Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices ...
The interval of time represented by marine isotope stages 11 and 12 (~360–470 ka) contains what may be the most extreme glacial and interglacial climate conditions of the Late Pleistocene. It has been suggested that sea level rose by ~160 m at the termination of glacial stage 12. This is 30% greater...
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Online Access: | https://dx.doi.org/10.1594/pangaea.758847 https://doi.pangaea.de/10.1594/PANGAEA.758847 |
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ftdatacite:10.1594/pangaea.758847 2024-09-15T18:21:47+00:00 Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices ... Thunell, Robert C Poli, Maria-Serena Rio, Domenico 2002 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.758847 https://doi.pangaea.de/10.1594/PANGAEA.758847 en eng PANGAEA https://dx.doi.org/10.1016/s0025-3227(02)00323-7 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label AGE Timeslice Sample code/label Cibicidoides wuellerstorfi, δ13C Drilling/drill rig Composite Core DSDP/ODP/IODP sample designation Mass spectrometer VG Optima Leg172 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 2002 ftdatacite https://doi.org/10.1594/pangaea.75884710.1016/s0025-3227(02)00323-7 2024-08-01T10:53:32Z The interval of time represented by marine isotope stages 11 and 12 (~360–470 ka) contains what may be the most extreme glacial and interglacial climate conditions of the Late Pleistocene. It has been suggested that sea level rose by ~160 m at the termination of glacial stage 12. This is 30% greater than the sea level rise that followed the most recent glacial maximum. There have been few detailed studies of the unique conditions that existed during the stage 11–12 time period because of the lack of high-quality core material. This problem has been addressed by the collection of high deposition rate cores from sediment drifts in the western North Atlantic during Ocean Drilling Project Leg 172. Benthic foraminiferal d13C data from cores collected between ~4600 and 1800 m were used to reconstruct bathymetric gradients in deep and intermediate water properties for selected time slices during this glacial–interglacial cycle. During glacial stage 12, the deep western North Atlantic was filled by a water mass that ... : Supplement to: Thunell, Robert C; Poli, Maria-Serena; Rio, Domenico (2002): Changes in deep and intermediate water properties in the western North Atlantic during marine isotope stages 11-12: evidence from ODP Leg 172. Marine Geology, 189(1-2), 63-77 ... Dataset North Atlantic DataCite |
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ftdatacite |
language |
English |
topic |
Event label AGE Timeslice Sample code/label Cibicidoides wuellerstorfi, δ13C Drilling/drill rig Composite Core DSDP/ODP/IODP sample designation Mass spectrometer VG Optima Leg172 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Event label AGE Timeslice Sample code/label Cibicidoides wuellerstorfi, δ13C Drilling/drill rig Composite Core DSDP/ODP/IODP sample designation Mass spectrometer VG Optima Leg172 Joides Resolution Ocean Drilling Program ODP Thunell, Robert C Poli, Maria-Serena Rio, Domenico Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices ... |
topic_facet |
Event label AGE Timeslice Sample code/label Cibicidoides wuellerstorfi, δ13C Drilling/drill rig Composite Core DSDP/ODP/IODP sample designation Mass spectrometer VG Optima Leg172 Joides Resolution Ocean Drilling Program ODP |
description |
The interval of time represented by marine isotope stages 11 and 12 (~360–470 ka) contains what may be the most extreme glacial and interglacial climate conditions of the Late Pleistocene. It has been suggested that sea level rose by ~160 m at the termination of glacial stage 12. This is 30% greater than the sea level rise that followed the most recent glacial maximum. There have been few detailed studies of the unique conditions that existed during the stage 11–12 time period because of the lack of high-quality core material. This problem has been addressed by the collection of high deposition rate cores from sediment drifts in the western North Atlantic during Ocean Drilling Project Leg 172. Benthic foraminiferal d13C data from cores collected between ~4600 and 1800 m were used to reconstruct bathymetric gradients in deep and intermediate water properties for selected time slices during this glacial–interglacial cycle. During glacial stage 12, the deep western North Atlantic was filled by a water mass that ... : Supplement to: Thunell, Robert C; Poli, Maria-Serena; Rio, Domenico (2002): Changes in deep and intermediate water properties in the western North Atlantic during marine isotope stages 11-12: evidence from ODP Leg 172. Marine Geology, 189(1-2), 63-77 ... |
format |
Dataset |
author |
Thunell, Robert C Poli, Maria-Serena Rio, Domenico |
author_facet |
Thunell, Robert C Poli, Maria-Serena Rio, Domenico |
author_sort |
Thunell, Robert C |
title |
Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices ... |
title_short |
Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices ... |
title_full |
Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices ... |
title_fullStr |
Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices ... |
title_full_unstemmed |
Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices ... |
title_sort |
stable carbon isotope ratios of cibicidoides wuellerstorfi of mis 2 time slices ... |
publisher |
PANGAEA |
publishDate |
2002 |
url |
https://dx.doi.org/10.1594/pangaea.758847 https://doi.pangaea.de/10.1594/PANGAEA.758847 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1016/s0025-3227(02)00323-7 |
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.75884710.1016/s0025-3227(02)00323-7 |
_version_ |
1810460708592156672 |