2016
DOI: 10.1016/j.csr.2016.02.014
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Summertime in situ monitoring of oxygen depletion in Amursky Bay (Japan/East Sea)

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Cited by 17 publications
(13 citation statements)
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“…Amursky Bay is a secondary bay of the PGB that regularly demonstrates hypoxic events in the bottom water in the late summer [16]. Available historical data clearly demonstrate that the lowest values of DO obtained in the summer in the bottom waters of Amursky Bay have been steadily decreasing over the last 80 years (Figure 2; [17]). The slope of the solid line in Figure 5b indicates summer acidifications of the bottom waters on the shelf of the JES caused by OM respiration, which varies from −0.0080 pH units/y (1932) to −0.0033 pH units/y (2014).…”
Section: Resultsmentioning
confidence: 99%
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“…Amursky Bay is a secondary bay of the PGB that regularly demonstrates hypoxic events in the bottom water in the late summer [16]. Available historical data clearly demonstrate that the lowest values of DO obtained in the summer in the bottom waters of Amursky Bay have been steadily decreasing over the last 80 years (Figure 2; [17]). The slope of the solid line in Figure 5b indicates summer acidifications of the bottom waters on the shelf of the JES caused by OM respiration, which varies from −0.0080 pH units/y (1932) to −0.0033 pH units/y (2014).…”
Section: Resultsmentioning
confidence: 99%
“…In 2007 and 2011, the DO saturation degree was 1.7 and 4.3, respectively. Additionally, it should be noted that under limited oxygen conditions (hypoxia), the rate of microbial oxidation of OM at the water/bottom sediment interface is low, because this reaction is of the first order [17].…”
Section: Resultsmentioning
confidence: 99%
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“…During autumn and winter, natural drivers (such as upwelling, decreased river runoff, and winter convection) alleviate hypoxia. At the same time, the available published historical data clearly demonstrate that the lowest values of DO obtained in the summer in the bottom waters of Amursky Bay have been systematically decreasing with time over the last 80 years, and there is a period between the 1960s and 1980s when Amursky Bay became hypoxic during the summer, most likely starting in the 1970s (Tishchenko et al, 2016). A direct biological consequence of hypoxia is the documented mortality of small fish (e.g.…”
Section: Peter the Great Baymentioning
confidence: 95%
“…As a rule, the formation of such zones due to a combination of several anthropogenic factorsexcessive intake of biogenic compounds (eutrophication), increased water turbidity and, as a result, decreased water transparency, siltation of the bottom, and the development of phytoplankton [5]. In addition, the vertical stratification as a result of the formation of thermocline and/or halocline, weak water mixing, summer temperature increase, and others can serve as a cause of the formation of hypoxic zones [6][7][8].…”
Section: Introductionmentioning
confidence: 99%