Use of molecular markers and compound-specific isotopic signatures to trace sources of black carbon in surface sediments of Peninsular Malaysia: Impacts of anthropogenic activities

Vaezzadeh, Vahab and Yi, Xin and Thomes, Margaret William and Bong, Chui Wei and Lee, Choon Weng and Zakaria, Mohamad Pauzi and Wang, Ai-Jun and Roslin, Putri Nadhirah Binti and Zhong, Guangcai and Zhang, Gan (2021) Use of molecular markers and compound-specific isotopic signatures to trace sources of black carbon in surface sediments of Peninsular Malaysia: Impacts of anthropogenic activities. Marine Chemistry, 237. ISSN 0304-4203, DOI https://doi.org/10.1016/j.marchem.2021.104032.

Full text not available from this repository.

Abstract

Black carbon (BC) acts as a reservoir of carbon in sediment due to its high persistency. Southeast Asia (SEA) is a main source region for BC emissions across the globe due to extensive biomass burning and escalating fossil fuel consumption. However, our understanding of the sources and sinks of BC in SEA is limited. Here, we have analysed BC structure using benzene polycarboxylic acid (BPCA) method in combination of stable carbon isotope (delta C-13) signatures for B5CA and B6CA using HPLC-IRMS in sediment samples from riverine, coastal and shelf areas in Peninsular Malaysia. BPCA molecular markers indicated higher degree of aromatic condensation and lighter isotopic composition in relatively pristine environment of the East coast compared to developed environment of the West and South coast. n-Alkane biomarkers clearly demonstrated higher anthropogenic impacts on the sediments of the West and South coast compared to the East coast. Biomass burning with the predominance of C-3 plants and the large share of natural gas in the energy mix in Malaysia are possibly the main reasons for the isotopically light composition of sedimentary BC (-45.4 to -26.4 parts per thousand). Atmospheric soot and petrogenic BC are the possible main sources of BC in the East coast sediments, while char residues of low temperature biomass burning likely contribute more to sedimentary BC in the West and South coast. The n-alkane indices implied that the sediments of the Kelantan adjacent shelf area receive great proportion of terrestrial organic matter and the associated BC.

Item Type: Article
Funders: International Partnership Program of Chinese Academy of Sciences[132744KYSB20170002], Guangdong Foundation for Program of Science and Technology Research[2017BT01Z134], Guangdong Foundation for Program of Science and Technology Research[2019B121205006], SKLOG open fund[SKLOG201744], Chinese Academy of Sciences President's International Fellowship for Visiting Scientists[2022VCC0006], Ministry of Education, Malaysia[LRGS/1/2016/UTM/01/1], Ministry of Education, Malaysia[LR006-2019], Higher Institution Centre of Excellence (HICoE) Programme [OES-2014D], Universiti Malaya[IIRG009B-2019IF030A2017], China-ASEAN Maritime Cooperation Fund Project "Monitoring and Conservation of the coastal ecosystem in the South China Sea", National Natural Science Foundation of China (NSFC)[41961144022]
Uncontrolled Keywords: Benzene polycarboxylic acids;Soot;Black carbon;Carbon isotope
Subjects: G Geography. Anthropology. Recreation
G Geography. Anthropology. Recreation > GC Oceanography
G Geography. Anthropology. Recreation > GE Environmental Sciences
Divisions: Faculty of Science
Depositing User: Ms Zaharah Ramly
Date Deposited: 13 Sep 2022 03:13
Last Modified: 13 Sep 2022 03:13
URI: http://eprints.um.edu.my/id/eprint/34396

Actions (login required)

View Item View Item