2021
DOI: 10.1016/j.ecss.2021.107437
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Benthic oxygen dynamics and implication for the maintenance of chronic hypoxia and ecosystem degradation in the Berre lagoon (France)

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Cited by 6 publications
(3 citation statements)
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References 32 publications
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“…The sediment of these lagoons, although quite recent, has served as an object of study to understand the changes that have taken place in the last thousands of years, as well as a record of the contamination received from the basin. Among these studies are those of the Albufera of Valencia [57], in which salinity changes in the lagoon are observed, the presence of contaminating metals such as in Bages [58] and Ghar El Melh [59], and the relationship between the conditions of the benthos and hypoxia in the water of the Berre lagoon [60].…”
Section: Discussionmentioning
confidence: 99%
“…The sediment of these lagoons, although quite recent, has served as an object of study to understand the changes that have taken place in the last thousands of years, as well as a record of the contamination received from the basin. Among these studies are those of the Albufera of Valencia [57], in which salinity changes in the lagoon are observed, the presence of contaminating metals such as in Bages [58] and Ghar El Melh [59], and the relationship between the conditions of the benthos and hypoxia in the water of the Berre lagoon [60].…”
Section: Discussionmentioning
confidence: 99%
“…Indeed, these features limit our ability to detect potential short and long-term effects of hypoxic stress on macrobenthic communities. Bottom hypoxia/anoxia is also known to predominantly take place in deep lagoons like Berre and Thau (Derolez et al, 2020a; Rigaud et al, 2021; Souchu et al, 1998), where wind derived water mixing is limited by depth. Nonetheless, anoxic crises inside coastal lagoons are expected to increase in frequency and intensity with climate change (Derolez et al, 2020a; Miyamoto et al, 2019).…”
Section: Discussionmentioning
confidence: 99%
“…Oxygen depletion generally takes place during the summer and is maximal at the end of the night/early morning (Newton et al, 2010), often starting near the bottom because of benthic organic matter mineralization ( e.g. sedimented phytoplankton, dead macroalgae) and low water renewal (Rigaud et al, 2021; Souchu et al, 1998). In the worst cases, these low to zero oxygen zones can spread to the entire water column and last for several days (Chapelle et al, 2001; Cladas et al, 2016), as seen during the 2018 dystrophic crisis in Thau lagoon (Derolez et al, 2020a).…”
Section: Discussionmentioning
confidence: 99%