New Perspectives on the 143Nd/144Nd Palaeoceanographic Tracer on Foraminifera: The State-of-the-Art Frontiers of Analytical Methods
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F22%3A00556466" target="_blank" >RIV/67985831:_____/22:00556466 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216208:11310/22:10456027
Výsledek na webu
<a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021GC010201" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021GC010201</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1029/2021GC010201" target="_blank" >10.1029/2021GC010201</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
New Perspectives on the 143Nd/144Nd Palaeoceanographic Tracer on Foraminifera: The State-of-the-Art Frontiers of Analytical Methods
Popis výsledku v původním jazyce
The 143Nd/144Nd isotopic composition of foraminifera represents one of the most prominent palaeoceanographic proxies enabling tracing of particular water masses due to the short residence time of Nd in seawater and large-scale provinciality resulting from its lithogenic origin. Despite its wide use, the applicability of foraminiferal Nd isotopic systematics as a palaeoceanographic tracer is largely hampered by the amount of material needed for precise analyses. Here, we analyzed for the first time foraminiferal samples of a combined weight of only ∼300–500 μg (ca. 300 pg to 1 ng Nd loaded). We followed a methodology that utilizes Nd separation from the matrix and provides precise 143Nd/144Nd determinations by thermal ionization mass spectrometry with sensitive 1013 Ω amplifiers. Two different techniques analyzing NdO+ and Nd+ (single/double filament configurations) were employed and tested to assess the limits both in terms of in-run precision and accuracy concluding that the former method yielded an external reproducibility on the determined 143Nd/144Nd better than ∼90 ppm (2RSD, relative standard deviation) for 100 pg Nd loads. The overall veracity was tested by multiple analyses of Holocene and Miocene foraminifera from the Mediterranean region. Pooled data were obtained in agreement with previous studies attesting that multiple analyses of even very low Nd loads (≤1 ng) can lead to sufficient precision. As revealed by our newly obtained data, individual foraminiferal species show a significant naturally induced 143Nd/144Nd variability that needs to be considered when pursuing Nd isotopic analysis.
Název v anglickém jazyce
New Perspectives on the 143Nd/144Nd Palaeoceanographic Tracer on Foraminifera: The State-of-the-Art Frontiers of Analytical Methods
Popis výsledku anglicky
The 143Nd/144Nd isotopic composition of foraminifera represents one of the most prominent palaeoceanographic proxies enabling tracing of particular water masses due to the short residence time of Nd in seawater and large-scale provinciality resulting from its lithogenic origin. Despite its wide use, the applicability of foraminiferal Nd isotopic systematics as a palaeoceanographic tracer is largely hampered by the amount of material needed for precise analyses. Here, we analyzed for the first time foraminiferal samples of a combined weight of only ∼300–500 μg (ca. 300 pg to 1 ng Nd loaded). We followed a methodology that utilizes Nd separation from the matrix and provides precise 143Nd/144Nd determinations by thermal ionization mass spectrometry with sensitive 1013 Ω amplifiers. Two different techniques analyzing NdO+ and Nd+ (single/double filament configurations) were employed and tested to assess the limits both in terms of in-run precision and accuracy concluding that the former method yielded an external reproducibility on the determined 143Nd/144Nd better than ∼90 ppm (2RSD, relative standard deviation) for 100 pg Nd loads. The overall veracity was tested by multiple analyses of Holocene and Miocene foraminifera from the Mediterranean region. Pooled data were obtained in agreement with previous studies attesting that multiple analyses of even very low Nd loads (≤1 ng) can lead to sufficient precision. As revealed by our newly obtained data, individual foraminiferal species show a significant naturally induced 143Nd/144Nd variability that needs to be considered when pursuing Nd isotopic analysis.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10506 - Paleontology
Návaznosti výsledku
Projekt
<a href="/cs/project/GA20-05872S" target="_blank" >GA20-05872S: Oceánografická záhada Mediterán-Paratethys v období langhu - hydrografie a paleoceánografie na základě izotopů neodymu ve schrákách foraminifer</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2022
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geochemistry, Geophysics, Geosystems
ISSN
1525-2027
e-ISSN
1525-2027
Svazek periodika
23
Číslo periodika v rámci svazku
3
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
19
Strana od-do
e2021GC010201
Kód UT WoS článku
000776516500021
EID výsledku v databázi Scopus
2-s2.0-85127358751