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首页> 外文期刊>Global change biology >Intertwined effects of climate and land use change on environmental dynamics and carbon accumulation in a mangrove-fringed coastal lagoon in Java, Indonesia
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Intertwined effects of climate and land use change on environmental dynamics and carbon accumulation in a mangrove-fringed coastal lagoon in Java, Indonesia

机译:在印度尼西亚Java的红树纹沿海泻湖环境动态和碳积累中的融合效果

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The identification and quantification of natural carbon (C) sinks is critical to global climate change mitigation efforts. Tropical coastal wetlands are considered important in this context, yet knowledge of their dynamics and quantitative data are still scarce. In order to quantify the C accumulation rate and understand how it is influenced by land use and climate change, a palaeoecological study was conducted in the mangrove-fringed Segara Anakan Lagoon (SAL) in Java, Indonesia. A sediment core was age-dated and analyzed for its pollen and spore, elemental and biogeochemical compositions. The results indicate that environmental dynamics in the SAL and its C accumulation over the past 400 years were controlled mainly by climate oscillations and anthropogenic activities. The interaction of these two factors changed the lagoon's sediment supply and salinity, which consequently altered the organic matter composition and deposition in the lagoon. Four phases with varying climates were identified. While autochthonous mangrove C was a significant contributor to carbon accumulation in SAL sediments throughout all four phases, varying admixtures of terrestrial C from the hinterland also contributed, with natural mixed forest C predominating in the early phases and agriculture soil C predominating in the later phases. In this context, climate-related precipitation changes are an overarching control, as surface water transport through rivers serves as the "delivery agent" for the outcomes of the anthropogenic impact in the catchment area into the lagoon. Amongst mangrove-dominated ecosystems globally, the SAL is one of the most effective C sinks due to high mangrove carbon input in combination with a high allochthonous carbon input from anthropogenically enhanced sediment from the hinterland and increased preservation. Given the substantial C sequestration capacity of the SAL and other mangrove-fringed coastal lagoons, conservation and restoration of these ecosystems is vitally important for climate change mitigation.
机译:天然碳(C)水槽的鉴定和定量对全球气候变化缓解努力至关重要。在这种背景下,热带沿海湿地被认为是重要的,但他们的动态和量化数据的了解仍然很少。为了量化C累积率并了解如何受土地利用和气候变化的影响,在印度尼西亚Java的红树林中,在红树林Segara Anakan Lagoon(Sal)中进行了一项古生学研究。沉积物核心是针对其花粉和孢子,元素和生物地球化学组合物进行了适应的和分析。结果表明,在过去4万年中,萨尔的环境动态及其C累积主要受气候振荡和人为活动的控制。这两个因素的相互作用改变了泻湖的沉积物供应和盐度,从而改变了泻湖中的有机物质组合物和沉积。确定了四个不同气候的阶段。虽然Autochthonous Mangrove C在所有四个阶段都是萨尔沉积物中碳积累的重要因素,但在腹地中的各种陆地C的不同混合也有助于,自然混合森林C优势在早期阶段和农业土壤中占优势在后期阶段。在这种情况下,气候相关的降水变化是总体控制,通过河流的地表水运输用作“递送剂”,以便将集水区中的人为影响进入泻湖。在全球红树丛主导的生态系统中,SAL是由于High Congrove碳输入,与来自腹地的人为增强沉积物的高外性碳投入,以及从腹地的人为增强的沉淀物组合,并且增加了,SAL是最有效的C水槽之一。鉴于萨尔和其他红树林沿海泻湖的实质性C隔离能力,这些生态系统的保护和恢复对气候变化缓解至关重要。

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