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首页> 外文期刊>New Zealand Journal of Marine and Freshwater Research >Reviewing the far-reaching ecological impacts of human-induced terrigenous sedimentation on shallow marine ecosystems in a northern-New Zealand embayment
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Reviewing the far-reaching ecological impacts of human-induced terrigenous sedimentation on shallow marine ecosystems in a northern-New Zealand embayment

机译:审查北方新西兰北方浅海生态系统对浅海生态系统的深远生态影响

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摘要

Human settlement in Bay of Islands, New Zealand, beginning similar to 1300 AD, wrought immense, conspicuous and enduring change to local shallow-water marine ecologies, this review addressing those transformations attributable to increased rates of anthropogenically induced, land-derived sedimentation. Elevated silt inflow, particularly after the late-1800s, in course led to similar to 130% expansion in mangrove (Avicennia marina) cover, with concomitant loss of saltmarsh, uppershore coarse-shell beaches/cheniers, and (probably) intertidal seagrass (Zostera muelleri). Sedimentation also led to widespread loss of estuarine shellfish habitat, and, although not necessarily categorically causal, seems, at the same time to have contributed to such degradation among cockle (Austrovenus stutchburyi) populations that few individuals attain their potential size. Most changes, many seemingly irreversible, can be described as ecologically catastrophic, with ecosystems altered and destroyed, and uncommon habitats threatened. Sedimentation appears the single-most important and enduring contributor to ecological degradation in shallow waters of this northern harbour, with time lags between stressor-onset and realisation of impact (decades to centuries) that only now are becoming clear. Outstanding issues concern establishing the extent of relationship between levels of terrigenous sedimentation and cockles seldom attaining their previous maximum sizes, and origins of the possibly new, widespread phenomenon of living cockles accumulating and dying atop beach surfaces.
机译:新西兰湾湾的人类沉降,开始与1300广告,对当地浅水海洋生态的造成巨大,显眼和持久的变化,这综述解决这些转化,归因于人为诱导的人为诱导的土地源性沉降率增加。淤泥流入升高,特别是在1800年代后期后,当然导致了红树林(avicennia marina)封面的130%扩张,伴随着盐沼,俯卧撑粗壳海滩/克莱斯和(可能)的跨国海草(Zostera Muelleri)。沉淀也导致了河口贝类栖息地的广泛丧失,虽然不一定是分歧的因果,但似乎有助于群沟(Austrovenus Stutchburyi)群体中的诸如少数个人达到潜在规模的群体。大多数变化,许多看似不可逆转的,可以被描述为生态灾难性,生态系统改变和摧毁,罕见的栖息地威胁。沉淀出现了这个北部港口浅水区的单一最重要和持久的贡献者,在压力响声和实现影响(十年到几个世纪)之间的时间滞后,现在只会变得明确。出色的问题涉及建立人民沉降和群斑之间的关系之间的关系,很少获得以前的最大尺寸,以及可能是新的,生活鸟蛤的可能性繁衍现象的起源,积累和染色的海滩表面。

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