Stable oxygen isotope (d18O), Mg/Ca and temperature records of foraminiferal species (G. bulloides, N. incompta, Uvigerina spp., C. wuellerstorfi, M. barleeanum) of core SO264_45-2 in sediment depth 6.03-8.32 m

Fuente: PANGAEA
Enregistré dans:
Détails bibliographiques
Auteurs principaux: Jacobi, Lara, Nürnberg, Dirk, Chao, Weng-si, Lembke-Jene, Lester, Tiedemann, Ralf
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2023
Sujets:
Accès en ligne:
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
_version_ 1867171040425148416
author Jacobi, Lara
Nürnberg, Dirk
Chao, Weng-si
Lembke-Jene, Lester
Tiedemann, Ralf
author_facet Jacobi, Lara
Nürnberg, Dirk
Chao, Weng-si
Lembke-Jene, Lester
Tiedemann, Ralf
collection Datos científicos de ciencias marinas y ambientales
contents Stable oxygen isotope (δ18O) measurements were performed on the benthic foraminiferal species C. wullerstorfi, Uvigeringa spp., and M. barleeanum as well as on the planktic foraminiferal species G. bulloides and N. incompta. Additionally Mg/Ca-measurements were performed on the two planktic species. The foraminiferal specimens were selected from gravity core SO264-45-2, which was recovered from Jimmu Seamount (46.5632°N 169.601211°E) from 2425 m water depth during R/V SONNE cruise SO264 (SONNE-EMPEROR) in August 2018. Sampling and analytical studies were carried out from 6.03 m – 8.32 m core depth at 2-4 cm spatial resolution. The isotope analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV carbonate preparation device. Trace metal analyses were performed on a VARIAN 720-ES Axial ICP-OES, a simultaneous, axial-viewing inductively coupled plasma - optical emission spectrometer coupled to a VARIAN SPS3 sample preparation system. Both systems were operated at GEOMAR. The proxy data provide stratigraphical information and were used to calculate water temperature and the ice volume-corrected δ18O of seawater. Contaminant phases of the trace metal analyses were added (Al/Ca, Fe/Ca, Mn/Ca in mmol/mol).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_962997
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Stable oxygen isotope (d18O), Mg/Ca and temperature records of foraminiferal species (G. bulloides, N. incompta, Uvigerina spp., C. wuellerstorfi, M. barleeanum) of core SO264_45-2 in sediment depth 6.03-8.32 m
Jacobi, Lara
Nürnberg, Dirk
Chao, Weng-si
Lembke-Jene, Lester
Tiedemann, Ralf
Cibicidoides wuellerstorfi, δ18O; d18O; DEPTH, sediment/rock; Emperor Seamounts Chain; GC; Globigerina bulloides, Aluminium/Calcium ratio; Globigerina bulloides, Iron/Calcium ratio; Globigerina bulloides, Magnesium/Calcium ratio; Globigerina bulloides, Manganese/Calcium ratio; Globigerina bulloides, δ18O; Gravity corer; Ice volume corrected; ICP-OES, VARIAN 720-ES; Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV; Melonis barleeanus, δ18O; Mg/Ca; Neogloboquadrina incompta, Aluminium/Calcium ratio; Neogloboquadrina incompta, Iron/Calcium ratio; Neogloboquadrina incompta, Magnesium/Calcium ratio; Neogloboquadrina incompta, Manganese/Calcium ratio; Neogloboquadrina incompta, δ18O; North Pacific; Sea surface temperature; SO264; SO264_45-2; Sonne_2; SST; Uvigerina spp., δ18O; δ18O, ice volume free, seawater; δ18O, stacked
Stable oxygen isotope (δ18O) measurements were performed on the benthic foraminiferal species C. wullerstorfi, Uvigeringa spp., and M. barleeanum as well as on the planktic foraminiferal species G. bulloides and N. incompta. Additionally Mg/Ca-measurements were performed on the two planktic species. The foraminiferal specimens were selected from gravity core SO264-45-2, which was recovered from Jimmu Seamount (46.5632°N 169.601211°E) from 2425 m water depth during R/V SONNE cruise SO264 (SONNE-EMPEROR) in August 2018. Sampling and analytical studies were carried out from 6.03 m – 8.32 m core depth at 2-4 cm spatial resolution. The isotope analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV carbonate preparation device. Trace metal analyses were performed on a VARIAN 720-ES Axial ICP-OES, a simultaneous, axial-viewing inductively coupled plasma - optical emission spectrometer coupled to a VARIAN SPS3 sample preparation system. Both systems were operated at GEOMAR. The proxy data provide stratigraphical information and were used to calculate water temperature and the ice volume-corrected δ18O of seawater. Contaminant phases of the trace metal analyses were added (Al/Ca, Fe/Ca, Mn/Ca in mmol/mol).
title Stable oxygen isotope (d18O), Mg/Ca and temperature records of foraminiferal species (G. bulloides, N. incompta, Uvigerina spp., C. wuellerstorfi, M. barleeanum) of core SO264_45-2 in sediment depth 6.03-8.32 m
topic Cibicidoides wuellerstorfi, δ18O; d18O; DEPTH, sediment/rock; Emperor Seamounts Chain; GC; Globigerina bulloides, Aluminium/Calcium ratio; Globigerina bulloides, Iron/Calcium ratio; Globigerina bulloides, Magnesium/Calcium ratio; Globigerina bulloides, Manganese/Calcium ratio; Globigerina bulloides, δ18O; Gravity corer; Ice volume corrected; ICP-OES, VARIAN 720-ES; Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV; Melonis barleeanus, δ18O; Mg/Ca; Neogloboquadrina incompta, Aluminium/Calcium ratio; Neogloboquadrina incompta, Iron/Calcium ratio; Neogloboquadrina incompta, Magnesium/Calcium ratio; Neogloboquadrina incompta, Manganese/Calcium ratio; Neogloboquadrina incompta, δ18O; North Pacific; Sea surface temperature; SO264; SO264_45-2; Sonne_2; SST; Uvigerina spp., δ18O; δ18O, ice volume free, seawater; δ18O, stacked
url https://doi.org/10.1594/PANGAEA.962997