2022
DOI: 10.1016/j.csr.2022.104716
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Evidence of hypoxia in the eastern coast of the Gulf of California as induced by stable nitrogen isotopes in surface sediments

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Cited by 5 publications
(3 citation statements)
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“…The d 15 N values cannot distinguish where denitrification is occurring, whether during N transport from the watershed or local processing within the estuary water column and sediment. Furthermore, denitrification is an anaerobic process, so hypoxia of the water column associated with eutrophication and hypoxic sediments increase d 15 N values (Ganeshram et al, 2000;Sańchez et al, 2022). Significant fractionation also occurs during nitrate uptake by biological assimilation in the estuary, therefore incomplete nitrate utilization would result in isotopically lighter d 15 N in organic matter that is then incorporated into sediments (Altabet, 2001).…”
Section: Limitations and Complexities Of Isotopesmentioning
confidence: 99%
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“…The d 15 N values cannot distinguish where denitrification is occurring, whether during N transport from the watershed or local processing within the estuary water column and sediment. Furthermore, denitrification is an anaerobic process, so hypoxia of the water column associated with eutrophication and hypoxic sediments increase d 15 N values (Ganeshram et al, 2000;Sańchez et al, 2022). Significant fractionation also occurs during nitrate uptake by biological assimilation in the estuary, therefore incomplete nitrate utilization would result in isotopically lighter d 15 N in organic matter that is then incorporated into sediments (Altabet, 2001).…”
Section: Limitations and Complexities Of Isotopesmentioning
confidence: 99%
“…Therefore, in areas of the modern estuary with high nitrate concentrations, incomplete nitrate utilization may drive a water column d 15 N signature that is even higher than represented in the sediments (White et al, 2013). Finally, degradation of N within the sediment layers over time increases d 15 N deeper in the core (Sańchez et al, 2022). We observed a trend of increasing d 15 N in modern sediments, opposite of the trend imparted by diagenesis, so the change may be even more pronounced than observed in sediment timeseries.…”
Section: Limitations and Complexities Of Isotopesmentioning
confidence: 99%
“…While increased temperature positively affects digenean transmission, other local factors may be more critical, so latitudinal gradients in infection levels may not be observed [43]. The eastern coast of the Gulf of California has spatially distinct environmental conditions influenced by agriculture, mariculture, upwellings, seasonal currents, river discharges, and hypoxia [44,45]; these environmental factors along the shallow coastal waters might influence host-parasite interactions differently, thereby making noticeable spatial patterns that are challenging to observe.…”
Section: Infection-level Changesmentioning
confidence: 99%