Geochemical composition of inorganic silicate fraction of surface sediment samples collected along a 131.5°W transect in the central Pacific

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Autores principales: Seo, Inah, Kim, Mun Gi, Yoo, Chan Min, Hyeong, Kiseong
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2021
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author Seo, Inah
Kim, Mun Gi
Yoo, Chan Min
Hyeong, Kiseong
author_facet Seo, Inah
Kim, Mun Gi
Yoo, Chan Min
Hyeong, Kiseong
collection Datos científicos de ciencias marinas y ambientales
contents This dataset includes neodymium isotope ratios and La, Yb, Sc, and Th concentrations of inorganic silicate fractions of surface sediments from the central Pacific, with relevant sampling information. The aim of the study is to identify latitudinal changes in hemispheric dust provenance. 16 sediment cores were collected along a 131.5°W transect from the equator to 16°N at ~1º intervals using a multiple corer and a piston corer on the R/V Onnuri during KODOS03-03 cruise (2003.07.03-2003.08.01; Chief Scientist: Woong-Seo Kim) and KODOS05-01 cruise (2005.07.17-2005.08.15; Chief Scientist: Woong-Seo Kim). Subsamples were taken at 1 cm intervals from the split cores, and those obtained within the top 10 cm of the cores (usually within the top 3 cm) were used to extract the inorganic silicate fraction. The inorganic silicate fractions of bulk sediments were isolated by sequential dissolution with 25% acetic acid, hot sodium citrate-sodium dithionite solution buffered with sodium bicarbonate, and hot sodium hydroxide solution. The elemental composition of the inorganic silicate fraction was determined using a quadrupole ICP-MS following conventional acid digestion. 143Nd/144Nd ratios were determined via multi-collector thermal ionization mass spectrometer using standard cation exchange techniques.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_934692
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Geochemical composition of inorganic silicate fraction of surface sediment samples collected along a 131.5°W transect in the central Pacific
Seo, Inah
Kim, Mun Gi
Yoo, Chan Min
Hyeong, Kiseong
Calculated, PAAS-normalized; Core; Cruise/expedition; DATE/TIME; DEPTH, water; Depth comment; Eolian dust; Event label; ICP-Q-MS; Inductively coupled plasma-quadrupole-mass spectrometry; KODOS03-03; KODOS03-03_MC03-03-N12; KODOS03-03_MC03-03-N13; KODOS03-03_MC03-03-N14; KODOS03-03_MC03-03-N16; KODOS03-03_MC03-03-N8; KODOS05-01; KODOS05-01_MC5107; KODOS05-01_MC5108; KODOS05-01_MC5109; KODOS05-01_MC5110; KODOS05-01_MC5111; KODOS05-01_MC5112; KODOS05-01_MC5114; KODOS05-01_MC5115; KODOS05-01_MC5117; KODOS05-01_MC5118; KODOS05-01_PC5104; Lanthanum; Lanthanum/Ytterbium ratio; LATITUDE; LONGITUDE; MC03-03-N12; MC03-03-N13; MC03-03-N14; MC03-03-N16; MC03-03-N8; MC5107; MC5108; MC5109; MC5110; MC5111; MC5112; MC5114; MC5115; MC5117; MC5118; MUC; Multi-collector thermal ionization mass spectrometer (TIMS); MultiCorer; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, standard deviation; Neodymium isotopes; North Pacific Ocean; Onnuri; PC; PC5104; Piston corer; Rare earth elements; Scandium; Thorium; Ytterbium; ε-Neodymium
This dataset includes neodymium isotope ratios and La, Yb, Sc, and Th concentrations of inorganic silicate fractions of surface sediments from the central Pacific, with relevant sampling information. The aim of the study is to identify latitudinal changes in hemispheric dust provenance. 16 sediment cores were collected along a 131.5°W transect from the equator to 16°N at ~1º intervals using a multiple corer and a piston corer on the R/V Onnuri during KODOS03-03 cruise (2003.07.03-2003.08.01; Chief Scientist: Woong-Seo Kim) and KODOS05-01 cruise (2005.07.17-2005.08.15; Chief Scientist: Woong-Seo Kim). Subsamples were taken at 1 cm intervals from the split cores, and those obtained within the top 10 cm of the cores (usually within the top 3 cm) were used to extract the inorganic silicate fraction. The inorganic silicate fractions of bulk sediments were isolated by sequential dissolution with 25% acetic acid, hot sodium citrate-sodium dithionite solution buffered with sodium bicarbonate, and hot sodium hydroxide solution. The elemental composition of the inorganic silicate fraction was determined using a quadrupole ICP-MS following conventional acid digestion. 143Nd/144Nd ratios were determined via multi-collector thermal ionization mass spectrometer using standard cation exchange techniques.
title Geochemical composition of inorganic silicate fraction of surface sediment samples collected along a 131.5°W transect in the central Pacific
topic Calculated, PAAS-normalized; Core; Cruise/expedition; DATE/TIME; DEPTH, water; Depth comment; Eolian dust; Event label; ICP-Q-MS; Inductively coupled plasma-quadrupole-mass spectrometry; KODOS03-03; KODOS03-03_MC03-03-N12; KODOS03-03_MC03-03-N13; KODOS03-03_MC03-03-N14; KODOS03-03_MC03-03-N16; KODOS03-03_MC03-03-N8; KODOS05-01; KODOS05-01_MC5107; KODOS05-01_MC5108; KODOS05-01_MC5109; KODOS05-01_MC5110; KODOS05-01_MC5111; KODOS05-01_MC5112; KODOS05-01_MC5114; KODOS05-01_MC5115; KODOS05-01_MC5117; KODOS05-01_MC5118; KODOS05-01_PC5104; Lanthanum; Lanthanum/Ytterbium ratio; LATITUDE; LONGITUDE; MC03-03-N12; MC03-03-N13; MC03-03-N14; MC03-03-N16; MC03-03-N8; MC5107; MC5108; MC5109; MC5110; MC5111; MC5112; MC5114; MC5115; MC5117; MC5118; MUC; Multi-collector thermal ionization mass spectrometer (TIMS); MultiCorer; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, standard deviation; Neodymium isotopes; North Pacific Ocean; Onnuri; PC; PC5104; Piston corer; Rare earth elements; Scandium; Thorium; Ytterbium; ε-Neodymium
url https://doi.org/10.1594/PANGAEA.934692