Deep Sea Research Part A. Oceanographic Research Papers
Volume 37, Issue 10, October 1990, Pages 1619-1637
Scavenging rates of dissolved manganese in a hydrothermal vent plume
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Cited by (117)
Hydrothermal signatures and prospecting indicators in sediments along the Carlsberg Ridge
2023, Sedimentary GeologyA review of zooplankton and deep carbon fixation contributions to carbon cycling in the dark ocean
2022, Journal of Marine SystemsSize speciation of dissolved trace metals in hydrothermal plumes on the Southwest Indian Ridge
2021, Science of the Total EnvironmentMetal isotope signatures from lava-seawater interaction during the 2018 eruption of Kīlauea
2020, Geochimica et Cosmochimica ActaMetal partitioning after in situ filtration at deep-sea vents of the Lucky Strike hydrothermal field (EMSO-Azores, Mid-Atlantic Ridge, 37°N)
2020, Deep-Sea Research Part I: Oceanographic Research PapersCitation Excerpt :This multivariate PCA was performed in R using the RStudio software (v. 1.0.153, RStudio Inc.) and the FactoMineR package (Lê et al., 2008). Dissolved Mn (dMn) is used as a conservative tracer of the hydrothermal input in the mixing gradient owing to its slow reactivity with particles (Cowen et al., 1990; Field and Sherrell, 2000). Indeed, the removal rate of Mn (weeks to year) is considerably slower than the emplacement of neutrally buoyant plumes (on the order of tens of minutes) (Radford-Knoery et al., 1998).
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