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量化印度尼西亚一个未排水热带泥炭地生态系统的碳损失通量。

Quantifying the fluxes of carbon loss from an undrained tropical peatland ecosystem in Indonesia.

作者信息

Asyhari Adibtya, Gangga Adi, Putra Chandra Agung Septiadi, Ritonga Rasis Putra, Candra Randi Ade, Anshari Gusti Z, Bowen Jennifer C, Perryman Clarice R, Novita Nisa

机构信息

Yayasan Konservasi Alam Nusantara, Jakarta, Indonesia.

Magister of Environmental Science, Tanjungpura University, Pontianak, Indonesia.

出版信息

Sci Rep. 2024 May 20;14(1):11459. doi: 10.1038/s41598-024-62233-6.

Abstract

Conservation of undrained tropical peatland ecosystems is critical for climate change mitigation as they store a tremendous amount of soil carbon that is preserved under anoxic water-logged conditions. Unfortunately, there are too few measurements of carbon fluxes from these ecosystems to estimate the climate change mitigation potential from such conservation efforts. Here, we measured carbon dioxide (CO) and methane (CH) fluxes as well as fluvial organic carbon export over the peat swamp forest within an undrained tropical peatland landscape in East Kalimantan, Indonesia. Our measurements throughout one year (Oct 2022-Sep 2023) showed that despite its water-logged condition, peat and water overlying the swamp forest on average emits 11.02 ± 0.49 MgCO ha yr of CO and 0.58 ± 0.04 MgCOe ha yr of CH. Further, the fluvial organic carbon export contributes to additional carbon loss of 1.68 ± 0.06 MgCOe ha yr. Our results help improve the accuracy of carbon accounting from undrained tropical peatlands, where we estimated a total carbon loss of 13.28 ± 0.50 MgCOe ha yr. Nevertheless, the total carbon loss reported from our sites is about half than what is reported from the drained peatland landscapes in the region and resulted in a larger onsite carbon sink potential estimate compared to other undrained peat swamp forests. Together, these findings indicate that conserving the remaining undrained peatland ecosystems in Indonesia from drainage and degradation is a promising natural climate solution strategy that avoids significant carbon emissions.

摘要

保护未排水的热带泥炭地生态系统对于缓解气候变化至关重要,因为它们储存了大量的土壤碳,这些碳在缺氧的水涝条件下得以保存。不幸的是,对这些生态系统的碳通量测量太少,无法估算这种保护措施对缓解气候变化的潜力。在此,我们测量了印度尼西亚东加里曼丹一个未排水的热带泥炭地景观中泥炭沼泽森林的二氧化碳(CO)和甲烷(CH)通量以及河流有机碳输出。我们在一整年(2022年10月至2023年9月)的测量结果表明,尽管处于水涝状态,但沼泽森林上覆的泥炭和水平均每年排放11.02±0.49 MgCO₂ ha⁻¹ yr⁻¹的CO₂和0.58±0.04 MgCO₂e ha⁻¹ yr⁻¹的CH₄。此外,河流有机碳输出导致每年额外的碳损失为1.68±0.06 MgCO₂e ha⁻¹。我们的结果有助于提高未排水热带泥炭地碳核算的准确性,据此我们估计总碳损失为13.28±0.50 MgCO₂e ha⁻¹ yr⁻¹。然而,我们研究地点报告的总碳损失约为该地区排水泥炭地景观报告值的一半,与其他未排水的泥炭沼泽森林相比,导致了更大的现场碳汇潜力估计值。总之,这些发现表明,保护印度尼西亚剩余的未排水泥炭地生态系统免受排水和退化影响是一种有前景的自然气候解决方案策略,可避免大量碳排放。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/47e8/11106321/7842e8002325/41598_2024_62233_Fig1_HTML.jpg

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