Contribution of phytoliths to total biogenic silica volumes in the tropical rivers of Malaysia and associated implications for the marine biogeochemical cycle

Jiaye Zang; Sen Liu; Yanguang Liu; Yongxing Ma; Xiangbin Ran

doi:10.1007/s00343-016-5116-z

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Contribution of phytoliths to total biogenic silica volumes in the tropical rivers of Malaysia and associated implications for the marine biogeochemical cycle

OriginalPaper | Updated：2023-05-16

- Contribution of phytoliths to total biogenic silica volumes in the tropical rivers of Malaysia and associated implications for the marine biogeochemical cycle
- Contribution of phytoliths to total biogenic silica volumes in the tropical rivers of Malaysia and associated implications for the marine biogeochemical cycle
- 海洋湖沼学报（英文） 2016年34卷第5期页码：1076-1084
- Affiliations：
  
  1. Marine Ecology Research Center First Institute of Oceanography State Oceanic Administration
  2. Tianjin Marine Environmental Monitoring Central Station State Oceanic Administration
  3. Key Laboratory of Marine Sedimentology and Environmental Geology First Institute of Oceanography State Oceanic Administration
  4. College of Chemistry and Engineering Qingdao University
- Author bio：
- Funds：
  
  Supported by the National Natural Science Foundation of China (Nos. 41106072, 41376093) and the International Collaboration Science Plan (No. GASI-01-02-01-04)
- DOI：10.1007/s00343-016-5116-z
  中图分类号：
- 网络首发：2016-01-28，
  
  纸质出版：2016
- Accepted：
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Contribution of phytoliths to total biogenic silica volumes in the tropical rivers of Malaysia and associated implications for the marine biogeochemical cycle[J]. 海洋湖沼学报（英文）, 2016,34(5):1076-1084.

Zang, J., Liu, S., Liu, Y. et al. Contribution of phytoliths to total biogenic silica volumes in the tropical rivers of Malaysia and associated implications for the marine biogeochemical cycle., Chin. J. Ocean. Limnol. 34, 1076–1084 (2016). https://doi.org/10.1007/s00343-016-5116-z
Contribution of phytoliths to total biogenic silica volumes in the tropical rivers of Malaysia and associated implications for the marine biogeochemical cycle[J]. 海洋湖沼学报（英文）, 2016,34(5):1076-1084. DOI： 10.1007/s00343-016-5116-z.

Zang, J., Liu, S., Liu, Y. et al. Contribution of phytoliths to total biogenic silica volumes in the tropical rivers of Malaysia and associated implications for the marine biogeochemical cycle., Chin. J. Ocean. Limnol. 34, 1076–1084 (2016). https://doi.org/10.1007/s00343-016-5116-z DOI：

摘要

Abstract

The contribution of phytoliths to total biogenic silica (BSi) volumes in rivers worldwide

and the associated implications for the biogeochemical cycle

require in-depth study. Based on samples from rivers in Peninsular Malaysia

this project investigated the source and characteristics of BSi found in Asian tropical rivers

as well as the process of reverse weathering taking place in these fluvial systems. Results indicated that BSi samples collected in sediments consisted of phytolith

diatom and sponge spicules. Phytoliths

predominantly of the elongate form

comprised 92.8%–98.3% of BSi in the Pahang River. Diatom BSi in this river consisted mainly of pennatae diatoms

but represented a relatively small proportion of the total BSi volume. However

diatom BSi (predominantly of the Centricae form) was more prevalent in the Pontian and Endau Rivers with shares of 68.8% and 79.3% of the total BSi volumes

respectively

than Pahang River. Carbon contents of the BSi particulates ranged from 1.85% to 10.8% with an average of 4.79%. These values are higher than those recorded in other studies to date

and indicate that BSi plays a major role in controlling permanent carbon burial. This study suggests that phytoliths from terrestrial plants are the primary constituents of BSi in the rivers of Peninsular Malaysia

and therefore represent a significant proportion of the coastal silica budget.

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references

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