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土地利用和土地覆盖变化对红树林蓝碳的影响:系统评价。

Effect of land-use and land-cover change on mangrove blue carbon: A systematic review.

机构信息

Research Institute for the Environment and Livelihoods (RIEL), Charles Darwin University, Darwin, NT, Australia.

Center for International Forestry Research (CIFOR), Bogor, Indonesia.

出版信息

Glob Chang Biol. 2019 Dec;25(12):4291-4302. doi: 10.1111/gcb.14774. Epub 2019 Aug 27.

Abstract

Mangroves shift from carbon sinks to sources when affected by anthropogenic land-use and land-cover change (LULCC). Yet, the magnitude and temporal scale of these impacts are largely unknown. We undertook a systematic review to examine the influence of LULCC on mangrove carbon stocks and soil greenhouse gas (GHG) effluxes. A search of 478 data points from the peer-reviewed literature revealed a substantial reduction of biomass (82% ± 35%) and soil (54% ± 13%) carbon stocks due to LULCC. The relative loss depended on LULCC type, time since LULCC and geographical and climatic conditions of sites. We also observed that the loss of soil carbon stocks was linked to the decreased soil carbon content and increased soil bulk density over the first 100 cm depth. We found no significant effect of LULCC on soil GHG effluxes. Regeneration efforts (i.e. restoration, rehabilitation and afforestation) led to biomass recovery after ~40 years. However, we found no clear patterns of mangrove soil carbon stock re-establishment following biomass recovery. Our findings suggest that regeneration may help restore carbon stocks back to pre-disturbed levels over decadal to century time scales only, with a faster rate for biomass recovery than for soil carbon stocks. Therefore, improved mangrove ecosystem management by preventing further LULCC and promoting rehabilitation is fundamental for effective climate change mitigation policy.

摘要

受人为土地利用和土地覆盖变化(LULCC)的影响,红树林会从碳汇转变为碳源。然而,这些影响的幅度和时间尺度在很大程度上尚未可知。我们进行了一项系统评价,以检验 LULCC 对红树林碳储量和土壤温室气体(GHG)排放通量的影响。从同行评议文献中搜索了 478 个数据点,结果表明,由于 LULCC,生物量(82%±35%)和土壤(54%±13%)碳储量大量减少。相对损失取决于 LULCC 类型、LULCC 发生以来的时间以及地点的地理和气候条件。我们还观察到,土壤碳储量的损失与土壤碳含量的降低和土壤容重的增加有关,这一现象发生在最初的 100 厘米深度内。我们没有发现 LULCC 对土壤 GHG 排放通量有显著影响。再生努力(即恢复、修复和造林)导致生物量恢复后约 40 年的生物量恢复。然而,我们没有发现生物量恢复后红树林土壤碳储量重建的明显模式。我们的研究结果表明,再生可能有助于在数十年到百年的时间尺度上使碳储量恢复到受干扰前的水平,而生物量的恢复速度快于土壤碳储量。因此,通过防止进一步的 LULCC 和促进恢复,改善红树林生态系统管理对于有效的气候变化缓解政策至关重要。

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