Restricted accessResearch articleFirst published online 2023-8
The record of sedimentary spheroidal carbonaceous particles (SCPs) in Beppu Bay,southern Japan,compared to historical trends of industrial activity and atmospheric pollution: Further evidence for SCPs as a marker for Anthropocene industrialization
Spheroidal carbonaceous particles (SCPs) are carbonaceous fly ash particles produced solely from industrial fossil fuel combustion. SCPs in sediments can be an indicator of past industrialization. We examined the sedimentary SCP record in Beppu Bay, southern Japan, and compared this record to historical trends of industrial activity and monitoring data for atmospheric pollutions in the region. Beppu Bay has varved sediments in the absence of bioturbation, providing an ideal situation for SCP study. Our results show that the temporal variation of SCP deposition is consistent with the trends of industrial activity and the temporal variation of status of atmospheric pollution. We conclude that undisturbed sediments such as Beppu Bay sediments have SCP records that adequately represent historical trends of industrial activity and atmospheric pollution in detail. These findings support that SCPs are a potential marker for the Anthropocene, characterized by industrialization.
AlliksaarTHörstedtPRenbergI (1998) Characteristic fly-ash particles from oil-shale combustion found in lake sediments. Water Air & Soil Pollution104(1–2): 149–160.
2.
EngelsSFongLSRZChenQ, et al. (2018) Historical atmospheric pollution trends in Southeast Asia inferred from lake sediment records. Environmental Pollution235: 907–917.
3.
GriffinJJGoldbergED (1979) Morphologies and origin of elemental carbon in the environment. Science206(4418): 563–565.
4.
GriffinJJGoldbergED (1981) Sphericity as a characteristic of solids from fossil fuel burning in a Lake Michigan sediment. Geochimica et Cosmochimica Acta45(5): 763–769.
5.
HammerØHarperDATRyanPD (2001) PAST: Paleontological statistics software package for education and data analysis. Palaeontologia Electronica4(1): 9.
6.
HoangAQAonoDWatanabeI, et al. (2021) Contamination levels and temporal trends of legacy and current-use brominated flame retardants in a dated sediment core from Beppu Bay, southwestern Japan. Chemosphere266: 129180.
7.
IkedaKYamajiKKanayaY, et al. (2014) Sensitivity analysis of source regions to PM2.5 concentration at Fukue Island, Japan. Journal of the Air & Waste Management Association64(4): 445–452.
8.
IkedaKYamajiKKanayaY, et al. (2015) Source region attribution of PM2.5 mass concentrations over Japan. Geochemical Journal49(2): 185–194.
9.
InoueJMomoseAOkudairaT, et al. (2014) Chemical characteristics of Northeast Asian fly ash particles: Implications for their long-range transportation. Atmospheric Environment95: 375–382.
10.
InoueJMoritsuguKOkudairaT, et al. (2020) Elemental compositions and sizes of carbonaceous fly ash particles from atmospheric deposition collected at Cape Hedo, Okinawa, Japan: Implications for their long-range transportation and source region variation. Atmospheric Pollution Research11(2): 393–400.
11.
InoueJOkuyamaCHayashiR, et al. (2021) Postglacial anthropogenic fires related to cultural changes in central Japan, inferred from sedimentary charcoal records spanning glacial–interglacial cycles. Journal of Quaternary Science36(4): 628–637.
12.
InoueJOkuyamaCTakemuraK (2018) Long-term fire activity under the East Asian monsoon responding to spring insolation, vegetation type, global climate, and human impact inferred from charcoal records in Lake Biwa sediments in central Japan. Quaternary Science Reviews179: 59–68.
13.
InoueJTomozawaAOkudairaT (2013) The use of size distributions of spheroidal carbonaceous particles in swimming pool deposits for evaluating atmospheric particle behaviour. Water Air & Soil Pollution224(5): 1580.
14.
KamedaTFujiwaraT (1995) Ventilation time and anoxia of the benthic cold water in Beppu Bay. Bulletin of Coastal Oceanography33: 59–68.
15.
KaneyasuNYamamotoSSatoK, et al. (2014) Impact of long-range transport of aerosols on the PM2.5 composition at a major metropolitan area in the northern Kyushu area of Japan. Atmospheric Environment97: 416–425.
16.
KuwaeMYamamotoMIkeharaK, et al. (2013) Stratigraphy and wiggle-matching-based age-depth model of late holocene marine sediments in Beppu Bay, southwest Japan. Journal of Asian Earth Sciences69: 133–148.
17.
KuwaeMTsugekiNKAmanoAet al. (2022) Human-induced marine degradation in anoxic coastal sediments of Beppu Bay, Japan, as an Anthropocene marker in East Asia. Anthropocene37: 100318.
18.
Kyushu Electric Power Co., Inc. (2021) Kyushu Electric Power Group Data Book. Fukuoka: Kyushu Electric Power Co., Inc. Available at: http://www.kyuden.co.jp/company_data_book.html (accessed 1 March 2022).
19.
MasumotoMKuwaeMHinataH (2018) Flux of sedimentary microplastics in Beppu Bay, Japan. Proceedings of Japan Society of Civil Engineers, Series B265: 1321–1326.
20.
MomoseAInoueJMurakami-KitaseA, et al. (2012) Characteristic differences in the chemical composition of spheroidal carbonaceous particles in Japanese and Chinese cities. Water Air & Soil Pollution223(8): 4761–4767.
21.
Murakami-KitaseAOkudairaTInoueJ (2010) Relationship between surface morphology and chemical composition of spheroidal carbonaceous particles within sediment core samples recovered from Osaka Bay, Japan. Environmental Earth Sciences59(8): 1723–1729.
22.
NagafuchiORoseNLHoshikaA, et al. (2009) The temporal record and sources of atmospherically deposited fly-ash particles in Lake Akagi-Konuma, a Japanese mountain lake. Journal of Paleolimnology42(3): 359–371.
23.
NishimutaKUenoDTakahashiS, et al. (2021) Use of comprehensive target analysis for determination of contaminants of emerging concern in a sediment core collected from Beppu Bay, Japan. Environmental Pollution272: 115587.
24.
RoseNL (1990) A method for the extraction of carbonaceous particles from lake sediment. Journal of Paleolimnology3: 45–53.
25.
RoseNL (1994) A note on further refinements to a procedure for the extraction of carbonaceous fly-ash particles from sediments. Journal of Paleolimnology11(2): 201–204.
26.
RoseNL (1995) Carbonaceous particle record in lake sediments from the Arctic and other remote areas of the northern hemisphere. The Science of the Total Environment160–161: 487–496.
27.
RoseNL (2001) Fly-ash particles. In: LastWMSmolJP (eds) Tracking Environmental Change Using Lake Sediments. Vol. 2: Physical and Geochemical Methods. Dordrecht: Kluwer Academic Publishers, pp.319–349.
28.
RoseNL (2008) Quality control in the analysis of lake sediments for spheroidal carbonaceous particles. Limnology and Oceanography Methods6: 172–179.
29.
RoseNL (2015) Spheroidal carbonaceous fly ash particles provide a globally synchronous stratigraphic marker for the Anthropocene. Environmental Science & Technology49(7): 4155–4162.
30.
RoseNLJugginsS (1994) A spatial relationship between carbonaceous particles in lake sediments and sulphur deposition. Atmospheric Environment28(2): 177–183.
31.
RoseNLJugginsSWattJ (1996) Fuel-type characterization of carbonaceous fly-ash particles using EDS-derived surface chemistries and its application to particles extracted from lake sediments. Proceedings of The Royal Society A Mathematical Physical and Engineering Sciences452(1947): 881–907.
32.
RoseNLJugginsSWattJ (1999) The characterisation of carbonaceous fly-ash particles from major European fossil-fuel types and applications to environmental samples. Atmospheric Environment33(17): 2699–2713.
33.
RoseNLRoseCLBoyleJF, et al. (2004) Lake-sediment evidence for local and remote sources of atmospherically deposited pollutants on Svalbard. Journal of Paleolimnology31(4): 499–513.
34.
RoseNLMonteithDT (2005) Temporal trends in spheroidal carbonaceous particle deposition derived from annual sediment traps and lake sediment cores and their relationship with non-marine sulphate. Environmental Pollution137(1): 151–163.
35.
SwindlesGTWatsonETurnerTE, et al. (2015) Spheroidal carbonaceous particles are a defining stratigraphic marker for the Anthropocene. Scientific Reports5: 10264.
36.
TakahashiSAnhHQWatanabeI, et al. (2020) Characterization of mono- to deca-chlorinated biphenyls in a well-preserved sediment core from Beppu Bay, southwestern Japan: Historical profiles, emission sources, and inventory. The Science of the Total Environment743: 140767.
37.
UnoIWangZYumimotoK, et al. (2017) Is PM2. 5 trans-boundary environmental problem in japan dramatically improving?Journal of Korean Society for Atmospheric Environment52(6): 177–184.
38.
VukićJFottJPetrusekA, et al. (2006) What can size distribution of spheroidal carbonaceous particles reveal about their source?Atmospheric Environment40(19): 3527–3535.
39.
WatersCNZalasiewiczJSummerhayesC, et al. (2016) The Anthropocene is functionally and stratigraphically distinct from the Holocene. Science351(6269): aad2622.
40.
WatersCNZalasiewiczJSummerhayesC, et al. (2018) Global boundary stratotype section and point (GSSP) for the Anthropocene series: Where and how to look for potential candidates. Earth-Science Reviews178: 379–429.
41.
WikMRenbergI (1991) Recent atmospheric deposition in Sweden of carbonaceous particles from fossil-fuel combustion surveyed using lake-sediments. Ambio20(7): 289–292.
42.
WikMRenbergIDarleyJ (1986) Sedimentary records of carbonaceous particles from fossil fuel combustion. Hydrobiologia143: 387–394.
43.
YinS (2021) Decadal trends of MERRA-estimated PM2.5 concentrations in East Asia and potential exposure from 1990 to 2019. Atmospheric Environment264: 118690.
44.
ZalasiewiczJWatersCNSummerhayesCP, et al. (2017) The working group on the Anthropocene: Summary of evidence and interim recommendations. Anthropocene19: 55–60.
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