Iron and titanium content of sediment cores from Gramberg Seamount station JC094-STN059 of the James Cook cruise JC094

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Autores principales: Ng, Hong Chin, Robinson, Laura F, Rowland, George Henry, Chen, Siyuan Sean, McManus, Jerry F
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2021
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author Ng, Hong Chin
Robinson, Laura F
Rowland, George Henry
Chen, Siyuan Sean
McManus, Jerry F
author_facet Ng, Hong Chin
Robinson, Laura F
Rowland, George Henry
Chen, Siyuan Sean
McManus, Jerry F
collection Datos científicos de ciencias marinas y ambientales
contents The radiogenic isotope ratio 231Pa/230Th of seawater and ocean sediments is a potentially powerful tool for tracing oceanic processes such as the ocean circulation and marine primary productivity. However, 231Pa/230Th reflects the combined signal of multiple controls associated with scavenging and oceanic transport, limiting its use as a paleo-proxy. Given that links between seawater and sedimentary 231Pa and 230Th distributions are crucial for understanding the cycling and removal fluxes of these nuclides, we carry out analysis of 231Pa and 230Th in both seawater (dissolved phase) and modern sediment samples acquired from five depth transects across the northern tropical Atlantic open ocean during the JC094 research expedition which took place in October-November 2013. Measurements of the radiogenic isotopes were performed using a MultiCollector-Inductively Coupled Plasma-Mass Spectrometer (MC-ICP-MS). In addition, CTD beam attenuation coefficient measurements and XRF scan Fe and Ti measurements of two sediment cores collected from the region during the same research expedition are presented to aid interpretation of 231Pa and 230Th data. Here we show the the Fe and Ti XRF scan data of the sediment core acquired from the Gramberg Seamount.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_926862
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Iron and titanium content of sediment cores from Gramberg Seamount station JC094-STN059 of the James Cook cruise JC094
Ng, Hong Chin
Robinson, Laura F
Rowland, George Henry
Chen, Siyuan Sean
McManus, Jerry F
beam attenuation coefficient; DEPTH, sediment/rock; Event label; GC; Gravity corer; Iron; James Cook; JC094; JC094-GVY14; JC094-STN059; Latitude of event; Longitude of event; Pa/Th; Titanium; tropical Atlantic; TROPICS; X-ray fluorescence ITRAX core scanner; XRF
The radiogenic isotope ratio 231Pa/230Th of seawater and ocean sediments is a potentially powerful tool for tracing oceanic processes such as the ocean circulation and marine primary productivity. However, 231Pa/230Th reflects the combined signal of multiple controls associated with scavenging and oceanic transport, limiting its use as a paleo-proxy. Given that links between seawater and sedimentary 231Pa and 230Th distributions are crucial for understanding the cycling and removal fluxes of these nuclides, we carry out analysis of 231Pa and 230Th in both seawater (dissolved phase) and modern sediment samples acquired from five depth transects across the northern tropical Atlantic open ocean during the JC094 research expedition which took place in October-November 2013. Measurements of the radiogenic isotopes were performed using a MultiCollector-Inductively Coupled Plasma-Mass Spectrometer (MC-ICP-MS). In addition, CTD beam attenuation coefficient measurements and XRF scan Fe and Ti measurements of two sediment cores collected from the region during the same research expedition are presented to aid interpretation of 231Pa and 230Th data. Here we show the the Fe and Ti XRF scan data of the sediment core acquired from the Gramberg Seamount.
title Iron and titanium content of sediment cores from Gramberg Seamount station JC094-STN059 of the James Cook cruise JC094
topic beam attenuation coefficient; DEPTH, sediment/rock; Event label; GC; Gravity corer; Iron; James Cook; JC094; JC094-GVY14; JC094-STN059; Latitude of event; Longitude of event; Pa/Th; Titanium; tropical Atlantic; TROPICS; X-ray fluorescence ITRAX core scanner; XRF
url https://doi.org/10.1594/PANGAEA.926862