Tracing highly oxidized events and its response to peat dynamic from the northwest Kapuas coastal wetlands, Indonesia

IF 5.6 2区 工程技术 Q2 ENERGY & FUELS
Aulia Agus Patria , Stephen P. Obrochta , Ferian Anggara
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Abstract

Peat deposits are highly sensitive to environmental changes and are well-suited to palaeobotanical investigations. Therefore, we assess the integration between organic petrology, palynology, and microcharcoal distributions to provide a robust interpretation on peatland dynamic and paleoenvironmental reconstruction. In addition, we propose a peat characterization using a quantitative color coordinate (CIELAB) to reduce biases while characterizing peat via qualitative comparisons to the Munsell soil color chart. This study was conducted in low-lying mires in the northwest Kapuas coastal plain, West Kalimantan, Indonesia. Five types of peat were identified: sapric muck, sapric shorts, sapric wood, coarse hemic, and fine hemic. The quantitative color coordinate analysis successfully recognizes the peat physical properties but is not directly related to the peat type. Higher values of the red-green chromaticity index (a*) indicate a greater preservation of plant material. Conversely, lower values represent charcoal or an oxidized layer of organic matter. Higher contents of inertinite or oxidized organic matter are comparable to the microcharcoal abundance, showing the presence of severe fires. At least eight fire events were reported, with decreasing intensity towards top of the core. Variation in microcharcoal abundances led to a degree of preservation changes, nutrient status and paleovegetation shift in the studied area. Four phases of peat dynamics were identified: initiation, early ombrogenous, late ombrogenous, and topogenous phases. In general, past vegetation shows an alternation community of mixed-riparian forest and open vegetation to present day mangrove low-lying topogenous mire. Our findings refer to the vulnerability of vegetation changes and peat dynamics concerning on highly oxidized events related to the fire intensity as an important driver in the northwest coastal wetlands of Kalimantan Island.
追踪高氧化事件及其对印尼西北卡普亚斯滨海湿地泥炭动态的响应
泥炭沉积物对环境变化高度敏感,非常适合古植物学研究。因此,我们评估了有机岩石学、孢粉学和微炭分布之间的整合,为泥炭地动态和古环境重建提供了强有力的解释。此外,我们建议使用定量颜色坐标(CIELAB)来表征泥炭,以减少偏差,同时通过与Munsell土壤颜色图的定性比较来表征泥炭。本研究在印度尼西亚西加里曼丹卡普阿斯海岸平原西北部的低洼泥潭中进行。泥炭分为五种类型:泥炭泥、泥炭短粒、泥炭木、泥炭粗粒和泥炭细粒。定量颜色坐标分析成功地识别了泥炭的物理性质,但与泥炭的类型没有直接关系。较高的红绿色度指数(a*)表明植物材料的保存程度较高。相反,较低的值代表木炭或氧化层的有机物。较高的惰质或氧化有机物含量与微炭丰度相当,表明存在严重的火灾。据报道,至少有8起火灾事件,核心顶部的强度逐渐降低。微炭丰度的变化导致了研究区保存程度的变化、营养状况和古植被的转移。泥炭动力学分为四个阶段:起始阶段、早生阶段、晚生阶段和地形生阶段。总体而言,过去的植被呈现出混合河岸林和开放植被与现在的红树林低洼地形沼泽的交替群落。研究结果表明,在加里曼丹岛西北沿海湿地,植被变化的脆弱性和泥炭动态变化与火灾强度有关,是一个重要的驱动因素。
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来源期刊
International Journal of Coal Geology
International Journal of Coal Geology 工程技术-地球科学综合
CiteScore
11.00
自引率
14.30%
发文量
145
审稿时长
38 days
期刊介绍: The International Journal of Coal Geology deals with fundamental and applied aspects of the geology and petrology of coal, oil/gas source rocks and shale gas resources. The journal aims to advance the exploration, exploitation and utilization of these resources, and to stimulate environmental awareness as well as advancement of engineering for effective resource management.
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