Examination of hydrothermal influences on oceanic beryllium using fluids, plume particles and sediments from the TAG hydrothermal field
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Spatial heterogeneity in beryllium isotopic distribution in the Indian Ocean
2023, Geochimica et Cosmochimica ActaCitation Excerpt :However, in the central Indian Ocean region (SK-312/08, 09, and 10), no significant increase in 9Be was observed, suggesting a minimal contribution of hydrothermal 9Be to the region. Though it demands further investigation, the plausible reason behind minimal hydrothermal 9Be contribution could be higher scavenging of 9Be within the proximity of hydrothermal vents due to high particle concentrations (Bourlès et al., 1994). Downcore variation of 9Be concentration in sediment core SK-312/09 also showed no drastic increase in 9Be, suggesting no significant hydrothermal 9Be contribution during the past 43 ka (Jena et al., 2022).
Beryllium isotopic systematics in island arc volcanic rocks from northeast Japan: Implications for the incorporation of oceanic sediments into island arc magmas
2016, Chemical GeologyCitation Excerpt :The 10Be/9Be value of the first leachate from an Esan sample in the sequential acid leaching process (Shimaoka et al., 2004) is similar to that of typical seawater (Kusakabe et al., 1987) and diminished rapidly during further leaching (Shimaoka et al., 2004). Bourles et al. (1994) reported that Be becomes reactive in the presence of Mn in an iron-rich hydrothermal particle. It is strongly adsorbed onto mineral surfaces at pH 7, whereas B, another useful tracer of sediment recycling, is not (e.g. Goldberg, 1997; Bauer and Velde, 2014).
Hydrothermal Processes
2013, Treatise on Geochemistry: Second EditionHydrothermal Processes
2003, Treatise on GeochemistryBeryllium geochemistry constraints on the hydraulic behavior of mud volcanoes: The Trinidad Island case
2002, Earth and Planetary Science LettersCitation Excerpt :As previously discussed, the REM II composition most likely ensues from hydrothermally diagenetic processes which have affected seawater (average 9Be concentration of 20–25×103 nM [28,29]) to result in a 9Be-enriched REM II solution characterized by a concentration of ∼1 nM. Such an enrichment is expected since in hydrothermal fluids 9Be concentrations can reach up to 30–50 nM [30]. 9Be concentrations in the fluid samples can be explained, firstly, by a mixing between two end-members (TD5, TD16 and TD20 fluid samples), and, secondly, by a surface enrichment process (TD11 fluid sample).
Hydrothermal scavenging on the Juan de Fuca Ridge: <sup>230</sup>Th<inf>xs</inf>, <sup>10</sup>Be, and REEs in ridge-flank sediments
1997, Geochimica et Cosmochimica Acta