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Benthic biological effects of seasonal hypoxia in a eutrophic estuary predate rapid coastal development

机译:富营养化河口季节性缺氧的底栖生物效应早于沿海快速发展

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Nutrient and organic loading associated with escalating human activities increases biological oxygen demand from microbial decomposition. In the Neuse River estuary, North Carolina, recurrent nuisance algal blooms, bottom-water hypoxic events, and fish kills during summers of the 1990s suggest that uncapped nutrient loading may have increased the frequency, duration, and/or spatial scope of important biological effects of hypoxia during summer, when persistent water column stratification can occur and microbial metabolism is greatest. We test the hypothesis that the severity of benthic biological effects of hypoxia in this estuary has increased over a 30-year period of dramatic human population growth in eastern North Carolina by comparing survival over summer of the benthic bivalve Macoma spp. between historical (1968—1970) and recent (1997—1998) years. Macoma is a demonstrated indicator of oxygen availability, the benthic biomass dominant in the Neuse and other temperate estuaries and the major prey link to higher trophic levels. All three historical summers exhibited patterns of collapse in Macoma populations indistinguishable from the recent summer of severe hypoxia (1997) but distinct from the modest changes documented during the mildly hypoxic summer of 1998. The only Macoma to survive any severely hypoxic summer were those in shallows where oxygen could be renewed by surface mixing. Thus, the biological effects of hypoxia observed in the Neuse River estuary in the late 1990s appear no more severe than 30 years before. Historic rates of organic loading to the Neuse River estuary may have been sufficient to induce widespread and intense hypoxia beneath the surface mixed layer, implying that even if algal blooms are diminished through nutrient reductions, the severity of biological effects of bottom-water hypoxia may not change detectably.
机译:与人类活动升级有关的营养和有机负荷增加了微生物分解产生的生物需氧量。在北卡罗来纳州的纳伊斯河河口,反复出现的令人讨厌的藻类繁殖,底水低氧事件和1990年代夏季的鱼类死亡表明,未加盖的养分负荷可能增加了重要生物效应的发生频率,持续时间和/或空间范围在夏季缺氧的情况下,当持续的水柱分层会发生并且微生物代谢最大时。我们通过比较底栖双壳类Macoma物种夏季的存活情况,验证了这一假设:在河口低氧的底栖生物影响的严重性在北卡罗来纳州东部人口急剧增长的30年期间已经增加。介于历史(1968-1970)和最近(1997-1998)年之间。 Macoma已证明是氧气供应的指标,在​​Neuse和其他温带河口占主导地位的底栖生物量,也是与较高营养水平相关的主要猎物。所有三个历史夏季均表现出Macoma种群崩溃的模式,与最近的严重低氧夏季(1997年)没有区别,但与1998年轻度低氧夏季记录的适度变化不同。唯一能在任何严重低氧的夏季生存下来的Macoma都是浅层Macoma。可以通过表面混合来更新氧气。因此,1990年代后期在Neuse河口观察到的缺氧的生物学效应似乎没有比30年前更严重。往Neuse河河口的有机负荷的历史速率可能足以在表面混合层下引起广泛而强烈的缺氧,这意味着即使通过减少养分来减少藻华,底水缺氧的生物学效应的严重性也可能不会变化可察觉。

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