2016
Oceans on the edge of anoxia
Abstract: Environmental crises can tip the ocean into O 2 depletion
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Cited by 44 publications
(21 citation statements)
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“…Under low oxygen conditions, for example, P is preferentially regenerated from marine sediments, (e.g., Ingall & Jahnke, 1994). This could lead to a positive feedback loop where more P is brought to the ocean surface enhancing primary production and organic matter export, and, in turn, enhancing organic matter transport to and remineralization at depth, further depleting bottom water oxygen through consumption of oxygen during remineralization (e.g., Kemena et al., 2019; Niemeyer et al., 2016; Palastanga et al., 2011; Van Cappellen & Ingall, 1994; Wallmann, 2010; Watson, 2016). Release of additional P from sediments could have a strong impact on δ 13 C (see e.g., Tschumi et al., 2011, for a step‐increase in the ocean's P inventory).…”
Section: Discussionmentioning
confidence: 99%
“…Under low oxygen conditions, for example, P is preferentially regenerated from marine sediments, (e.g., Ingall & Jahnke, 1994). This could lead to a positive feedback loop where more P is brought to the ocean surface enhancing primary production and organic matter export, and, in turn, enhancing organic matter transport to and remineralization at depth, further depleting bottom water oxygen through consumption of oxygen during remineralization (e.g., Kemena et al., 2019; Niemeyer et al., 2016; Palastanga et al., 2011; Van Cappellen & Ingall, 1994; Wallmann, 2010; Watson, 2016). Release of additional P from sediments could have a strong impact on δ 13 C (see e.g., Tschumi et al., 2011, for a step‐increase in the ocean's P inventory).…”
Section: Discussionmentioning
confidence: 99%
“…This de-cline is partially countered when greater ecological complexity and flexible stoichiometry is introduced as well, with a shift to smaller plankton classes in response to oligotrophication leading to a 21st century ocean carbon sink reduction of ∼ 5.9 PgC. Other processes that are not resolved in this configuration of ecoGEnIE could also substantially affect the biological pump, such as ballasting, calcifier-silicifier tradeoffs, nitrogen cycle and stoichiometry-acidification feedbacks (Buchanan et al, 2019;Dutkiewicz et al, 2015;Landolfi et al, 2017;Riebesell et al, 2007;Somes et al, 2016;Tagliabue et al, 2011), deep chlorophyll maxima, and (on longer timescales) redox-dependent feedbacks (Niemeyer et al, 2017;Watson, 2016). Limited physical resolution can have significant impacts on biogeochemistry (Sinha et al, 2010), also limiting our results.…”
Section: Discussionmentioning
confidence: 99%
“…The oxygen content of the ocean constrains productivity, biodiversity, and biogeochemical cycles. Major extinction events in Earth's history have been associated with warm climates and oxygen-deficient oceans (7), and under current trajectories, anthropogenic activities could drive the ocean toward widespread oxygen deficiency within the next thousand years (8). In this Review, we refer to "coastal waters" as systems that are strongly influenced by their watershed, and the "open ocean" as waters in which such influences are secondary.…”
mentioning
confidence: 99%
