_fullStr |
(Table 1) Summary of general lithology in IODP Exp302 cores ... |
title_full_unstemmed |
(Table 1) Summary of general lithology in IODP Exp302 cores ... |
title_sort |
(table 1) summary of general lithology in iodp exp302 cores ... |
publisher |
PANGAEA |
publishDate |
2010 |
url |
https://dx.doi.org/10.1594/pangaea.734547 https://doi.pangaea.de/10.1594/PANGAEA.734547 |
genre |
Antarc* Antarctic Lomonosov Ridge Sea ice |
genre_facet |
Antarc* Antarctic Lomonosov Ridge Sea ice |
op_relation |
https://dx.doi.org/10.1029/2007pa001483 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.73454710.1029/2007pa001483 |
_version_ |
1810496654204207104 |