(Table 1) Tie points between IODP Site 306-U1314 benthic δ¹⁸O and the global benthic δ¹⁸O stack LR04 ...
Stable carbon and oxygen isotopes from benthic and planktic foraminifers, planktic foraminifer assemblages and ice rafted debris from the North Atlantic Site U1314 (Integrated Ocean Drilling Program Expedition 306) were examined to investigate orbital and millennial-scale climate variability in the...
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Online Access: | https://dx.doi.org/10.1594/pangaea.816304 https://doi.pangaea.de/10.1594/PANGAEA.816304 |
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ftdatacite:10.1594/pangaea.816304 2023-11-05T03:42:20+01:00 (Table 1) Tie points between IODP Site 306-U1314 benthic δ¹⁸O and the global benthic δ¹⁸O stack LR04 ... Alonso-Garcia, Montserrat Sierro, Francisco Javier Kucera, Michal Flores, José-Abel Cacho, Isabel Andersen, Nils 2011 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.816304 https://doi.pangaea.de/10.1594/PANGAEA.816304 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.820282 https://dx.doi.org/10.1016/j.quascirev.2011.08.005 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Age model Composite Core Age model according to Lisiecki & Raymo 2005 [LR04] Exp306 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Dataset dataset 2011 ftdatacite https://doi.org/10.1594/pangaea.81630410.1594/pangaea.82028210.1016/j.quascirev.2011.08.005 2023-10-09T11:06:58Z Stable carbon and oxygen isotopes from benthic and planktic foraminifers, planktic foraminifer assemblages and ice rafted debris from the North Atlantic Site U1314 (Integrated Ocean Drilling Program Expedition 306) were examined to investigate orbital and millennial-scale climate variability in the North Atlantic and its impact on global circulation focusing on the development of glacial periods during the mid-Pleistocene (ca 800-400 ka). Glacial initiations were characterized by a rapid cooling (6-10 °C in less than 7 kyr) in the mean annual sea surface temperature (SST), increasing benthic d18O values and high benthic d13C values. The continuous increase in benthic d18O suggests a continuous ice sheet growth whereas the positive benthic d13C values indicate that the flow of the Iceland Scotland Overflow water (ISOW) was vigorous. Strong deep water formation in the Norwegian Greenland Sea promoted a high transfer of freshwater from the ocean to the continents. However, low SSTs at Site U1314 suggest a ... : Between tie points ages were calculated by linear interpolation. ... Dataset Greenland Greenland Sea Ice Sheet Iceland North Atlantic DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, sediment/rock Age model Composite Core Age model according to Lisiecki & Raymo 2005 [LR04] Exp306 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
spellingShingle |
DEPTH, sediment/rock Age model Composite Core Age model according to Lisiecki & Raymo 2005 [LR04] Exp306 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Alonso-Garcia, Montserrat Sierro, Francisco Javier Kucera, Michal Flores, José-Abel Cacho, Isabel Andersen, Nils (Table 1) Tie points between IODP Site 306-U1314 benthic δ¹⁸O and the global benthic δ¹⁸O stack LR04 ... |
topic_facet |
DEPTH, sediment/rock Age model Composite Core Age model according to Lisiecki & Raymo 2005 [LR04] Exp306 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
description |
Stable carbon and oxygen isotopes from benthic and planktic foraminifers, planktic foraminifer assemblages and ice rafted debris from the North Atlantic Site U1314 (Integrated Ocean Drilling Program Expedition 306) were examined to investigate orbital and millennial-scale climate variability in the North Atlantic and its impact on global circulation focusing on the development of glacial periods during the mid-Pleistocene (ca 800-400 ka). Glacial initiations were characterized by a rapid cooling (6-10 °C in less than 7 kyr) in the mean annual sea surface temperature (SST), increasing benthic d18O values and high benthic d13C values. The continuous increase in benthic d18O suggests a continuous ice sheet growth whereas the positive benthic d13C values indicate that the flow of the Iceland Scotland Overflow water (ISOW) was vigorous. Strong deep water formation in the Norwegian Greenland Sea promoted a high transfer of freshwater from the ocean to the continents. However, low SSTs at Site U1314 suggest a ... : Between tie points ages were calculated by linear interpolation. ... |
format |
Dataset |
author |
Alonso-Garcia, Montserrat Sierro, Francisco Javier Kucera, Michal Flores, José-Abel Cacho, Isabel Andersen, Nils |
author_facet |
Alonso-Garcia, Montserrat Sierro, Francisco Javier Kucera, Michal Flores, José-Abel Cacho, Isabel Andersen, Nils |
author_sort |
Alonso-Garcia, Montserrat |
title |
(Table 1) Tie points between IODP Site 306-U1314 benthic δ¹⁸O and the global benthic δ¹⁸O stack LR04 ... |
title_short |
(Table 1) Tie points between IODP Site 306-U1314 benthic δ¹⁸O and the global benthic δ¹⁸O stack LR04 ... |
title_full |
(Table 1) Tie points between IODP Site 306-U1314 benthic δ¹⁸O and the global benthic δ¹⁸O stack LR04 ... |
title_fullStr |
(Table 1) Tie points between IODP Site 306-U1314 benthic δ¹⁸O and the global benthic δ¹⁸O stack LR04 ... |
title_full_unstemmed |
(Table 1) Tie points between IODP Site 306-U1314 benthic δ¹⁸O and the global benthic δ¹⁸O stack LR04 ... |
title_sort |
(table 1) tie points between iodp site 306-u1314 benthic δ¹⁸o and the global benthic δ¹⁸o stack lr04 ... |
publisher |
PANGAEA |
publishDate |
2011 |
url |
https://dx.doi.org/10.1594/pangaea.816304 https://doi.pangaea.de/10.1594/PANGAEA.816304 |
genre |
Greenland Greenland Sea Ice Sheet Iceland North Atlantic |
genre_facet |
Greenland Greenland Sea Ice Sheet Iceland North Atlantic |
op_relation |
https://dx.doi.org/10.1594/pangaea.820282 https://dx.doi.org/10.1016/j.quascirev.2011.08.005 |
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.81630410.1594/pangaea.82028210.1016/j.quascirev.2011.08.005 |
_version_ |
1781699376028057600 |