Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)

Oxygen-isotope analyses of planktonic foraminifera from 57 western Pacific deep-sea cores are compared for the Holocene and the Last Glacial Maximum (LGM). Carbonate dissolution, sedimentation rates/bioturbation, sample density, and vital effects are assessed before the sea-surface salinity signal o...

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Main Authors: Martínez, José Ignacio, De Deckker, Patrick, Chivas, Allan R
Format: Dataset
Language:English
Published: PANGAEA 1997
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.690363
https://doi.org/10.1594/PANGAEA.690363
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.690363
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.690363 2023-05-15T18:01:05+02:00 Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2) Martínez, José Ignacio De Deckker, Patrick Chivas, Allan R LATITUDE: -15.288000 * LONGITUDE: 166.284000 * DATE/TIME START: 1990-10-25T11:00:00 * DATE/TIME END: 1990-10-26T21:30:00 * MINIMUM DEPTH, sediment/rock: 0.45 m * MAXIMUM DEPTH, sediment/rock: 61.62 m 1997-03-28 text/tab-separated-values, 657 data points https://doi.pangaea.de/10.1594/PANGAEA.690363 https://doi.org/10.1594/PANGAEA.690363 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.690363 https://doi.org/10.1594/PANGAEA.690363 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Martínez, José Ignacio; De Deckker, Patrick; Chivas, Allan R (1997): New estimates for salinity changes in the Western Pacific Warm Pool during the Last Glacial Maximum: oxygen-isotope evidence. Marine Micropaleontology, 32(3-4), 311-340, https://doi.org/10.1016/S0377-8398(97)00029-7 134-828A Coral Sea DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Globigerinoides sacculifer δ13C δ18O Joides Resolution Leg134 Mass spectrometer Finnigan MAT 251 Ocean Drilling Program ODP Sample code/label Dataset 1997 ftpangaea https://doi.org/10.1594/PANGAEA.690363 https://doi.org/10.1016/S0377-8398(97)00029-7 2023-01-20T08:45:38Z Oxygen-isotope analyses of planktonic foraminifera from 57 western Pacific deep-sea cores are compared for the Holocene and the Last Glacial Maximum (LGM). Carbonate dissolution, sedimentation rates/bioturbation, sample density, and vital effects are assessed before the sea-surface salinity signal of these records is reconstructed. Average glacial-interglacial Delta delta18O values in the western Pacific are found to be close to those in the Atlantic Ocean (1.76 ‰ in the Pacific compared to 1.80 ‰ in the Atlantic), questioning previous suggestions of a larger salinity difference between the Atlantic and the Pacific oceans during the LGM. During the LGM, sea-surface salinity was higher in the western Pacific than today (by >~1 ‰), implying that evaporation minus precipitation was higher all over the region. The minimum change in sea-surface salinity occurred around the equator at the core of the Western Pacific Warm Pool. Holocene high-amplitude, high-frequency fluctuations in planktonic delta18O records north and south of the present limits of the Western Pacific Warm Pool are indicative of sea-surface temperature and/or sea-surface salinity variations related to its expansion and contraction at the scale of thousands of years. Such high-amplitude, high-frequency fluctuations at the edge of the WPWP are best documented in the delta18O signal of ODP Hole 828A offshore Vanuatu, so far the best high-resolution record for the western Pacific. Dataset Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science Pacific ENVELOPE(166.284000,166.284000,-15.288000,-15.288000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 134-828A
Coral Sea
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Globigerinoides sacculifer
δ13C
δ18O
Joides Resolution
Leg134
Mass spectrometer Finnigan MAT 251
Ocean Drilling Program
ODP
Sample code/label
spellingShingle 134-828A
Coral Sea
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Globigerinoides sacculifer
δ13C
δ18O
Joides Resolution
Leg134
Mass spectrometer Finnigan MAT 251
Ocean Drilling Program
ODP
Sample code/label
Martínez, José Ignacio
De Deckker, Patrick
Chivas, Allan R
Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)
topic_facet 134-828A
Coral Sea
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Globigerinoides sacculifer
δ13C
δ18O
Joides Resolution
Leg134
Mass spectrometer Finnigan MAT 251
Ocean Drilling Program
ODP
Sample code/label
description Oxygen-isotope analyses of planktonic foraminifera from 57 western Pacific deep-sea cores are compared for the Holocene and the Last Glacial Maximum (LGM). Carbonate dissolution, sedimentation rates/bioturbation, sample density, and vital effects are assessed before the sea-surface salinity signal of these records is reconstructed. Average glacial-interglacial Delta delta18O values in the western Pacific are found to be close to those in the Atlantic Ocean (1.76 ‰ in the Pacific compared to 1.80 ‰ in the Atlantic), questioning previous suggestions of a larger salinity difference between the Atlantic and the Pacific oceans during the LGM. During the LGM, sea-surface salinity was higher in the western Pacific than today (by >~1 ‰), implying that evaporation minus precipitation was higher all over the region. The minimum change in sea-surface salinity occurred around the equator at the core of the Western Pacific Warm Pool. Holocene high-amplitude, high-frequency fluctuations in planktonic delta18O records north and south of the present limits of the Western Pacific Warm Pool are indicative of sea-surface temperature and/or sea-surface salinity variations related to its expansion and contraction at the scale of thousands of years. Such high-amplitude, high-frequency fluctuations at the edge of the WPWP are best documented in the delta18O signal of ODP Hole 828A offshore Vanuatu, so far the best high-resolution record for the western Pacific.
format Dataset
author Martínez, José Ignacio
De Deckker, Patrick
Chivas, Allan R
author_facet Martínez, José Ignacio
De Deckker, Patrick
Chivas, Allan R
author_sort Martínez, José Ignacio
title Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)
title_short Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)
title_full Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)
title_fullStr Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)
title_full_unstemmed Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)
title_sort stable oxygen and carbon isotope ratios of globigerinoides sacculifer of odp hole 134-828a from the southwest pacific (table 2)
publisher PANGAEA
publishDate 1997
url https://doi.pangaea.de/10.1594/PANGAEA.690363
https://doi.org/10.1594/PANGAEA.690363
op_coverage LATITUDE: -15.288000 * LONGITUDE: 166.284000 * DATE/TIME START: 1990-10-25T11:00:00 * DATE/TIME END: 1990-10-26T21:30:00 * MINIMUM DEPTH, sediment/rock: 0.45 m * MAXIMUM DEPTH, sediment/rock: 61.62 m
long_lat ENVELOPE(166.284000,166.284000,-15.288000,-15.288000)
geographic Pacific
geographic_facet Pacific
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source Supplement to: Martínez, José Ignacio; De Deckker, Patrick; Chivas, Allan R (1997): New estimates for salinity changes in the Western Pacific Warm Pool during the Last Glacial Maximum: oxygen-isotope evidence. Marine Micropaleontology, 32(3-4), 311-340, https://doi.org/10.1016/S0377-8398(97)00029-7
op_relation https://doi.pangaea.de/10.1594/PANGAEA.690363
https://doi.org/10.1594/PANGAEA.690363
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.690363
https://doi.org/10.1016/S0377-8398(97)00029-7
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