Oxygen and Carbon stable isotope ratios for Site U1334 ...
The Oligocene-Miocene transition (OMT) (~23 Ma) is interpreted as a transient global cooling event, associated with a large-scale Antarctic ice sheet expansion. Here we present a 2.23 Myr long high-resolution (~3 kyr) benthic foraminiferal oxygen and carbon isotope (d18O and d13C) record from Integr...
Main Authors: | , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
2016
|
Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.858332 https://doi.pangaea.de/10.1594/PANGAEA.858332 |
id |
ftdatacite:10.1594/pangaea.858332 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.1594/pangaea.858332 2024-06-09T07:40:04+00:00 Oxygen and Carbon stable isotope ratios for Site U1334 ... Beddow, Helen M Liebrand, Diederik Sluijs, Appy Wade, Bridget S Lourens, Lucas Joost 2016 application/zip https://dx.doi.org/10.1594/pangaea.858332 https://doi.pangaea.de/10.1594/PANGAEA.858332 en eng PANGAEA https://dx.doi.org/10.1002/2015pa002820 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Drilling/drill rig Exp320 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Collection article Supplementary Publication Series of Datasets 2016 ftdatacite https://doi.org/10.1594/pangaea.85833210.1002/2015pa002820 2024-05-13T13:41:18Z The Oligocene-Miocene transition (OMT) (~23 Ma) is interpreted as a transient global cooling event, associated with a large-scale Antarctic ice sheet expansion. Here we present a 2.23 Myr long high-resolution (~3 kyr) benthic foraminiferal oxygen and carbon isotope (d18O and d13C) record from Integrated Ocean Drilling Program Site U1334 (eastern equatorial Pacific Ocean), covering the interval from 21.91 to 24.14 Ma. To date, five other high-resolution benthic foraminiferal stable isotope stratigraphies across this time interval have been published, showing a ~1 per mil increase in benthic foraminiferal d18O across the OMT. However, these records are still few and spatially limited and no clear understanding exists of the global versus local imprints. We show that trends and the amplitudes of change are similar at Site U1334 as in other high-resolution stable isotope records, suggesting that these represent global deep water signals. We create a benthic foraminiferal stable isotope stack across the OMT by ... : Supplement to: Beddow, Helen M; Liebrand, Diederik; Sluijs, Appy; Wade, Bridget S; Lourens, Lucas Joost (2016): Global change across the Oligocene-Miocene transition: High-resolution stable isotope records from IODP Site U1334 (equatorial Pacific Ocean). Paleoceanography, 31(1), 81-97 ... Article in Journal/Newspaper Antarc* Antarctic Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Antarctic Pacific |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Composite Core Drilling/drill rig Exp320 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
spellingShingle |
Composite Core Drilling/drill rig Exp320 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Beddow, Helen M Liebrand, Diederik Sluijs, Appy Wade, Bridget S Lourens, Lucas Joost Oxygen and Carbon stable isotope ratios for Site U1334 ... |
topic_facet |
Composite Core Drilling/drill rig Exp320 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
description |
The Oligocene-Miocene transition (OMT) (~23 Ma) is interpreted as a transient global cooling event, associated with a large-scale Antarctic ice sheet expansion. Here we present a 2.23 Myr long high-resolution (~3 kyr) benthic foraminiferal oxygen and carbon isotope (d18O and d13C) record from Integrated Ocean Drilling Program Site U1334 (eastern equatorial Pacific Ocean), covering the interval from 21.91 to 24.14 Ma. To date, five other high-resolution benthic foraminiferal stable isotope stratigraphies across this time interval have been published, showing a ~1 per mil increase in benthic foraminiferal d18O across the OMT. However, these records are still few and spatially limited and no clear understanding exists of the global versus local imprints. We show that trends and the amplitudes of change are similar at Site U1334 as in other high-resolution stable isotope records, suggesting that these represent global deep water signals. We create a benthic foraminiferal stable isotope stack across the OMT by ... : Supplement to: Beddow, Helen M; Liebrand, Diederik; Sluijs, Appy; Wade, Bridget S; Lourens, Lucas Joost (2016): Global change across the Oligocene-Miocene transition: High-resolution stable isotope records from IODP Site U1334 (equatorial Pacific Ocean). Paleoceanography, 31(1), 81-97 ... |
format |
Article in Journal/Newspaper |
author |
Beddow, Helen M Liebrand, Diederik Sluijs, Appy Wade, Bridget S Lourens, Lucas Joost |
author_facet |
Beddow, Helen M Liebrand, Diederik Sluijs, Appy Wade, Bridget S Lourens, Lucas Joost |
author_sort |
Beddow, Helen M |
title |
Oxygen and Carbon stable isotope ratios for Site U1334 ... |
title_short |
Oxygen and Carbon stable isotope ratios for Site U1334 ... |
title_full |
Oxygen and Carbon stable isotope ratios for Site U1334 ... |
title_fullStr |
Oxygen and Carbon stable isotope ratios for Site U1334 ... |
title_full_unstemmed |
Oxygen and Carbon stable isotope ratios for Site U1334 ... |
title_sort |
oxygen and carbon stable isotope ratios for site u1334 ... |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://dx.doi.org/10.1594/pangaea.858332 https://doi.pangaea.de/10.1594/PANGAEA.858332 |
geographic |
Antarctic Pacific |
geographic_facet |
Antarctic Pacific |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_relation |
https://dx.doi.org/10.1002/2015pa002820 |
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.85833210.1002/2015pa002820 |
_version_ |
1801383577768689664 |