Geochemical and mineralogical composition of the 2018 volcanic deposits of Mt. Anak Krakatau

Fiantis, Dian; Ginting, Frisa Irawan; Seprianto,; Halfero, Farid; Saputra, Adi Praja; Nelson, Malik; Ranst, Éric Van; Minasny, Budiman

doi:10.1016/j.geodrs.2021.e00393

Cited by 7 publications

(5 citation statements)

References 42 publications

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“…The primary succession starts from bare rock [7] and includes various ecological processes, such as those associated with vegetation, soil, and microorganisms. Studies found in the literature mainly relate to the characterization of volcanic soil formation, soil physicochemical properties, soil development and plant vegetation, and vegetation dynamics [8][9][10][11]. However, research investigating soil microbial populations is scarce.…”

Section: Introductionmentioning

confidence: 99%

Comparison of Microbial Diversity of Two Typical Volcanic Soils in Wudalianchi, China

Huang,

Yang,

Cao

et al. 2024

Microorganisms

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Volcanic lava is an excellent model of primary succession, in which basalt-associated microorganisms drive the cycling of different elements such as nitrogen, carbon, and other nutrients. Microbial communities in volcanic soils are of particular interest for study on the emergence and evolution of life within special and extreme conditions. The initial processes of colonization and subsequent rock weathering by microbial communities are still poorly understood. We analyzed the soil bacterial and fungal communities and diversities associated with lava (LBL) and kipuka (BK) sites in Wudalianchi using 16S and ITS rRNA Illumina Miseq sequencing techniques. The results showed that soil physical and chemical properties (pH, MC, TOC, TN, TP, AP, DOC, and DON) significantly differed between LBL and BK. The Shannon, Ace, and Pd indexes of fungi in the two sites showed a significant difference (p < 0.05). The dominant bacterial phyla forming communities at LBL and BK sites were Acidobacteria, Proteobacteria, Actinobacteria, and Basidiomycota, and their differences were driven by Gemmatimonadetes and Verrucomicrobia. The dominant fungal phyla of LBL and BK sites were Ascomycota, Zygomycota, and Rozellomcota, which differed significantly between the two sites. The microbial communities showed extremely significant differences (p < 0.05), with MC, pH, and nitrogen being the main influencing factors according to RDA/CCA and correlation analysis. Microbial functional prediction analysis across the two sites showed that the relative abundance of advantageous functional groups was significantly different (p < 0.05). The combined results drive us to conclude that the volcanic soil differences in the deposits appear to be the main factor shaping the microbial communities in Wudalianchi (WDLC) volcanic ecosystems.

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Section: Introductionmentioning

confidence: 99%

Comparison of Microbial Diversity of Two Typical Volcanic Soils in Wudalianchi, China

Huang,

Yang,

Cao

et al. 2024

Microorganisms

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“…The distribution of pyroclastic material increased each year (Figure 10 From our field survey, we observed the pyroclastic material thickness varied from 13,24 cm to 219 cm. At some point, we could measure it instantly cause the infiltration condition created some erosion path [12]. This data is obtained after processing with the kriging method and strengthened by field data (Figure 11).…”

Section: Pyroclastic Materials Depositmentioning

confidence: 99%

Detection of pyroclastic material and deformation of the lava dome in Mt. Sinabung with multi-temporal analysis (2010-2020)

Hidayat,

Ginting,

Agustian

et al. 2024

IOP Conf. Ser.: Earth Environ. Sci.

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The persistent eruptions of Mt. Sinabung resulted in the lava dome’s deformation and blanketed the surrounding area with pyroclastic material. This research focused on determining the changes in Mt. Sinabung during the prolonged eruptions from 2010-2020. A total of 22 volcanic ash samples were collected following a 1x1 km grid interval spread over from the East to South slope of Mt. Sinabung. The studied area is the most affected by the volcanic eruption. Digital elevation models from the shuttle radar topographic mission and sentinel-1 were utilized to monitor deformations of the lava dome and the distribution of pyroclastic material on Mt. Sinabung. Sentinel Application Platform and Google Earth Engine were used as the main tools in multi-temporal digital elevation model (DEM) data processing. The eruption of Mt. Sinabung from 2010 to 2020 changed the height from 2,460 m to 2,404.3 m and created a new crater (5.35 ha). The lava dome volume from 2010 to 2020 is about 2,308,041 m3 and has collapsed to produce pyroclastic material which deposits to the surrounding area of Mt. Sinabung during the eruption. The distribution of pyroclastic material increased from 2010 to 2019, covered up an area of 103.27 ha (2010), 846.48 ha (2013), 1,029.74 ha (2016), 1,235.97 ha (2017) and 1,463.62 ha (2019). The thickness of the pyroclastic material deposits at Mt. Sinabung until 2020 varied from 13,24 cm to 219 cm. The findings from this study can be used as a reference for observing topographic changes due to volcanic activities and drawing a mitigation and contingency plan for a volcanic disaster program in the active volcanic region of Indonesia.

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“…We survey aerial plume heights from other recent submarine eruptions to illustrate the broad importance of understanding the factors that control plume height. Specifically, the 2018 basaltic eruption of Anak Krakatau that created an 18 km ice-rich plume 23,48 and the 2016-2017 trachy-basaltic eruptions of Bogoslof, Alaska generated water-rich aerial plumes that reached up to ~12 km over nine-months 24,25,49 . The January 2022 eruption of Hunga Tonga Hunga Ha'apai created a plume that rose more than 30 km and deposited ash over the Kingdom of Tonga 2 .…”

Section: Comparison To Other Recent Subaqueous Eruptionsmentioning

confidence: 99%

Simultaneous creation of a large vapor plume and pumice raft by a shallow submarine eruption

Fauria

Jutzeler²,

Mittal

et al. 2022

Preprint

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The August 12, 2021 eruption of Fukutoku-Okanoba, a shallow submarine volcano in the Izu-Bonin arc of Japan, is one of few documented submarine eruptions to make a large aerial plume and floating pumice raft. Relative to past eruptions, this event was well-covered by multiple high resolution satellite remote sensors. Here we use satellite remote sensing to assess the eruption style, rates, and products. We find that the 16 km plume was water-rich. Furthermore, we conclude that the 0.1 kmˆ3 raft and 16 km plume were co-genetic and suggest that pumice clasts were delivered to the raft by tephra jets rather than plume fallout. Finally, this eruption highlights a discrepancy between small erupted volumes and high plume heights that may be common for shallow explosive subaqueous eruptions.

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Geochemical and mineralogical composition of the 2018 volcanic deposits of Mt. Anak Krakatau

Cited by 7 publications

References 42 publications

Comparison of Microbial Diversity of Two Typical Volcanic Soils in Wudalianchi, China

Comparison of Microbial Diversity of Two Typical Volcanic Soils in Wudalianchi, China

Detection of pyroclastic material and deformation of the lava dome in Mt. Sinabung with multi-temporal analysis (2010-2020)

Simultaneous creation of a large vapor plume and pumice raft by a shallow submarine eruption

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