ArticleDissolved Al in sediments and waters of the East China Sea: Implications for authigenic mineral formation
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Cited by (105)
Reactive-transport modeling of neodymium and its radiogenic isotope in deep-sea sediments: The roles of authigenesis, marine silicate weathering and reverse weathering
2022, Earth and Planetary Science LettersCitation Excerpt :We compare the modeled Al-Si relationship with published seawater and pore water data to evaluate if model results are reasonable (Fig. 8). Al-Si trends in the “fast clay” and “normal clay” models follow that of deep ocean water (GEOTRACES Intermediate Data Product Group, 2021) and East China Sea pore water (Mackin and Aller, 1984). Al-Si trends in the “normal clay” and “slow clay” models bracket pore water data from the North Atlantic, Southern Ocean and Amazon shelf (Mackin and Aller, 1986, 1986; Stoffyn-Egli, 1982; Van Beueskom et al., 1997).
Stable silicon isotopes uncover a mineralogical control on the benthic silicon cycle in the Arctic Barents Sea
2022, Geochimica et Cosmochimica ActaReverse weathering may amplify post-Snowball atmospheric carbon dioxide levels
2021, Precambrian Research
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Present address: Marine Sciences Research Center, SUNY at Stony Brook, Stony Brook, NY 11794.
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